Irreversible declines in freshwater storage projected in parts of Asia by 2060

Irreversible declines in freshwater storage projected in parts of Asia by 2060
Time series of reconstructed terrestrial water storage anomalies (TWSA) and TWSA estimated from GRACE JPL-M over the (a) Amu Darya and (b) Indus basins. The red line shows GRACE observations, whereas the blue line shows the ensemble mean of reconstructed TWSA from nine GCMs (Table S2). Shadows represent uncertainty range of ±1 standard deviation among outputs from different GCMs. Credit: Penn State, Tsinghua University

The Tibetan Plateau, known as the "water tower" of Asia, supplies freshwater for nearly 2 billion people who live downstream. New research led by scientists at Penn State, Tsinghua University and the University of Texas at Austin projects that climate change, under a scenario of weak climate policy, will cause irreversible declines in freshwater storage in the region, constituting a total collapse of the water supply for central Asia and Afghanistan and a near-total collapse for Northern India, Kashmir and Pakistan by the middle of the century.

"The prognosis is not good," said Michael Mann, distinguished professor of atmospheric science, Penn State. "In a 'business as usual' scenario, where we fail to meaningfully curtail fossil fuel burning in the decades ahead, we can expect a near collapse—that is, nearly 100% loss—of water availability to downstream regions of the Tibetan Plateau. I was surprised at just how large the predicted decrease is even under a scenario of modest climate policy."

According to the researchers, despite its importance, the impacts of on past and future terrestrial water storage (TWS)—which includes all the above- and below-ground water—in the Tibetan Plateau have largely been underexplored.

"The Tibetan Plateau supplies a substantial portion of the water demand for almost 2 billion people," said Di Long, associate professor of hydrologic engineering, Tsinghua University. "Terrestrial water storage across this region is crucial in determining water availability, and it is highly sensitive to climate change."

Mann added that a solid benchmark for the TWS changes that have already occurred in the Tibetan Plateau has been lacking. In addition, he said, the absence of reliable future projections of TWS limits any guidance on policymaking, despite the fact that the Tibetan Plateau has long been considered a climate change hotspot.

To fill these knowledge gaps, the team used "top-down"—or satellite-based—and "bottom-up"—or ground-based—measurements of water mass in glaciers, lakes and below-ground sources, combined with machine learning techniques to provide a benchmark of observed TWS changes over the past two decades (2002‒2020) and projections over the next four decades (2021–2060).

Irreversible declines in freshwater storage projected in parts of Asia by 2060
Lakes, glaciers, and major river basins on the Tibetan Plateau. Endorheic basins are shown in light purple and exorheic basins in light yellow. Bar plots show TWS changes (TWSC) for each basin (only basins with TWS trends ≥ 1.0 Gt/yr are shown) during 2002‒2017, estimated from the GRACE JPL-M solution. Blue bars represent mass gain in TWS, whereas red bars represent mass loss, and bar size represents the magnitude of TWS changes (Gt/yr). Specific values for TWS changes are shown in each basin. Credit: Penn State, Tsinghua University

Mann explained that advances in Gravity Recovery and Climate Experiment (GRACE) satellite missions have provided unprecedented opportunities to quantify TWS changes at large scales. Yet, previous studies have not explored the sensitivity of GRACE solutions using independent, ground-based data sources, leading to a lack of consensus regarding TWS changes in the region.

"Compared to previous studies, establishing consistency between top-down and bottom-up approaches is what gives us confidence in this study that we can accurately measure the declines in TWS that have already occurred in this critical region," he said.

Next, the researchers used a novel neural net-based machine learning technique to relate these observed changes in total water storage to key climate variables, including air temperature, precipitation, humidity, cloud cover and incoming sunlight. Once they "trained" this artificial neural net model, they were able to look at how projected future changes in climate are likely to impact water storage in this region.

Among their results, which published today (August 15) in the journal Nature Climate Change, the team found that climate change in recent decades has led to severe depletion in TWS (-15.8 gigatons/year) in certain areas of the Tibetan Plateau and substantial increases in TWS (5.6 gigatons/year) in others, likely due to the competing effects of glacier retreat, degradation of seasonally frozen ground, and lake expansion.

The team's projections for future TWS under a moderate carbon emissions scenario—specifically, the mid-range SSP2-4.5 emissions scenario—suggest that the entire Tibetan Plateau could experience a net loss of about 230 gigatons by the mid-21st century (2031‒2060) relative to an early 21st century (2002‒2030) baseline.

More specifically, excess water loss projections for the Amu Darya basin—which supplies water to central Asia and Afghanistan—and the Indus basin—which supplies water to Northern India, Kashmir and Pakistan—indicate a decline of 119% and 79% in water-supply capacity, respectively.

Irreversible declines in freshwater storage projected in parts of Asia by 2060
Projected changes in TWS and associated climate drivers over the TP until the mid-21st century under SSP2-4.5. (a‒c) Spatial patterns of linear trends for DNN-reconstructed TWS on the TP during the (a) past two decades (2002‒2020), (b) the coming decade (2021‒2030), and (c) the mid-twenty-first century (2031‒2060). Stippling in (a) and (b) marks regions that have a significant trend (the Mann-Kendall test at a 5% significance level). (d‒g) The difference between the 30-year averaged state for the 2031‒2060 period relative to the average for the 2002‒2021 period in (d) reconstructed TWS, (e) annual precipitation, (f) annual average temperature, and (g) solar radiation. All results were estimated from the ensemble mean of nine GCMs under the mid-range SSP2-4.5 scenario. Credit: Penn State, Tsinghua University

"Our study provides insights into hydrologic processes affecting high-mountain freshwater supplies that serve large downstream Asian populations," said Long. "By examining the interactions between climate change and the TWS in the historical period and future by 2060, this study serves as a basis to guide future research and the management by governments and institutions of improved adaptation strategies."

Indeed, Mann added, "Substantial reductions in over the next decade, as the U.S. is now on the verge of achieving thanks to the recent Inflation Reduction Act, can limit the additional warming and associated climate changes behind the predicted collapse of the Tibetan Plateau water towers. But even in a best-case scenario, further losses are likely unavoidable, which will require substantial adaptation to decreasing water resources in this vulnerable, highly populated region of the world."

Mann noted that more alternative water supply sources, including intensified groundwater extraction and water transfer projects, may be necessary to meet the amplified water shortage in the future.

More information: Di Long, Climate change threatens terrestrial water storage over the Tibetan plateau, Nature Climate Change (2022). DOI: 10.1038/s41558-022-01443-0.

Journal information: Nature Climate Change

Citation: Irreversible declines in freshwater storage projected in parts of Asia by 2060 (2022, August 15) retrieved 28 January 2023 from
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