Diel variation in CO2 flux is substantial in many lakes

Elvira de Eyto, Robyn L. Smyth, Rachel M. Pilla, Alo Laas, Amir Reza Shahabinia, Angela Baldocchi, Ankur R. Desai, Anna Lupon, Annalea Lohila, Biel Obrador, Blaize A. Denfeld, Cayelan C. Carey, David Bastviken, David Reed, David Rudberg, Eva‐Ingrid Rõõm, Francois Clayer, Gesa A. Weyhenmeyer, Hannah E. Chmiel, Hans Peter GrossartHeleen A. de Wit, Ilga Kokorite, Jan‐Erik Thrane, Jānis Bikše, James A. Rusak, Jorge Encinas Fernández, José Fernandes Bezerra‐Neto, Ludmila S. Brighenti, Matthias Koschorreck, Mika Aurela, Nathan Barros, Philipp S. Keller, R. Iestyn Woolway, Rafael Marcé, Ryan P. McClure, Samuel Haverinen, Sari Juutinen, Sarian Kosten, Steve Sadro, Brian C. Doyle

Research output: Contribution to journalLetterpeer-review

10 Downloads (Pure)

Abstract

Lakes play a significant role in the global carbon cycle, acting as sources and sinks of carbon dioxide (CO2). In situ measurements of CO2 flux (FCO2) from lakes have generally been collected during daylight, despite indications of significant diel variability. This introduces bias when scaling up to whole‐lake annual aquatic carbon budgets. We conducted an international sampling program to ascertain the extent of diel variation in FCO2 across lakes. We sampled 21 lakes over 41 campaigns and measured FCO2 at 4‐h intervals over a full diel cycle. Rates of FCO2 ranged from −3.16 to 4.39 mmol m−2 h−1. Integrated over a day, FCO2 ranged from −381.68 to 878.49 mg C m−2 d−1 (mean = 76.54) across campaigns. We identified three characteristic diel patterns in FCO2 related to trophic status and show that for half of the campaigns, daily flux estimates were biased by > 50% if based on a single (daytime) measurement.
Original languageEnglish
JournalLimnology and Oceanography Letters
Early online date19 Sept 2025
DOIs
Publication statusE-pub ahead of print - 19 Sept 2025

Fingerprint

Dive into the research topics of 'Diel variation in CO2 flux is substantial in many lakes'. Together they form a unique fingerprint.

Cite this