Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China
Institute of Carbon Neutrality, Peking University, Beijing, 100871, China
Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China
Institute of Carbon Neutrality, Peking University, Beijing, 100871, China
Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China
Institute of Carbon Neutrality, Peking University, Beijing, 100871, China
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Total article views: 1,811 (including HTML, PDF, and XML)
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1,447
316
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397
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Total article views: 2,632 (including HTML, PDF, and XML)
Thereof 2,577 with geography defined
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Total article views: 1,811 (including HTML, PDF, and XML)
Thereof 1,778 with geography defined
and 33 with unknown origin.
Total article views: 821 (including HTML, PDF, and XML)
Thereof 799 with geography defined
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Compared to the silicate weathering fluxes measured at large river basins, the current models tend to systematically overestimate the fluxes over the tropical region, which leads to an overestimation of the global total weathering flux. The most possible cause of such bias is found to be the overestimation of tropical surface erosion, which indicates that the tropical vegetation likely slows down physical erosion significantly. We propose a way of taking this effect into account in models.
Compared to the silicate weathering fluxes measured at large river basins, the current models...
