中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Biogeophysical warming effects of vegetation growth in the temperate water-limited region

文献类型:期刊论文

作者Lan, Lihua1,2; Zhao, Wei1,2; Wang, Zhenbo1,2; He, Fei1,2
刊名AGRICULTURAL AND FOREST METEOROLOGY
出版日期2025-12-15
卷号375页码:110886
关键词The temperate water-limited region Vegetation growth Biogeophysical effects Seasons and diurnal scale Land use types Land surface temperature
ISSN号0168-1923
DOI10.1016/j.agrformet.2025.110886
产权排序1
文献子类Article
英文摘要Vegetation growth modulates land surface temperature (LST) through biogeophysical processes, yet these mechanisms remain insufficiently quantified. This study analyzed LST variations and their response to key biogeophysical factors-Albedo, evapotranspiration (ET), leaf area index (LAI), and soil moisture (SM)-across forests, grasslands, and croplands from 2000 to 2020. LST exhibited distinct daily (daytime vs. nighttime) and seasonal (growing vs. non-growing seasons) trend patterns. While annual LST remained stable (Slope (S) =0.0014 K/yr, p > 0.05), significant seasonal contrasts emerged: cooling during growing seasons (S = -0.05 K/yr, p < 0.05) and mild warming in non-growing seasons (S = 0.076 K/yr, p > 0.05). Diurnal asymmetry was evident, with daytime LST cooling (S=-0.106 K/yr, p < 0.05) and nighttime LST warming (S = 0.064 K/yr, p = 0.06). Grasslands showed unique warming trends in both annual (S = 0.093 K/yr, p = 0.08) and non-growing seasons (S = 0.22 K/yr, p < 0.05), contrasting with cooling in croplands and forests. The reduction in daytime LST was primarily driven by ET, contributing -0.08 K/yr, while the increase in nighttime LST was mainly regulated by Albedo, with a contribution of 0.07 K/yr. During growing seasons, SM was the key driver of cooling, contributing -0.028 K/yr. In contrast, LST warming in the non-growing seasons was co-regulated by Albedo (0.038 K/yr) and LAI (0.059 K/yr). Compared to croplands and forests, grasslands exhibited increasing LST in annual and non-growing season, largely influenced by Albedo (0.07 K/yr), ET (0.05K/yr), and LAI (0.1 K/yr). These findings highlighted the role of the biogeophysical effects of vegetation and land-use types in shaping LST variations, offering critical insights for climate-land interactions and sustainable land management.
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WOS关键词LAND-COVER CHANGE ; SURFACE-TEMPERATURE ; CLIMATE-CHANGE ; SOIL-MOISTURE ; GRASSLAND VEGETATION ; NIGHT TEMPERATURE ; AIR-TEMPERATURE ; LOESS PLATEAU ; IMPACT ; AFFORESTATION
WOS研究方向Agriculture ; Forestry ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:001598974500001
出版者ELSEVIER
源URL[http://ir.igsnrr.ac.cn/handle/311030/217483]  
专题区域可持续发展分析与模拟院重点实验室_外文论文
通讯作者Wang, Zhenbo
作者单位1.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100190, Peoples R China
2.Inst Geog Sci & Nat Resources Res, Chinese Acad Sci, Beijing 100101, Peoples R China;
推荐引用方式
GB/T 7714
Lan, Lihua,Zhao, Wei,Wang, Zhenbo,et al. Biogeophysical warming effects of vegetation growth in the temperate water-limited region[J]. AGRICULTURAL AND FOREST METEOROLOGY,2025,375:110886.
APA Lan, Lihua,Zhao, Wei,Wang, Zhenbo,&He, Fei.(2025).Biogeophysical warming effects of vegetation growth in the temperate water-limited region.AGRICULTURAL AND FOREST METEOROLOGY,375,110886.
MLA Lan, Lihua,et al."Biogeophysical warming effects of vegetation growth in the temperate water-limited region".AGRICULTURAL AND FOREST METEOROLOGY 375(2025):110886.

入库方式: OAI收割

来源:地理科学与资源研究所

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