February 28, 2007
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FROM VOLUME 5, NUMBER 1, JANUARY 1992
EARTH RADIATION BUDGET
"The Radiative Effects of Clouds and Their Impact on Climate,"
A. Arking (NASA-Goddard, Greenbelt MD 20771), Bull. Amer. Meteor. Soc.,
71(6), 795-813, June 1991.
An overview prepared at the request of the Radiation Commission of IAMAP,
examining key results published over the last 15-20 years, along with some
unpublished model studies. The annual global mean effect of clouds is generally
agreed to cool the climate system, but there is disagreement on magnitude.
Observational data are insufficient to adequately determine cloud sensitivity
(the differential response of top-of-the-atmosphere fluxes to changes in cloud
cover parameters), a critical factor in cloud feedback. Climate simulations
indicate clouds may have a strong influence on climate change, but we are far
from knowing either the magnitude or the sign of the influence.
"Reflectivities of Uniform and Broken Layered Clouds," J.A.
Coakley Jr. (Dept. Atmos. Sci., Oregon State Univ., Corvallis OR 97331), Tellus,
43B(5), 420-433, Nov. 1991.
AVHRR 1 km imagery data from NOAA satellites, collected during the FIRE
Marine Stratocumulus Intensive Field Observations, were used to compare
reflectivities of the two types of clouds from the same layers. Reflectivities
of broken clouds can be estimated by simply reducing the values obtained with
Two items from J. Geophys. Res., 96(D10), Oct. 20, 1991:
"Shortwave, Longwave and Net Cloud-Radiative Forcing as Determined from
Nimbus 7 Observations," P.E. Ardanuy (Res.-Data Syst. Corp., Greenbelt MD
20770), L.L. Stowe et al., 18,537-18,549.
The total effect of clouds on the Earth's radiation budget components is
evaluated using statistically generated models of cloud forcing that correlate
simultaneous satellite observations of cloud properties and radiation budget
parameters. Although there is a general compensation over much of the Earth
between the warming and cooling effects of clouds, the net effect is cooling,
primarily due to effects of clouds over the summer hemisphere oceans.
"Surface Albedo Derived from METEOSAT Imagery with an Application to
Africa," G. Nacke (Inst. Meeresknd., Dusternbrooker Weg 20, D-2300 Kiel,
Presents a method based on radiative transfer simulations followed by a
multivariate analysis. Comparison with in situ data from the Sahara shows good
agreement in cases of large, homogeneous surfaces where point measurement
represents larger areas.
"A Theoretical and Observational Study of the Radiative Properties of
Cirrus: Results from FIRE 1986," P.W. Stackhouse Jr. (Dept. Atmos. Sci.,
Colorado State Univ., Ft. Collins CO 80523), G.L. Stephens, J. Atmos. Sci.,
48(18), 2044-2059, Sep. 15, 1991.
To investigate the sensitivity of cloud radiative properties to altitude,
depth and particle size distribution, simulations from a two-stream radiative
transfer model were compared with observations. One result is that it may not be
possible to use Mie scattering to model the cloud albedo.
"Further Analysis of the Global Outgoing Longwave Radiative Flux
Observed by Nimbus," L.H. Auer (Earth-Atmos. Sci., Los Alamos Nat. Lab.,
Los Alamos NM 87545), C.-Y.J. Kao, J. Geophys. Res., 96(D9),
17,367-17,370, Sep. 20, 1991.
Presents further analysis of a decreasing trend in outgoing longwave
radiation (OLR): to demonstrate that the decrease cannot possibly be attributed
to a drift in instrument sensitivity; to ascertain that the relative changes in
OLR between the two hemispheres are consistent with changes in hemispheric Ts;
and to note that a decreasing trend is also found in the insolation data.
"On the Cause of the Relative Greenhouse Strength of Gases such as
the Halocarbons," K.P. Shine (Dept. Meteor., Univ. Reading, 2 Earley Gate,
Whiteknights, POB 239, Reading RG6 2AU, UK), J. Atmos. Sci., 48(12),
1513-1518, June 15, 1991.
