C240B/C160. Remote Sensing. (4) Lecture, three hours.
Concurrently.
Requisites: courses C203C/C165 or instructor's
consent
Introduction to remote sensing based on the principle of radiative
transfer; Atmospheric spectroscopy and spectral channels for atmospheric
and surface remote sensing from space; Remote sensing of aerosols and
ozone; Introduction of the Fredholm equation of the first kind and
discussion of the direct and constrained linear inversions; Satellite
remote sensing of temperature and humidity using the thermal emission
principle in the infrared; Satellite remote sensing of clouds using
reflection, polarization, and reflected line spectrum from sunlight;
Satellite remote sensing of precipitation and temperature from microwave;
Active lidar (laser radar) and millimeter-wave radar remote sensing of
clouds and aerosols.
Textbook: An
Introduction to Atmospheric Radiation, Academic Press, 2002, Chapter 7;
additional references will also be provided.
Letter
grades: students are required to carry out a numerical exercise
involving the inversion of aerosol size distribution from radiometric
measurements and to write a term paper on an aspect of remote sensing that
interests them.
Outline
of the course
- INTRODUCTION:
meaning of remote sensing; uniqueness; active and passive; key
milestones of atmospheric sounding from satellites
- REMOTE SENSING USING
TRANSMITTED SUNLIGHT: determination of aerosol optical depth
and size distribution; direct and constrained linear inversions;
determination of total ozone concentration
-
REMOTE
SENSING USING REFLECTED SUNLIGHT: satellite-sun geometry and
theoretical foundation; satellite remote sensing of ozone, aerosols, and
land surfaces; cloud optical depth and particle size from bidirectional
reflectance, polarization, and reflected line
measurements
- REMOTE SENSING USING
EMITTED MICROWAVE RADIATION: microwave spectrum and microwave
radiative transfer; microwave remote sensing of rainfall rate and
temperature
- REMOTE SENSING USING
LASER AND MICROWAVE ENERGIES: backscattering equation; lidar
differential absorption and depolarization techniques for the remote
sensing of gases and aerosols; millimeter-wave radar for cloud study