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Things we can do now that we could not do before: Developing and using a cross-scalar, state-wide database to support geomorphologically-informed river management

  • Kirstie Fryirs ,

    Roles Conceptualization, Data curation, Formal analysis, Funding acquisition, Investigation, Methodology, Project administration, Resources, Supervision, Validation, Visualization, Writing – original draft, Writing – review & editing

    kirstie.fryirs@mq.edu.au

    Affiliation Department of Earth and Environmental Sciences, Macquarie University, North Ryde, NSW, Australia

  • Fergus Hancock,

    Roles Data curation, Formal analysis, Funding acquisition, Investigation, Methodology, Project administration, Resources, Validation, Visualization, Writing – review & editing

    Affiliation NSW Department of Planning, Industry and Environment, Water Division, NSW, Australia

  • Michael Healey,

    Roles Data curation, Formal analysis, Investigation, Methodology, Visualization, Writing – review & editing

    Affiliation NSW Department of Planning, Industry and Environment, Water Division, NSW, Australia

  • Simon Mould,

    Roles Conceptualization, Data curation, Formal analysis, Investigation, Methodology, Validation, Visualization, Writing – original draft

    Affiliations Department of Earth and Environmental Sciences, Macquarie University, North Ryde, NSW, Australia, NSW Department of Planning, Industry and Environment, Water Division, NSW, Australia

  • Lucy Dobbs,

    Roles Data curation, Investigation, Visualization

    Affiliation NSW Department of Planning, Industry and Environment, Water Division, NSW, Australia

  • Marcus Riches,

    Roles Data curation, Investigation, Validation, Writing – review & editing

    Affiliation Coastal Systems Unit, NSW Department Primary Industries–Fisheries, NSW, Australia

  • Allan Raine,

    Roles Funding acquisition, Investigation, Project administration, Writing – review & editing

    Affiliation NSW Department of Planning, Industry and Environment, Water Division, NSW, Australia

  • Gary Brierley

    Roles Conceptualization, Funding acquisition, Investigation, Methodology, Project administration, Supervision, Validation, Writing – original draft, Writing – review & editing

    Affiliations Department of Earth and Environmental Sciences, Macquarie University, North Ryde, NSW, Australia, School of Environment, University of Auckland, Auckland, New Zealand

Abstract

A fundamental premise of river management is that practitioners understand the resource they are working with. In river management this requires that baseline information is available on the structure, function, health and trajectory of rivers. Such information provides the basis to contextualise, to plan, to be proactive, to prioritise, to set visions, to set goals and to undertake objective, pragmatic, transparent and evidence-based decision making. In this paper we present the State-wide NSW River Styles database, the largest and most comprehensive dataset of geomorphic river type, condition and recovery potential available in Australia. The database is an Open Access product covering over 216,600 km of stream length in an area of 802,000 km2. The availability of the database presents unprecedented opportunities to systematically consider river management issues at local, catchment, regional and state-wide scales, and appropriately contextualise applications in relation to programs at other scales (e.g. internationally)–something that cannot be achieved independent from, or without, such a database. We present summary findings from the database and demonstrate through use of examples how the database has been used in geomorphologically-informed river management. We also provide a cautionary note on the limitations of the database and expert advice on lessons learnt during its development to aid others who are undertaking similar analyses.

Introduction

Applied fluvial geomorphologists have produced many frameworks, approaches, manuals and recommendations to support the use of geomorphology in river management [118]. While understandings of river geomorphology are far from a panacea for management applications, effective outcomes are unlikely to be achieved and sustained independent from insights into geomorphic river character and behaviour, sensitivity to adjustment, measures of condition and the evolutionary trajectory and recovery potential of rivers. These are vital components of proactive planning, risk assessment and the design and implementation of management practices that work with the river, rather than against it [1921]. Geomorphic principles document the physical template of a river system, providing a cross-scalar landscape platform upon which a host of biophysical and socio-cultural layers can be added and interpreted [2229]. Concerns for biodiversity management, for example, build upon understandings of the dynamic physical habitat template of river systems, and associated process connections in longitudinal (upstream-downstream), lateral (channel-floodplain) and vertical (surface-subsurface) dimensions [30, 31]. Critically, a catchment perspective provides a basis to analyse the sediment regime of a river [32], underpinning assessment of system responses to disturbance events (including management actions; [33]). Building on these foundations, geomorphology provides a platform for river conservation and restoration activities, both in terms of planning and on-the-ground actions [3436]. Despite all this promise and potential, it is not possible to make effective use of geomorphic understandings unless a reliable, coherent, systematic database is available. Systematic information bases are required to develop decision support systems that recognise diversity, consider condition and recovery prospects, and co-ordinate and prioritise actions as part of adaptive management practice [33, 37].

However, many challenges remain in the design and development of coherent scientifically-framed information databases, the process of making such databases available and Open Access, and the appropriate use of such databases in practice by suitably qualified practitioners. While a wealth of foundation understanding and knowledge may be in place, it is often fragmented and poorly coordinated. Therefore, many projects occur independently of such knowledge and understanding [3840]. In other cases multiple approaches have been used or single approaches have been applied inconsistently and non-systematically. As work on riverscapes becomes more multi-disciplinary [25, 41] and information technology changes how data is collected, interpreted, presented, stored and made available [27, 42], it is time for geomorphologists to be become better at developing and using coherent cross-scalar databases to support geomorphologically-informed river management [43].

In New South Wales (NSW), the State Government has coordinated and facilitated the derivation of state-wide coverage of a geomorphic layer to inform river management applications. This work has been completed using the River Styles Framework [11]. NSW Department of Planning, Industry and Environment (DPIE) have now published this state-wide spatial database via Creative Commons. The NSW River Styles database is the largest and most comprehensive dataset of geomorphic river character and condition available in Australia.

The database comprises analyses of river diversity (River Styles), geomorphic river condition [44] and geomorphic recovery potential [45], thereby providing a platform for geomorphologically-informed approaches to prioritisation of management activities. In its own right, this geomorphic database does NOT provide a comprehensive solution to all river management issues that require geomorphic understanding, let alone the vast range of other information that is required. However, many management applications are likely to be compromised unless they build upon such understanding and use such databases to support the generation of integrative scientifically-informed approaches to river management [25, 46].

The NSW River Styles database presents a coherent platform for learning and adaptive management–a living database that can be readily adjusted, updated and used. On the one hand, it provides a consistent and data-rich platform for the development of geomorphologically-informed river management tools, systems and strategies, something that has been called for several decades [47]. On the other hand, it presents an opportunity to share understandings of geomorphic river diversity, condition and recovery potential to a range of audiences who can use this evidence base to support coherent management practices. The availability of the database presents unprecedented opportunities to systematically consider management issues at local, catchment, regional and state-wide scales, and appropriately contextualise applications in relation to programs at other scales (e.g. internationally)–something that cannot be achieved independent from, or without, such a database [47].

There is no equivalent systematically-derived geomorphic database, conducted at such a scale and incorporating these layers of analysis and insight, in Australia. Importantly, this particular database extends far beyond an automated, off-site, appraisal of remote sensing imagery conducted using machine-learning models and applications [27, 4851]. A careful mix of remotely-sensed data and generic tools has been combined with targeted field verification to compile the database. This database has largely been derived by locally-based practitioners with considerable knowledge of ‘their’ rivers. In many places it has been verified in the field.

Essentially, this paper outlines what the River Styles database is, how it has been derived, how it has been used, and how it can/could be used into the future to support geomorphologically-informed approaches to river management. We outline the core attributes of this dataset, summarising some of the results that emerge from an initial overview of each layer. Following this, the discussion outlines how transformations of these data can, and have been used to inform different types of river management initiatives. We highlight issues that cannot be appraised independent from such data, and the critical importance of understanding interactions between each layer of information (i.e. the use of a scaffolded information base to inform coherent management applications). The discussion provides recommendations and limitations in the use of this database, ensuring that it not perceived as a panacea, but rather as a coherent framework that can underpin systematic approaches to river management practice.

Methods

How the database was derived

Development of the NSW River Styles database.

