Measurement and Parameterization of Sea-Air Trace Gas Transfer Using Micrometeorological Techniques: A Decade of Progress
C. Fairall1, J.E. Hare2, J.B. Edson3, B. Huebert4, W. McGillis5 and D. Helmig6
1NOAA Earth System Research Laboratory, 325 Broadway, Boulder, CO 80305; 303-497-3253, E-mail: chris.fairall@noaa.gov
2Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309
3University of Connecticut, Storrs, CT 06269
4Department of Oceanography, University of Hawaii, Honolulu, HI 96822
5Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964
6Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309
In May-June 1998 a team of the NOAA and university scientists executed the first motion-corrected, direct covariance measurements of the transfer velocity of CO2 from a ship in the joint NOAA National Science Foundation (NSF) Gas Exchange field program, GasEx1998. Since then, CO2 observations have been repeated in two subsequent GasEx field programs (2001 and 2008). Furthermore, the development of fast sensors for Dimethylsulfide (DMS) and Ozone has permitted similar direct measurements of transfer velocities for those gases in a series of NOAA and NSF-sponsored field programs. These observations have yielded insights into the physics of near-surface oceanic processes driving gas transfer over the ocean. This has led to the development of the NOAA Cuppled Ocean Atomsphere Response Experiment (COARE) gas transfer algorithm, which can be applied generally to most gases with known solubility and Schmidt number (air and water). In this talk we will discuss the measurement technology, recent field programs, and provide a synthesis of progress to date. Figure 1 shows a summary of observations of gas transfer velocity for CO2 and DMS from this series of field projects.
