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Joint ETL/PMEL Ocean and Atmosphere Observations Yield Climate Insights
October 5, 2004
Contact: Chris Fairall
This month, October 2004, ETL personnel aboard the NOAA Ship Ronald H.
Brown will mark the 10th cruise in a series of joint ETL/PMEL
observations in the Eastern Equatorial Pacific as part of a strategy of
enhanced observations for NOAA's Climate Variability (CLIVAR) PACS and
Climate Observations (CO) Programs. These studies include
state-of-the-art surface flux and cloud observations by ETL operating in
piggyback mode aboard NOAA vessels servicing the TAO buoys at 95 W and
110 W in the Pacific. PMEL has enhanced the sensor set on the 95 W buoys
to allow measurements of all components of the oceanic surface energy
budget. The ship-based observations provide both quality assurance and
broader interpretation of the buoy measurements.
Using the comprehensive surface, boundary layer, and cloud information
from the twice-yearly ETL observations, parameterizations of clear sky
radiative fluxes have been developed that allow buoy observations to be
used in a quantitative assessment how clouds affect radiative fluxes
throughout the annual cycle. Two publications have recently been
submitted on the analysis of these data, including characterization of
the annual cycle of each term of the surface energy budget between 8 S
and 12 N at 95 W and the effects of clouds on the overall energy
balance. Intercomparisons with buoy and satellite observations indicate
some problems with operational flux products, particularly with clouds
in the equatorial region. Comparisons of the net surface heat budget
(local forcing) and the time derivative of the mixed-layer heat content
indicate the strong role of ocean processes at this location. Recent
manuscripts from this project can be found at
ftp://ftp.etl.noaa.gov/user/cfairall/EPIC/epicmonitor/pacs_pubs/.
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