TITLE
Collocating satellite-based radar and radiometer measurements to develop an ice water path retrieval
AUTHOR
Holl, Gerrit
DEPARTMENT
Space Science, Kiruna
SUMMARY
Remote sensing satellites can roughly be divided in operational satellites
and scientific satellites. Generally speaking, operational satellites have a
long lifetime and often several near-identical copies, whereas scientific
satellites are unique and have a more limited lifetime, but produce more
advanced data. An example of a scientific satellite is the CloudSat, a NASA
satellite flying in the so-called "A-Train" formation with other satellites.
Examples of operational satellites are the NOAA and MetOp meteorological
satellite series.
CloudSat carries a 94 GHz nadir viewing radar instrument measuring profiles
of clouds. The NOAA-15 to NOAA-18 and MetOp-A satellites carry radiometers at
various frequencies ranging from the infrared (3.76 micrometer) to around 183
GHz (approximately 1.6 mm). The full range is covered by the High Resolution
Infrared Radiation Sounder (HIRS) and the Advanced Microwave Sounding Units
(AMSU-A and AMSU-B). On newer satellites, AMSU-B has been replaced by the
Microwave Humidity Sounder (MHS) with nearly the same characteristics. Those
instruments scan the atmosphere at angles from approximately -50 to +50
degrees perpendicular to the ground track.
The large amount of data from operational satellites is interesting to the
scientific community, particularly when combined with measurements from a
scientific satellite. The degree project focuses on this combination and
consists of two parts:
* The first part of the project involves searching for collocations between
the CloudSat radar and one of the NOAA or MetOp-A instruments. A collocation
between two instruments is defined to occur when both look at the same place
at the same time (within pre-set thresholds). This has been done with
software developed by the student.
* Those collocations are then used to find the relation between the radiances
and physical data (such as Ice Water Path (IWP)) derived from
CloudSat measurements. For the tropical ocean, this relation has been
compared with data from models. Additionally, an artificial neural network
has been trained to retrieve IWP.
ISSN 1653-0187 / ISRN LTU-PB-EX--09/029--SE / NR 2009:029
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