Figures
Abstract
The production of maple syrup is an important cultural and economic activity directly related to the climate of northeastern North America. As a result, there are signs that climate change could have negative impacts on maple syrup production in the next decades, particularly for regions located at the southern margins of the sugar maple (Acer saccharum Marsh.) range. The purpose of this survey study is to present the beliefs and opinions of maple syrup producers of Canada (N = 241) and the U.S. (N = 113) on climate change in general, its impacts on sugar maple health and maple syrup production, and potential adaptation measures. Using conditional inference classification trees, we examined how the socio-economic profile of respondents and the geographic location and size of respondents’ sugar bushes shaped the responses of survey participants. While a majority (75%) of respondents are confident that the average temperature on Earth is increasing, less than half (46%) believe that climate change will have negative impacts on maple syrup yield in the next 30 years. Political view was a significant predictor of these results, with respondents at the right right and center-right of the political spectrum being less likely to believe in climate change and less likely to anticipate negative effects of climate change on maple syrup production. In addition, 77% of the participants indicated an interest in adopting adaptation strategies if those could increase maple syrup production. This interest was greater for respondents using vacuum tubing for sap collection than other collection methods. However, for many respondents (particularly in Canada), lack of information was identified as a constraint limiting adaptation to climate change.
Citation: Legault S, Houle D, Plouffe A, Ameztegui A, Kuehn D, Chase L, et al. (2019) Perceptions of U.S. and Canadian maple syrup producers toward climate change, its impacts, and potential adaptation measures. PLoS ONE 14(4): e0215511. https://doi.org/10.1371/journal.pone.0215511
Editor: Caroline Ummenhofer, Woods Hole Oceanographic Institution, UNITED STATES
Received: December 7, 2018; Accepted: April 3, 2019; Published: April 25, 2019
Copyright: © 2019 Legault et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Data Availability: All relevant data are within the manuscript and its Supporting Information files.
Funding: SL and AP were partly funded by the CICan Career-Launcher Internship program. AA was supported by Spanish Government through the Juan de la Cierva fellowship program (IJCI-2016-30049). The funders had no role in study desing, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Introduction
Maple syrup is a unique and important non-timber forest product in northeastern North America. Its production, probably originating with the indigenous population, continues to be a cultural tradition and a source of income for many family-based businesses in Canada and the United States [1,2]. Maple syrup is produced by the concentration of sap of maple trees by boiling (now often preceded by reverse osmosis), and thus annual yield depends on the volume of sap harvested and its sweetness [3].
The sap volume harvested each season is determined by the harvesting methods utilized [4], and most importantly, by climate. Indeed, the strongest and best-understood factor affecting sap flow is temperature: water uptake from the soil and sap exudation, which involves alternating negative and positive pressure in the trunk and branches of the tree, is favored by cold nights (˂ 0 °C) followed by thaws during days (~ 3–7 °C) [5]. Depending on regional climate, these freeze-thaw cycles occur between February and April, but the beginning, end, and duration of the sap flow period can vary widely from year to year [6]. The tapping season generally ends with bud break and the development of microorganisms in taps when temperatures become warm (˃ 10 °C) for several days [7].
Sap sweetness (i.e., sugar content) is influenced by tree health and the maple species tapped. Healthy trees with large crowns and high growth rates tend to provide sweeter sap [8]. Sap from the sugar maple (Acer saccharum Marsh.), whose range covers southeastern Canada and the northeastern United States (Fig 1), is preferred for maple syrup production because its sugar concentration is superior to other species such as the red maple (Acer rubrum L.) [9,10]. Warm summer temperatures (which stimulate maple growth) and cold winter temperatures increase sap sugar concentrations in the following sap flow season [11].
Sugar maple range (adapted from [18,19]), maple syrup regions as defined by Murphy et al. [20], and approximate location of sugar bushes whose owners participated in the survey presented in this document. The locations are based on the postal code provided by the respondents and do not necessarily represent the exact location of their sugar bush.
Several phenomena can also affect the health of sugar maple trees and potentially reduce sap sweetness and syrup yield. These include droughts [12,13], pest outbreaks [14,15], soil fertility [16], acid depositions and air pollution, forest management, and stand maturation [17].
Because of the close link between climate and maple syrup production [11,21], climate change is expected to affect the maple syrup industry. Anticipated changes include increased summer and winter temperatures, a decrease in snow cover duration, and a time shift in the freeze-thaw period [22]. Inverse relationships between syrup production and average temperatures from January to April in Northeastern U.S. states have already been detected [23]. The projections of Skinner et al. [24] indicate that warming winter temperatures will result in a shorter sap flow period if traditional tapping schedules are maintained. The results of Duchesne et al. [25] are somewhat similar, but indicate that decreases in maple syrup yields could be avoided in Quebec if producers shift the tapping period 12 days earlier by 2050 and 19 days earlier by 2100. Finally, the study of Guilbert et al. [26] projects a decrease of 7–11 days suitable for maple syrup production by 2040–2069 and 2070–2099 in the Lake Champlain Basin, and that suitable days will occur earlier in the season.
With regard to all these potential threats, concerns have been raised about the future of maple syrup production in both Canada and the U.S. [20,27–31]. The survey of Mozumber et al. (N = 102) [30] suggests that a majority of North American producers believe that the quantity and quality of maple sap is decreasing because of climate change, and about one-third missed the first sap flow of the season in recent years. In the province of Quebec, the survey of Rondeau [27] revealed that 66% of respondents (N = 63) where highly or moderately worried about the profitability of production in the face of climate change. In Ontario, a small survey (N = 33) completed in 2009 showed that 50% of the respondents already observed the effects of climate change on their production [28]. In the U.S., a recent survey (N = 264) revealed that more than half of the maple syrup producers from New York and Vermont are apprehensive about climate change [31]. Contrarily, another recent survey (N = 353), focusing on maple syrup producers from Minnesota, Wisconsin and Michigan, reported that only a small percentage of respondents expressed concerns about climate change impacts on their operations [32].
