Warming-driven rise in soil moisture entropy signals destabilization of the Asian Water Tower
Yiran Xie, Teng Liu, Xuan Ma, Yingshuo Lyu, Xu Wang, Yatong Qian, Yongwen Zhang, Ming Wang, Xiaosong Chen

TL;DR
This study uses an entropy-based approach to analyze soil moisture changes on the Tibetan Plateau, revealing a shift from increased stability due to wetting to potential destabilization caused by future warming, with implications for water security.
Contribution
It introduces an entropy framework to assess soil moisture system stability and demonstrates how climate warming may reverse current stability trends on the Tibetan Plateau.
Findings
Wetting has increased system stability from 2000 to 2024.
Future warming is projected to increase soil moisture entropy, indicating destabilization.
ENSO modulates regional heterogeneity and stability of soil moisture.
Abstract
The Tibetan Plateau (TP), known as the "Asian Water Tower," is currently undergoing a rapid wetting trend. While this moisture increase is often viewed as beneficial for water availability, it remains unclear whether the hydrological system itself is becoming more resilient or drifting toward instability. Here, we apply an entropy-based framework to quantify the changing structural organization of the TP's soil moisture system. We show that from 2000 to 2024, regional wetting has driven a long-term decline in entropy, reflecting an increase in system order and stability due to enhanced hydrological buffering capacity. This stability is modulated by the El Ni\~no-Southern Oscillation (ENSO), which regulates regional heterogeneity via a distinct spatial dipole. Crucially, however, CMIP6 climate projections reveal an alarming reversal: future warming triggers a rise in entropy. This…
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Taxonomy
TopicsClimate variability and models · Ecosystem dynamics and resilience · Hydrology and Watershed Management Studies
