Impact of livestock activity on near-surface ground temperatures in Mongolia

Grazing by livestock can alter the surface conditions at grassland sites, impacting the transfer of energy between the atmosphere and ground and consequentially ground temperatures. In this study, we investigate surface cover in summer and winter and measure ground surface temperatures over 14 month...

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Bibliographic Details
Main Authors: Zweigel, Robin B., Dashtseren, Avirmed, Temuujin, Khurelbaatar, Sharkhuu, Anarmaa, Webster, Clare, Lee, Hanna, Westermann, Sebastian
Format: Text
Language:English
Published: 2024
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2024-1790
https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1790/
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Summary:Grazing by livestock can alter the surface conditions at grassland sites, impacting the transfer of energy between the atmosphere and ground and consequentially ground temperatures. In this study, we investigate surface cover in summer and winter and measure ground surface temperatures over 14 months at sites in Central Mongolia that feature different grazing intensities (intensely and ungrazed) and topographic aspects (north- and south-facing). Overall, intense grazing leads to a substantially reduced vegetation cover, altered snow conditions and lack of surface litter accumulation. Comparing  intensely grazed and ungrazed plots shows large seasonal differences in ground surface temperatures, with grazed plots being up to +5.1 °C warmer in summer and −5.4 °C colder in winter at a south-facing site. We find smaller seasonal differences of +1.4 °C and −2.5 °C between grazed and ungrazed plots at a north-facing site which receives less solar radiation and where differences in vegetation cover between open and fenced plots are smaller. For both aspects, the seasonal differences largely offset each other, with both a small net cooling and warming depending on effects in spring and autumn. Our study suggests that livestock management might be used to modify the annual ground temperature dynamics, possibly even influencing local permafrost dynamics.