Unfortunately, previous surveys documenting maple syrup producers’ perceptions towards climate change all used very different survey questions and methodologies, and used either small sample sizes [20,27,28], or a sampling pool from a limited geographic area [31–33]. In addition, generalizations using previous surveys would underrepresent the views of Quebec’s producers, who are responsible for approximately 70% of the world maple syrup production [34]. Altogether, these factors prevent the establishment of a clear global picture for the maple syrup industry. Furthermore, because the impacts of climate change on maple syrup production are expected to vary geographically, adaptation measures to climate change could potentially be implemented differently according to regional specificities. Thus, understanding the variations in producers’ perceptions across a climate gradient is crucial.
In the past years, there have been extensive efforts to examine the variables that are most closely correlated with acceptance of anthropogenic climate change [35–39]. In a recent meta-analysis, Hornsey et al. [39] synthetized the results of 171 academic studies across 56 countries and concluded that the factor that correlates most with climate change belief is political view. In Canada and the U.S., this factor is very important for explaining the acceptance of anthropogenic climate change, with conservatives being less likely to believe in climate change than liberals [40–42]. In the forest sector in particular, it has been shown that concerns regarding climate change vary with political views and geographical context (e.g. the province of origin; [43]), but also with individual factors such as specific forest utilisation, knowledge of forestry, and level of economic dependence on forests [44]. It has also been shown that forest managers’ beliefs about climate change are correlated with their willingness to try specific adaptation or mitigation measures [45]. These studies thus show that determining the main factors influencing maple syrup producers’ perceptions of climate change is very important for the identification of potential adaptation strategies for the maple syrup industry in the face of climate change.
The primary objective of this study was to examine the perceptions of maple syrup producers from Canada and the U.S. toward (i) climate change in general, (ii) its effects on sugar bushes health and productivity, and (iii) potential adaptation measures. For this purpose, we conducted an online survey addressed to maple syrup producers from all producing regions of Canada and the U.S. Because maple syrup production is highly climate-dependent [11,21], we hypothesized that maple syrup producers would generally be more sensitive to the concerns raised by the scientific community in relation to climate change than the general population. We therefore expected that maple producers’ perceptions would not be significantly related to their political views. Also, given the ongoing shift of the climatic envelope suitable for maple syrup production toward northward latitudes [24], we expected an effect of spatial context on producer’s opinions. More specifically, we expected that producers in southerly regions of our study area, being potentially more affected by climate change impacts than producers from more northerly regions, would have higher levels of concern about future climate change impacts on maple syrup production. Finally, as implementing adaptation measures can be viewed as costly for producers [31], we hypothesized that factors associated with the size of the sugar bush would be important in predicting responses rates for questions or statements associated with adaptation measures, with large-scale producers more inclined to adopt adaptation measures than small-scale producers.
Methods
Survey design and distribution
The survey used in this study was distributed to Canadian and American maple syrup producers (specifically those who were members of maple producer associations) via an internet-based survey platform (SurveyGizmo, Boulder, CO, USA). To seek responses from as many respondents as possible, we contacted the maple syrup producers’ associations from all regions of the study area (delineated by the sugar maple’s range; Fig 1) and asked them to send a link of the survey to their members and publicize the survey through websites, social media pages, and letters to members. We also publicized the survey on various maple producers’ forums in Canada and the U.S. (e.g. MapleTrader.com, Lessucriers.com, and Sugarbush.info) and through paper journals (e.g. Maple News and Maple Digest).
The survey was divided in three sections: (i) questions and statements about general perceptions of climate change (eight statements), (ii) climate change impact on maple syrup production (11 statements), and (iii) adaptation strategies to climate change (13 statements). For most statements, respondents specified their degree of agreement using a 5 or 7-grade Likert scale. For each proposed adaptation strategy, respondents specified if it was efficient, and if they planned to use it, or were already using it. For some questions, a Yes/No answer was collected. Furthermore, we recorded as potential predictor variables socio-economic information about the respondents (age, gender, education level, and political view), characteristics of the sugar bush (number of taps, age of the largest maples, harvesting method, years of experience in the maple syrup industry, someone to take over once retired, percentage of household income contributed by maple sugar business, investment planning during the next 10 years, and yield in 2016), and sugar bush location (country, region, latitude, and longitude). Because of the low number of respondents in many provinces/states, we grouped respondents according to regions as delimited by Murphy et al. [20] (Canada: Ontario, Québec, and Atlantic; U.S.: Northeast, and Midwest-Southeast; Fig 1). The full questionnaire and the distribution of responses for each question and statement can be found in the Supplementary Material 1.
Data analyses
To determine the relative influence of predictors (socio-economic information about the respondents, characteristics of the sugar bush, and its spatial location) in explaining the distribution of responses by survey respondents, we used a conditional inference classification tree approach. In contrast with traditional approaches such as multiple regression, this technique has the advantage of accommodating a large number of explanatory variables, even if they are highly correlated [46,47]. In addition, this approach makes it possible to include variables of different types (nominal, ordinal, interval and quantitative), as in our dataset. This approach has been used successfully in several research areas [48–50], including studies identifying the factors influencing responses in climate change-related surveys [36,43].
As suggested by Lee et al. [36], we used a two-step approach during data analyses in order to avoid an excessive number of explanatory variables in each tree model (one for each question/statement of the survey). First, we determined the most influential variable(s) using a random forests permutation-based procedure, as implemented in the R package VSURF [51]. This process ranks the predictors iteratively based on an importance metric, and returns a small subset of variables with minimal redundancy between them. Second, a single conditional inference tree was produced for each question of the survey, using as input only the variables selected during the first step. For this procedure, we used the R function ctree, as implemented in the partykit package [52]. In summary, this recursive function performs univariate divisions of the response variable based on the values of a set of covariates. For this step, we used a random training subset consisting of 80% of the respondents. A default threshold of p = 0.05 was used to determine if variables were dropped from the model. Finally, for each question/statement of the survey, we calculated the classification accuracy (CA; [36]) of each conditional tree by calculating the proportion of correct predictions using the remaining 20% of the dataset.
