Cimate-Chemical Weathering
Authors: | |
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Owners: | Salvatore Calabrese |
Type: | Resource |
Storage: | The size of this resource is 22.7 KB |
Created: | Jun 19, 2020 at 4:12 p.m. |
Last updated: | Jun 22, 2020 at 7:34 p.m. (Metadata update) |
Published date: | Jun 22, 2020 at 7:34 p.m. |
DOI: | 10.4211/hs.94feed861b184722846363bd28b7306d |
Citation: | See how to cite this resource |
Sharing Status: | Published |
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Views: | 1466 |
Downloads: | 30 |
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Abstract
This dataset contains measurements of chemical depletion fraction (CDF), from three published articles, and estimates for each location of the dryness index (PET/P). To estimate the dryness index, long-term potential evapotranspiration (PET) was retrieved from climate data, while precipitation was provided by the three publication alongside the CDF measurements. The data reveal the strong nonlinear relation between CDF and wetness at the global scale.
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Related Resources
The content of this resource is derived from | Rasmussen, Craig, et al. "Strong climate and tectonic control on plagioclase weathering in granitic terrain." Earth and Planetary Science Letters 301.3-4 (2011): 521-530. |
The content of this resource is derived from | Dere, Ashlee L., et al. "Climate dependence of feldspar weathering in shale soils along a latitudinal gradient." Geochimica et Cosmochimica Acta 122 (2013): 101-126. |
The content of this resource is derived from | Riebe, Clifford S., James W. Kirchner, and Robert C. Finkel. "Erosional and climatic effects on long-term chemical weathering rates in granitic landscapes spanning diverse climate regimes." Earth and Planetary Science Letters 224.3-4 (2004): 547-562. |
The content of this resource is derived from | Harris, I. P. D. J., et al. "Updated high‐resolution grids of monthly climatic observations–the CRU TS3. 10 Dataset." International journal of climatology 34.3 (2014): 623-642. |
How to Cite
Calabrese, S., A. Porporato (2020). Cimate-Chemical Weathering, HydroShare, https://doi.org/10.4211/hs.94feed861b184722846363bd28b7306d
This resource is shared under the Creative Commons Attribution CC BY.
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