Hydroclimatic Variability Shapes Long‐Term Water Balance
Year: 2026
Type: article
Abstract: Long‐term water availability is commonly interpreted through mean precipitation () and potential evapotranspiration (), yet hydroclimatic variability spans seasonal to event scales and may influence water partitioning beyond what mean climate alone captures. Although the aridity index () explains much of the spatial variability in evaporative fraction (), systematic departures from classical relationships suggest that additional modes of variability shape long‐term . Here, using large‐sample observations from catchments across the United States, Australia, and Brazil, we show that seasonal covariance, monthly variance, and event‐scale storm structure leave persistent, organized imprints on long‐term water balance. We introduce a hypothesis‐driven expansion of the aridity framework that incorporates these variability terms and demonstrates that sub‐annual climate organization can be explicitly embedded within long‐term water‐balance theory. This variability‐aware perspective provides a mechanistic pathway for assessing how shifts in climate variability, even under approximately stationary long‐term means, may propagate into future water yields.
Source: Geophysical Research Letters
DOI: 10.1029/2025gl121486
Language: English
Subfield: Water Science and Technology
Field: Environmental Science
Domain: Physical Sciences
SDG: Climate action
Open Access status: gold
Estimated APC paid: $3,190
OpenAlex ID: W7147544933
