Applicability and consequences of the integration of alternative models for CO<sub>2</sub> transfer velocity into a process-based lake model
-
Published:2019-09-04
Issue:17
Volume:16
Page:3297-3317
-
ISSN:1726-4189
-
Container-title:Biogeosciences
-
language:en
-
Short-container-title:Biogeosciences
Author:
Kiuru PetriORCID, Ojala Anne, Mammarella Ivan, Heiskanen Jouni, Erkkilä Kukka-MaariaORCID, Miettinen HeliORCID, Vesala Timo, Huttula Timo
Abstract
Abstract. Freshwater lakes are important in carbon cycling, especially in the boreal zone where many lakes are supersaturated with the greenhouse gas carbon dioxide (CO2) and emit it to the atmosphere, thus ventilating carbon originally fixed by the terrestrial system. The exchange of CO2 between water and the atmosphere is commonly estimated using simple wind-based parameterizations or models of gas transfer velocity (k). More complex surface renewal models, however, have been shown to yield more correct estimates of k in comparison with direct CO2 flux measurements. We incorporated four gas exchange models with different complexity into a vertical process-based physico-biochemical lake model, MyLake C, and assessed the performance and applicability of the alternative lake model versions to simulate air–water CO2 fluxes over a small boreal lake. None of the incorporated gas exchange models significantly outperformed the other models in the simulations in comparison to the measured near-surface CO2 concentrations or respective air–water CO2 fluxes calculated directly with the gas exchange models using measurement data as input. The use of more complex gas exchange models in the simulation, on the contrary, led to difficulties in obtaining a sufficient gain of CO2 in the water column and thus resulted in lower CO2 fluxes and water column CO2 concentrations compared to the respective measurement-based values. The inclusion of sophisticated and more correct models for air–water CO2 exchange in process-based lake models is crucial in efforts to properly assess lacustrine carbon budgets through model simulations in both single lakes and on a larger scale. However, finding higher estimates for both the internal and external sources of inorganic carbon in boreal lakes is important if improved knowledge of the magnitude of CO2 evasion from lakes is included in future studies on lake carbon budgets.
Funder
Koneen Säätiö European Commission Academy of Finland
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
Reference65 articles.
1. Air-Sea: Air-Sea Toolbox by Rich Pawlowicz and Bob Bearsley, available
at: https://sea-mat.github.io/sea-mat (last access: 27 February 2019),
1999. a 2. Algesten, G., Sobek, S., Bergström, A.-K., Ågren, A., Tranvik, L. J.,
and Jansson, M.: Role of lakes for organic carbon cycling in the boreal zone,
Glob. Change Biol., 10, 141–147, https://doi.org/10.1111/j.1365-2486.2003.00721.x,
2014. a 3. Bade, D. L., Carpenter, S. R., Cole, J. J., Hanson, P. C., and Hesslein, R. H.:
Controls of δ13C-DIC in lakes: Geochemistry, lake metabolism, and
morphometry, Limnol. Oceanogr., 49, 1160–1172,
https://doi.org/10.4319/lo.2004.49.4.1160, 2004. a 4. Banerjee, S.: The Air-Water Interface: Turbulence and Scalar Exchange, in:
Transport at the Air-Sea Interface: Measurements, Models and
Parametrizations, edited by: Garbe, C. S., Handler, R. A., and Jähne, B.,
87–101, Springer, Berlin, Heidelberg, 2007. a 5. Battin, T. J., Luyssaert, S., Kaplan, L. A., Aufdenkampe, A. K., Richter, A.,
and Tranvik, L. J.: The boundless carbon cycle, Nat. Geosci., 2, 598–600,
https://doi.org/10.1038/ngeo618, 2009. a, b
Cited by
6 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|