Water and sediment transport from rivers to oceans play a crucial role in the global geochemical cycle. Unlike runoff, river sediment discharge is highly sensitive to variations in climate and surface processes, making it a key indicator for quantifying land degradation and the depletion of soil resources. It also serves as a significant pathway in the geochemical cycle.

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Cryospheric River Sediment

  • Jia Qin,
  • Xiangying Li

摘要

Water and sediment transport from rivers to oceans play a crucial role in the global geochemical cycle. Unlike runoff, river sediment discharge is highly sensitive to variations in climate and surface processes, making it a key indicator for quantifying land degradation and the depletion of soil resources. It also serves as a significant pathway in the geochemical cycle.