@article{a47ff6ad36f8434183afa26dc2b95965,
title = "Linking surface and subterranean climate: implications for the study of hibernating bats and other cave dwellers",
abstract = "Caves and other subterranean features provide unique environments for many species. The importance of cave microclimate is particularly relevant at temperate latitudes where bats make seasonal use of caves for hibernation. White-nose syndrome (WNS), a fungal disease that has devastated populations of hibernating bats across eastern and central North America, has brought renewed interest in bat hibernation and hibernaculum conditions. A recent review synthesized current understanding of cave climatology, exploring the qualitative relationship between cave and surface climate with implications for hibernaculum suitability. However, a more quantitative understanding of the conditions in which bats hibernate and how they may promote or mediate WNS impacts is required. We compiled subterranean temperatures from caves and mines across the western United States and Canada to (1) quantify the hypothesized relationship between mean annual surface temperature (MAST) and subterranean temperature and how it is influenced by measurable site attributes, and (2) use readily available gridded data to predict and continuously map the range of temperatures that may be available in caves and mines. Our analysis supports qualitative predictions that subterranean winter temperatures are correlated with MAST, that temperatures are warmer and less variable farther from the surface, and that even deep within-cave temperatures tend to be lower than MAST. Effects of other site attributes (e.g., topography, vegetation, and precipitation) on subterranean temperatures were not detected. We then assessed the plausibility of model-predicted temperatures using knowledge of winter bat distributions and preferred hibernaculum temperatures. Our model unavoidably simplifies complex subterranean environments and is not intended to explain all variability in subterranean temperatures. Rather, our results offer researchers and managers improved broad-scale estimates of the geographic distribution of potential hibernaculum conditions compared to reliance on MAST alone. We expect this information to better support range-scale estimation of winter bat distributions and projection of likely WNS impacts across the west. We suggest that our model predictions should serve as hypotheses to be further tested and refined as additional data become available.",
keywords = "bats, caves, hibernacula, microclimate, temperature, white-nose syndrome",
author = "McClure, {Meredith L.} and Daniel Crowley and Haase, {Catherine G.} and McGuire, {Liam P.} and Fuller, {Nathan W.} and Hayman, {David T.S.} and Lausen, {Cori L.} and Plowright, {Raina K.} and Dickson, {Brett G.} and Olson, {Sarah H.}",
note = "Funding Information: This project has been funded in whole or in part by Federal funds from the Department of Defense Environmental Research and Development Program (SERDP), under Contract Number W912HQ‐16‐C‐0015. DTSH is funded by Royal Society Te Aparangi, grant number MAU1701. Microclimate logger data were provided by WCS Canada (Jason Rae), Colorado Parks and Wildlife (David Klute), Nevada Department of Wildlife (Jason Williams), Oregon Caves National Monument and the National Park Service—Klamath Network (Ivan Yates), The Nature Conservancy (Katie Gillies), Wyoming Game and Fish Department (Laura Beard), and Jessica Oster (Vanderbilt University). We thank Reed Hranac, Luke Zachmann, Nathan Justice, Fred Frick, and Tina Cheng for their valuable input on the focal questions and methods that helped frame and improve the manuscript. Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the government. Olson, McGuire, Hayman, Lausen, Plowright, and Dickson conceived the study. Haase, Fuller, and Lausen collected a subset of the temperature data. Crowley compiled and supported analysis of the temperature data. McClure derived and compiled predictor data, designed and conducted the final analyses, and drafted the manuscript. Haase and McGuire supported design of the analyses, and all contributed to paper framing and revision. The authors have no competing interests to disclose. Funding Information: This project has been funded in whole or in part by Federal funds from the Department of Defense Environmental Research and Development Program (SERDP), under Contract Number W912HQ-16-C-0015. DTSH is funded by Royal Society Te Aparangi, grant number MAU1701. Microclimate logger data were provided by WCS Canada (Jason Rae), Colorado Parks and Wildlife (David Klute), Nevada Department of Wildlife (Jason Williams), Oregon Caves National Monument and the National Park Service—Klamath Network (Ivan Yates), The Nature Conservancy (Katie Gillies), Wyoming Game and Fish Department (Laura Beard), and Jessica Oster (Vanderbilt University). We thank Reed Hranac, Luke Zachmann, Nathan Justice, Fred Frick, and Tina Cheng for their valuable input on the focal questions and methods that helped frame and improve the manuscript. Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the government. Olson, McGuire, Hayman, Lausen, Plowright, and Dickson conceived the study. Haase, Fuller, and Lausen collected a subset of the temperature data. Crowley compiled and supported analysis of the temperature data. McClure derived and compiled predictor data, designed and conducted the final analyses, and drafted the manuscript. Haase and McGuire supported design of the analyses, and all contributed to paper framing and revision. The authors have no competing interests to disclose. Publisher Copyright: {\textcopyright} 2020 The Authors.",
year = "2020",
month = oct,
day = "1",
doi = "10.1002/ecs2.3274",
language = "English (US)",
volume = "11",
journal = "Ecosphere",
issn = "2150-8925",
publisher = "Ecological Society of America",
number = "10",
}