The River Styles Framework is a structured set of procedures for describing and interpreting rivers in geomorphic terms, to inform science-based river management [11]. The Framework has four stages (Fig 1): Stage 1 describes the geomorphic character of rivers and interprets their behaviour in terms of geomorphic process; Stage 2 determines geomorphic condition (integrity); Stage 3 evaluates the potential for a river to recover (improve in geomorphic condition) and Stage 4 identifies priorities for conservation and rehabilitation at the catchment scale [11]. The NSW Department of Planning, Industry and Environment (DPIE) added fields, including inherent fragility, to adapt the framework for its use. Using the River Styles Framework, rivers are characterised according to their present range of variability and diversity with process understandings and behavioural analysis undertaken through interpretation of form-process associations of geomorphic units [11, 52, 53] (Fig 2). Condition is assessed in terms of what is expected for a particular river (Fig 3; [44]) and recovery potential is determined according to what is realistically achievable given the character, behaviour and condition (Fig 4; [45, 54]).

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Fig 2. Geomorphic river diversity (River Styles) in NSW.

Four of the 47 different types of rivers found in NSW. Source of photos; Google Earth, K. Fryirs and G. Brierley as noted.

https://doi.org/10.1371/journal.pone.0244719.g002

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Fig 3. Geomorphic condition principles for a Confined floodplain pockets sand bed River Style in Bega catchment.

Uses same examples as in Fig 4. Source of photos; Google Earth and K. Fryirs.

https://doi.org/10.1371/journal.pone.0244719.g003

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Fig 4. Geomorphic river recovery principles and potential management actions (based on [44, 45]).

Uses same examples as in Fig 3. Source of photos K. Fryirs.

https://doi.org/10.1371/journal.pone.0244719.g004

The history of River Styles development and impact on river management practice is reported in [55]. The purpose of the River Styles Framework has always been to use foundation geomorphic principles to support scientifically-informed approaches to river management. The framework was designed to be flexible, assessing geomorphic attributes that are relevant/pertinent to a particular system. Hence, a generic, carefully scaffolded approach was designed to derive a coherent package of catchment-specific geomorphic information, relating process-based insights that can be applied to all rivers, everywhere [11, 24, 56]. Data and analyses are conducted within a hierarchical, cross-scalar framework [24, 57, 58]. Systematic approaches to data collection are used to explain spatial variability in geomorphic river character, behaviour, pattern, condition and recovery. Consistent application can help situate any given application within a much broader context, allowing consideration of the representativeness and transferability of understandings, and by extension, management decisions and responses.

The NSW River Styles database (the database hereafter) was developed by NSW Department of Planning, Industry and Environment (DPIE), in consultation with Macquarie University. It is based on River Styles reports completed by various analysts in various agencies over the past two decades (see acknowledgments). The database has spatial layers that correspond well to stages in the Framework. The river diversity layer divides rivers into reaches of the same River Style, classifying and naming them using the River Styles naming convention [59]. The condition layer classes reaches as good, moderate or poor geomorphic condition. The recovery potential layer combines assessment of both recovery potential and prioritisation to identify reaches with high, moderate or low recovery potential. These reaches are differentiated from conservation reaches, which are relatively intact (little or no recovery necessary) and strategic reaches that contain threatening processes that may impact on reaches with high conservation and rehabilitation value [45, 54]. The database also contains other attributes in its metadata that were developed by NSW DPIE Water such as fragility, change in condition, threatening processes and refugia type [60]. The database is available as an Open Access product at: https://trade.maps.arcgis.com/apps/webappviewer/index.html?id=425c7364e9dc4a71a90c4ba353b8949f.

Application trials of the River Styles Framework were initially conducted in the Bega [61, 62], Hawkesbury-Nepean and Manning catchments by Macquarie University, the NSW Department of Land and Water Conservation (now NSW Department of Planning, Infrastructure and Environment) and Catchment Management Authorities (now Local Lands Services NSW). Subsequent roll-out across the state was conducted by various agency personnel and consultants as part of State-wide assessment and mapping between 2009–2012, funded by DPIE Water, that culminated in a major effort to complete the State-wide River Styles mapping in 2011–2012. River Styles mapping was completed in support of the State-wide Catchment Action Plan activities the former CMAs were undertaking. An alignment process was developed whereby the State agencies brought in their products to align/inform CMA Natural Resource Management activities. Applications were mostly conducted by practitioners who had received professional development training and accreditation via the River Styles Short Course. Each report was reviewed by senior geomorphologists to ensure accuracy and consistency of application and interpretations. Applications were conducted using both field-derived and remote-sensing data, from aerial photographs in the early years, through the advent of Google Earth, to the use of Digital Elevation Models (DEMs). Importantly, 93% of the database has been verified in the field and confidence limits placed on the metadata.

Results

The raw data of the NSW River Styles database

The outward-facing database contains a series of maps showing findings from use of the different stages of the River Styles Framework. Because the database has a zoom-in and zoom-out function it can be used as a basis for undertaking fine-scale analyses (e.g. reach-scale) alongside state-wide assessments. Here, we simply provide a broad overview of the scale, extent and resolution of the database, and a summary of state-wide insights into river diversity, river condition, river recovery and related implications for prioritisation of management activities as part of geomorphologically-informed approaches to proactive, cost-effective river management. Embedded behind the maps is the master database that can be requested from NSW DPIE for use. To produce the results for this paper, the master data has been cleaned and processed. For example, some data pertaining to estuarine systems has been removed. S1S3 Tables provide summary, cleaned data.

The achievement: Scale, extent and resolution of the database

The database covers a total stream length of 216,600 km over an area of 802,000 km2. This is an area that is 70% the size of Colombia, 65% the size of South Africa, 25% the size of India, 10% the size of Brazil, the size of the United Kingdom and France combined, the size of the USA states of Texas and Kentucky combined or three-times the size of New Zealand. The resolution is approximately 1:1000. Reaches scale in length from 120 m to 15.5 km. It is important to note that, to date, only 3rd order streams and above have been analysed.

River diversity.

The database identifies 47 River Styles across the state, four of which are in a confined valley setting, 15 in a partly-confined valley setting and 28 in a laterally unconfined valley setting (20 with continuous channel and eight with discontinuous channel) (Fig 5). This enables analyses of the frequency of occurrence (stream length) of differing types of rivers and appraisal of controls upon their patterns (S1 Table). Confined and partly-confined rivers dominate on and East of the Great Dividing Range whereas laterally unconfined rivers dominate West of the divide (Fig 5C).

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Fig 5. The diversity of River Styles identified in the NSW River Styles Database.

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The most ubiquitous River Styles by stream length were the Confined headwater (10.9%) Confined occasional floodplain pockets gravel bed (9.5%) River Styles, reflecting their position in the headwaters of catchments, where drainage density is typically greater than mid- and lower-catchment positions. The rarest River Styles by stream length were the Partly confined bedrock controlled low sinuosity gravel, Laterally unconfined multi-channel sand belt and discontinuous sand bed variants (all accounting for <0.1% of total stream length statewide). Given that River Styles analysis has only been conducted, to date, on 3rd order streams or higher, lower order watercourses (including upland valley fills) are under-represented.

There is marked variability in rivers east and west of the great divide (inland-draining and coastal catchments), and notable differences between rivers on the North and South Coast (Fig 5). For example, Laterally unconfined meandering fine grained rivers tend to be found on inland rivers, and coastal rivers are dominated by Confined and Partly confined rivers (some 83% of stream length in coastal catchments is comprised of confined and partly confined variants). Partly confined planform controlled meandering rivers are present in northern coastal catchments but not in southern coastal catchments, and anabranching rivers are found exclusively inland. The catchment with greatest diversity of River Styles (33) are in the Hunter, likely owing to this catchment’s topographic setting and intersection between diverse geologies. Aside from Sydney Metro catchment, the Barwon-Darling had the lowest diversity with nine River Styles.

River condition.

