Basin scale controls on CO2 and CH4 emissions from the Upper Mississippi River

Geophysical Research Letters
By: , and 



The Upper Mississippi River, engineered for river navigation in the 1930s, includes a series of low-head dams and navigation pools receiving elevated sediment and nutrient loads from the mostly agricultural basin. Using high-resolution, spatially resolved water quality sensor measurements along 1385 river kilometers, we show that primary productivity and organic matter accumulation affect river carbon dioxide and methane emissions to the atmosphere. Phytoplankton drive CO2to near or below atmospheric equilibrium during the growing season, while anaerobic carbon oxidation supports a large proportion of the CO2 and CH4 production. Reductions of suspended sediment load, absent of dramatic reductions in nutrients, will likely further reduce net CO2emissions from the river. Large river pools, like Lake Pepin, which removes the majority of upstream sediments, and large agricultural tributaries downstream that deliver significant quantities of sediments and nutrients, are likely to persist as major geographical drivers of greenhouse gas emissions.

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Publication type Article
Publication Subtype Journal Article
Title Basin scale controls on CO2 and CH4 emissions from the Upper Mississippi River
Series title Geophysical Research Letters
DOI 10.1002/2015GL067599
Volume 43
Issue 5
Year Published 2016
Language English
Publisher AGU Publications
Contributing office(s) National Research Program - Central Branch
Description 7 p.
First page 1973
Last page 1979
Country United States
Other Geospatial Upper Mississippi River
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