Higher temperatures along with moister climates generally increase the rate of

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Higher temperatures and moister climates accelerate both biological and chemical weathering processes. Biological weathering is enhanced as warmer and wetter conditions promote the growth of organisms that break down rocks, while chemical weathering reactions occur more rapidly under the same conditions. Mechanical weathering, however, is more influenced by physical processes such as freeze-thaw cycles and does not directly depend on temperature and moisture in the same way.

Higher Temperatures Along with Moister Climates Generally Increase the Rate