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Sökning: onr:"swepub:oai:lup.lub.lu.se:9929872a-8b6d-4df4-b359-3b3977809b89" > Variations in net e...

Variations in net ecosystem exchange of carbon dioxide in a boreal mire: Modeling mechanisms linked to water table position

Yurova, Alla (författare)
Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science,Lund Univ, Dept Phys Geog & Ecosyst Anal, Solvegatan 12, SE-22362 Lund, Sweden.,Lund University, Sweden
Wolf, Annett (författare)
Umeå universitet,Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science,Lund Univ, Dept Phys Geog & Ecosyst Anal, Solvegatan 12, SE-22362 Lund, Sweden.,Lund University, Sweden
Sagerfors, Jorgen (författare)
Swedish University of Agricultural Sciences, Sweden
visa fler...
Nilsson, Mats (författare)
Swedish University of Agricultural Sciences, Sweden
visa färre...
 (creator_code:org_t)
John Wiley & Sons, 2007
2007
Engelska.
Ingår i: Journal of Geophysical Research. - : John Wiley & Sons. - 2156-2202 .- 0148-0227. ; 112:G2
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • [1] In mires, which occupy large areas of the boreal region, net ecosystem CO2 exchange ( NEE) rates vary significantly over various timescales. In order to examine the effect of one of the most influencing variables, the water table depth, on NEE the general ecosystem model GUESS-ROMUL was modified to predict mire daily CO2 exchange rates. A simulation was conducted for a lawn, the most common microtopographical feature of boreal oligotrophic minerotrophic mires. The results were validated against eddy covariance CO2 flux measurements from Degero Stormyr, northern Sweden, obtained during the period 2001 - 2003. Both measurements and model simulations revealed that CO2 uptake was clearly controlled by interactions between water table depth and temperature. Maximum uptake occurred when the water table level was between 10 and 20 cm and the air temperature was above 15 degrees C. When the water table was higher, the CO2 uptake rate was lower, owing to reduced rates of photosynthetic carbon fixation. When the water table was lower, NEE decreased owing to the increased rate of decomposition of organic matter. When the water table level was between 10 and 20 cm, the NEE was quite stable and relatively insensitive to both changes within this range and any air temperature changes above + 15 degrees C. The optimal water table level range for NEE corresponds to that characteristic of mire lawn plant communities, indicating that the annual NEE will not change dramatically if climatic conditions remain within the optimal range for the current plant community.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Nyckelord

model
GUESS-ROMUL.
boreal mire
water table depth
NEE
Ecology

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