Surface radiation budget data have the potential for contributing
significantly to improved understanding of the four major components of the
climate system: the oceans, the land surface, the cryosphere, and the
atmosphere. Radiative fluxes into the ocean surface provide an important
boundary forcing for the ocean general circulation. Furthermore, since the
radiative fluxes into the ocean surface are significantly modulated by boundary
layer parameters (e.g., clouds, atmospheric humidity, and temperature), SRB may
be an important factor in air-sea interactions. With respect to the land
surface, the net radiative balance governs the turbulent fluxes of latent and
sensible heat from the surface into the atmosphere. Surface radiative fluxes
are also needed for studies related to the energy and water balance of plant
canopies. For the cryosphere, the pack ice and its interaction with surface
temperature and solar radiation provides the so-called ice-albedo feedback
which is a vital component governing climate trends on decadal to longer time
scales. Finally, the knowledge of SRB together with top-of-atmosphere Earth
radiation budget data can yield, for the first time, observational estimates of
tropospheric radiative heating and cloud radiative forcing.
The mission objectives of SRB are to use the ISCCP C1 data
supplemented with ERBE data as input to the SRB satellite algorithms to
estimate various top-of-atmosphere and surface parameters. Where GEBA data are
available and determined by Satellite Data Analysis Center (SDAC) to be
accurate, it is compared with both algorithm's calculation of downward
shortwave irradiance at the surface.
Discipline(s):
Earth Science
Geographic Region(s):
Global.
Detailed Project/Campaign Description:
The Surface Radiation Budget (SRB) data sets are derived from
a variety of data sources. The primary data source is the International
Satellite Cloud Climatology Project (ISCCP) C1 data product. Using the ISCCP
C1 parameters as input, SRB results are generated using two different algorithms.
The Pinker algorithm (developed jointly by Drs. R.T. Pinker and I. Laszlo
form the University of Maryland) is a physical model which uses an iterative
procedure based on delta-Eddington radiative transfer calculations. The
Staylor algorithm (developed by Mr. W.F. Staylor from the NASA Langley Research
Center) is a parameterized physical model in which both cloud and aerosol
transmission characteristics have been separately tuned to historical data
at various locations around the globe. Earth Radiation Budget Experiment
(ERBE) data are also used as input to the models, as well as for top-of-atmosphere
(TOA) irradiance comparisons with the Pinker Model output. The Swiss Federal
Institute of Technology, Zurich, provides ground-truth fluxes from the Global
Energy Budget Archive (GEBA). These data are used for validation of the
Pinker and Staylor calculated downward shortwave surface irradiances. SRB
uses the same equal area grid system as that used by ISCCP for its C1 product.
The equal-area grid contains 6596 cells covering the globe; where a cell
is approximately 280 km x 280 km at the equator.
Langley DAAC User and Data Services Office
NASA Langley Research Center
Mail Stop 157D
Hampton, Virginia 23681-2199
USA
Telephone: (757) 864-8656
FAX: (757) 864-8807
E-mail: larc@eos.nasa.gov
Contact Information:
Langley DAAC User and Data Services Office
NASA Langley Research Center
Mail Stop 157D
Hampton, Virginia 23681-2199
USA
Telephone: (757) 864-8656
FAX: (757) 864-8807
E-mail: larc@eos.nasa.gov
Dr. Paul W. Stackhouse
Mail Stop 420
NASA Langley Research Center
Hampton, VA 23681-2199
USA
Phone: (757) 864-5368
FAX: (757) 864-7996
E-mail: Paul.W.Stackhouse@nasa.gov
Brest, C. L. and W. B. Rossow. 1991. Radiometric Calibration and
Monitoring of NOAA AVHRR Data for ISCCP Int. J. Remote Sensing, In Press.
Gautier, C. and R. Frouin. 1988. Sensitivity of Satellite-Derived Net
Shortwave Irradiance at the Earth's Surface to Radiometric Calibration. In
Proc. 4th International Colloquium on Spectral Signatures of Objects in Remote
Sensing, Aussois, France, January 18-22, 1988, ESA SP-287; ESA Paris, 179-183.
Rossow, W. B., L. C. Gardner, P-J. Lu, and A. W. Walker. 1988.
International Satellite Cloud Climatology Project (ISCCP) Description of
Reduced Resolution Data. WMO/TD-No. 266, World Meteorological Organization,
Geneva.
