Stream CO2 emissions are overestimated without consideration of diel water and atmospheric CO2 variability

Theresa Reichenpfader, Katrin Attermeyer (Korresp. Autor*in)

Veröffentlichungen: Beitrag in FachzeitschriftShort CommunicationPeer Reviewed

Abstract

Streams are significant emitters of carbon dioxide (CO2) to the atmosphere that are influenced by diel CO2 dynamics. However, we know little about diel CO2 variability within streams, the diel dynamics of CO2 in the air above streams, and the consequences for emission calculations. We studied five pre-alpine streams by equipping three sites per stream in close proximity (~ 1 km apart) with automatic logging stations that continuously recorded water and air CO2 partial pressures (pCO2) for 2–4 d. All streams and sites showed increased pCO2 at night and decreased pCO2 during the day, however, with fourfold higher diel amplitudes for atmospheric pCO2 compared to the water. Calculating diffusive CO2 fluxes with fixed compared to dynamic measured atmospheric CO2 resulted in negligible to 431% lower estimates. We might thus currently overestimate fluvial CO2 emissions and should include diel water and air CO2 variability to more accurately assess stream CO2 emissions.

OriginalspracheEnglisch
Seiten (von - bis)543-552
Seitenumfang10
FachzeitschriftLimnology And Oceanography Letters
Jahrgang9
Ausgabenummer5
Frühes Online-Datum16 Mai 2024
DOIs
PublikationsstatusVeröffentlicht - Okt. 2024

Fördermittel

We thank Hermann Hofbauer for his help with the construction of the automatic monitoring stations and chambers, as well as Gertraud Steniczka and Irina Ludwig for the analyses of the water samples and Leonie T. Haferkemper for the map. We are grateful to Jovan Kalem and Tabea Prestel for their help in the field. We would also like to thank Pascal Bodmer for his comments on an earlier version of this manuscript and Laura Coulson for her ideas, comments, and language editing. Open access funding provided by University of Vienna.

ÖFOS 2012

  • 106020 Limnologie
  • 105205 Klimawandel

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