Seasonal Variations of Recharge-Storage-Runoff Process over the Tibetan Plateau

The Tibetan Plateau (TP) is a vital and vulnerable water tower that supports the livelihoods of billions of people. The use of a data-driven recharge-storage-runoff perspective enables a more comprehensive estimation of multiple aspects of the water cycle. Through an analysis of the diagnostic net water flux from ERA5, water storage changes (dS/dt) from GRACE, runoff estimations (R) from the land-atmosphere water balance, and river discharge measurements (Rd), the annual cycle of recharge-storage-runoff has been studied over the TP and its basins. The net water flux determines a recharge of 326 mm yr(-1) over the TP. Recharge in coupled storages, leading to an increase in water mass (dS/dt > 0) and runoff (R > 0) during the wet season, is considered the fast response and is measured using the ratio of runoff to net water flux (r1). Conversely, the slow response determined by the water storage release (dS/dt , 0) during the dry season is quantified by the ratio of storage release to runoff (r2). The ratios of r1 and r2 are influenced by climatic and terrain drivers, indicating specific characteristics of recharge-storage-runoff at the basin scale. Small r1 values and large r2 values suggest high buffer capacity, while the basin of Amu Darya (Salween) is characterized by the highest (lowest) buffer capacity over the TP. However, measurements of river discharge at Amu Darya suggest an uncoupled recharge- storage-runoff. The imbalance between river discharge and runoff estimation was most severe in the first decade of the twenty-first century but has been mitigated since 2012. River discharge at Amu Darya is likely constrained by energy summer.

Automated summary

The Tibetan Plateau is an important and vulnerable water tower that supports livelihoods. By analyzing data, a comprehensive understanding of the annual cycle of recharge-storage-runoff is obtained, considering factors such as net water flux, water storage changes, runoff estimations, and river discharge measurements. Ratios of r1 and r2 reflect characteristics at the basin scale, such as buffer capacity. However, there is an imbalance between river discharge and runoff estimation in the Amu Darya basin.