Rossow, W. B., C. L. Brest, and L. C. Garder. 1989. Global, Seasonal Surface
Variations form Satellite Radiance Measurements. J. Climate 2(3): 214-247.
Sellers, P. J., S. I. Rasool, and H. -J. Bolle. 1990. A Review of Satellite
Data Algorithms for Studies of the Land Surface. Bull. Amer. Meteor. Soc. 71
(10): 1429-1477.
Staylor, W. F., and A. C. Wilber. 1990.
Global Surface Albedos Estimated from ERBE Data. In Proc. AMS 7th Conference on
Atmospheric Radiation, San Francisco, California, July 23-27, 1990, 231-236.
Staylor, W. F., and A. C. Wilber. 1990. Global surface albedos estimated
from ERBE data. Proceedings of AMS Conf. on Atmospheric Radiation, July 23-27,
1990, San Francisco, CA, pp 231-236.
Suttles, J. T., R. N. Green, P. Minnis, G. L. Smith, W. F. Staylor, B. A.
Wielicki, I. J. Walker, D. F. Young, V. R. Taylor, and L. L, Stowe. 1988.
Angular Radiation Models for Earth-Atmosphere System, Volume I-Shortwave
Radiation. NASA RP-1184; NASA Langley Research Center, Hampton, VA 23665-5225.
WCRP. 1988. International Satellite Cloud Climatology Project (ISCCP)
Working Group on Data Management, Sixth Session. Ft. Collins, CO, June 16-18,
1987, WMO/TD-No. 210,Geneva.
Whitlock C. H., W. F. Staylor, J. T. Suttles, G. Smith, R, Levin, R.
Frouin, C. Gautier, P. M. Teillet, P. N. Slater, Y. J. Kaufman, B. N. Holben,
W. B. Rossow, C., Brest, and S. R. LeCroy. 1990a. AVHRR and VISSR Satellite
Instrument Calibration Results for both Cirrus and Marine Stratocumulus IFO
Periods. In Proc. FIRE Science Meeting, Vail, Co., July 11-15,1988, NASA
CP-3083, NASA Langley Research Center, Hampton, VA 23665-5225, 141-146.
Whitlock, C. H., W. F. Staylor, W. L. Darnell, M-D. Chou, G. Dedieu, P. Y.
Deschamps, J. Ellis, C. Gautier, R. Frouin, R. T. Pinker, I. Laslo, W. B.
Rossow, and D. Tarpley. 1990b. Comparison of Surface Radiation Budget
Satellite Algorithms for Downwelled Shortwave Irradiance With Wisconsin
FIRE/SRB Surface Truth Data. In Proc. AMS 7th Conference on Atmospheric
Radiation, San Francisco, California, July 23-27, 1990, 237-242.
Lacis, A. A. and J. E. Hansen, 1974. A
parameterization for the absorption of solar radiation in the earth's
atmosphere. J. Atmos. Sci. 31:118-133.
Pinker, R. and J. Ewing, 1985. Modeling
surface solar radiation: Model formulation and validation. J. Climate Appl.
Meteor. 24:389-401.
Pinker, R. T. and I. Laszlo. 1992.
Modeling surface solar irradiance for satellite applications on a global
scale. J. Appl. Meteor., February issue. Stephens, G. L., S. Ackerman and E.
Smith. 1984. A shortwave parameterization revised to improve cloud absorption.
J. Atmos. Sci. 41:687-690.
WCP-55. 1983. World Climate Research report of the experts meeting on
aerosols and their climatic effects. Williamsburg, Virginia, 28-30 March 1983,
A. Deepak and H. E. Gerber, Eds. 107 pp.
Hoyt, D. V., 1978. A model for the
calculation of solar global insolation. Sol. Energy 21:27-35.
Lacis, A. A., and J. E. Hansen. 1978. A parameterization for the
absorption of solar radiation in the Earth's atmosphere. J. Atmos. Sci.
31:118-133.
The Astronomical Almanac, Nautical Almanac Office, U. S. Naval Observatory,
Washington, D. C., 1985, 1980.
Schiffer, R. A., and W. B. Rossow, 1983.
The International Satellite Cloud Climatology Project (ISCCP): The first
project of the World Climate Research Programme. Bull. Amer. Met. Soc. 64:779-784.