The database shows how geomorphic river condition varies according to attributes such as valley setting as well as allowing comparison between catchments. Across NSW, 39% of total stream length was in good geomorphic condition, 42% moderate, 19% poor and <1% with no data (Fig 6). Rivers in confined valley settings tended to be in the best overall condition, with the highest proportion of stream length in good condition (65%) and the smallest proportion in moderate (25%) or poor (9%) condition. This likely reflects the limited potential for rivers in confined settings to adjust, as well as their position in the catchment, often in steep areas unsuitable for intensive land use.

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Fig 6. The geomorphic condition of rivers identified in the NSW River Styles database.

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Partly confined rivers had the highest proportion of stream length in either moderate or poor condition (16% good, 54% moderate and 29% poor) and laterally unconfined rivers with continuous channels were in similar overall condition (24% good, 51% moderate and 25% poor). Laterally unconfined rivers with discontinuous channels were overall in better condition, with 46% of stream length in good condition, 42% moderate and 12% poor. While these results may seem surprising, these discontinuous watercourses are often remnants and ‘degraded’ reaches have often been channelised and therefore characterised as a different River Style (Laterally unconfined, channelised fill). Once disturbed, discontinuous watercourses often experience river change (a wholesale shift in river character, behaviour and therefore river type) [63].

Coastal catchments overall were in better condition than inland catchments, but there were notable exceptions. For example, the Hunter catchment (coastal) had the highest percentage of stream length in poor condition (45%) and the Western region (inland) had the second-highest percentage of stream length in good condition (62%). River Styles Geomorphic Condition Index (RSGCI) scores were calculated for all catchments using the method described in the NSW Government’s River Condition Index [60], where:

The average RSGCI score across the state was 0.62 out of a maximum score of 1.0 (S2 Table). Nine regions scored at or above average (Central Coast, Hawkesbury-Nepean, Lower North Coast, Northern Rivers, Southern Rivers, Sydney Metro, Barwon-Darling, Lachlan and Western). Eight catchments scored below average, of which six were in an inland setting. The Hunter Catchment was the lowest scoring (0.37), followed by the Namoi Catchment (0.40).

River recovery potential and prioritisation.

The database combines elements of Stages 3 and 4 of the River Styles Framework. This layer provides a statewide picture of geomorphic recovery potential, which, when combined with geomorphic condition, can inform prioritisation of conservation and rehabilitation efforts at various scales. Intact reaches assigned conservation status accounted for 39% of stream length (Fig 7). Strategic and high recovery potential accounted for 22% when combined, leaving 39% in the lower priority categories of moderate (25%) or low (14%).

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Fig 7. The recovery potential and prioritisation of rivers identified in the NSW River Styles database.

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Coastal catchments in general had greater recovery potential than inland catchments, with a marginally greater percentage of overall stream length with Conservation or High recovery potential and a much smaller percentage in Low condition (6.6% and 6.9% Low in North and South coastal catchments compared with 19% inland) (S3 Table). Catchment with significant stream length of Conservation or High recovery potential status occur in the Northern Rivers, Southern Rivers, Central West, Lachlan and Western regions. Central Coast, Sydney Metropolitan and Border Rivers also had high percentages of stream length with Conservation or High recovery potential, although these catchments have significantly less total stream length. Note that large portions of the Sydney Metropolitan catchment were not assessed due to urban development. Hotspots of Moderate and Low recovery potential included the Hunter, Central West–Castlereagh, Central West–Macquarie Bogan and Namoi catchments.

By valley setting, confined River Styles had the greatest percentage of stream length with conservation (65%) and high (14%) recovery potential as well as the smallest percentage of stream length with moderate (15%) and low (4%) recovery potential. This likely reflects the limited capacity for confined River Styles to adjust (greater resilience).

However, the second-largest percentage of stream length with Conservation status was found in the laterally unconfined–discontinuous channel setting. This group of River Styles also had the second-lowest percentage of stream length with Moderate (25%) or Low (10%) recovery potential. River Styles in partly-confined and laterally unconfined–continuous channel settings had the poorest overall recovery potential, with the majority of stream length being classified as Low or Moderate.

Discussion

With this database, what can we do now that we could not do before?

The NSW River Styles database provides a new opportunity for us to better ‘know our rivers’ and undertake geomorphologically-informed decision making in river management. Some uses of the database that are now possible, at a range of different scales are outlined in Table 1. Some of these uses are already occurring, while others are yet to be realised.

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Table 1. Uses of database data at different scales–developed uses, potential uses and uses that are not yet realised.

https://doi.org/10.1371/journal.pone.0244719.t001

While the database is not perfect (no database ever is), it does provide for the first time an unprecedented big picture view of geomorphology for the purposes of river management, with diversity, geomorphic condition and recovery potential analyses contained in one place. As such, the database provides an integrating platform to do things that were not possible before. Such things include the capacity to compare like-with-like, analyse the diversity and patterns of river types across the State, understand where rivers are in good, moderate or poor geomorphic condition and where rivers have potential to recover. The database also allows users to situate their work by placing habitat-, site- and reach-scale analyses and management measures into a broader context–catchments and regions [24, 47]. This provides opportunities to scale-up management approaches and decisions to assess what works where and why. For example, it provides opportunities to combine and analyse datasets (eg aquatic habitat, threatened species and fish community mapping) and strategically target priority rehabilitation reaches with targeted funding and resources, which have to date been largely ad-hoc in their delivery [64].

The construction of a database develops a feedback process between researchers, end-users and

managers, as authorities who provide the data seek to implement the findings of the research. The process of standardisation provides a higher level mechanism for quality assurance and quality control, thus making each database more valuable. Generation and provision of the database outlined in this study can now support geomorphic and scientifically-informed, evidence-based, transparent decision making and river management, particularly in terms of prioritisation and resourcing. Each map provides foundation/baseline information that can be used for a range of purposes by a range of different stakeholders at a range of different scales [25]. Because the maps are contained within a GIS environment, they can be zoomed-in and zoomed-out to obtain information and make evidence-based decisions at a range of scales. Moving beyond the use of the database as a reporting tool or a static map, it provides information that allows users to ask a range of questions of importance for river conservation and management [65]. The ability to question across layers provides opportunities to query, interpret and explain broad patterns using multiple lines of evidence [27]. It allows users to question and interpret relationships between river character, condition and recovery potential, appraise similarity and variability, representativeness and transferability, rarity and threat. For example, visual comparison of statewide river condition and recovery potential data (Figs 6 and 7) suggests that rivers in poor condition were more likely to have low recovery potential in inland settings and moderate recovery potential in coastal settings. A possible explanation is provided by interpretation of the river diversity data, that considers the river type, its capacity to adjust and the materials that make up that river. It is very difficult to repair fine-grained rivers that are prevalent in inland catchments once they become degraded (Fig 8A). For these rivers, the trapping of fine-grained materials that support or enhance recovery is more difficult to achieve when compared to sand or gravel based rivers found in coastal catchments that can readily form benches that become stabilised by vegetation [54] (Fig 8A and 8B). In this simple example, information from multiple layers of the database enable deeper questioning and understanding of patterns in the data, providing one part of an evidence-base for subsequent decision making.

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Fig 8. Fine-grained river in inland NSW and sand bed river in coastal NSW.

Source of photos; K. Fryirs as noted.

https://doi.org/10.1371/journal.pone.0244719.g008

At the local scale (site and reach scale) the database provides a place-based information resource for local communities and landowners. People like to understand ‘their’ river, situating relations and understandings of ‘their’ river in the context of rivers elsewhere (e.g. diversity, key attributes, behaviour, condition). Promoted and used effectively, the database could provide a vehicle for community engagement and communication, supporting efforts to evaluate and look after things that matter (e.g. local values, assets, infrastructure etc).

