Controls of Climate Seasonality and Vegetation Dynamics on the Seasonal Variability of Terrestrial Water Storage Under Diverse Climate Regimes

Abstract Terrestrial water storage change (Δ S ) is an important indicator of climate change that can monitor and predict hydrological changes. However, the interactions between Δ S and climate, vegetation, and soil factors add complexity in temporal variability of Δ S , particularly at seasonal scale. Here, we conduct a systematic assessment in the roles that seasonal variabilities of climate and vegetation modulate seasonal variability of Δ S in 769 basins covering a wide range of climate regimes and vegetation types globally. The variance decomposition method of Δ S based on the Budyko framework is used to estimate the contributions of climate factors (precipitation P and potential evapotranspiration PET ) and runoff ( R ) to Δ S variability for different vegetation types. Results indicate that the increased climatic ( P , PET ) and R seasonal variabilities enhances Δ S seasonal variability under both in‐phase (IP) and out‐of‐phase (OP) seasonal relations between P and PET , with a larger contribution from P than PET and R . However, the P ‐ PET covariance tends to reduce (enhance) Δ S seasonal variability under the IP (OP) relation, while the P ‐ R covariance tends to reduce Δ S variability for both IP and OP relations. Climate seasonality influencing Δ S is regulated through vegetation dynamics, mainly via extending plant roots to access deeper soil water under water stress or by seasonally adapting water use efficiency and primary production. The growth of seasonal vegetation under the IP P ‐ PET relation can cope with limited soil water, while the growth of evergreen vegetation under OP P ‐ PET relation depends on soil water availability throughout the year.