Smells strongly like junk or shoddy science, again featured by the the AAAS! Plus, it is a Chinese study (any possible political motive in this case?).
Only 40 years of history (satellite imagery) is nothing or definitely not enough data! What about other human factors that may have contributed to this phenomenon (overpopulation, increasing tourism etc.)?
If you believe in global warming/climate change then everything is automatically related to it. These scientists most likely suffered from this bias!
"High in the Himalayas, a system of rivers and glaciers known as the “Water Tower of Asia” supplies freshwater to roughly two billion people downstream. Scientists who examined 40 years of satellite imagery from three major river basins—the Yarlung Tsangpo, Indus, and Ganges—observed that, due to climate change, the waters there have started wandering more.
As rivers flow, they rarely follow a straight path, curving in different directions and forming bends called meanders. Since water erodes the outer bank over time and deposits sediment on the inner bank, those bends move across the floodplain and the river shifts sideways, in a “meandering migration.” Researchers found that, in the Himalayas, rates of lateral channel migration nearly doubled between 1980 and 2020. Rivers also abandoned meandering loops, jumped channels, and changed patterns more often, drastically reshaping downstream ecosystems.
Scientists believe the changes are caused by the thawing and retreat of the region’s ice and frozen ground, a phenomenon known as “cryosphere degradation.” As temperatures in the upper Himalayas rise at roughly twice the global average rate, glacial melt accelerates, frozen ground thaws, and riverbanks lose the icy cohesion that once held them in place. This rise in meandering is part of a broader pattern, geophysical scientists Shawn Chartrand and Jonas Eschenfelder argue in an accompanying Science Perspective, noting that the dynamics of rivers in cold regions “ can be early indicators of environmental change under a warming climate.”"
From the abstract of the Perspective:
"Surface sediments in polar and high mountain regions underlain by permafrost—ground that is frozen for two consecutive years or longer—undergo seasonal freezing and thawing. This yearly cycle influences river dynamics by changing water flow and susceptibility to erosion.
Consequently, a warming climate can change river configurations in cold landscapes. However, elucidating a causal link between atmospheric temperature trends and river erosion is more difficult than it appears. Despite previous efforts, there is no generally accepted theory describing river erosion in permafrost-dominated basins, in part because of a lack of long-term observations. On page 716 of this issue, Lin et al. (8) report that rates of river migration in high Himalayan river basins accelerated over the past two decades. This suggests that cold-region river dynamics can be early indicators of environmental change under a warming climate."
From the editor's summary and abstract:
"Editor’s summary
High mountain ranges are particularly sensitive to climate change [???], and their landscapes provide an early warning for how surface processes may shift with warming. Using 40 years of satellite imagery, Lin et al. compiled river migration data across three major high Himalayan drainages ... Measures of channel mobility for over 1000 river bends indicated a near doubling of migration rates between 1980 and 2020 in response to melting glaciers, higher sediment loads, and warmer ground. The accelerated meandering of upland rivers will alter soil and sediment fluxes and could have a destabilizing effect on downstream ecosystems, infrastructure, and human populations. ...
Structured Abstract
INTRODUCTION
River meandering and migration are two of the most ubiquitous geomorphic processes on Earth, governing floodplain evolution, ecosystem disturbance, and infrastructure stability. A long-standing, but largely untested, hypothesis proposes that climate change systematically alters the pace of river planform morphodynamics [???]. The upper high Himalayas, where temperatures are rising nearly twice as fast as the global average, offer a critical natural laboratory to detect climatic imprints within upland rivers that sustain billions of people downstream.
RATIONALE
River meandering is controlled by complex interactions between channel dynamics, hydrology, sediment supply, bank strength, and external disturbances. Climate warming may [???] influence these controls through multiple pathways, including cryosphere degradation such as increased runoff or permafrost thaw, vegetation change, and altered hydrosedimentary regimes. However, distinguishing climatic forcing from intrinsic self-organization processes, human disturbances, and geological controls has remained a fundamental challenge, particularly at regional scales. To address this gap, we conducted a multidecadal analysis of river planform dynamics across the upper high Himalayas and evaluated the relative contributions of nonclimate and climatic drivers.
RESULTS
We show that unconfined Himalayan rivers experienced a widespread and coherent acceleration of morphodynamics over the past four decades.
Mean lateral migration nearly doubled between 1980–2000 and 2000–2020, accompanied by increases in cutoff frequency (115%), avulsion activity (77%), and channel pattern transitions (97%). The integrated river planform morphodynamics index more than doubled, whereas characteristic migration timescales shortened by 40%.
Sensitivity tests confirmed that these accelerations are robust across temporal resolutions, sinuosity classes, and ground thermal regimes.
Statistical analyses support significant associations between accelerated morphodynamics and rising temperature and related environmental changes.
By using structural equation modeling, we show that climate warming has both direct and indirect impacts on meandering and migration dynamics by weakening bank stability, modifying vegetation conditions, and altering hydrosedimentary regimes, whereas nonclimate factors such as geological structures, river slope, or channel width contribute comparatively little at regional scales. [no human factors???]
CONCLUSION
Our study reveals that river morphodynamics in the Himalayan uplands have detectably and substantially accelerated in response to climate warming over the past four decades and are primarily driven by cryosphere degradation rather than anthropogenic disturbances, local topography, or channel self-organization. Unlike Arctic permafrost rivers, where warming decelerates meandering through shrub-induced bank stabilization, sparsely vegetated Himalayan uplands lack this buffering mechanism, making this region a sensitive sentinel of climate-driven fluvial change.
Channel planform dynamics of Himalayan rivers serve as an emerging geomorphic signal of climate change and underscore a previously underappreciated pathway through which warming reshapes landscape evolution.
The doubling of lateral channel mobility over four decades accelerates sediment reworking, shortening organic carbon residence times on upland floodplains and posing potential risks to water security, infrastructure stability, and riparian ecosystems, which warrants further attention to climate change impacts on upland river systems.
Our findings underscore the urgency of integrating climate-fluvial feedback into sustainable development strategies for this vulnerable region."
ScienceAdviser