How winds above Tibet quietly replenish water for nearly 2 billion people

The “Asian Water Towers” (AWTs), a high-altitude region with a mean elevation exceeding 4,000 meters, serve as the primary freshwater source for nearly 2 billion people. While the Indian summer monsoon is well known for shaping seasonal rainfall patterns that help feed the AWTs, the hydrological role of the mid-latitude westerlies—which dominate regional weather patterns for three-quarters of the year—has been unclear.

New insight into westerly moisture transport

Now, a research team led by Profs. Gao Jing and Yao Tandong from the Institute of Tibetan Plateau Research of the Chinese Academy of Sciences, in collaboration with international scientists, has determined how the westerlies integrate their moisture into the local water cycle under non-precipitating conditions.

Specifically, the researchers have identified a “vertical conveyor” atmospheric mechanism whereby moisture carried by high-altitude winds is transported toward the plateau through a complex process of nocturnal “decoupling.”

The results were published in Proceedings of the National Academy of Sciences on May 6.

Balloon observations and advanced modeling

In this study, the researchers combined in situ vertical observations with the state-of-the-art ECHAM6-wiso isotope-enabled atmospheric model, providing the first unified, process-based picture of how the AWTs’ atmospheric water is supplied.

Using specialized helium-tethered “Jimu balloons,” the researchers collected 32 unprecedented vertical profiles of atmospheric water vapor stable isotopes (δDᵥ and d-excessᵥ) and meteorological parameters at two locations on the Tibetan Plateau: Lulang, a forested moisture corridor, and Nam Co, a high-altitude inland lake.

A three-layered atmospheric structure

These isotopes allowed the researchers to identify a highly stratified atmospheric structure comprising three layers: the atmospheric boundary layer, located at roughly 600 to 900 meters, where locally sourced moisture is shaped by diurnal cycles; the mixed layer, an intermediate zone between 600 and 1,600 meters, characterized by minimal isotopic variance; and the free troposphere, found above 1,600 to 1,800 meters, where large-scale westerlies transport moisture across the Himalayan barrier.

The researchers found that atmospheric water vapor transported by the westerlies undergoes subsidence, with large-scale descent of this moisture toward the AWTs’ atmospheric boundary layer. As this moisture sinks, it interacts with local air, creating two distinct thermal inversion layers. These layers act as physical “caps” that suppress vertical mixing and decouple atmospheric water vapor into distinct layers.

Nocturnal decoupling and moisture integration

This decoupling isolates the moisture aloft transported by the westerlies from the relatively moist, local air trapped within the atmospheric boundary layer. The condensation below these thermal inversion layers during the decoupling integrates the moisture brought by the westerlies into the local moisture budget. This process constitutes a primary pathway for integrating westerlies-advected moisture into the local moisture budget without precipitation, sustaining near-surface moisture accumulation.

The researchers discovered that even without precipitation, approximately 30% of the moisture transported by the westerlies is integrated into the local cycle through phase transitions at night.

Implications for a warming climate

These findings are significant as anthropogenic warming drives rapid hydrological transitions—including accelerated glacier retreat and altered runoff patterns—that affect the amount of moisture fed into the AWTs. The findings provide critical benchmarks for improving atmospheric models, optimizing climate projections for the AWTs’ water cycle, and advancing the climatic interpretation of regional isotopic records, such as those from ice cores.

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