@article {33424,
	title = {Warming-driven erosion and sediment transport in cold regions},
	journal = {Nature Reviews Earth \&amp; Environment},
	volume = {3},
	year = {2022},
	month = {2022-11-01},
	pages = {832{\textendash}851},
	abstract = {Rapid atmospheric warming since the mid-twentieth century has increased temperature-dependent erosion and sediment-transport processes in cold environments, affecting food, energy and water security. In this Review, we summarize landscape changes in cold environments and provide a global inventory of increases in erosion and sediment yield driven by cryosphere degradation. Anthropogenic climate change, deglaciation, and thermokarst disturbances are causing increased sediment mobilization and transport processes in glacierized and periglacierized basins. With continuous cryosphere degradation, sediment transport will continue to increase until reaching a maximum (peak sediment). Thereafter, transport is likely to shift from a temperature-dependent regime toward a rainfall-dependent regime roughly between 2100{\textendash}2200. The timing of the regime shift would be regulated by changes in meltwater, erosive rainfall and landscape erodibility, and complicated by geomorphic feedbacks and connectivity. Further progress in integrating multisource sediment observations, developing physics-based sediment-transport models, and enhancing interdisciplinary and international scientific collaboration is needed to predict sediment dynamics in a warming world.},
	isbn = {2662-138X},
	url = {https://doi.org/10.1038/s43017-022-00362-0},
	author = {Ting Zhang and Li, Dongfeng and East, Amy E. and Walling, Desmond E. and Lane, Stuart and Overeem, Irina and Beylich, Achim A. and Koppes, Mich{\`e}le and Lu, Xixi}
}