Results and discussion
Using an online survey, we examined the perceptions of maple syrup producers from North America about (i) climate change in general, (ii) its current and future impacts on the health of sugar bushes and maple syrup yield, and (iii) their opinions about adaptation to climate change and their willingness to adopt different adaptation strategies. A total of 354 individuals completed the survey. The complete questionnaire (S1 File) as well as the complete dataset (S2 File) can be found in the Supplementary Material. Sixty-eight percent of the respondents were Canadian producers (N = 241), and 32% were Americans (N = 113) (Table 1). When considering the distribution of maple syrup farms in Canada and the U.S., our study slightly over-represents the opinions of Canadian producers–mainly those from the province of Quebec–and under-represents the views of U.S. producers (Table 1). In terms of average tap yield, Canadian respondents reported slightly lower yields than the country average, while yields reported by U.S. respondents were more similar to the country average (Table 1).
Most survey respondents were male (87.4%), the mean respondents’ age was 49.1 (±13.7), and 66.9% had at least a college degree. A quarter (24.6%) of the respondents described their political view as being on the left or center-left of the political spectrum, 40.6% on the center, and 34.8% on the center-right or right. The average number of tap per farm was 6442 (±13,180), the average yield was 3.35 (±1.29) pounds per tap, and 71.0% of the respondent reported using tubing with vacuum to harvest sap. Most respondents were small-scale producers, as the percentage of household income contributed by maple sugar business was higher than 50% for only 20.2% of the respondents (Section D in S1 File).
To verify if our sample was representative of the larger population of maple syrup producers, we compared some characteristics of the survey respondents with available data from census made in the province of Quebec by the Ministère de l’Agriculture, des Pêcheries et de l’Alimentation du Québec [56] and in the U.S. by the United States Department of Agriculture [57]. The percentage of women in our sample was slightly lower than the larger population of maple syrup producers, as was the average age of respondents (Table 2). In Quebec, fewer respondents declared to hold a post-secondary diploma (61%) compared to the larger population of maple syrup producers in that province (71%) [56]. In the U.S., fewer respondents declared that their maple syrup business contributed to at least 50% of their household income (9%) compared to the larger population of maple syrup producers in the U.S. (22%) [57].
Using conditional inference trees, we quantified the influence of socio-economic factors, characteristics of the sugar bush, and the spatial location of the sugar bush on responses given by survey participants. In the following sections, we present and discuss the main findings of our study and their consequences for implementing short- and long-term adaptation strategies in the maple syrup industry. The most influential variable(s) retained for each question or statement of the survey during data analyses can be found in Table 3.
Part 1: General perceptions of climate change
Given the close links between climate and maple syrup production, and the close contacts between sugaring operations and the forest environment, we hypothesized that (i) maple syrup producers would be more sensitive to the concerns raised by the scientific community about climate change than the general population, and that (ii) their perceptions would be relatively independent of political view. Our results do not support these hypotheses. Instead, we found that surveyed Canadian maple syrup producers were a bit less confident that the average temperature on Earth is increasing (77.2%) than the general population of the Ontario, Quebec and Atlantic regions of Canada (81.1%) [84]. This difference might be related to the fact that most survey respondents were men (Table 2), as recent studies have shown that sex was an important predictor of climate change perception in the general population in the U.S. [85] and for cranberry growers in Massachusetts [86]. In the U.S., respondents were as likely to believe in global warming (70.4%) than the general population of the Midwest and Northeast regions (69.9%) in 2016 [87]. This is in agreement with a study on U.S. farmers that shown that 65% of them believe that climate change is a reality, which is fairly similar than the general public (67–73%) [88].
Furthermore, as for the general population of Canada and the U.S. [40–42], political view was the strongest predictor of the responses for this statement (Table 3): while a majority (75%) of maple syrup producers were very or fairly confident that the average temperature on Earth is increasing (Fig 2a), this proportion was much higher (~ 90%) for respondents that positioned themselves at the left or center-left of the political spectrum (Fig 2b).
a) Responses of the survey participants to the question How confident are you that the average temperature on Earth is increasing? b) Conditional inference classification tree predicting the responses. Only significant predictors at p ˂ 0.05 were retained by the algorithm. Sample size used to build the tree can be calculated by adding sample sizes indicated at each terminal node. CA value is the classification accuracy.
Regarding the perceived causes of climate change, 32% of the respondents identified human activity as the main driver, 50% identified a combination between human activity and natural patterns, and 15% attributed the causes to natural patterns only (Fig 3a). Again, political view was the main predictor of the responses to this question, with respondents from the left and center-left being more inclined to identify human activity as the main driver of climate change (~ 65%) than other respondents (~ 20%) (Fig 3b).
a) Responses of the survey participants for the question Is the Earth getting warmer mostly because of human activity such as burning fossil fuels or mostly because of natural patterns in the Earth’s environment? b) Conditional inference classification tree predicting the responses. Only significant predictors at p ˂ 0.05 were retained by the algorithm. Sample size used to build the tree can be calculated by adding sample sizes indicated at each terminal node. CA value is the classification accuracy.
For the perceived impacts of climate change (Fig 4a), political view was also the most important factor determining the responses of survey participants (Table 3). Respondents at the left of the political spectrum were less likely to agree that climate change impacts are happening slowly enough to let them adapt as the impacts appear (Fig A in S3 File), and that the projected impacts of climate change are exaggerated (Fig D in S3 File). Also, these respondents were more likely to agree that climate change is noticeable in their region (Fig B in S3 File). Education level significantly explained the responses of participants for the statement The impact of climate change on me and my community is tangible, with university-graduated respondents being more likely to agree (Fig C in S3 File).
a) Responses of the survey participants for general statements about climate change. b) Responses of the survey participants for the question What do you think is the probability that the following climatic events will happen more frequently in the next 30 years? Statements followed by a * symbol indicate a significant effect of at least one predictor (see Table 3 and S3 File).
Finally, regarding the probability that specific climatic events (e.g. high annual mean temperature, heavy rainfall episodes, etc.) would happen more frequently in the next 30 years (Fig 4b), political view was frequently a significant predictor (Table 3). For a majority of these questions, respondents at the left of the political spectrum were more inclined to believe that the probability of an increased frequency of extreme climatic events in the next 30 years was high or very high (Figs. F-P in S3 File). Other variables that significantly explained the responses of the survey participants for this subsection of the survey included educational level, latitude, region and percentage of household income contributed by the maple sugar business (Table 3; Figs. E, G, and P in S3 File).
