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Upcoming 2012 JCSDA Seminars
About JCSDA's Seminar Series
Simulated AIRS
brightness temperatures for channel 787
on a 3km-resolution WRF simulation, 4-10-2008,
using the CRTM radiative transfer package. Courtesy of Tom Auligné (NCAR)
The JCSDA seminar series includes presentations on satellite observing
instruments, radiative transfer models for use in satellite data
assimilation, algorithms for deriving information on the Earth's
atmosphere, oceans, and land surface from satellite observations,
advances in data assimilation techniques, preparations for
assimilation of data from new satellite instruments, and impacts of
satellite data on weather and climate predictions. The seminars are
about 1 hour in duration (including discussion period) and are held
monthly, usually on the 3rd Wednesday of each month at 2 PM, and are
open to the public.
The audience for the seminars generally consists of remote sensing
researchers from NOAA/NESDIS, data assimilation experts and modelers
from NOAA/NCEP and NASA/Goddard Space Flight Center Global Modeling
and Assimilation Office, and students/faculty from the University of Maryland.
Slides for each presentation should be available for download in PDF
format on this page, the day before each talk.
Unless specifically noted otherwise, the contact for
the JCSDA seminar series is George Ohring.
Title
The Assimilation of Surface Sensitive Microwave Observations Over Land: Recent Results and Open Issues
One of the many scientific challenges in the field of numerical
weather prediction is to extract useful information on the
atmospheric boundary layer using observations from remote sensing
microwave instruments such as AMSU-A, AMSU-B/MHS or SSMIS. These
data contribute increasingly to improve short to medium range
forecasts, but also to improve re-analyses. Better use of these
data often requires appropriate representation of the surface in
the models, in both emissivity and temperature. This is achieved
over sea, and satellite data have a tremendous impact on the
atmospheric analyses over oceans. Over land, the surface
emissivity is highly variable and may cause biases in the forward
model if its temporal and spatial variability are not well taken
into account. In such a situation, the model cannot produce
realistic simulations of observations sensitive to the surface and
may reject useful observations, including those not sensitive to
the surface. This case concerns in particular the land and sea ice
surfaces for which the surface emissivity is particularly
challenging to model. During the seminar, some of the work carried
out at Météo-France for a better description of the emissivity of
land and sea ice surfaces will be summarized. The methodology used
for estimating the emissivity in the model and its impact on the
performance of the radiative transfer model will be presented. The
impact of a proper modeling of the land and sea ice emissivity, in
terms of forecast skill and quality of analyses, will be
discussed.