Beate Liepert (PI)
Lamont-Doherty Earth Observatory
liepert@ldeo.columbia.edu
Interannual Variability of Surface Radiation Budget and Climate Feedback
The proposed study investigates the interannual variability of surface
radiative fluxes, the possible causes of the variability and the impacts
on the climate system. The investigations of cloud feedback mechanisms
in combination with the general circulation are of particular interest.
Hence the goal of this study lies within the scope of the NASA's Earth
System Enterprise NRA namely the investigation of changes in the Earth's
radiation and climate. Recent studies show an unexpectedly high variability
of surface solar radiation (''dimming'') of about 7 watts per square
meter in the last decades with a recent recovery back to mid last century
values in some regions. Cloud coverage decreases have also been reported
for the 1990s. It is suspected that part of this variability in the shortwave
irradiance is due to the influence of aerosol effects from anthropogenic
sources, and from major volcanic eruptions. Furthermore, cloud feedbacks
and global warming with its feedbacks modify both shortwave and longwave
surface radiative fluxes. The surface solar radiation is highly sensitive
to aerosol forcing because the surface fluxes are reduced by scattered
and by absorbed solar energy. The latter one cannot be seen from the
top of the atmosphere. Since radiative fluxes at the surface are balanced
by non-radiative fluxes, small changes lead to direct changes in latent
heat and sensible heat fluxes that modify convection and evaporation.
The proposed analysis of surface radiative fluxes in climate models and
observations is therefore a crucial component in assessing the impact
of aerosols and greenhouse gas forcing on the hydrological cycle. We
plan to focus our investigation on the time period of satellite observations
from 1983 to present. Surface radiation data and cloud information from
ISCCP-FD will be analyzed together with in situ measurements from Baseline
Surface Radiation Network BSRN stations for various climatic conditions
(e.g. El Nino and monsoon system). Surface radiative and non-radiative
fluxes of GISS-GCM experiments with varying forcings will be analyzed.
Additional model experiments with the GISS modelE will be designed and
performed to test hypothesis for explaining possible changes in surface
radiation and cloud feedbacks. The proposed project aims to improve our
prediction ability of future climate change by explaining observed interannual
variability of surface radiation with climate simulations and observational
data analysis.
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