TY - JOUR
T1 - Satellites reveal hotspots of global river extent change
AU - Wu, Qianhan
AU - Ke, Linghong
AU - Wang, Jida
AU - Pavelsky, Tamlin M.
AU - Allen, George H.
AU - Sheng, Yongwei
AU - Duan, Xuejun
AU - Zhu, Yunqiang
AU - Wu, Jin
AU - Wang, Lei
AU - Liu, Kai
AU - Chen, Tan
AU - Zhang, Wensong
AU - Fan, Chenyu
AU - Yong, Bin
AU - Song, Chunqiao
N1 - Funding Information:
We acknowledge the use of discharge gauging data from the World Meteorological Organization Global Runoff Data Center (GRDC) and the Ministry of Water Resources of China. This study was supported by the National Key R&D Program of China (Grant No. 2018YFD1100101, 2018YFD0900804, 2018YFA0605402, 2022YFF0711603), the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA23100102, XDA28020503), the Science and Technology Planning Project of NIGLAS (Grant No. 2022NIGLAS-CJH04, 2022NIGLAS-TJ18), the Second Tibetan Plateau Scientific Expedition and Research (STEP) (Grant No. 2019QZKK0202), and the National Natural Science Foundation of China (Grant No. 41901374; Grant No. 41971403; Grant No. 31922090). The authors would like to thank three anonymous reviewers for their constructive suggestions and comments that helped improve the manuscript.
Funding Information:
We acknowledge the use of discharge gauging data from the World Meteorological Organization Global Runoff Data Center (GRDC) and the Ministry of Water Resources of China. This study was supported by the National Key R&D Program of China (Grant No. 2018YFD1100101, 2018YFD0900804, 2018YFA0605402, 2022YFF0711603), the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA23100102, XDA28020503), the Science and Technology Planning Project of NIGLAS (Grant No. 2022NIGLAS-CJH04, 2022NIGLAS-TJ18), the Second Tibetan Plateau Scientific Expedition and Research (STEP) (Grant No. 2019QZKK0202), and the National Natural Science Foundation of China (Grant No. 41901374; Grant No. 41971403; Grant No. 31922090). The authors would like to thank three anonymous reviewers for their constructive suggestions and comments that helped improve the manuscript.
Publisher Copyright:
© 2023, The Author(s).
PY - 2023/12
Y1 - 2023/12
N2 - Rivers are among the most diverse, dynamic, and productive ecosystems on Earth. River flow regimes are constantly changing, but characterizing and understanding such changes have been challenging from a long-term and global perspective. By analyzing water extent variations observed from four-decade Landsat imagery, we here provide a global attribution of the recent changes in river regime to morphological dynamics (e.g., channel shifting and anabranching), expansion induced by new dams, and hydrological signals of widening and narrowing. Morphological dynamics prevailed in ~20% of the global river area. Booming reservoir constructions, mostly skewed in Asia and South America, contributed to ~32% of the river widening. The remaining hydrological signals were characterized by contrasting hotspots, including prominent river widening in alpine and pan-Arctic regions and narrowing in the arid/semi-arid continental interiors, driven by varying trends in climate forcing, cryospheric response to warming, and human water management. Our findings suggest that the recent river extent dynamics diverge based on hydroclimate and socio-economic conditions, and besides reflecting ongoing morphodynamical processes, river extent changes show close connections with external forcings, including climate change and anthropogenic interference.
AB - Rivers are among the most diverse, dynamic, and productive ecosystems on Earth. River flow regimes are constantly changing, but characterizing and understanding such changes have been challenging from a long-term and global perspective. By analyzing water extent variations observed from four-decade Landsat imagery, we here provide a global attribution of the recent changes in river regime to morphological dynamics (e.g., channel shifting and anabranching), expansion induced by new dams, and hydrological signals of widening and narrowing. Morphological dynamics prevailed in ~20% of the global river area. Booming reservoir constructions, mostly skewed in Asia and South America, contributed to ~32% of the river widening. The remaining hydrological signals were characterized by contrasting hotspots, including prominent river widening in alpine and pan-Arctic regions and narrowing in the arid/semi-arid continental interiors, driven by varying trends in climate forcing, cryospheric response to warming, and human water management. Our findings suggest that the recent river extent dynamics diverge based on hydroclimate and socio-economic conditions, and besides reflecting ongoing morphodynamical processes, river extent changes show close connections with external forcings, including climate change and anthropogenic interference.
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U2 - 10.1038/s41467-023-37061-3
DO - 10.1038/s41467-023-37061-3
M3 - Article
C2 - 36949069
AN - SCOPUS:85150795764
SN - 2041-1723
VL - 14
JO - Nature communications
JF - Nature communications
IS - 1
M1 - 1587
ER -