Chaofan Zhou , Huili Gong , Beibei Chen , Xiaojuan Li , Lin Zhu , Mengxuan Bao , Jiajun Zhu
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引用次数: 0
Abstract
Soil moisture (SM) is a key component of land–atmosphere interactions. However, the vertical variability of soil moisture memory (SMM) and its sensitivity to climatic drivers remain insufficiently understood. In this study, we analyzed monthly ERA5-Land SM data (January 2001–December 2024) for four depth layers (0–7, 7–28, 28–100, and 100–289 cm) across Inner Mongolia to characterize the vertical differentiation of SM. Pearson correlation and meta-analysis were applied to quantify the relationships between SM and climatic drivers. The results show that, (1) SM exhibits a pronounced east–west gradient, decreasing from moist conditions in the east to arid conditions in the west. (2) Precipitation is the primary driver of SM dynamics at all depths, yet its influence diminishes markedly with depth. In surface layers, SM is predominantly negative correlation with evapotranspiration (ET) in the southeastern and western regions, and positively correlated with the normalized difference vegetation index (NDVI). In deeper layers, these relationships weaken or reverse. (3) The surface layer (0–7 cm) of SMM has the shortest memory (4–6 months) with a half-life of 1.49 months, whereas deeper layers exhibit substantially longer persistence.
期刊介绍:
The Journal of Arid Environments is an international journal publishing original scientific and technical research articles on physical, biological and cultural aspects of arid, semi-arid, and desert environments. As a forum of multi-disciplinary and interdisciplinary dialogue it addresses research on all aspects of arid environments and their past, present and future use.