Part 2: Climate change impact on maple syrup production
Potential impacts of climate change on maple syrup production include changes in the exposure of the sugar maple stands to extreme climatic events [21], sap flow timing [24–26], and maple syrup yield [23]. With the northward shift of the climatic envelope favorable to the sugar maple [78], production in U.S. states in the southern portion of the maple’s range could be more at risk by the end of the century than in northern regions. For this reason, we expected a latitudinal gradient on producers’ opinions about the effects of climate change on sugar bush health and maple syrup production. Partly in line with this hypothesis, we found a few geographic variables had a significant effect on responses to some questions, but political view was also an important and significant factor shaping the responses, particularly with regard to future impacts (Table 3).
From a list of climatic hazards, windstorms and tornadoes were identified by the largest proportion of respondents as having caused significant damage to their sugar bush in the last decades (53%), followed by ice storms (40%), insect outbreaks (17%), droughts (14%), and invasive plant species (12%) (Fig 5). Significant models were obtained only for ice storms (Fig Q in S3 File) and insect outbreaks (Fig R in S3 File). Interestingly, respondents from southern Canada with more than 10 years of experience were more likely to report damages by ice storms to their sugar bushes during the last decades (Fig Q in S3 File). This pattern can be explained by the large areas of forest damaged by the ice storm of January 1998 that befell on the province of Quebec [89–91].
Responses of the survey participants for the question In the last decades, which of these climatic events have caused significant damages to your sugar bush? Statements followed by a * symbol indicate a significant effect of at least one predictor (see Table 3 and Supplementary Material 3).
When asked for their perceptions of the impacts climate change has had on tap yield in recent decades, almost half (49%) of the respondents reported no impacts, 32% reported positive or mostly positive impacts, and 19% reported negative or mostly negative impacts (Fig 6a). However, the proportion of producers reporting negative impacts was significantly higher for respondents from lower latitudes (i.e. ≤ 40°) (Fig 6b). This result suggests that maple syrup production in the southern portion of the study area in the U.S. has already been impacted by global warming in recent years, potentially revealing the first manifestation of the expected northward shift of the climatic envelope favorable to sap flow [24]. For the next 30 years, a higher proportion (45%) of the respondents are anticipating negative or mostly negative impacts (Fig 6a), with respondents from the left to the center of the political spectrum being more likely to anticipate negative impacts (Fig 6c). These results are somewhat surprising since political view appears to be a stronger predictor of producers’ beliefs about future climate change impacts than personal experience due to past exposure to climate change effects. In other words, while maple syrup producers recognize impacts of climate change based on their personal experience, political ideology is more important in shaping their beliefs about future impacts. Interestingly, a similar result has been found among Idaho’ farmers: while many are noticing changes in precipitations, winter temperatures and growing season lengths, only a few connect these with anthropogenic climate change, indicating that direct experience of climate change manifestations is not sufficient to overcome the influence of political views [92].
a) Responses of the survey participants for the questions What have been/will be the impact of climate change on tap yield in the last decades and in the next 30 years? b and c) Conditional inference classification trees predicting the responses. Only significant predictors at p ˂ 0.05 were retained by the algorithm. Sample size used to build the tree can be calculated by adding sample sizes indicated at each terminal node. CA value are the classification accuracies.
A substantial majority (86%) of participants strongly agreed that maple syrup production is closely linked to climate, but only a minority observed an increase in maple dieback because of climate change (Fig 7). Regarding the beginning of the tapping season, 59% of producers answered that they have already observed its earlier occurrence because of climate change. A similar proportion of respondents agreed with the idea that this trend will continue in the future (Fig 7), but the proportion was significantly lower for respondents at the right end of the political spectrum (Fig W in S3 File). For statements concerning the variability in the beginning of the tapping season from year to years, 63% of the respondents agreed to a certain degree that climate change has led to higher variability, and 60% agreed that the trend will continue in the next 30 years (Fig 7). For these two statements, political view was the most important predictor of response, with participants from the right of the political spectrum having less agreement with the two statements (Figs. T and V in S3 File). Finally, only 29% of the respondents agreed with the statement that it is now easy to determine the best moment to tap maples (Fig 7), this proportion being lowest for respondents from U.S. regions (Fig U in S3 File). About half (51%) of the respondents agreed with the statement that in the future, it will be harder and harder to determine the best moment to tap maples (Fig 7); there was no difference between countries (Table 3).
Part 3: Adaptation strategies to climate change
Regarding questions and statements about adaptation to climate change, we hypothesized a significant influence of the scale of the sugaring operation on respondents’ responses, with large-scale producers being more inclined to adopt adaptation measures. We first proposed general statements on adaptation to climate change for maple syrup production (Fig 8). Sap harvesting method (i.e. buckets or bags, tubing with or without vacuum) is generally related to the size of sugaring operations, and was often selected as the stronger predictor of responses (Table 3). For example, producers using vacuum tubing to collect sap were more likely to agree with the statement that new ways to adapt to climate change are needed in the maple syrup industry, and that they will adopt climate adaptation strategies that will increase maple syrup production (Fig AB in S3 File). Also, respondents using tubing for sap collection were more likely to agree that new maple syrup technologies will help mitigate challenges related to climate change, and that they would probably adopt adaptation strategies if they will increase maple syrup production (Fig AA-AB in S3 File).
Responses of the survey participants for statements about adaptation to climate change for maple syrup production. Statements followed by a * symbol indicate a significant effect of at least one predictor (see Table 3 and S3 File).
Survey participants were then asked if various adaptation measures would effectively allow maple syrup producers to adapt to climate change, and if they would like to use these strategies in the future (Fig 9a; Table 4). The measures most frequently identified as efficient by respondents were keeping track of new research about maple syrup production, doing sylvicultural management, and adopting extensive spout and tubing sanitation practices (heavy use of sanitizers and/or annual replacement of spouts to lengthen taphole viability and enhance yield). Less popular measures included increasing a sugar bush’s number of taps, using maples adapted to future climate conditions, and tapping red maples (Fig 9a). When asked which of these adaptation measures they would like to use themselves, the perceptions of the respondents were generally in line with those of the previous question (Fig 9a). When asked which adaptation measures they would like to see developed by the maple syrup industry, however, the two positively viewed measures were selecting maples that are adapted to future climatic conditions, and promoting the distinctive syrup harvested in the very late season (Fig 9b).
