Professor Daniel Kirk-Davidoff is
leading research efforts in this exciting subject.
Satellite climate observations offer broad and consistent spatial
sampling, complementing surface-based observations, which may be
compromised by correlations with anthropogenic or natural changes in
surface conditions near observation sites, and which may be spatially
biased by ease or difficulty of access to a given location on the
surface. However, imperfect temporal sampling introduces random errors
(due to aperiodic weather noise) and biases that can substantially
reduce the accuracy of satellite observations of the state of the
atmosphere. Selection of the number of satellites, their orbital
configuration, and their scanning pattern all contribute to satellite
sampling for climate studies. Dr. Daniel Kirk-Davidoff is using
geostationary satellite brightness temperature data as a proxy to
determine the sensitivity of bias and random errors to the choice of
orbit for LEO climate monitoring satellites. He has shown that a
single precessing polar orbiter is capable of producing very high
accuracy annual mean brightness temperature records.