Uses a detailed model of radiative transfer in the thermal infrared to
examine some of the reasons for the relative greenhouse strength of gases such
as CFCs, which (unlike CO2) are at relatively low concentrations and therefore
close to their optically thin limit. The latter fact implies a relatively large
impact as their concentrations increase.
"Global Monitoring of Net Solar Irradiance at the Ocean Surface:
Climatological Variability and the 1982-1983 El Ni?o," B. Chertock
(ERL, NOAA, 325 Broadway, Boulder CO 80303), R. Frouin et al., J. Clim.,
4(6), 639-650, June 1991.
A new method has been used to generate the first satellite-based long-term
climatology of surface solar irradiance over the world oceans, resulting in the
first large-scale observation-based examination of cloud solar forcing at the
ocean surface. Seasonal and interannual variations are examined.
Two items from J. Geophys. Res., 96(D5), May 20, 1991.
"Scene Identification and Its Effect on Cloud Radiative Forcing in the
Arctic," Z. Li (Dept. Meteor., McGill Univ., Montr?al, Qu?.
H3A 2K6, Can.), H.G. Leighton, 9175-9188.
Measurements of cloud radiative forcing in polar regions are less reliable
because of difficulty in distinguishing between clouds and ice- or snow-covered
surfaces. Comparison of scenes identified by the ERBE algorithm with those
deduced from AVHRR radiances showed that they differed both in geotype and cloud
"Differences in Global Data Sets of Atmospheric and Surface Parameters
and Their Impact on Outgoing Longwave Radiation and Surface Downward Flux
Calculations," M.L.C. Wu (Lab. Atmos., NASA-Goddard, Greenbelt MD 20771),
L.A. Chang, 9227-9262.
Studied the effect of clouds on the computation of longwave radiation budget
parameters using two sets of cloud fields obtained from two different satellite
systems with different retrieval schemes (HIRS2/MSU and ISCCP). Despite
differences in global mean coverage, outgoing longwave radiation estimates are
very close, but surface downward fluxes differ greatly. Examined the effects of
different temperature-humidity fields on budget calculations by using five
alternative data sets produced by agencies in the U.S. and Europe.
"Consistency of Earth Radiation Budget Experiment Bidirectional
Models and the Observed Anisotropy of Reflected Sunlight," D.G. Baldwin
(Dept. Aerospace Eng., Univ. Colorado, Boulder CO 80309), J.A. Coakley Jr., J.
Geophys. Res., 96(D3), 5195-5207, Mar. 20, 1991. Assesses the
validity of bidirectional models used to estimate radiative fluxes in the Earth
Radiation Budget Experiment (ERBE), by comparing model results with the
anisotropy directly observed by the ERBE scanner on the Earth Radiation Budget
"A Parameterization of Broad Band Radiative Transfer Properties of
Water, Ice and Mixed Clouds," B. Rockel (GKSS Forschungszentrum, Inst.
Phys., Postfach 1160, D-2054 Geesthacht, Ger.), E. Raschke, B. Weyres, Beitr.
Phys. Atmos., 64(1), 1-12, Feb. 1991.
Presents a broad band radiative transfer scheme based on approximate
relations derived from exact calculations using Mie theory. For water clouds, 32
different drop size distributions are considered; for ice clouds, a spherical
parameterization is compared with one assuming randomly oriented hexagonal ice
"Deep Optically Thin Cirrus Clouds in the Polar Regions. Part I:
Infrared Extinction Characteristics," C. Prabhakara (Code 613,
NASA-Goddard, Greenbelt MD 20771), J.-M. Yoo et al., J. Appl. Meteor.,
29(12), 1313-1329, Dec. 1990.
Spectral data obtained by the Nimbus satellite in 1970 indicated the
existence of optically thin ice clouds in the upper troposphere that probably
extended into the lower stratosphere in the polar regions during winter and
early spring. Theoretical simulations of infrared spectra in the 8-25 micro m
region indicate they have a vertical stratification in particle size.
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