Responses of the survey participants for questions about specific adaptation measures that a) maple syrup producers or b) the maple syrup industry can adopt to mitigate climate change impacts. Statements followed by a * symbol indicate a significant effect of at least one predictor (see Table 3 and Supplementary Material 3).
Producers using high vacuum tubing systems (>20 Hg) were more likely to identify sylvicultural management as efficient to adapt to climate change (Fig AD in S3 File) and were already using sylvicultural management in a larger proportion (Fig AK in S3 File). In addition, they were more likely to already be using strong sanitation practices already (Fig AL in S3 File). Producers using high vacuum tubing were also more likely to be tapping earlier in the year (Fig AM in S3 File), more likely to say they have a wide knowledge of newest tapping technologies (Fig Z in S3 File), and to already be keeping track of new research about maple syrup production (Fig AJ in S3 File). Finally, respondents using high vacuum tubing were more likely to agree that their business could quickly change its labor organisation (number of workers, and/or hours worked) following climate change impacts (Fig AS in S3 File).
The geographic location of the sugar bush was another important predictor of response for questions and statements about adaptation (Table 3). Only 23% of respondents from Canadian regions agreed with the statement that there are many ways to adapt to climate change for maple syrup production, compared to 43% of respondents from U.S. regions (Fig Y in S3 File). Respondents from these warmer regions within the study area were also more likely to identify the adoption of strong sanitation practices and earlier tapping as effective adaptation measures to mitigate climate change impacts (Fig AE-AF in S3 File), but less likely to identify liming and fertilizing as effective (Fig AH and AO in S3 File). There is, however, a considerable contrast between the producers of the two countries regarding the best moment to implement adaptation measures: the majority of U.S. producers (67%) believe that it is necessary to wait till they observe the effects of climate change, while Canadian producers are much more divided on this issue (Fig AC in S3 File).
The last segment of the third part of the survey focused on the adaptability of respondents’ sugar bush, and barriers to adapting to climate change. Only a minority of respondents agreed that their business could quickly adapt to climate change impacts experienced through adjustments of labor, production technologies, or how sap is collected (Fig 10a). Regarding constraints to adaptation through the use of new technologies, lack of financial means was the most frequently identified (Fig 10b), particularly for younger respondents (Fig AV in S3 File). This constraint was followed in importance by the lack of information, particularly for Canadian respondents (Fig AU in S3 File), and the lack of technical support, particularly for respondents with lower sugar bush yields (Fig AV in S3 File). Finally, 25% of respondents identified their lack of belief in climate change as a constraint to adopting new technologies for coping with the challenges of climate change. This proportion was higher (almost 50%) for respondents at the right or center-right of the political spectrum, and respondents without high school diplomas (Fig AX in S3 File).
12. Responses of the survey participants for questions about a) adaptability and b) potential barriers to adaptation. Statements followed by a * symbol indicate a significant effect of at least one predictor (see Table 3 and S3 File).
A more detailed discussion of findings associated with specific adaptation measures can be found in Table 4.
Conclusions
In this study, we used a web survey to examine the perceptions of maple syrup producers from Canada and the U.S. about climate change in general, its effects on sugar bush health and productivity, and adaptation to climate change.
The first part of the survey focused on general perceptions of climate change. Overall, we found that a majority of respondents are confident that the average temperature on Earth is increasing. These levels of belief in climate change were somewhat similar than that of the general populations of Canada and the U.S. living in the areas covered by our survey [84,87]. As for the general population of both countries [40–42], political view was a very strong predictor of respondents’ general beliefs in climate change.
For the second part of the survey, which focused on current and future impacts of climate change on maple syrup production, our analyses retained a more diverse set of predictors, but political view was still the most frequent. One of the results indicate that almost half of respondents expect climate change to negatively impact tap yield in the next 30 years.
For the third part of the survey, which focused on adaptation strategies to climate change, influential predictors were most frequently associated with geography (e.g. latitude, region), and the scale of the sugaring operations (e.g. harvesting method, number of taps). Interestingly, a very large majority of respondents would adopt adaptation strategies if they believed it would increase maple syrup production. These include forest management to keep sugar bushes healthy and resilient to climatic hazards, investments in new technologies to boost productivity, and new varieties of resilient and productive sugar maple trees. However, the most important barriers to the implementation of these strategies appears to be the lack of easily accessible information about the effects of climate change on maple syrup production, followed by the lack of financial means and technical support.
Finally, about a quarter of respondents identified their lack of belief in climate change impacts on maple syrup production as limiting their adoption of adaptation measures. As increased in exposure to extreme climatic events can raise awareness and influence climate change beliefs [38,93], these respondents may change their opinions in the future. In the meantime, we believe that continuing to study the effects of climate change on maple syrup production and improving the ways of transmitting new information to maple syrup producers will help prepare the maple syrup industry for the climate of the future.
Data limitations and future directions
In addition to the possible biases identified in Tables 1 and 2, it is important to mention that our sample may not be representative of all North American producers. Indeed, our analysis focuses mainly on producers that accepted to answer the survey. As a result, these producers may be more engaged about climate change, and may have access to more information than those who did not respond.
As our results suggest, the factors determining the opinions of maple syrup producers in the face of climate change are many and varied. Consequently, the adaptation of the maple industry to climate change will probably need a variety of strategies, each adapted to the climatic and socio-cultural specificities of each regions.
Supporting information
S1 File. Survey questionnaire.
Survey questionnaire in the format presented to participants, with total responses indicated for each question.
https://doi.org/10.1371/journal.pone.0215511.s001
(PDF)
S2 File. Full dataset.
Excel file containing the full dataset used for analyses. Column numbers correspond to Table 3 and S1 File. The geographic locations of the sugar bushes (i.e. latitude and longitude coordinates) have been removed from the table to ensure the anonymity of the respondents.
https://doi.org/10.1371/journal.pone.0215511.s002
(XLSX)
S3 File. Conditional inference (CI) classification trees.