At the local scale (site and reach scale), information in the database can be used to identify high priority and strategic reaches for conservation and/or rehabilitation (Fig 9). This helps in the design of rehabilitation (e.g. placement of wood and revegetation) options that are tailored to the type of river, its condition and recovery potential, ensuring that appropriate techniques are used in the right places for the character and behaviour of the river (Fig 10). For example, weed management and revegetation plans relate selection of species to geomorphic attributes such as the substrate, hydrological and seedbank conditions of differing geomorphic surfaces along the river [66] and wood placement is appropriate for the adjustment potential and habitat needs of the river. Using the fragility layer, processes that threaten the geomorphic integrity of reaches can be identified and decisions made about treatment responses. Working with condition and recovery shifts the emphasis from reactive to proactive river management practice, tailoring approaches that suit the conditions at any particular site or reach. Importantly, identification of reaches that are self-healing helps decision-makers to know when they can choose to opt-out of direct intervention measures, allowing the river to ‘work itself out’ as a form of passive management practice [54, 67, 68]. Such thinking has already been successfully applied in on-ground works in NSW conducted by Catchment Management Authorities, NSW Local Land Services, and other non-government agencies (e.g. Australian River Restoration Centre).

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Fig 9. High priority and strategic reaches for conservation and rehabilitation generated from the recovery layer in the NSW River Styles database.

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Fig 10. River rehabilitation panning.

The Upper Hunter River Rehabilitation Initiative. Sources as noted.

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Working with condition and recovery at the site and reach scale also allows for identification of ‘basket cases’, those rivers that are in poor condition and have low recovery potential [69, 70]. Decisions can be made about whether to invest resources and finance in the rehabilitation of such reaches (or not) and if so, what is a reasonable and socially acceptable level of intervention to take [69]? Knowing whether an intervention is geomorphologically-informed or socially-driven helps decision makers and investors to set realistic expectations about the intended outcomes of management practices. As an example, the NSW database could be used to ensure such measures are applied to appropriate reaches framed in their catchment context on the one hand [33], while supporting investment in high priority and strategic reaches on the other [27].

Local scale (site and reach scale) insights from the database can be used alongside biodiversity and hydrology data to assess local habitat, flow and refugia conditions [30]. For example, the geomorphic recovery potential layer in the NSW database has been matched with hydrological stress to help set water extraction rules at the local scale [70] (Fig 11). Such analyses have also been up-scaled to reach, subcatchment and catchment scales to develop Water Sharing Plans [71] that are harmonised with Catchment Action Plans (CAPs) [60]. Beyond this, NSW DPI (Fisheries) has combined the database with standard statistical analysis and internationally recognised spatial distribution models to provide a delineation and spatial recognition of the status of fish communities and threatened freshwater fish species distributions across NSW [64]. The example shown in Fig 12 uses the River Styles database to relate the distribution of fish and threatened frogs to certain types of habitats along different river types. In the USA, the Columbia Habitat Monitoring Program (CHaMP) has developed its own database for fish habitat mapping and monitoring, appraising life-cycle processes and carrying capacity of rivers from local to catchment scales [72, 73].

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Fig 11. Matching geomorphic recovery potential to hydrological stress for water extraction rule-setting as part of Water Sharing Plans (WSPs).

DPIE Water Risk assessment includes hydrology and geomorphic recovery potential. Shown for the Namoi Catchment in 2018.

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Fig 12. Linking geomorphic river type to general fish community status derived from condition indicators of expectedness, nativeness and recruitment and indicative threatened fish distribution and threatened frog species.

Source of photograph: Sloane’s Froglet from Peter Robertson at grasslands.ecolinc.vic.edu.au.

https://doi.org/10.1371/journal.pone.0244719.g012

At a broader sub-catchment and catchment scale, the database has been used by NSW DPIE and Catchment Management Authorities to generate Water Sharing Plans (e.g. Fig 11), Catchment Action Plans and River Health Strategies. Such programmes inform water licensing and compliance activities, risk and threat analysis and prioritisation of on-ground rehabilitation initiatives. Incorporation of geomorphology (River Styles condition) within monitoring and evaluation programmes that apply the NSW River Condition Index (RCI) show how the physical condition of the system is a key limiting factor in river health in some instances (e.g. Fig 13). For example, several streams in the headwaters of the Namoi Catchment are in poor overall condition. They have a very poor River Styles condition, vegetation quality is very poor, but hydrological stress is moderate. For these systems the condition of the geomorphology and riparian vegetation are limiting. To improve the overall health of these systems will require rehabilitation of the geomorphology and riparian vegetation (i.e. the physical habitat template) rather than the hydrology. Finer-scale metadata in the River Styles condition layer of the database can help users determine what to treat and what to leave alone [44, 54]. Conversely, the good to very good condition of geomorphic and riparian vegetation attributes of some western parts of the Murrumbidgee catchment are not the limiting factor to river health; rather, these streams are subjected to high hydrological stress (Fig 13). These examples show how interrogation of patterns in the database can aid objective and pragmatic decision making on what to prioritise and treat (or not) in river management practice. Such information can be fed directly into decision support tools to support the design and implementation of on-ground actions. Similar approaches to analysis in other parts of the world have built upon these principles (e.g. European MQI [74, 75]; UK MoRPh [76, 77]).

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Fig 13. NSW River Condition Index that integrates across multiple layers of attributes including River Styles (geomorphic) condition.

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Applications of the database at regional and state/territory scales can help to articulate state-wide priorities and match these with regional bodies and organisations that are mandated to implement river and water management policies. This now provides a vehicle to incorporate previously overlooked geomorphic criteria (attributes of the physical habitat mosaic) within consistent, more inclusive approaches to State of Environment reporting and Regional Biodiversity assessments. Such applications now inform and influence state water policy. For example, state-wide applications of the NSW riverine High Ecological Value Aquatic Ecosystem (HEVAE) project identify and define a range of instream values and levels of importance for freshwater river reaches in NSW (e.g. Fig 14). This unprecedented catchment and reach-scale resource supports prioritisation of management actions in relations to areas at risk of disturbance. Such water management practices will benefit all water users and riparian environments across the State [71]. Fig 15 shows the level of detail that can be obtained at the sub-catchment and reach-scales for the inland draining systems, demonstrating how an integrative set of value variables can be used to undertake an assessment of risk to instream values. The example presented is for the Border Rivers-Gwydir catchment (former CMA) in the central north of the State.

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Fig 14. State-wide High Ecological Value Aquatic Ecosystem (HEVAE) assessment that includes River Styles value as one layer.

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Fig 15. High Ecological Value Aquatic Ecosystem (HEVAE) and prioritisation based on risk of physical disturbance to instream values at the catchment and reach scales.

Instream value contains analysis of the values such as geomorphic (River Styles), threatened species, water sharing, environmental assists and high conservation vegetation. The likelihood of physical disturbance to these values is then assessed to produce risk to instream values maps that can be used in prioritisation activities.

https://doi.org/10.1371/journal.pone.0244719.g015

Although each layer within the NSW database presents a static representation of a particular attribute, there is prospect to incorporate new and emerging datasets such as Google Earth Engine to make this a dynamic interface [78, 79]. Even in its current form, however, the database provides a snapshot in time that can support monitoring programs, helping to ensure that measures are tailored to the river type and provide a reliable relevant signal of river condition [44, 70, 80]. With a state-wide database in-hand, it is possible to address two important considerations that could not previously be appraised in a systematic manner. First, conservation targets such as distinctive, rare or threatened types of river can be managed in a proactive manner [71] (Fig 16). Second, incorporation of timeslices within the recovery layer can help to track changes over time (i.e. changes in colours and patterns), thereby supporting systematic appraisal of threatening processes.

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Fig 16. Rarity and threatened River Styles in NSW.

Source of photos as noted.

https://doi.org/10.1371/journal.pone.0244719.g016

At the national scale, the database provides a systematic reporting tool, prospectively supporting efforts to match and align state-wide priorities and reporting with National scale reporting frameworks in a more robust and consistent manner (Table 1). Potentially this could help situate national policies in relation to broader international or intercontinental programs, such as International Water programmes, conservation initiatives (e.g. Ramsar Convention on Wetlands of International Importance) or efforts to meet UN Sustainability Goals (Table 1). In Australia the River Styles database has been incorporated into the Sustainable River Audits and Australian National Aquatic Ecosystem (ANAE) classification (e.g. for the Murray-Darling Basin) [81] and used to align NSW DPIE Water instream value assessments with national frameworks such as HEVAE (e.g. Figs 14 and 15).

