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Peter A. Raymond

Researcher at Yale University

Publications -  180
Citations -  24244

Peter A. Raymond is an academic researcher from Yale University. The author has contributed to research in topics: Dissolved organic carbon & Carbon cycle. The author has an hindex of 65, co-authored 164 publications receiving 18177 citations. Previous affiliations of Peter A. Raymond include Marine Biological Laboratory & United States Geological Survey.

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A decrease in discharge‐normalized DOC export by the Yukon River during summer through autumn

TL;DR: In the 831,400 km2 Yukon River basin, water discharge (Q) corrected DOC export significantly decreased during the growing season from 1978-80 to 2001-03, indicating a major shift in terrestrial to aquatic C transfer as mentioned in this paper.
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Terrestrial carbon inputs to inland waters: A current synthesis of estimates and uncertainty

TL;DR: A review of flux estimates over the last decade has revealed an average increase of ∼ 0.3 Pg C yr−1, indicating a historical underestimation of the amount of terrestrial-C exported to inland waters.
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Increase in the Export of Alkalinity from North America's Largest River

TL;DR: During the past half-century, the export of carbonate alkalinity from North America's largest river, the Mississippi, has increased dramatically, in part the result of increased flow resulting from higher rainfall in the Mississippi basin.
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Lability of DOC transported by Alaskan rivers to the Arctic Ocean

TL;DR: In this article, the authors show that there is substantial seasonal variability in the lability of DOC transported by Alaskan rivers to the Arctic Ocean: little DOC is lost during incubations of samples collected during summer, but substantial losses (20-40%) occur during incubation of sample collected during the spring freshet when the majority of the annual DOC flux occurs.
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Environmental turbulent mixing controls on air-water gas exchange in marine and aquatic systems

TL;DR: In this paper, a new mechanistic model based on surface water turbulence was proposed to predict gas exchange for a range of aquatic and marine processes, showing that the gas transfer rate varies linearly with the turbulent dissipation rate to the 1/4 power.