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  4. Land-Use Feedback under Global Warming—A Transition from Radiative to Hydrological Feedback Regime
 
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Land-Use Feedback under Global Warming—A Transition from Radiative to Hydrological Feedback Regime

Journal
Journal of Climate
Journal Volume
37
Journal Issue
14
Start Page
3847
End Page
3866
ISSN
0894-8755
1520-0442
Date Issued
2024-07-15
Author(s)
Singh, Arshdeep
Kumar, Sanjiv
Chen, Liang
Maruf, Montasir
Lawrence, Peter
Lo, Min-Hui  
DOI
10.1175/jcli-d-23-0426.1
URI
https://www.scopus.com/pages/publications/105002284877
https://scholars.lib.ntu.edu.tw/handle/123456789/734787
Abstract
This study examines the effects of land-use (LU) change on regional climate, comparing historical and future scenarios using seven climate models from phase 6 of Coupled Model Intercomparison Project–Land Use Model Intercomparison Project experiments. LU changes are evaluated relative to land-use conditions during the preindustrial climate. Using the Community Earth System Model, version 2–Large Ensemble (CESM2-LE) experiment, we distinguish LU impacts from natural climate variability. We assess LU impact locally by comparing the impacts of climate change in neighboring areas with and without LU changes. Further, we conduct CESM2 experiments with and without LU changes to investigate LU-related climate processes. A multimodel analysis reveals a shift in LU-induced climate impacts, from cooling in the past to warming in the future climate across midlatitude regions. For instance, in North America, LU’s effect on air temperature changes from –0.24° ± 0.18°C historically to 0.62°C ± 0.27°C in the future during the boreal summer. The CESM2-LE shows a decrease in LU-driven cooling from –0.92° ± 0.09°C in the past to –0.09° ± 0.09°C in future boreal summers in North America. A hydroclimatic perspective linking LU and climate feedback indicates LU changes causing soil moisture drying in the midlatitude regions. This contrasts with hydrology-only views showing wetter soil conditions due to LU changes. Furthermore, global warming causes widespread drying of soil moisture across various regions. Midlatitude regions shift from a historically wet regime to a water-limited transitional regime in the future climate. This results in reduced evapotranspiration, weakening LU-driven cooling in future climate projections. A strong linear relationship exists between soil moisture and evaporative fraction in midlatitudes.
Subjects
Atmosphere–land interaction
Feedback
Land surface model
Land use
Soil moisture
SDGs

[SDGs]SDG13

Publisher
American Meteorological Society
Type
journal article

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