scholarly journals Anthropogenic refugia ameliorate the severe climate-related decline of a montane mammal along its trailing edge

2012 ◽  
Vol 279 (1745) ◽  
pp. 4279-4286 ◽  
Author(s):  
Toni Lyn Morelli ◽  
Adam B. Smith ◽  
Christina R. Kastely ◽  
Ilaria Mastroserio ◽  
Craig Moritz ◽  
...  

We conducted detailed resurveys of a montane mammal, Urocitellus beldingi , to examine the effects of climate change on persistence along the trailing edge of its range. Of 74 California sites where U. beldingi were historically recorded (1902–1966), 42 per cent were extirpated, with no evidence for colonization of previously unoccupied sites. Increases in both precipitation and temperature predicted site extirpations, potentially owing to snowcover loss. Surprisingly, human land-use change buffered climate change impacts, leading to increased persistence and abundance. Excluding human-modified sites, U. beldingi has shown an upslope range retraction of 255 m. Generalized additive models of past distribution were predictive of modern range contractions (AUC = 0.76) and projected extreme reductions (52% and 99%, respectively) of U. beldingi's southwestern range to 2080 climates (Hadley and CCCMA A2). Our study suggests the strong impacts of climate change on montane species at their trailing edge and how anthropogenic refugia may mitigate these effects.

2016 ◽  
Vol 6 (13) ◽  
pp. 4468-4477 ◽  
Author(s):  
Betsy A. Bancroft ◽  
Joshua J. Lawler ◽  
Nathan H. Schumaker

2016 ◽  
Vol 572 ◽  
pp. 1507-1519 ◽  
Author(s):  
Gianbattista Bussi ◽  
Paul G. Whitehead ◽  
Michael J. Bowes ◽  
Daniel S. Read ◽  
Christel Prudhomme ◽  
...  

2021 ◽  
Author(s):  
Arshdeep Singh ◽  
Sanjiv Kumar

<p>Land-use change (LU) is a major regional climate forcing that affects carbon-water-energy fluxes and, therefore, near-surface air temperature. Although there are uncertainties in LU impacts in the historical climate, there is a growing consensus towards a cooling influence in the mid-latitudes. However, how a drier and warmer land surface condition in the future climate can change the LU impacts are not investigated well.</p><p>We use a comprehensive set of five coupled climate models from the CMIP6-LUMIP project to assess the changing influence of the LU change. We use two methodologies: (1) direct method – where LU impacts are estimated by subtracting the ‘no-LU’ climate experiment from the control experiment that includes LU, and (2) Kumar et al., 2013 (K13) method where LU impacts are estimated by comparing climate change impacts between LU and no-LU neighboring regions.</p><p>First, we compared the LU impacts in the historical climate and between the direct method and K13 methods using the multi-model analysis. In the North America LU change region, the direct method shows a cooling impact of (-0.14 ± 0.13°C). The K13 methods show a smaller cooling impact (-0.09 ± 0.08°C). In terms of energy balance, the direct method shows a reduction of net shortwave radiation (-0.82 ± 0.91 watts/m<sup>2</sup>) the K13 method shows a cleaner result of (-1.25 ± 0.60 watts/m<sup>2</sup>), as expected. We suspect that a more substantial influence of the LU change in the direct method is due to large-scale circulation driven response or due to the internal variability that has been canceled out in the K13 method.</p><p>Next, we extend the K13 method to assess the LU impacts in the future climate. Direct methods are not available for the future climate experiment in CMIP6-LUMIP datasets. We find that a cooling impact of LU change has become statistically insignificant in the future climate (-0.17 ± 0.19°C). A similar influence is also found in the reduction of the net shortwave radiation (-1.92 ± 3.34 watts/m<sup>2</sup>). We also found that climate change impacts on temperature are an order of magnitude greater than LU impact in the future climate. Hence, we hypothesize that higher warming has contributed to the larger uncertainty in LU impacts. We will also discuss LU impacts in Eurasia and Indian subcontinent.</p><p><img src="https://contentmanager.copernicus.org/fileStorageProxy.php?f=gnp.967d8b47f50063273001161/sdaolpUECMynit/12UGE&app=m&a=0&c=6fbaa64b9acfb208f665dca0184a6955&ct=x&pn=gnp.elif&d=1" alt=""></p><p> </p><p> </p><p>Reference</p><p>Kumar, S., Dirmeyer, P. A., Merwade, V., DelSole, T., Adams, J. M., & Niyogi, D. (2013). Land use/cover change impacts in CMIP5 climate simulations: A new methodology and 21st century challenges. Journal of Geophysical Research: Atmospheres, 118(12), 6337-6353.</p>


2019 ◽  
Vol 8 (9) ◽  
pp. 368
Author(s):  
Dejian Zhang ◽  
Wenjie Fu ◽  
Qiaoying Lin ◽  
Xingwei Chen

This study developed a web-based open-source framework based on the Soil and Water Assessment Tool (SWAT), named WOF-SWAT (web-based open-source framework for SWAT), to investigate individual and combined impacts of climate change, land use change, and point-source pollutants on watershed-scale hydrological and chemical processes. The architecture, workflows, interfaces, and key processes of WOF-SWAT are described and discussed. Using a previously developed well-calibrated hydrological model of the Jinjiang River basin, four scenarios were simulated in WOF-SWAT and other traditional desktop-based tools (i.e., ArcSWAT and SWAT-CUP) to examine the credibility, efficiency, and functionality of WOF-SWAT. The results show that, in combination with a well-calibrated watershed model, WOF-SWAT is sufficiently sound and reasonable to investigate individual and combined impacts of climate change, land use change, and point-source pollutants. We thus conclude that WOF-SWAT can be used as a substitute for other tools to carry out similar tasks in a web-based environment while providing more user-friendly interfaces, accessibility, and efficiency. We also discuss ongoing and possible future efforts to develop WOF-SWAT into a fully-fledged watershed research and management framework.


2002 ◽  
Vol 28 (4) ◽  
pp. 568-582 ◽  
Author(s):  
Michael J. Barlage ◽  
Paul L. Richards ◽  
Peter J. Sousounis ◽  
Andrew J. Brenner

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