Construct · 1 fields · 1 citations

silicate weathering feedback: a standalone construct

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Geochemistry

the long-term stabilization of climate as warmer conditions speed silicate rock weathering, which draws down carbon dioxide.

In geochemistry, silicate weathering feedback refers to the long-term stabilization of climate as warmer conditions speed silicate rock weathering, which draws down carbon dioxide. This meaning comes from Walker (1981) in Journal of Geophysical Research: Oceans.[1]

Unit
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Nearby constructs

climate3 fields · 3 citationsjingle · one word, three constructs feedback4 fields · 5 citationsjingle · one word, four constructs weathering3 fields · 4 citationsjingle · one word, three constructs

References

Walker, J. C. G., Hays, P. B., & Kasting, J. F. (1981). A negative feedback mechanism for the long‐term stabilization of Earth's surface temperature. Journal of Geophysical Research: Oceans, 86(C10), 9776-9782. https://doi.org/10.1029/jc086ic10p09776

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