Distinct concentration‐discharge dynamics in temperate streams and rivers: CO 2 exhibits chemostasis while CH 4 exhibits source limitation due to temperature control-Reference-Cited by-同舟云学术

Distinct concentration‐discharge dynamics in temperate streams and rivers: CO 2 exhibits chemostasis while CH 4 exhibits source limitation due to temperature control

Published:2021-08-16 Issue:10 Volume:66 Page:3656-3668
ISSN:0024-3590
Container-title:Limnology and Oceanography
language:en
Short-container-title:Limnol Oceanogr

Author:

Aho Kelly S.¹^ORCID,Fair Jennifer H.¹^ORCID,Hosen Jacob D.¹²^ORCID,Kyzivat Ethan D.¹³⁴^ORCID,Logozzo Laura A.¹^ORCID,Rocher‐Ros Gerard⁵^ORCID,Weber Lisa C.¹,Yoon Byungman¹⁶^ORCID,Raymond Peter A.¹^ORCID

Affiliation:

1. School of the Environment Yale University New Haven Connecticut USA

2. Department of Forestry and Natural Resources Purdue University West Lafayette Indiana USA

3. Department of Earth, Environmental and Planetary Sciences Brown University Providence Rhode Island USA

4. Institute at Brown for Environment and Society Brown University Providence Rhode Island USA

5. Climate Impacts Research Centre (CIRC), Department of Ecology and Environmental Science Umeå University Umeå Sweden

6. Departments of Marine and Environmental Sciences, Chemistry and Chemical Biology, and Civil and Environmental Engineering Northeastern University Boston Massachusetts USA

Funder

Institute for Biospheric Studies, Yale University

National Aeronautics and Space Administration

National Science Foundation

Publisher

Wiley

Subject

Aquatic Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11906

Reference63 articles.

1. Aho K. and others.2021a.Dissolved CO2and CH4concentrations in the Connecticut River Watershed ver 1. Environmental Data Initiative. Available fromhttps://doi.org/10.6073/pasta/af4daec813775b7f426a1db574cbebc7. Accessed 9 August 2021.

2. Differential Response of Greenhouse Gas Evasion to Storms in Forested and Wetland Streams

3. Highest rates of gross primary productivity maintained despite CO 2 depletion in a temperate river network

4. Riverine coupling of biogeochemical cycles between land, oceans, and atmosphere

5. Riverine Export of Aged Carbon Driven by Flow Path Depth and Residence Time

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