Limitations and lessons learnt during the development and application of the NSW River Styles database–it’s not a panacea

No dataset or database is without its limitations. Inevitably, each dataset reflects a particular set of drivers, methods and contexts that were established at a particular moment in time, then amended and updated periodically. This may reflect advances in data generation techniques or changing institutional goals, priorities, needs and legislated requirements. Here we present a brief overview of limitations in the framing, derivation and reporting of the NSW River Styles database.

While the database is coherent and directly applicable to various management issues outlined above, it is not purpose built for all applications. For example, the data layers are presented in a static form and focus largely on the structural characteristics of rivers. Much of the mapping was conducted at the scale of available aerial photographic imagery. If conducted today, maps would be produced at scales that are directly appropriate for each section of river system. In a zoom-in, zoom-out world of Google Earth, landscapes can be examined and analysed across the full range of hierarchical scales [58, 82]. Also, systematic availability of DEMs now allows analysis of all parts of landscapes [27]. Comprehensive ‘whole of landscape’ analyses are now possible and gaps will be filled as resources become available in future.

Analyses of process, behaviour and evolution are not presented in the database. But, it does present a coherent platform to start to undertake systematic analyses at unprecedented scales, as baseline fluvial geomorphic information is now available state-wide. For example, decadal reassessments will incorporate comparisons in geomorphic condition over time to establish trends in condition and priorities [60]. Also, it would now be relatively easy to supplement the existing database by incorporating analyses from Google Earth Engine or other remote sensing technologies to help transition the dataset into a ‘dynamic entity’ to inform scientific and management applications [21, 79, 83].

Given various practical considerations in the long-term development of the dataset, over a period of around 20 years, insufficient resources were available to implement effective and long-lasting quality assurance and quality control (QA/QC) procedures across the dataset as a whole (accompanying metadata are under-reported). More systematic emphasis upon assigning confidence limits to the data, and consistent application of the River Styles naming convention would also have been preferred [59]. As procedures are now in-hand to accomplish such tasks, this situation can be more readily addressed into the future, in the derivation and enhancement of this and other datasets [84]. Both the QA/QC and renaming of River Styles has been a time consuming ex-post exercise that could have been avoided if rigorous QA/QC had been developed. However, the process of ‘standardisation’ has provided a level of QA/QC that makes the database more useable and valuable [65]. Better metadata statements that carefully document different operators, scales of analysis and approaches to field testing and verification that were undertaken are needed [84]. Related to this, insufficient time and resources were given to verifying interpretations in the field. Time limits were placed on delivery of assessments that did not align with the spatial scale or resolution of the analyses being conducted in different places. For example, insufficient time to analyse catchments with >20,000 km of stream length or assessments conducted very quickly (e.g. in < 12 months) lead to excessive ‘clumping’ of River Styles or condition analyses at the sub-catchment scale.

Applications of the River Styles Framework have demonstrated that it has significant explanatory power [72, 73, 85]. However, this also comes with risks and potential for misuse, with untrained or inexperienced users using the Framework and database for purposes other than those for which they were initially derived. For example, great caution must be applied when using the database as the primary source of information for setting water availability and extraction rules, and compliance, or for justifying engineering interventions in rivers [70]. Although such applications may be perceived as required, and geomorphic information may be useful to them, they may need different forms of geomorphic insight. Just because the River Styles database may be the only available systematic, state-wide information base does NOT mean it is relevant to all instances in which geomorphic insight is required. The River Styles database is not a panacea that can be used for all riverine-related projects and to solve all problems. Hence, any extrapolations in application need to be rigorously tested to ensure that they are appropriately fit for purpose. If multi-purpose layers are to be used, they must build appropriately on strong foundations. Inappropriate applications may draw into question confidence in uptake for other purposes that align directly with initially-intended purposes. Herein lie concerns for professional credibility and integrity.

Table 2 presents a summary of some lessons learnt in the derivation and application of the NSW River Styles database, so others who are embarking on development of their own databases can learn from our experiences. A key message is that co-ordination of activities at the science-management interface is challenging [86], especially in longer-term projects and commitments conducted in relation to inevitable (and recurrent) changes in personnel and institutional arrangements (restructuring). Long-standing research, engagement and impact collaboration was, and remains, essential for this work [55, 70, 87].

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Table 2. Lessons learned in the development and application of the NSW River Styles database.

https://doi.org/10.1371/journal.pone.0244719.t002

Moving forward: Situating the River Styles database for use in science and management

It is one thing to have the NSW River Styles database, but quite another to contemplate the usefulness and practical application of this valuable resource. With a decent information base in-hand, the potential for geomorphologically-informed river management is high. Prospectively, the NSW River Styles database can enhance integrative river management in ways that are not possible with unconsolidated or fragmented data [46]. Untold benefits, impacts and end-users, many unimagined at this time, could emerge in the future [55]. However, as we have learnt on this journey–training is critical. Knowing what such databases hold and how to use this information ‘correctly’ is critical. Suitably qualified and trained professionals are needed if geomorphologically-informed river management is to achieve best practice.

River management is much more than a collection of projects; it is an ongoing commitment, obligation and responsibility [38, 39, 88]. Appreciation of the proper use and value of the River Styles database requires ongoing engagement and education. Improving community comprehension of risk to river integrity and consequences of river degradation needs ongoing contact and education [89]. Ongoing commitment by government and industry is required to ensure that the River Styles database and the assessments that underpin it remain a living project, meeting practitioner, industry and community needs and expectations [90].

Perhaps one test of such a database lies in its capacity to act as a medium for relating local knowledges to geomorphologically-informed river management practices. It can act as a pivot for developing a collective sense of riverscapes, that relates place-based local connections and knowledges to broader scale (state, national or international) programmes and applications [9194] and support participatory engagement and collective commitment and championship of a duty of care in river management [86, 9598].

The construction of the database has, in itself, developed a feedback process between researchers, practitioners, managers and end-users [65]. Effective, coherent and inclusive approaches to river management now need to build upon, and value-add to, this collectively-owned information and the understandings that come with it. As the NSW database is Open Access, there is considerable opportunity to develop a coordinated whole-of-government (and non-government programmes) that use a consistent information base [97]. In turn, the database could provide a sense of common ground that helps facilitate cross-scalar, cross-institutional approaches to river management, acting as a communication platform between people, within communities and across organisations–domestically and internationally.

Proactive and strategic measures are not possible in the absence of such databases and the understandings that accompany them, inhibiting prospects to determine what is realistically achievable through management efforts, and what measures must be applied to achieve and sustain the outcomes pursued [32, 98]. Without such databases, it is not possible to ‘be ready’ with capacity to ‘hold steady at times of crisis’, limiting management responses to renewed reapplication of reactive measures, many of which we know will not work in the long term [88]. Reactive management is costly and restricts future prospects. Even more alarmingly, such reactive measures set path dependencies that compromise prospects for more generative programmes into the future.

While the NSW database has been developed using a combination of ‘traditional’ desk-top and field methods and is currently presented as a set of static maps, its value should not be diminished. Use of the River Styles Framework has contributed to the adoption of process-based river management in NSW [c.f. 36, 99]. To produce the outputs presented in this paper requires interpretation of river behaviour, evolution, patterns and (dis)connectivity that extend well beyond the production of a map [100102]. Nowadays however, new technologies and analysis techniques simply make the job of developing some parts of a River Styles database more time and cost-efficient (e.g. using Google Earth and Google Earth Engine (GEE) along with Geomorphic Change Detection (GCD) and automated tools for geomorphic analysis of rivers) [78, 88, 83]. We are not yet at a situation where databases such as the NSW database can be fully automated, but certain parts of the analysis can be semi-automated using available and emerging ‘plug-in’ tools for analysis [88] and by tapping into large-scale remote sensing datasets and toolboxes held in Open Access or consortium-based repositories [27, 51, 83]. Such advances provide a fantastic opportunity to now juxtapose a static map with analyses conducted using GEE or GCD (for example) to display river adjustment, behaviour and change over time [21, 79]. Such analyses are sparking a wave of innovation and collaboration in the development of semi-automated tools to support geomorphic analyses of rivers, allowing new science questions to be asked about river diversity, behaviour, condition, trajectory and forecasting. However, it is rare that approaches to generation and use of geomorphic datasets are undertaken using a coherent framework that is applied consistently and at the scales needed for catchment, state, national or international planning and decision making. The NSW database provides an example of what can be achieved and what is needed moving forward. It provides a fantastic basis for considerable value-adding, extension and multi-use uptake by government, industry and community in years to come.

