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Thermal enhancement of gas transfer velocity of CO 2 in an Amazon floodplain lake revealed by eddy covariance measurements
Author(s) -
Polsenaere Pierre,
Deborde Jonathan,
Detandt Guillaume,
Vidal Luciana O.,
Pérez Marcela A. P.,
Marieu Vincent,
Abril Gwenaël
Publication year - 2013
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/grl.50291
Subject(s) - eddy covariance , wind speed , environmental science , sensible heat , atmospheric sciences , floodplain , amazon rainforest , carbon dioxide , latent heat , hydrology (agriculture) , meteorology , geology , physics , ecosystem , geography , chemistry , biology , ecology , cartography , geotechnical engineering , organic chemistry
In November 2011, the partial pressures of carbon dioxide (pCO 2 ) in water and air in a floodplain lake of the Amazon River in Brazil were 800 ± 75 and 387 ± 8 ppmv, respectively. Turbulent CO 2 fluxes from the lake measured with eddy covariance ranged from 0.05 to 2.2 µmol m −2 s −1 . The corresponding gas transfer velocities k 600 ranged from 1.3 to 31.6 cm h −1 , averaging 12.2 ± 6.7 cm h −1 . At moderate to high wind speed, k 600 increased with wind speed, with values above parameterizations for other lake ecosystems. During the prevailing tropical low wind speed (below 2.7 m s −1 ) and high insolation conditions, unexpected high k 600 values (up to 20 cm h −1 ) were obtained and correlated with latent heat and sensible heat fluxes. In Amazonian open lakes, owing to long quiescent periods of low wind speed but extremely high daytime insolation and heat fluxes, thermal enhancement makes time‐integrated gas transfer velocities four to five times higher than those computed from classic wind parameterization.