Selected conditional inference classification tree predicting the response rates of survey questions using only predictors identified as important during the random forest variable importance evaluation step of the analyses (see Table 1). For each tree, only significant predictors at p ˂ 0.05 were retained by the algorithm. Sample size used to build each tree can be calculated by adding sample sizes indicated at each terminal node. The classification accuracy was calculated for each tree using a subset of 20% the dataset.
https://doi.org/10.1371/journal.pone.0215511.s003
(PDF)
Acknowledgments
For sharing the survey with their audiences, we thank the Fédération des producteurs acéricoles du Québec and the NYS Maple Producers’ Association, the maple producers’ forums MapleTrader.com, Lessucriers.com, and Sugarbush.info, and the paper journals Maple News and Maple Digest. We also thank Yves Bois (ACER center) and Paul Rouillard (Fédération des producteurs acéricoles du Québec) for their useful comments on the project. Finally we thank Erick Lachapelle for his comments on the survey questions.
References
- 1. Hinrichs CC. Sideline and Lifeline: The Cultural Economy of Maple Syrup Production. Rural Sociol. 1998;63: 507–532.
- 2. Whitney GG, Upmeyer MM. Sweet trees, sour circumstances: the long search for sustainability in the North American maple products industry. For Ecol Manage. 2004;200: 313–333.
- 3.
Taylor FH. Variation in sugar content of maple sap. 1956.
- 4.
Smith HC, Gibbs CB. Comparison of vacuum and gravity sap flows from paired sugar maple trees. [Internet]. Research Notes. Northeastern Forest Experiment Station. 1970. https://www.cabdirect.org/cabdirect/abstract/19700604317
- 5. Marvin JW, Erickson RO. A statistical evaluation of some of the factors responsible for the flow of sap from the sugar maple. Plant Physiol. 1956;31: 57–61. https://www.jstor.org/stable/4258995 pmid:16654837
- 6. Houle D, Paquette A, Côté B, Logan T, Power H, Charron I, et al. Impacts of climate change on the timing of the production season of maple syrup in eastern Canada. PLoS One. 2015;10: e0144844. pmid:26682889
- 7. Ching TM, Mericle LW. Some evidences of premature stoppage of sugar maple sap production. For Sci. 1960;6: 270–275.
- 8. Laing FM, Howard DB. Sap sweetness consistency vs. growth rates in young sugar maples. North J Appl For. 1990;7: 5–9.
- 9. Gregory RA, Hawley GJ. Sap extraction and measurement of soluble sap sugars in sugar maple. Can J For Res. 1983;13: 400–404.
- 10. Larochelle F, Forget É, Rainville A, Bousquet J. Sources of temporal variation in sap sugar content in a mature sugar maple (Acer saccharum) plantation. For Ecol Manage. 1998;106: 307–313.
- 11. Duchesne L, Houle D. Interannual and spatial variability of maple syrup yield as related to climatic factors. PeerJ. 2014;2: e428. pmid:24949244
- 12. Houle D, Bouffard A, Duchesne L, Logan T, Harvey R, Houle D, et al. Projections of future soil temperature and water content for three southern Quebec forested sites. J Clim. 2012;25: 7690–7701.
- 13. Collins AR, Burton AJ, Cavaleri MA. Effects of experimental soil warming and water addition on the transpiration of mature sugar maple. Ecosystems. 2018;21: 98–111.
- 14. Dodds KJ, Orwig DA. An invasive urban forest pest invades natural environments—Asian longhorned beetle in northeastern US hardwood forests. Can J For Res. 2011;41: 1729–1742.
- 15. Bal TL, Richter DL, Storer AJ, Jurgensen MF. The Relationship of the Sapstreak Fungus, Ceratocystis virescens, to Sugar Maple Dieback and Decay in Northern Michigan. Am J Plant Sci. 2013;4: 436–443.
- 16. Wild AD, Yanai RD. Soil nutrients affect sweetness of sugar maple sap. For Ecol Manage. 2015;341: 30–36.
- 17. Bal TL, Storer AJ, Jurgensen MF, Doskey P V., Amacher MC. Nutrient stress predisposes and contributes to sugar maple dieback across its northern range: a review. For An Int J For Res. 2015;88: 64–83.
- 18.
Little, E. L. J. Atlas of United States trees. Volume 1. Conifers and important hardwoods. Misc Publ United States Dep Agric. 1971;
- 19.
Prasad A, Iverson L. Little’s range and FIA importance value database for 135 eastern US tree species. USDA Forest Service. Northeastern Research Station; 2003.
- 20. Murphy BL, Chretien AR, Brown LJ. Non-timber forest products, Maple syrup and climate change. J Rural Community Dev. 2012;7: 42–64.
- 21.
MacIver DC, Karsh M, Comer N, Klaassen J, Auld H, Fenech A. Atmospheric influences on the sugar maple industry in North America. 2006.
- 22.
Logan T, Charron I, Chaumont D, Houle D. Atlas of climate scenarios for Québec forests. Report produced by Ouranos for the Ministère des Ressources Naturelles et de la Faune du Québec. 2011.
- 23.
Rock B, Spencer S. Case Study 2—The Maple Sugar Industry. Preparing for a Changing Climate: The Potential Consequences of Climate Variability and Change New England Regional Overview, US Global Change Research Program. University of New Hampshire; 2001. pp. 39–42.
- 24. Skinner CB, DeGaetano AT, Chabot BF. Implications of twenty-first century climate change on Northeastern United States maple syrup production: impacts and adaptations. Clim Change. 2010;100: 685–702.
- 25. Duchesne L, Houle D, Côté M-A, Logan T. Modelling the effect of climate on maple syrup production in Québec, Canada. For Ecol Manage. 2009;258: 2683–2689.
- 26. Guilbert J, Beckage B, Winter JM, Horton RM, Perkins T, Bomblies A, et al. Impacts of projected climate change over the Lake Champlain Basin in Vermont. J Appl Meteorol Climatol. 2014;53: 1861–1875.
- 27.
Rondeau A. L’acériculture face aux changements climatiques: inventaire des impacts potentiels et mesures d’adaptation. Université de Sherbrooke. 2007.
- 28. Murphy B, Chretien A, Brown L. How do we come to know? Exploring maple syrup production and climate change in near north Ontario. Environments. 2009;37: 1–34.
- 29.
Richardson K. Sugar bush management in Ontario: Identification of resilient adaptation strategies for a changing climate. Geography and Environmental Studies Major Research Papers. 2015.
