A catchment-scale carbon and greenhouse gas budget of a subarctic landscape

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Standard

A catchment-scale carbon and greenhouse gas budget of a subarctic landscape. / Christensen, Torben R.; Johansson, Paul Torbjörn; Olsrud, Maria; Ström, Lena; Lindroth, Anders; Mastepanov, Makhail; Malmer, N.; Friborg, Thomas; Crill, Patrick; Callaghan, Terry.

I: Philosophical Transactions of the Royal Society, Series A, Bind 365, Nr. 1856, 2007, s. 1643-1656.

Publikation: Bidrag til tidsskriftTidsskriftartikelForskningfagfællebedømt

Harvard

Christensen, TR, Johansson, PT, Olsrud, M, Ström, L, Lindroth, A, Mastepanov, M, Malmer, N, Friborg, T, Crill, P & Callaghan, T 2007, 'A catchment-scale carbon and greenhouse gas budget of a subarctic landscape', Philosophical Transactions of the Royal Society, Series A, bind 365, nr. 1856, s. 1643-1656. https://doi.org/10.1098/rsta.2007.2035

APA

Christensen, T. R., Johansson, P. T., Olsrud, M., Ström, L., Lindroth, A., Mastepanov, M., Malmer, N., Friborg, T., Crill, P., & Callaghan, T. (2007). A catchment-scale carbon and greenhouse gas budget of a subarctic landscape. Philosophical Transactions of the Royal Society, Series A, 365(1856), 1643-1656. https://doi.org/10.1098/rsta.2007.2035

Vancouver

Christensen TR, Johansson PT, Olsrud M, Ström L, Lindroth A, Mastepanov M o.a. A catchment-scale carbon and greenhouse gas budget of a subarctic landscape. Philosophical Transactions of the Royal Society, Series A. 2007;365(1856):1643-1656. https://doi.org/10.1098/rsta.2007.2035

Author

Christensen, Torben R. ; Johansson, Paul Torbjörn ; Olsrud, Maria ; Ström, Lena ; Lindroth, Anders ; Mastepanov, Makhail ; Malmer, N. ; Friborg, Thomas ; Crill, Patrick ; Callaghan, Terry. / A catchment-scale carbon and greenhouse gas budget of a subarctic landscape. I: Philosophical Transactions of the Royal Society, Series A. 2007 ; Bind 365, Nr. 1856. s. 1643-1656.

Bibtex

@article{845147e0c81511dcbee902004c4f4f50,
title = "A catchment-scale carbon and greenhouse gas budget of a subarctic landscape",
abstract = "This is the first attempt to budget average current annual carbon (C) and associated greenhouse gas (GHG) exchanges and transfers in a subarctic landscape, the Lake Tornetr{\"a}sk catchment in northern Sweden. This is a heterogeneous area consisting of almost 4000km2 of mixed heath, birch and pine forest, and mires, lakes and alpine ecosystems. The magnitudes of atmospheric exchange of carbon in the form of the GHGs, CO2 and CH4 in these various ecosystems differ significantly, ranging from little or no flux in barren ecosystems over a small CO2 sink function and low rates of CH4 exchange in the heaths to significant CO2 uptake in the forests and also large emissions of CH4 from the mires and small lakes. The overall catchment budget, given the size distribution of the individual ecosystem types and a first approximation of run-off as dissolved organic carbon, reveals a landscape currently with a significant sink capacity for atmospheric CO2. This sink capacity is, however, extremely sensitive to environmental changes, particularly those that affect the birch forest ecosystem. Climatic drying or wetting and episodic events such as insect outbreaks may cause significant changes in the sink function. Changes in the sources of CH4 through increased permafrost melting may also easily change the sign of the current radiative forcing, due to the stronger impact per gram of CH4 relative to CO2. Hence, to access impacts on climate, the atmospheric C balance alone has to be weighed in a radiative forcing perspective. When considering the emissions of CH4 from the mires and lakes as CO2 equivalents, the Tornetr{\"a}sk catchment is currently a smaller sink of radiative forcing, but it can still be estimated as representing the equivalent of approximately 14000 average Swedish inhabitants' emissions of CO2. This can be compared with the carbon emissions of less than 200 people who live permanently in the catchment, although this comparison disregards substantial emissions from the non-Swedish tourism and transportation activities.",
author = "Christensen, {Torben R.} and Johansson, {Paul Torbj{\"o}rn} and Maria Olsrud and Lena Str{\"o}m and Anders Lindroth and Makhail Mastepanov and N. Malmer and Thomas Friborg and Patrick Crill and Terry Callaghan",
year = "2007",
doi = "10.1098/rsta.2007.2035",
language = "English",
volume = "365",
pages = "1643--1656",
journal = "Philosophical Transactions of the Royal Society, Series A",
publisher = "Royal Society",
number = "1856",

}

RIS

TY - JOUR

T1 - A catchment-scale carbon and greenhouse gas budget of a subarctic landscape

AU - Christensen, Torben R.