Conclusion

The NSW Government has facilitated state-wide delivery of a geomorphic layer for the analysis of rivers. This database has been crafted and implemented using procedures from the River Styles Framework. Although this does not provide a comprehensive answer or solution to all river management problems, we are unaware of an equivalent database produced to support a systematic, geomorphologically-informed approach river management practice. Done properly, this supports a whole-of-government approach. After all, fragmented science can only engender fragmented management.

Supporting information

S1 Table. Total stream length of River Styles in the NSW River Styles database.

Note: the raw data in the master database has been processed to produce this summary.

https://doi.org/10.1371/journal.pone.0244719.s001

(DOCX)

S2 Table. Scores for RSGCI by catchment.

Scores in bold are below average.

https://doi.org/10.1371/journal.pone.0244719.s002

(DOCX)

S3 Table. Percentages of stream length in each region and catchment that are in different recovery potential and prioritisation classes in the NSW River Styles database.

Note: the raw data in the master database has been processed to produce this summary.

https://doi.org/10.1371/journal.pone.0244719.s003

(DOCX)

Acknowledgments

Release of the NSW River Styles database is the result of around 20 years of collaboration between the NSW DPIE team and Macquarie University. It has involved the expertise of many practitioners and geomorphic experts to further progress the framework and roll it out across the State. We would particularly like to acknowledge the contributions of David Outhet, Nick Cook, Rob Ferguson, Guy Lampert, Ivars Renfelds, Tim Cohen, Rachel Nanson, Carolyn Young, George Schneider, Elisa Zavadil, Tony Broderick, Fiona Marshall, Paul Bennett, Jenny Weingott, Alison Lewis, Bilal Hossain and David Workman.

