7.2
The inclusion of a diurnally varying sea surface temperature in surface energy budget calculations
Alec Setnor Bogdanoff, Florida State University, Tallahassee, FL; and C. A. Clayson
With nearly three-quarters of the globe covered by oceans, in order to accurately depict our climate, we must accurately calculate the ocean surface energy budget. Air-sea turbulent fluxes and upwelling longwave (ULW) radiation contain large amounts of variability among the components in the global energy budget calculations. Therefore, in order to better understand our climate, we must better properly calculate or model the variability in the turbulent fluxes and ULW, including the addition of a diurnally varying sea surface temperature (SST). Techniques to calculate the diurnal SST, or difference in maximum and minimum daily SST, rely on a physical understanding of ocean warming. The current version of the SeaFlux turbulent flux data set includes a diurnally varying SST. The fluxes were recalculated using the Reynolds Daily OI-SST and a pre-dawn SST (generally the lowest SST for a day). Initial comparisons indicate that the lack of inclusion of a diurnally varying SST can produce instantaneous local differences in the fluxes of 50%, as well as biases on weekly, monthly and seasonal and yearly timescales on the order of 10 Wm-2. An intercomparison of the difference using the three SST products will provide further insight into the importance of using an appropriate product for turbulent flux calculations.
Session 7, Air-Sea Flux Estimation and Parameterization: 3. Models
Wednesday, 29 September 2010, 10:30 AM-12:00 PM, Capitol AB
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