On the southeastern edge of the Tibetan Plateau, at the convergence of the Hengduan Mountains and the Himalayas, abundant moisture creates a unique climate and ecological environment. [Zhao Wanglin/For China daily]
Chinese scientists' recent commentary published in Nature challenged a previous study published in the same journal that suggested Atlantic meteorological droughts threaten the water resource security of the Tibetan Plateau.
The academic commentary by scientists from the Chinese Academy of Sciences published in the "Matters Arising" section of the journal on Thursday, argues that Atlantic meteorological droughts do not pose a threat to the water resource security of the Asian Water Tower.
The Tibetan Plateau provides a robust safeguard for water resource demands in the surrounding Himalayan region. Due to global warming, the Tibetan Plateau is undergoing significant changes, and how it will evolve in the future is a critical scientific issue concerning the sustainable development of the Himalayan region, said Zhao Yutong from the Institute of Tibetan Plateau Research, CAS, who is also a co-corresponding author of the article.
A 2023 study conducted by a joint research team of scientists from China, the United States, and Switzerland, published in Nature, claimed that meteorological droughts in the North Atlantic, where evaporation exceeds precipitation, triggered a significant decline in terrestrial water storage on the Tibetan Plateau between 2003 and 2016.
Based on this, the study further predicted that this declining trend would intensify in the future, posing severe challenges to the water resource security.
"The two key pieces of evidence supporting the aforementioned conclusions are untenable," Zhao said.
The authors of the original study used a water vapor tracking model and suggested that the North Atlantic transports substantial water vapor to the Tibetan Plateau via mid-latitude westerlies, contributing significantly to its annual precipitation.
"Observations from water vapor stable isotopes identify that the Indian Ocean monsoon is the primary source of water vapor instead of the North Atlantic, a claim contradicted by the 2023 research," Zhao said.
When water vapor moves from the Atlantic Ocean to the plateau, precipitation, diffusion, and other processes occur, causing deposition along the way, potentially accounting for a significant portion of the total. The original research overlooked this important process, thus exaggerating the contribution of the Atlantic, Zhao said.
Furthermore, although the original authors claimed that a significant negative correlation was observed between North Atlantic meteorological droughts and changes in terrestrial water storage on the Tibetan Plateau from 2003 to 2016, Zhao's team found that the teleconnection between the Atlantic and the Tibetan Plateau is temporally unstable.
"A sliding window analysis revealed that the significant correlation between the two completely disappeared from 2008 to 2021. Therefore, the conclusion that future terrestrial water storage will continue to decline based on a statistical relationship lacking physical mechanisms is unreliable," she said.
The commentary emphasized that traditional water vapor tracing models are inadequate for accurately capturing the complex three-dimensional water vapor transport and transformation processes over the plateau.
"To better understand the water resource security of the Asian Water Tower, it's necessary to expand the coverage of the water vapor observation network across the plateau and conduct detailed monitoring," Zhao said.
The commentary said that by tracking the complete water cycle chain — including external water vapor transport and runoff — it would be possible to accurately analyze and predict the spatiotemporal evolution of water storage on the Tibetan Plateau.