References

  1. 1. Petts GE. Impounded rivers: perspectives for ecological management. Wiley; 1984.
  2. 2. Sear DA. River restoration and geomorphology. Aquatic Conservation: Marine and Freshwater Ecosystems. 1994 Jun;4(2):169–77.
  3. 3. Challenges Brookes A. and objectives for geomorphology in UK river management. Earth Surface Processes and Landforms. 1995 Nov;20(7):593–610.
  4. 4. Sear DA, Newson MD, Brookes A. Sediment‐related river maintenance: the role of fluvial geomorphology. Earth Surface Processes and Landforms. 1995 Nov;20(7):629–47.
  5. 5. Bravard JP, Landon N, Peiry JL, Piégay H. Principles of engineering geomorphology for managing channel erosion and bedload transport, examples from French rivers. Geomorphology. 1999 Dec 1;31(1–4):291–311.
  6. 6. Gilvear DJ. Fluvial geomorphology and river engineering: future roles utilizing a fluvial hydrosystems framework. Geomorphology. 1999 Dec 1;31(1–4):229–45.
  7. 7. Thorne CR. Stream reconnaissance handbook: geomorphological investigation and analysis of river channels. John Wiley & Sons Ltd; 1998.
  8. 8. Rutherfurd ID, Jerie K, Marsh N. A rehabilitation manual for Australian streams. Canberra: Land and Water Resources Research and Development Corporation and Cooperative Research Centre for Catchment Hydrology (Vol 1 and 2); 2000.
  9. 9. Kondolf GM, Piégay H. Tools in fluvial geomorphology. John Wiley and Sons; 2003.
  10. 10. Downs P, Gregory K. River channel management: towards sustainable catchment hydrosystems. Routledge; 2004.
  11. 11. Brierley GJ, Fryirs KA. Geomorphology and river management: Applications of the River Styles Framework. John Wiley & Sons; 2005.
  12. 12. Thorne C, Hey R, Newson M. Applied fluvial geomorphology for river engineering and management. John Wiley and Sons Ltd; 2005.
  13. 13. Newson MD, Large AR. ‘Natural’rivers,‘hydromorphological quality’and river restoration: a challenging new agenda for applied fluvial geomorphology. Earth Surface Processes and Landforms: The Journal of the British Geomorphological Research Group. 2006 Nov;31(13):1606–24.
  14. 14. Darby S, Sear D, editors. River restoration: managing the uncertainty in restoring physical habitat. John Wiley & Sons; 2008.
  15. 15. Newson M. Land, water and development: sustainable and adaptive management of rivers. Routledge; 2009.
  16. 16. Sear DA, Newson MD, Thorne CR. Guidebook of applied fluvial geomorphology. Thomas Telford Ltd; 2010.
  17. 17. Simon A, Bennett SJ, Castro JM, editors. Stream restoration in dynamic fluvial systems: Scientific approaches, analyses, and tools. John Wiley & Sons; 2013.
  18. 18. Rhoads BL. River Dynamics: Geomorphology to Support Management. Cambridge University Press; 2020.
  19. 19. Biron PM, Buffin-Bélanger T, Larocque M, Choné G, Cloutier CA, Ouellet MA, et al. Freedom space for rivers: a sustainable management approach to enhance river resilience. Environmental management. 2014 Nov 1;54(5):1056–73. pmid:25195034
  20. 20. Buffin-Bélanger T, Biron PM, Larocque M, Demers S, Olsen T, Choné G, et al. Freedom space for rivers: An economically viable river management concept in a changing climate. Geomorphology. 2015 Dec 15;251:137–48.
  21. 21. Williams RD, Bangen S, Gillies E, Kramer N, Moir H, Wheaton J. Let the river erode! Enabling lateral migration increases geomorphic unit diversity. Science of The Total Environment. 2020 May 1;715:136817. pmid:32040992
  22. 22. Thorp JH, Thoms MC, Delong MD. The riverine ecosystem synthesis: biocomplexity in river networks across space and time. River Research and Applications. 2006 Feb;22(2):123–47.
  23. 23. Sayer J, Sunderland T, Ghazoul J, Pfund JL, Sheil D, Meijaard E, et al. Ten principles for a landscape approach to reconciling agriculture, conservation, and other competing land uses. Proceedings of the national academy of sciences. 2013 May 21;110(21):8349–56.
  24. 24. Gurnell AM, Rinaldi M, Belletti B, Bizzi S, Blamauer B, Braca G, et al. A multi-scale hierarchical framework for developing understanding of river behaviour to support river management. Aquatic Sciences. 2016 Jan 1;78(1):1–6.
  25. 25. Hawley RJ. Making stream restoration more sustainable: A geomorphically, ecologically, and socioeconomically principled approach to bridge the practice with the science. BioScience. 2018 Jul 1;68(7):517–28. pmid:30002563
  26. 26. McManamay RA, Troia MJ, DeRolph CR, Olivero Sheldon A, Barnett AR, Kao SC, et al. A stream classification system to explore the physical habitat diversity and anthropogenic impacts in riverscapes of the eastern United States. PloS one. 2018 Jun 20;13(6):e0198439. pmid:29924829
  27. 27. Dallaire CO, Lehner B, Sayre R, Thieme M. A multidisciplinary framework to derive global river reach classifications at high spatial resolution. Environmental Research Letters. 2019 Jan 25;14(2):024003.
  28. 28. Johnson MF, Thorne CR, Castro JM, Kondolf GM, Mazzacano CS, Rood SB, et al. Biomic river restoration: A new focus for river management. River Research and Applications. 2020 Jan;36(1):3–12.
  29. 29. Polvi LE, Lind L, Persson H, Miranda-Melo A, Pilotto F, Su X, et al. Facets and scales in river restoration: Nestedness and interdependence of hydrological, geomorphic, ecological, and biogeochemical processes. Journal of Environmental Management. 2020 Jul 1;265:110288. pmid:32421567
  30. 30. Thomson JR, Taylor MP, Fryirs KA, Brierley GJ. A geomorphological framework for river characterization and habitat assessment. Aquatic Conservation: Marine and Freshwater Ecosystems. 2001 Sep;11(5):373–89.
  31. 31. Kondolf GM, Boulton AJ, O'Daniel S, Poole GC, Rahel FJ, Stanley EH, et al. Process-based ecological river restoration: visualizing three-dimensional connectivity and dynamic vectors to recover lost linkages. Ecology and society. 2006 Dec 1;11(2).
  32. 32. Wohl E, Lane SN, Wilcox AC. The science and practice of river restoration. Water Resources Research. 2015 Aug 1;51(8):5974–97.
  33. 33. Brierley G, Fryirs K. Don’t fight the site: three geomorphic considerations in catchment-scale river rehabilitation planning. Environmental Management. 2009 Jun 1;43(6):1201–18. pmid:19301067
  34. 34. Wohl E, Angermeier PL, Bledsoe B, Kondolf GM, MacDonnell L, Merritt DM, et al. River restoration. Water Resources Research. 2005 Oct;41(10).
  35. 35. Wohl E, Bledsoe BP, Jacobson RB, Poff NL, Rathburn SL, Walters DM, et al. The natural sediment regime in rivers: broadening the foundation for ecosystem management. BioScience. 2015 Apr 1;65(4):358–71.
  36. 36. Wheaton JM, Bennett SN, Bouwes NW, Maestas JD, Shahverdian SM, editors. Low-tech Process-based Restoration of Riverscapes: Design Manual. Utah State University Restoration Consortium; 2019.
  37. 37. Boitsidis AJ, Gurnell AM, Scott M, Petts GE, Armitage PD. A decision support system for identifying the habitat quality and rehabilitation potential of urban rivers. Water and Environment Journal. 2006 Sep;20(3):130–40.
  38. 38. Bernhardt ES, Palmer MA, Allan JD, Alexander G, Barnas K, Brooks S, et al. Synthesizing US river restoration efforts. Science. 2005 Apr; 308(5722):636–637. pmid:15860611
  39. 39. Spink A, Hillman M, Fryirs K, Brierley G, Lloyd K. Has river rehabilitation begun? Social perspectives from the upper hunter catchment, New South Wales, Australia. Geoforum. 2010 May 1;41(3):399–409.
  40. 40. Pedersen ML, Kristensen KK, Friberg N. Re-meandering of lowland streams: will disobeying the laws of geomorphology have ecological consequences?. PloS one. 2014 Sep 29;9(9):e108558. pmid:25264627
  41. 41. Castro JM, Thorne CR. The stream evolution triangle: Integrating geology, hydrology, and biology. River Research and Applications. 2019 May;35(4):315–26.
  42. 42. Allen GH, Pavelsky TM. Global extent of rivers and streams. Science. 2018 Aug 10;361(6402):585–8. pmid:29954985
  43. 43. Koppes M, King L. Beyond x, y, z (t); Navigating new landscapes of science in the science of landscapes. Journal of Geophysical Research: Earth Surface.:e2020JF005588.
  44. 44. Fryirs KA. Developing and using geomorphic condition assessments for river rehabilitation planning, implementation and monitoring. Wiley Interdisciplinary Reviews: Water. 2015 Nov;2(6):649–67.
  45. 45. Fryirs KA, Brierley GJ. Assessing the geomorphic recovery potential of rivers: forecasting future trajectories of adjustment for use in management. Wiley Interdisciplinary Reviews: Water. 2016 Sep;3(5):727–48.
  46. 46. Brierley GJ, Fryirs KA. River futures: An integrative scientific approach to river repair. Island Press; 2012 Sep 26.
  47. 47. Newson MD, Newson CL. Geomorphology, ecology and river channel habitat: mesoscale approaches to basin-scale challenges. Progress in Physical Geography. 2000 Jun;24(2):195–217.
  48. 48. Casado MR, Gonzalez RB, Kriechbaumer T, Veal A. Automated identification of river hydromorphological features using UAV high resolution aerial imagery. Sensors. 2015 Nov;15(11):27969–89.
  49. 49. Roux C, Alber A, Bertrand M, Vaudor L, Piégay H. “FluvialCorridor”: A new ArcGIS toolbox package for multiscale riverscape exploration. Geomorphology. 2015 Aug 1;242:29–37.
  50. 50. Martínez-Fernández V, Solana-Gutiérrez J, del Tánago MG, de Jalón DG. Automatic procedures for river reach delineation: Univariate and multivariate approaches in a fluvial context. Geomorphology. 2016 Jan 15;253:38–47.
  51. 51. Guillon H, Byrne CF, Lane BA, Sandoval Solis S, Pasternack GB. Machine learning predicts reach‐scale channel types from coarse‐scale geospatial data in a large river basin. Water Resources Research. 2020 Mar;56(3):e2019WR026691.
  52. 52. Fryirs KA, Brierley GJ. Geomorphic analysis of river systems: An approach to reading the landscape. John Wiley & Sons; 2012.
  53. 53. Wheaton JM, Fryirs KA, Brierley G, Bangen SG, Bouwes N, O'Brien G. Geomorphic mapping and taxonomy of fluvial landforms. Geomorphology. 2015 Nov 1;248:273–95.
  54. 54. Fryirs KA, Brierley GJ, Hancock F, Cohen TJ, Brooks AP, Reinfelds I, et al. Tracking geomorphic recovery in process‐based river management. Land Degradation & Development. 2018 Sep;29(9):3221–44.
