On the relationship between water table depth and water vapor and carbon dioxide fluxes in a minerotrophic fen

2009 ◽  
Vol 16 (6) ◽  
pp. 1762-1776 ◽  
Author(s):  
O. SONNENTAG ◽  
G. Van Der KAMP ◽  
A. G. BARR ◽  
J. M. CHEN
2017 ◽  
Vol 9 (6) ◽  
pp. 965-980
Author(s):  
N. V. Belotelov ◽  
Tamara G. Apal’kova ◽  
Vadim V. Mamkin ◽  
Yulia A. Kurbatova ◽  
A. V. Olchev

2018 ◽  
Vol 32 (7) ◽  
pp. 1087-1106 ◽  
Author(s):  
Janne Rinne ◽  
Eeva-Stiina Tuittila ◽  
Olli Peltola ◽  
Xuefei Li ◽  
Maarit Raivonen ◽  
...  

2021 ◽  
Vol 132 ◽  
pp. 108320
Author(s):  
Ciara Dwyer ◽  
Jonathan Millett ◽  
Robin J. Pakeman ◽  
Laurence Jones

2009 ◽  
Vol 6 (6) ◽  
pp. 1115-1126 ◽  
Author(s):  
B. N. Sulman ◽  
A. R. Desai ◽  
B. D. Cook ◽  
N. Saliendra ◽  
D. S. Mackay

Abstract. Wetland biogeochemistry is strongly influenced by water and temperature dynamics, and these interactions are currently poorly represented in ecosystem and climate models. A decline in water table of approximately 30 cm was observed at a wetland in Northern Wisconsin, USA over a period from 2001–2007, which was highly correlated with an increase in daily soil temperature variability. Eddy covariance measurements of carbon dioxide exchange were compared with measured CO2 fluxes at two nearby forests in order to distinguish wetland effects from regional trends. As wetland water table declined, both ecosystem respiration and ecosystem production increased by over 20% at the wetland, while forest CO2 fluxes had no significant trends. Net ecosystem exchange of carbon dioxide at the wetland was not correlated with water table, but wetland evapotranspiration decreased substantially as the water table declined. These results suggest that changes in hydrology may not have a large impact on shrub wetland carbon balance over inter-annual time scales due to opposing responses in both ecosystem respiration and productivity.


2005 ◽  
Vol 6 (6) ◽  
pp. 954-960 ◽  
Author(s):  
J. H. Prueger ◽  
J. L. Hatfield ◽  
T. B. Parkin ◽  
W. P. Kustas ◽  
L. E. Hipps ◽  
...  

Abstract A network of eddy covariance (EC) and micrometeorological flux (METFLUX) stations over corn (Zea mays L.) and soybean [Glycine max (L.) Merr.] canopies was established as part of the Soil Moisture–Atmosphere Coupling Experiment (SMACEX) in central Iowa during the summer of 2002 to measure fluxes of heat, water vapor, and carbon dioxide (CO2) during the growing season. Additionally, EC measurements of water vapor and CO2 fluxes from an aircraft platform complemented the tower-based measurements. Sensible heat, water vapor, and CO2 fluxes showed the greatest spatial and temporal variability during the early crop growth stage. Differences in all of the energy balance components were detectable between corn and soybean as well as within similar crops throughout the study period. Tower network–averaged fluxes of sensible heat, water vapor, and CO2 were observed to be in good agreement with area-averaged aircraft flux measurements.


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