Geochemistry of west Siberian streams and their potential response to permafrost degradation
[1] Measurements of solute concentrations from previously unstudied watersheds throughout west Siberia suggest that warming and permafrost degradation will likely amplify the transport of dissolved solids to the Kara Sea and adjacent Arctic Ocean. We present concentrations of Ca2+, K+, Mg2+, Na+, Si...
Published in: | Water Resources Research |
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Main Authors: | , , |
Format: | Text |
Language: | unknown |
Published: |
Clark Digital Commons
2007
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Subjects: | |
Online Access: | https://commons.clarku.edu/faculty_geography/247 https://doi.org/10.1029/2006WR004902 https://commons.clarku.edu/context/faculty_geography/article/1246/viewcontent/GeogFacWorks_Frey_Geochemistry_2007.pdf |