TY - JOUR
T1 - CO2 flux measurements over the sea surface by eddy correlation and aerodynamic techniques
AU - Iwata, Toru
AU - Yoshikawa, Keiko
AU - Nishimura, Katsutoshi
AU - Higuchi, Yoshihisa
AU - Yamashita, Takao
AU - Kato, Shigeru
AU - Ohtaki, Eiji
N1 - Funding Information:
We wish to express our hearty thanks to Mr. K. Uchiyama of Kyoto University for his kind help during the experiments. We are indebted to anonymous reviewers for their constructive criticism of the manuscript. This work was partly supported by the Grant-in-Aid for Scientific Research (C) (No. 13680603) of The Ministry of Education, Culture, Sports, Science and Technology.
PY - 2004/11
Y1 - 2004/11
N2 - The measurements of the vertical transport of CO2 were carried out over the Sea of Japan using the specially designed pier of Kyoto University on September 20 to 22, 2000. CO2 fluxes were measured by the eddy correlation and aerodynamic techniques. Both techniques showed comparable CO2 fluxes during sea breeze conditions: -0.001 to -0.08 mg m-2s-1 with the mean of -0.05 mg m-2s-1. This means that the measuring site satisfies the fetch requirement for meteorological observations under sea breeze conditions. Moreover, the eddy diffusivity coefficient used in the aerodynamic technique is found to be consistent with the coefficient used in the eddy correlation technique. The present result leads us to conclude that the aerodynamic technique may be applicable to underway CO2 flux measurements over the ocean and may be used in place of the bulk technique. The important point is the need to maintain a measuring accuracy of CO2 concentration difference of the order of 0.1 ppmv on the research vessels or the buoys.
AB - The measurements of the vertical transport of CO2 were carried out over the Sea of Japan using the specially designed pier of Kyoto University on September 20 to 22, 2000. CO2 fluxes were measured by the eddy correlation and aerodynamic techniques. Both techniques showed comparable CO2 fluxes during sea breeze conditions: -0.001 to -0.08 mg m-2s-1 with the mean of -0.05 mg m-2s-1. This means that the measuring site satisfies the fetch requirement for meteorological observations under sea breeze conditions. Moreover, the eddy diffusivity coefficient used in the aerodynamic technique is found to be consistent with the coefficient used in the eddy correlation technique. The present result leads us to conclude that the aerodynamic technique may be applicable to underway CO2 flux measurements over the ocean and may be used in place of the bulk technique. The important point is the need to maintain a measuring accuracy of CO2 concentration difference of the order of 0.1 ppmv on the research vessels or the buoys.
KW - Aerodynamic technique
KW - Air-sea interaction
KW - CO flux
KW - Eddy correlation technique
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U2 - 10.1007/s10872-005-0007-5
DO - 10.1007/s10872-005-0007-5
M3 - Article
AN - SCOPUS:22844443875
SN - 0916-8370
VL - 60
SP - 995
EP - 1000
JO - Journal of Oceanography
JF - Journal of Oceanography
IS - 6
ER -