THE UNIVERSITY of EDINBURGH

DEGREE REGULATIONS & PROGRAMMES OF STUDY 2016/2017

University Homepage
DRPS Homepage
DRPS Search
DRPS Contact
DRPS : Course Catalogue : School of Geosciences : Postgraduate Courses (School of GeoSciences)

Postgraduate Course: Radiative Transfer (PGGE11055)

This course will be closed from 13 January 2017

Course Outline
SchoolSchool of Geosciences CollegeCollege of Science and Engineering
Credit level (Normal year taken)SCQF Level 11 (Postgraduate) AvailabilityAvailable to all students
SCQF Credits10 ECTS Credits5
SummaryRadiative transfer is the theory that describes how electromagnetic radiation propagates through and interacts with matter. The varied imprints of these interactions on top-of-atmosphere radiance spectra are the data that make possible much remote sensing. Account also needs to be taken of the transfer of radiation through the observing instrument to its detectors. The aim of this course is therefore that students understand radiative transfer theory at a level of detail sufficient to underpin remote sensing of surface characteristics and of the state of the atmosphere.
Course description Not entered
Entry Requirements (not applicable to Visiting Students)
Pre-requisites Co-requisites
Prohibited Combinations Other requirements None
Information for Visiting Students
Pre-requisitesNone
Course Delivery Information
Not being delivered
Learning Outcomes
In this course we shall confine our attention
to remote sensing of planetary atmospheres and surfaces using electromagnetic radiation, using
instruments carried on satellites. Many of the techniques thus covered are of relevance in other
applications however.
A major advantage of remote sensing is global coverage; a polar orbiting satellite typically makes
14 orbits per day while the earth rotates underneath, so that the sub-satellite point passes within
about o 15 longitude of any point twice per day. Another advantage is uniformity; in situ
measurements suffer from the fact that different observations are made with different instruments
so that variations in calibration may be difficult to remove. Remotely sensed data from a single
satellite instrument are relatively free from this difficulty.
To be able to be able to interpret the signals from satellite instruments in terms of the geophysical
entities which were ultimately responsible for them it is necessary to understand how radiation is
emitted, scattered and absorbed by the surface and the atmosphere. This understanding is the
subject of radiative transfer theory. This theory can be conveniently divided into two parts, the
forward problem, namely, for a given state of the surface and atmosphere calculate what would be
observed by the satellite, and the inverse problem, namely for a given measurement at the satellite,
deduce what state of surface and/or atmosphere produced it. Ability to solve the forward problem is
a pre-requisite for the inverse problem. Accordingly this is considered first in Radiative Transfer (Semester 1).
Discussion of the inverse problem is given in Inverse Theory (Semester 2).
Reading List
None
Additional Information
Course URL http://www.geos.ed.ac.uk/postgraduate/MSc/mscprogrammes/remotesip/
Graduate Attributes and Skills Not entered
KeywordsPGGE11055
Contacts
Course organiserDr Chris Merchant
Tel: (0131 6)50 5097
Email: v1cmarc3@exseed.ed.ac.uk
Course secretaryMs Caroline Keir
Tel: (0131 6)51 7192
Email: caroline.keir@ed.ac.uk
Navigation
Help & Information
Home
Introduction
Glossary
Search DPTs and Courses
Regulations
Regulations
Degree Programmes
Introduction
Browse DPTs
Courses
Introduction
Humanities and Social Science
Science and Engineering
Medicine and Veterinary Medicine
Other Information
Combined Course Timetable
Prospectuses
Important Information
 
© Copyright 2016 The University of Edinburgh - 3 February 2017 4:54 am