  55. 55. Fryirs KA, Brierley GJ, Dixon T. Engaging with research impact assessment for an environmental science case study. Nature communications. 2019 Oct 4;10(1):1–0. pmid:30602773
  56. 56. Kasprak A, Hough-Snee N, Beechie T, Bouwes N, Brierley G, Camp R, et al. The blurred line between form and process: a comparison of stream channel classification frameworks. PloS one. 2016 Mar 16;11(3):e0150293. pmid:26982076
  57. 57. Frissell CA, Liss WJ, Warren CE, Hurley MD. A hierarchical framework for stream habitat classification: viewing streams in a watershed context. Environmental management. 1986 Mar 1;10(2):199–214.
  58. 58. Fryirs KA, Ralph TJ, Larkin ZT, Tooth S, Humphries M, McCarthy T, et al. A nested hierarchical perspective to enhance interpretations and communication in fluvial geomorphology for use in water resources management: Lessons from the Okavango Delta, Botswana. The Geographical Journal. 2018 Jun;184(2):192–207.
  59. 59. Fryirs KA, Brierley GJ. What’s in a name? A naming convention for geomorphic river types using the River Styles Framework. PloS one. 2018 Sep 19;13(9):e0201909. pmid:30231079
  60. 60. Healey M, Raine A, Parsons L, Cook N. River condition index in New South Wales: method development and application. NSW Office of Water: Sydney, NSW. 2012.
  61. 61. Brierley GJ, Fryirs K. River styles, a geomorphic approach to catchment characterization: Implications for river rehabilitation in Bega catchment, New South Wales, Australia. Environmental Management. 2000 Jun 1;25(6):661–79. pmid:10790530
  62. 62. Fryirs K, Brierley G. Practical applications of the River Styles framework as a tool for catchment-wide river management: a case study from Bega Catchment, NSW, Australia. Macquarie University. 2005:227.
  63. 63. Fryirs K, Brierley GJ, Erskine WD. Use of ergodic reasoning to reconstruct the historical range of variability and evolutionary trajectory of rivers. Earth Surface Processes and Landforms. 2012 Jun 15;37(7):763–73.
  64. 64. Riches M, Gilligan D, Danaher K, Pursey J. Fish Community and Threated Species Distributions of NSW. NSW Department of Primary Industries, Wollongbar. 2016.
  65. 65. Beier U, Degerman E, Melcher A, Rogers C, Wirlöf H. Processes of collating a European fisheries database to meet the objectives of the European Union Water Framework Directive. Fisheries Management and Ecology. 2007 Dec;14(6):407–16.
  66. 66. O'Donnell J, Fryirs KA, Leishman MR. Seed banks as a source of vegetation regeneration to support the recovery of degraded rivers: a comparison of river reaches of varying condition. Science of the Total Environment. 2016 Jan 15;542:591–602. pmid:26544888
  67. 67. Piégay H, Darby SE, Mosselman E, Surian N. A review of techniques available for delimiting the erodible river corridor: a sustainable approach to managing bank erosion. River research and applications. 2005 Sep;21(7):773–89.
  68. 68. Kondolf GM. Setting goals in river restoration: When and where can the river “heal itself”. Stream Restoration in Dynamic Fluvial Systems. 2011 Jan 1;194:29–43.
  69. 69. Rutherfurd I, Jerie K, Walker M, Marsh N. Don’t raise the titanic: how to set priorities for stream rehabilitation. In Proceedings of the 2nd Australian Stream Management Conference, Adelaide 1999 Feb (Vol. 2, pp. 527–532).
  70. 70. Brierley G, Fryirs K, Cook N, Outhet D, Raine A, Parsons L, et al. Geomorphology in action: Linking policy with on-the-ground actions through applications of the River Styles framework. Applied Geography. 2011 Jul 1;31(3):1132–43.
  71. 71. Healey M, Raine A, Lewis A, Hossain B, Hancock F, Sayers J, et al. Applying the High Ecological Value Aquatic Ecosystem (HEVAE) Framework to Riverine Ecosystems. NSW Department of Industry, Sydney. 2018.
  72. 72. Wheaton JM, Bouwes N, Mchugh P, Saunders C, Bangen S, Bailey P, et al. Upscaling site‐scale ecohydraulic models to inform salmonid population‐level life cycle modeling and restoration actions–Lessons from the Columbia River Basin. Earth Surface Processes and Landforms. 2018 Jan;43(1):21–44.
  73. 73. O’Brien GR, Wheaton J, Fryirs K, McHugh P, Bouwes N, Brierley G, et al. A geomorphic assessment to inform strategic stream restoration planning in the Middle Fork John Day Watershed, Oregon, USA. Journal of Maps. 2017 Nov 30;13(2):369–81.
  74. 74. Rinaldi M, Surian N, Comiti F, Bussettini M. A method for the assessment and analysis of the hydromorphological condition of Italian streams: The Morphological Quality Index (MQI). Geomorphology. 2013 Jan 1;180:96–108.
  75. 75. Rinaldi M, Surian N, Comiti F, Bussettini M. A methodological framework for hydromorphological assessment, analysis and monitoring (IDRAIM) aimed at promoting integrated river management. Geomorphology. 2015 Dec 15;251:122–36.
  76. 76. Shuker LJ, Gurnell AM, Wharton G, Gurnell DJ, England J, Finn Leeming BF, et al. MoRPh: a citizen science tool for monitoring and appraising physical habitat changes in rivers. Water and Environment Journal. 2017 Aug;31(3):418–24.
  77. 77. Gurnell AM, Scott SJ, England J, Gurnell D, Jeffries R, Shuker L, et al. Assessing river condition: A multiscale approach designed for operational application in the context of biodiversity net gain. River Research and Applications. 2020 Jul 13.
  78. 78. Gorelick N, Hancher M, Dixon M, Ilyushchenko S, Thau D, Moore R. Google Earth Engine: Planetary-scale geospatial analysis for everyone. Remote sensing of Environment. 2017 Dec 1;202:18–27.
  79. 79. Henshaw AJ, Sekarsari PW, Zolezzi G, Gurnell AM. Google Earth as a data source for investigating river forms and processes: Discriminating river types using form‐based process indicators. Earth Surface Processes and Landforms. 2020 Feb;45(2):331–44.
  80. 80. Brierley G, Reid H, Fryirs K, Trahan N. What are we monitoring and why? Using geomorphic principles to frame eco-hydrological assessments of river condition. Science of the Total Environment. 2010 Apr 1;408(9):2025–33. pmid:20170940
  81. 81. AETG (Aquatic Ecosystems Task Group). Aquatic Ecosystems Toolkit. Module 2. Interim Australian National Aquatic Ecosystem Classification Framework. Australian Government Department of Sustainability, Environment, Water, Population and Communities, Canberra. 2012.
  82. 82. Tooth S. Virtual globes: a catalyst for the re‐enchantment of geomorphology?. Earth Surface Processes and Landforms. 2006 Aug;31(9):1192–4.
  83. 83. Piégay H, Arnaud F, Belletti B, Bertrand M, Bizzi S, Carbonneau P, et al. Remotely sensed rivers in the Anthropocene: State of the art and prospects. Earth Surface Processes and Landforms. 2020 Jan;45(1):157–88.
  84. 84. Park JR. Metadata quality in digital repositories: A survey of the current state of the art. Cataloging & classification quarterly. 2009 Apr 9;47(3–4):213–28.
  85. 85. Eze PN, Knight J. A geomorphological characterisation of river systems in South Africa: A case study of the Sabie River. Physics and Chemistry of the Earth. 2018 Jun 1;105:196–205.
  86. 86. Rogers KH. The real river management challenge: integrating scientists, stakeholders and service agencies. River Research and Applications. 2006 Feb;22(2):269–80.
  87. 87. Brierley G, Fryirs K, Outhet D, Massey C. Application of the River Styles framework as a basis for river management in New South Wales, Australia. Applied Geography. 2002 Jan 1;22(1):91–122.
  88. 88. Fryirs KA, Wheaton JM, Bizzi S, Williams R, Brierley GJ. To plug‐in or not to plug‐in? Geomorphic analysis of rivers using the River Styles Framework in an era of big data acquisition and automation. Wiley Interdisciplinary Reviews: Water. 2019 Sep;6(5):e1372.
  89. 89. Mould S, Fryirs K, Howitt R. The importance of relational values in river management: understanding enablers and barriers for effective participation. Ecology and Society. 2020 May 29;25(2).
  90. 90. Mould S, Fryirs K, Howitt R. Relationships, social networks and the emergence of recovery-based river management: Implications for environmental policy. Marine and Freshwater Research. 2020 https://doi.org/10.1071/MF20065
  91. 91. Wilcock D, Brierley G, Howitt R. Ethnogeomorphology. Progress in Physical Geography. 2013 Oct;37(5):573–600.
  92. 92. Lane SN. Acting, predicting and intervening in a socio-hydrological world. Hydrology and Earth System Sciences. 2014 Mar 1;18(3):927.
  93. 93. Ashmore P. Towards a sociogeomorphology of rivers. Geomorphology. 2015 Dec 15;251:149–56.
  94. 94. Mould SA, Fryirs K, Howitt R. Practicing sociogeomorphology: Relationships and dialog in river research and management. Society & Natural Resources. 2018 Jan 2;31(1):106–20.
  95. 95. Fryirs K, Brierley GJ. Naturalness and place in river rehabilitation. Ecology and Society. 2009 Jun 1;14(1).
  96. 96. Mould S, Fryirs K, Lovett S, Howitt R. Supporting champions in river management. Wiley Interdisciplinary Reviews: Water. 2020 May 5:e1445.
  97. 97. Hüesker F, Moss T. The politics of multi-scalar action in river basin management: implementing the EU Water Framework Directive (WFD). Land Use Policy. 2015 Jan 1;42:38–47.
  98. 98. Kondolf GM. Five elements for effective evaluation of stream restoration. Restoration ecology. 1995 Jun;3(2):133–6.
  99. 99. Beechie TJ, Sear DA, Olden JD, Pess GR, Buffington JM, Moir H, et al. Process-based principles for restoring river ecosystems. BioScience. 2010 Mar 1;60(3):209–22.
  100. 100. Wohl E. What should these rivers look like? Historical range of variability and human impacts in the Colorado Front Range, USA. Earth Surface Processes and Landforms. 2011 Aug;36(10):1378–90.
  101. 101. Wohl E, Brierley G, Cadol D, Coulthard TJ, Covino T, Fryirs KA, et al. Connectivity as an emergent property of geomorphic systems. Earth Surface Processes and Landforms. 2019 Jan;44(1):4–26.
  102. 102. Poeppl RE, Fryirs KA, Tunnicliffe J, Brierley GJ. Managing sediment (dis) connectivity in fluvial systems. Science of The Total Environment. 2020 Sep 20;736:139627. pmid:32485383