- 30. Mozumder P, Randhir TO, Vásquez WF, Jerath M. Risk perceptions and adaptation to climate variability: Survey evidence from maple syrup farmers. Int J Ecol Econ Stat. 2015;36: 1–17.
- 31. Kuehn D, Chase L, Sharkey T. Adapting to climate change: Perceptions of maple producers in New York and Vermont. J Agric Food Syst Community Dev. 2017;7: 1–23.
- 32.
Snyder SA, Kilgore MA, Emery MR, Schmitz M. A profile of Lake States maple syrup producers and their attitudes and responses to economic, social, ecological and climate challenges. Staff Paper Series No. 248. St. Paul, MN; 2018.
- 33. Snyder SA, Kilgore MA, Emery MR, Schmitz M. Maple syrup producers of the Lake States, USA: Attitudes towards and adaptation to social, ecological, and climate conditions. Environ Manage. 2019;63: 185–199. pmid:30688998
- 34.
Fédération des producteurs acéricoles du Québec. Statistiques acéricoles 2016. 2016.
- 35. Hamilton LC, Hartter J, Lemcke-Stampone M, Moore DW, Safford TG. Tracking public beliefs about anthropogenic climate change. PLoS One. 2015;10: e0138208. pmid:26422694
- 36. Lee TM, Markowitz EM, Howe PD, Ko C-Y, Leiserowitz AA. Predictors of public climate change awareness and risk perception around the world. Nat Clim Chang. 2015;5: 1014–1020.
- 37. Weber EU. What shapes perceptions of climate change? Wiley Interdiscip Rev Clim Chang. 2010;1: 332–342.
- 38. Weber EU. What shapes perceptions of climate change? New research since 2010. Wiley Interdiscip Rev Clim Chang. 2016;7: 125–134.
- 39. Hornsey MJ, Harris EA, Bain PG, Fielding KS. Meta-analyses of the determinants and outcomes of belief in climate change. Nat Clim Chang. 2016;6: 622–626.
- 40. Lachapelle E, Borick CP, Rabe B. Public attitudes toward climate science and climate policy in federal systems: Canada and the United States compared. Rev Policy Res. 2012;29: 334–357.
- 41.
Lachapelle E, Borick CP, Rabe BG. Public opinion on climate change and support for various policy instruments in Canada and the US: Findings from a comparative 2013 poll. 2014.
- 42.
Lachapelle E, Dinan S, Borick C, Rabe B, Mills S. Mind the gap: climate change opinions in Canada and the United States. Presented at the Woodrow Wilson International Center for Scholars. 2015. p. 8.
- 43. Ameztegui A, Solarik KA, Parkins JR, Houle D, Messier C, Gravel D. Perceptions of climate change across the Canadian forest sector: The key factors of institutional and geographical environment. PLoS One. 2018;13: e0197689. pmid:29897977
- 44. Bissonnette J-F, Dupras J, Doyon F, Chion C, Tardif J. Perceptions of small private forest owner’s vulnerability and adaptive capacity to environmental disturbances and climate change: Views from a heterogeneous population in southern Quebec, Canada. Small-scale For. 2017;16: 367–393.
- 45. Lenart M, Jones C. Perceptions on Climate Change Correlate with Willingness to Undertake Some Forestry Adaptation and Mitigation Practices. J For. 2014;112: 553–563.
- 46. Strobl C, Boulesteix A-L, Kneib T, Augustin T, Zeileis A. Conditional variable importance for random forests. BMC Bioinformatics. 2008;9: 307. pmid:18620558
- 47. Strobl C, Malley J, Tutz G. An introduction to recursive partitioning: Rationale, application, and characteristics of classification and regression trees, bagging, and random forests. Psychol Methods. 2009;14: 323–348. pmid:19968396
- 48. Johnstone CP, Lill A, Reina RD. Habitat loss, fragmentation and degradation effects on small mammals: Analysis with conditional inference tree statistical modelling. Biol Conserv. 2014;176: 80–98.
- 49. Rehbein F, Kliem S, Baier D, Mößle T, Petry NM. Prevalence of internet gaming disorder in German adolescents: diagnostic contribution of the nine DSM-5 criteria in a state-wide representative sample. Addiction. 2015;110: 842–851. pmid:25598040
- 50. Wu Z, Su X, Sheng H, Chen Y, Gao X, Bao L, et al. Conditional inference tree for multiple gene-environment interactions on myocardial infarction. Arch Med Res. 2017;48: 546–552. pmid:29258680
- 51. Genuer R, Poggi J-M, Tuleau-Malot C. VSURF: An R package for variable selection using random forests. R J. 2015;7: 19–33.
- 52. Hothorn T, Zeileis A, Cheng E:, Ong S. partykit: A modular toolkit for recursive partytioning in R. J Mach Learn Res. 2015;16: 3905–3909.
- 53.
United States Department of Agriculture. 2012 Census of Agriculture. Summary and State Data. 2014.
- 54.
Agriculture and Agri-Food Canada. Statistical overview of the Canadian maple industry, 2017. 2018.
- 55.
United States Department of Agriculture. United States maple syrup production. 2017.
- 56.
Ministère de l’Agriculture des Pêcheries et de l’Alimentation du Québec. Recensement de la relève agricole établie 2016. 2018.
- 57.
United States Department of Agriculture. 2012 Census of Agriculture. Speciality Crops. 2015.
- 58.
Fédération des producteurs acéricoles du Québec. La Fédération des producteurs acéricoles du Québec devient les Producteurs et productrices acéricoles du Québec. Nov 2018. https://www.ppaq.ca/wp-content/uploads/2018/11/FPAQ_Changement_nom_2018.pdf. Accessed 14 Mar 2019.
- 59.
Grenier Y, Gaucher C, Guay S, Lavoie J, Boudreault G. Étude de l’effet de la date d’entaillage sur le potentiel de coulée et le volume de la zone de compartimentation. St-Norbert d’Arthabaska; 2007.
- 60. Wilmot TR. The timing of tapping for maple sap collection. Maple Syrup Dig. 2008;20A: 20–27.
- 61.
Allard G. L’entaillage des érables ACER. Québec; 1999.
