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Annual cycle of cloud fraction and surface radiative cloud forcing in the South-East Pacific Stratocumulus region. Virendra P. Ghate and Bruce A. Albrecht (U Miami) Christopher W. Fairall (NOAA ESRL) Robert A. Weller (Woods Hole Oceanographic Institution).
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Annual cycle of cloud fraction and surface radiative cloud forcing in the South-East Pacific Stratocumulus region Virendra P. Ghate and Bruce A. Albrecht (U Miami) Christopher W. Fairall (NOAA ESRL) Robert A. Weller (Woods Hole Oceanographic Institution)
Significant Component of Earth’s radiation budget. • 20% increase can offset global warming due to doubling of CO2. • Strong feedback with ENSO Klein & Hartmann 1993
WORS • Wood’s Hole Oceanographic Institute (WHOI)’s Ocean Reference Station (WORS). • Location: 20° S 85° W • Continuous observations of surface broadband radiative fluxes and thermodynamic variables since October 2000. • http://uop.whoi.edu/archives/dataarchives.htm
Seasonal Variations: Other Properties Surface fluxes of sensible and latent heat, LCL, convective velocity scale, and temperature and moisture advection
Estimating Low Cloud Fraction fro a Buoy • LW = Measured downwelling longwave radiation at the surface. • CF = Cloud Fraction • LWcld = Cloud emitted longwave radiation • LWclr = Clear sky longwave radiation.
Technique • LW = Observed at WORS • LWcld = σTLCL4 • LWclr = f(qsfc,Tsfc,IVsfc); Fairall et al. 2007
Seasonal Cycle: Monthly Means Cloud Fraction Annual cycle 0.5-0.7 Cloud Forcing: Surface radiative fluxes Annual Cycle: Solar -125 to -65 W/m2 IR 55 to 35 W/m2
More Detailed Data Sets • Annual Cruises • VOCALS field Program Fall 2008 http://www.esrl.noaa.gov/psd/people/Simon.deSzoeke/synthesis.html http://www.eol.ucar.edu/projects/vocals/