AU - Johansson, Paul Torbjörn

AU - Olsrud, Maria

AU - Ström, Lena

AU - Lindroth, Anders

AU - Mastepanov, Makhail

AU - Malmer, N.

AU - Friborg, Thomas

AU - Crill, Patrick

AU - Callaghan, Terry

PY - 2007

Y1 - 2007

N2 - This is the first attempt to budget average current annual carbon (C) and associated greenhouse gas (GHG) exchanges and transfers in a subarctic landscape, the Lake Torneträsk catchment in northern Sweden. This is a heterogeneous area consisting of almost 4000km2 of mixed heath, birch and pine forest, and mires, lakes and alpine ecosystems. The magnitudes of atmospheric exchange of carbon in the form of the GHGs, CO2 and CH4 in these various ecosystems differ significantly, ranging from little or no flux in barren ecosystems over a small CO2 sink function and low rates of CH4 exchange in the heaths to significant CO2 uptake in the forests and also large emissions of CH4 from the mires and small lakes. The overall catchment budget, given the size distribution of the individual ecosystem types and a first approximation of run-off as dissolved organic carbon, reveals a landscape currently with a significant sink capacity for atmospheric CO2. This sink capacity is, however, extremely sensitive to environmental changes, particularly those that affect the birch forest ecosystem. Climatic drying or wetting and episodic events such as insect outbreaks may cause significant changes in the sink function. Changes in the sources of CH4 through increased permafrost melting may also easily change the sign of the current radiative forcing, due to the stronger impact per gram of CH4 relative to CO2. Hence, to access impacts on climate, the atmospheric C balance alone has to be weighed in a radiative forcing perspective. When considering the emissions of CH4 from the mires and lakes as CO2 equivalents, the Torneträsk catchment is currently a smaller sink of radiative forcing, but it can still be estimated as representing the equivalent of approximately 14000 average Swedish inhabitants' emissions of CO2. This can be compared with the carbon emissions of less than 200 people who live permanently in the catchment, although this comparison disregards substantial emissions from the non-Swedish tourism and transportation activities.

AB - This is the first attempt to budget average current annual carbon (C) and associated greenhouse gas (GHG) exchanges and transfers in a subarctic landscape, the Lake Torneträsk catchment in northern Sweden. This is a heterogeneous area consisting of almost 4000km2 of mixed heath, birch and pine forest, and mires, lakes and alpine ecosystems. The magnitudes of atmospheric exchange of carbon in the form of the GHGs, CO2 and CH4 in these various ecosystems differ significantly, ranging from little or no flux in barren ecosystems over a small CO2 sink function and low rates of CH4 exchange in the heaths to significant CO2 uptake in the forests and also large emissions of CH4 from the mires and small lakes. The overall catchment budget, given the size distribution of the individual ecosystem types and a first approximation of run-off as dissolved organic carbon, reveals a landscape currently with a significant sink capacity for atmospheric CO2. This sink capacity is, however, extremely sensitive to environmental changes, particularly those that affect the birch forest ecosystem. Climatic drying or wetting and episodic events such as insect outbreaks may cause significant changes in the sink function. Changes in the sources of CH4 through increased permafrost melting may also easily change the sign of the current radiative forcing, due to the stronger impact per gram of CH4 relative to CO2. Hence, to access impacts on climate, the atmospheric C balance alone has to be weighed in a radiative forcing perspective. When considering the emissions of CH4 from the mires and lakes as CO2 equivalents, the Torneträsk catchment is currently a smaller sink of radiative forcing, but it can still be estimated as representing the equivalent of approximately 14000 average Swedish inhabitants' emissions of CO2. This can be compared with the carbon emissions of less than 200 people who live permanently in the catchment, although this comparison disregards substantial emissions from the non-Swedish tourism and transportation activities.

U2 - 10.1098/rsta.2007.2035

DO - 10.1098/rsta.2007.2035

M3 - Journal article

C2 - 17513266

VL - 365

SP - 1643

EP - 1656

JO - Philosophical Transactions of the Royal Society, Series A

JF - Philosophical Transactions of the Royal Society, Series A

IS - 1856

ER -

ID: 2385935