Eddy covariance measurements of carbon exchange and latent and sensible heat fluxes over a boreal lake for a full open‐water period
Timo Vesala,Jussi Huotari,Üllar Rannik,Tanja Suni,Sampo Smolander,A. Sogachev,Samuli Launiainen,Anne Ojala +7 more
TLDR
In this paper, the authors applied the statistical criteria for CO2 concentration and vertical wind speed, averaging over a 5min period and selecting only the wind direction with longest fetch, to obtain lake-representative CO2 fluxes.Abstract:
was >0 W/m 2 at night and <0 W/m 2 in daytime. The latent heat flux dominated clearly over H in spring and summer; that is, the Bowen ratio was less than 1. Highermoment turbulence statistics proved to be efficient in detection of frequent nonstationary situations. Applying the statistical criteria for CO2 concentration and vertical wind speed, averaging over a 5-min period and selecting only the wind direction with longest fetch, we could obtain lake-representative CO2 fluxes. Footprint analysis based on a closure model revealed that the source areas were relatively short because of the presence of turbulence generated by the surrounding forest, compared to a larger lake with an extended smooth surface. We observed a net CO2 source of 0.2–0.4 mmol m � 2 s � 1 excluding July, when the flux was closer to zero. The results are consistent with the gradient method, based on more infrequent sampling, and both methods gave the same average flux, 0.2 mmol m � 2 s � 1 , over the whole open-water period.read more
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Reviews and syntheses: Effects of permafrost thaw on Arctic aquatic ecosystems
Jorien E. Vonk,Suzanne E. Tank,William B. Bowden,Isabelle Laurion,Warwick F. Vincent,Pavel Alekseychik,Marc Amyot,M. F. Billet,João Canário,Rose M. Cory,Bethany Deshpande,Manuel Helbig,M. Jammet,Jan Karlsson,Julia R. Larouche,Gwyneth A. MacMillan,Milla Rautio,K. M. Walter Anthony,Kimberly P. Wickland +18 more
TL;DR: In this article, the effects of permafrost thaw on lakes and streams in the Arctic were explored, where the authors explored the effect of both thermokarst (thawing and collapse of ice-rich permaculture) and deepening of the active layer (the surface soil layer that thaws and refreezes each year).
Journal ArticleDOI
An improved lake model for climate simulations: Model structure, evaluation, and sensitivity analyses in CESM1
TL;DR: Subin et al. as mentioned in this paper developed the Lake, Ice, Snow, and Sediment Simulator (LISSS) for inclusion in the land-surface component (CLM4) of an earth system model (CESM1).
Journal ArticleDOI
Evasion of CO2 from streams - the dominant component of the carbon export through the aquatic conduit in a boreal landscape.
Marcus B. Wallin,Marcus B. Wallin,Thomas Grabs,Ishi Buffam,Hjalmar Laudon,Anneli Ågren,Mats G. Öquist,Kevin Bishop,Kevin Bishop +8 more
TL;DR: It is shown that evasion of C is greater than all the total dissolved C exported downstream in the waters of a boreal landscape as it more than doubled the magnitude of the aquatic conduit for C from this landscape.
Journal ArticleDOI
Long-term energy flux measurements and energy balance over a small boreal lake using eddy covariance technique
Annika Nordbo,Samuli Launiainen,Ivan Mammarella,Matti Leppäranta,Jussi Huotari,Anne Ojala,Timo Vesala +6 more
TL;DR: In this article, the energy balance of a small boreal lake (area 0.041 km2, mean depth 2.5 m) in southern Finland was measured during four open water periods (April-October) in 2005-2008.
Journal ArticleDOI
Annual cycle of methane emission from a subarctic peatland
Marcin Jackowicz-Korczynski,Torben R. Christensen,Kristina Bäckstrand,Patrick M. Crill,Thomas Friborg,Mikhail Mastepanov,Lena Ström +6 more
TL;DR: Although much attention in recent years has been devoted to methane (CH4) emissions from northern wetlands, measurement based data sets providing full annual budgets are still limited in number as mentioned in this paper, which is a problem.
References
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