期刊
THEORETICAL AND APPLIED CLIMATOLOGY
卷 145, 期 3-4, 页码 891-901出版社
SPRINGER WIEN
DOI: 10.1007/s00704-021-03664-3
关键词
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资金
- Second Tibetan Plateau Scientific Expedition and Research (STEP) Project [2019QZKK0103]
- National Natural Science Foundation of China [41775016, 41975007, 41905008]
- Scientific Research Foundation of CUIT [KYTZ201822]
The soil temperature on the Tibetan Plateau is showing a significant warming trend, especially in winter and spring. Factors such as air temperature, total precipitation, maximum snow depth, and maximum frozen ground depth are all significantly correlated with soil temperature, with air temperature having the strongest influence across all seasons.
The changing characteristics of the frozen ground are essential indicators of climate change. The soil temperature on the Tibetan Plateau (TP) during 1987-2018 is simulated using the coupled model of RegCM4.7-CLM4.5. The results show that there is a significant warming trend in the soil temperature on the TP, and the warming trend is higher in October-May (0.040 degrees C.decade(-1)) than in June-September (0.026 degrees C.decade(-1)), with the maximum value in February (0.058 degrees C.decade(-1)). Spatially, the warming is most significant in the Three River Source Region (0.15 similar to 0.20 degrees C.decade(-1)) and near the Himalayas and Kunlun Mountains (0.20 similar to 25 degrees C.decade(-1)), with the warming trend greater in winter and spring than in summer and autumn. Air temperature, total precipitation, maximum snow depth, and maximum frozen ground depth are all significantly correlated to soil temperature. Air temperature (R = 0.851) and total precipitation (R = 0.411) are positively correlated with soil temperature, while maximum snow depth (R = -0.381) and maximum frozen ground depth (R = -0.770) are negatively correlated with it. Air temperature has a strong influence on the soil temperature in all the four seasons, while the effect of the total precipitation is strongest in autumn (R = 0.836). The retarding effects of maximum snow depth and maximum frozen ground depth are strongest in summer (R = -0.772 and -0.35, respectively). The frozen ground on the TP shows a degradation trend, and the consequent hydrological, ecological, and climatic effects deserve sufficient attention.
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