- 62. Bauer P, Thorpe A, Brunet G. The quiet revolution of numerical weather prediction. Nature. 2015;525: 47–55. pmid:26333465
- 63. Long RP, Horsley SB, Lilja PR. Impact of forest liming on growth and crown vigor of sugar maple and associated hardwoods. Can J For Res. 1997;27: 1560–1573. https://doi.org/10.1139/x97-074
- 64. Moore J-D, Camiré C, Ouimet R. Effects of liming on the nutrition, vigor, and growth of sugar maple at the Lake Clair Watershed, Québec, Canada. Can J For Res. 2000;30: 725–732.
- 65. Annecou C. Chaulage diagnostic de l’état de santé de l’érablière d’abord! Info-Sirop. Fédération des Producteurs Acéricoles du Québec; 2011;Winter 201: 6–7.
- 66. Duchesne L, Ouimet R, Houle D. Basal area growth of sugar maple in relation to acid deposition, stand health, and soil nutrients. J Environ Qual. 2002;31: 1676. pmid:12371186
- 67. Bernier B, Brazeau M. Foliar nutrient status in relation to sugar maple dieback and decline in the Quebec Appalachians. Can J For Res. 1988;18: 754–761.
- 68. Abrams MD. The Red Maple Paradox. Bioscience. 1998;48: 355–364.
- 69. Fei S, Steiner KC. Evidence for Increasing Red Maple Abundance in the Eastern United States. For Sci. 2007;53: 473–477.
- 70. Fei S, Steiner KC. Rapid capture of growing space by red maple. Can J For Res. 2009;39: 1444–1452.
- 71. Jones ARC, Alli I. Sap yields, sugar content, and soluble carbohydrates of saps and syrups of some Canadian birch and maple species. Can J For Res. 1987;17: 263–266.
- 72.
Grenier Y, Lavoie J, Boudreault G. Vers la formulation de nouvelles normes d’entaillage pour conserver la production acéricole à long terme. St-Norbert d’Arthabaska; 2008.
- 73. Perkins TD, van den Berg AK. Relationships Between Tubing System Age and Sap Yield. Maple Syrup Dig. 2012;24A: 11–16.
- 74.
Pelletier M. État de la recherche sur le sirop de bourgeon. Revue Coopérateur, section Affaires agricoles; 2017. pp. 48–49.
- 75. Aider M, de Halleux D, Belkacemi K. Production of granulated sugar from maple syrup with high content of inverted sugar. J Food Eng. 2007;80: 791–797.
- 76. St-Pierre P, Pilon G, Dumais V, Dion C, Dubois M-J, Dubé P, et al. Comparative analysis of maple syrup to other natural sweeteners and evaluation of their metabolic responses in healthy rats. J Funct Foods. 2014;11: 460–471.
- 77. Zhang Y, Yuan T, Li L, Nahar P, Slitt A, Seeram NP. Chemical Compositional, Biological, and Safety Studies of a Novel Maple Syrup Derived Extract for Nutraceutical Applications. J Agric Food Chem. 2014;62: 6687–6698. pmid:24983789
- 78.
Périé C, de Blois S, Lambert M-C, Casajus N. Effets anticipés des changements climatiques sur l’habitat des espèces arborescentes au Québec. Mémoire de recherche forestière no 173. 2014.
- 79. Hampe A. Plants on the move: The role of seed dispersal and initial population establishment for climate-driven range expansions. Acta Oecologica. 2011;37: 666–673.
- 80. Sittaro F, Paquette A, Messier C, Nock CA. Tree range expansion in eastern North America fails to keep pace with climate warming at northern range limits. Glob Chang Biol. 2017;23: 3292–3301. pmid:28165187
- 81. Williams MI, Dumroese RK. Preparing for Climate Change: Forestry and Assisted Migration. J For. 2013;111: 287–297.
- 82. Wheeler NC, Steiner KC, Schlarbaum SE, Neale DB. The Evolution of Forest Genetics and Tree Improvement Research in the United States. J For. 2015;113: 500–510.
- 83. Krasny ME, Staats LJ, Smallidge PJ, Winship CE. The Sugar Maple Story: Collaborative Research with Extension Agents and Growers. J For. 2001;99: 26–32.
- 84. Mildenberger M, Howe PD, Lachapelle E, Stokes LC, Marlon JR, Gravelle TB. The Distribution of Climate Change Public Opinion in Canada. SSRN Electron J. 2016; pmid:27486659
- 85. McCright AM, Dunlap RE. Cool dudes: The denial of climate change among conservative white males in the United States. Glob Environ Chang. 2011;21: 1163–1172.
- 86. Gareau BJ, Huang X, Gareau TP. Social and ecological conditions of cranberry production and climate change attitudes in New England. PLoS One. 2018;13: e0207237. pmid:30540743
- 87. Howe PD, Mildenberger M, Marlon JR, Leiserowitz A. Geographic variation in opinions on climate change at state and local scales in the USA. Nat Clim Chang. 2015;5: 596–603.
- 88. Chatrchyan AM, Erlebacher RC, Chaopricha NT, Chan J, Tobin D, Allred SB. United States agricultural stakeholder views and decisions on climate change. Wiley Interdiscip Rev Clim Chang. 2017;8: e469.
- 89. DeGaetano AT. Climatic Perspective and Impacts of the 1998 Northern New York and New England Ice Storm. Bull Am Meteorol Soc. 2000;81: 237–254.
- 90. Zarnovican R. Impact du verglas de 1998 dans une érablière à bouleau jaune en Estrie : Situation après trois ans. For Chron. 2002;78: 415–421.
- 91. J Pisaric MF, King DJ, MacIntosh AJM, Bemrose R. Impact of the 1998 Ice Storm on the Health and Growth of Sugar Maple (Acer saccharum Marsh.) Dominated Forests in Gatineau Park, Quebec. J Torrey Bot Soc. 2008;135: 530–539. https://www.jstor.org/stable/40207607
- 92. Running K, Burke J, Shipley K. Perceptions of environmental change and climate concern among Idaho’s farmers. Soc Nat Resour. 2017;30: 659–673.
- 93. Myers TA, Maibach EW, Roser-Renouf C, Akerlof K, Leiserowitz AA. The relationship between personal experience and belief in the reality of global warming. Nat Clim Chang. 2013;3: 343–347.