toa direct radiative effect of aerosols - nasa · may 4, 2005, gfdl toa direct radiative effect of...
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May 4, 2005, GFDL
TOA Direct Radiative Effect of Aerosols
Norman G. LoebHampton University/NASA Langley Research Center, VA
Natividad Manalo-SmithAnalytical Services and Materials, Hampton, VA
- Do models and observations provide consistent estimates of the total (natural+anthropogenic) direct radiative effect of aerosols (DREA)?
- What are the uncertainties in the observations and how can they be reduced?
- What is the seasonal and interannual variability in the DREA?
- What observations are needed to determine the natural and anthropogenic components of the total DREA?
Introduction
All
0 20 40 60 80 100
0.64
4-μ m
Aer
osol
Opt
ical
Dep
th
0.06
0.08
0.10
0.12
0.14
0.16
0.18
0.20
0.22
NOAA-SSFMOD04-SSF
Intersection
0 20 40 60 80 1000.06
0.08
0.10
0.12
0.14
0.16
0.18
0.20
0.22
All
Cloud Fraction (%)0 20 40 60 80 100
No.
of C
ER
ES
FO
Vs w
ith A
eros
ol
0.0
5.0e+5
1.0e+6
1.5e+6
2.0e+6
2.5e+6
NOAA-SSFMOD04-SSF
Intersection
Cloud Fraction (%)0 20 40 60 80 100
0.0
5.0e+5
1.0e+6
1.5e+6
2.0e+6
2.5e+6
0.644-μm Aerosol Optical Depth vs Cloud Fraction (JJA 2000)
-5.1-4.6-3.2SH-5.7-6.4-4.4NH
-5.4-5.5-3.8GlobalChou_2002MOD04NOAA-SSF
SW Direct Effect of Aerosols (W m-2)
Annual Average Clear-Sky SW Direct Radiative Effect: Comparison with Chou et al. (2002)
JAN, 2001 APR, 2001
JUL, 2001 OCT, 2001
Global Direct Radiative Effect of Aerosols(CERES+MOD04+MOD43)
CERES Minus Aeronet (W m-2)Aerosol Direct Effect (W m-2)
Rel
ativ
e Fr
eque
ncy
(%)
Direct Radiative Effect of Aerosols Over Land (Comparison with Aeronet-Derived Values)
Aeronet-derived DREA provided by Stefan Kinne
- Global ocean clear-sky SW direct radiative effect of aerosolsestimated to be -5.5 W m-2 (MOD04) and -3.8 W m-2 (NOAA-SSF).
- Large regional and global uncertainty due to cloud mask differences, especially near desert regions.-> CALIPSO should help with this.
- The DREA has pronounced seasonal cycle in the Northern Hemisphere and large year-to-year fluctuations between 30°-60°N.
- No systematic trend in deseasonalized anomalies of the DREA is observed over the 46-month time series considered
Summary