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AVHRR CDR
AVHRR CDR
Overview
One of the most pressing climate issues identified by the IPCC's
Fourth Assessment is the need for a long-term analysis of cloud
properties to better understand the impact of cloud and aerosol
radiative forcing on various aspects of climate, especially surface
temperature and its diurnal variation. Cloud and aerosol radiative
forcing are linked by the indirect effects of aerosols on the the
microphysical properties of clouds and the subsequent impact on the
radiative absorption of those clouds. To understand radiative forcing
over long time periods, it is necessary to measure cloud and aerosol
properties over the globe using a consistent set of proven algorithms
applied to a long-term record of consistently calibrated and quality-
controlled
satellite imager data. Knowing how clouds vary with climate change
and how well climate models reproduce such variability through modeled
feedbacks is critical to understanding how well the models can predict
climate. In a complementary fashion, it is also essential to monitor
the changes in Earth surface properties when clouds are not present.
A fundamental parameter is clear-sky radiance, which can be used to
determine a variety of surface properties including land or sea
surface skin temperature, surface spectral albedo, and vegetation
index. Relating those properties and surface air temperature to
changes in vegetation and urbanization is another important component
of understanding climate change.
As part of the NOAA NCDC Climate Data Record (CDR) program, the NASA
Langley Cloud and Radiation Research group (PI: Dr. Patrick Minnis) is
currently developing a Thematic CDR (TCDR) consisting of cloud amount,
phase, optical depth, effective particle size, height, and temperature
extending back to 1978 using data from the AVHRR instrument. The TCDR
will be consistent with CERES MODIS cloud properties, though some
modifications to these algorithms will be required to operate on the 5-
channel and lower spatial resolution AVHRR Global Area Coverage (GAC)
data. The CERES MODIS cloud property retrieval algorithm has a
reliable 10-year data record and will continue to operate with NPP
VIIRS.
In addition to having a suite of mature, robust cloud and clear-sky
analysis algorithms, it is essential that the satellite data are
properly calibrated to produce reliable cloud and clear sky
properties. Detection of small climate trends requires high accuracy
in the initial radiance. An addition component of this NOAA NCDC CDR
effort is the development of a Fundamental CDR (FCDR) consisting of a
calibration record of visible (0.65 micrometer) and near-infrared
(0.87 and 1.6 micrometers) channels for: 1) AVHRR instruments on
NOAA-5 through NOAA-18 and MetOp-A, 2) US geostationary (GEO) imagers
for SMS-1 through GOES-13, and 3) Non-US GEO imagers such as GMS,
Meteosat, MTSAT, FY-2, and Kalpana after 1982. Stable and accurate
visible channel calibration is ensured through matching modern AVHRR
and GEO data with that of Aqua MODIS using the Nearly Simultaneous Ray-
matched Technique and the Deep Convective Cloud Technique. These
calibrations are then transferred back in time through the use of time-
overlapping LEO and GEO data.
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