Remote sensing /
The parts of the electromagnetic spectrum are discussed, with the type(s) of sensor(s) required to record energy in each part. A review is given of the classes of airborne (and satellite) remote sensor data which are available to geoscientists. Different types of remote sensor data are described and...
Main Authors: | , |
---|---|
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://hdl.handle.net/2027/mdp.39015095133784 |
id |
ftumichgbhathi:oai:quod.lib.umich.edu:MIU01-102198213 |
---|---|
record_format |
openpolar |
spelling |
ftumichgbhathi:oai:quod.lib.umich.edu:MIU01-102198213 2023-05-15T13:51:56+02:00 Remote sensing / Svensson, Harald. Air Force Cambridge Research Laboratories (U.S.) bib http://hdl.handle.net/2027/mdp.39015095133784 eng eng http://hdl.handle.net/2027/mdp.39015095133784 Items in this record are available as Public Domain, Google-digitized. View access and use profile at http://www.hathitrust.org/access_use#pd-google. Please see individual items for rights and use statements. PDM Remote sensing Natural resources Aerial reconnaissance text ftumichgbhathi 2019-11-08T01:22:55Z The parts of the electromagnetic spectrum are discussed, with the type(s) of sensor(s) required to record energy in each part. A review is given of the classes of airborne (and satellite) remote sensor data which are available to geoscientists. Different types of remote sensor data are described and examples provided, including panchromatic, infrared, color, and color infrared aerial photography (Kullaberg, Sweden); multispectral aerial photography (with importance of optimum film/filter combination for specific phenomena); airborne thermal infrared imagery (Kullaberg, Sweden and Surtsey, Iceland); side-looking airborne radar (Tuskahoma Syncline, Oklahoma); and radio sounding of glacial ice (Antarctica). The projected future increase in amount of remote sensor data will require computer processing techniques, although man will serve the most important role in the analysis and use of remote sensor information of the earth's surface. Translation supported by the Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force (L.G. Hanscom Field, Mass.), and translated by the Translation Center of New England, Somerville, Massachusetts. Translated from Forskaning och Fromsteg, No. 5, pp. 10-19, 1969. AFCRL Research Laboratory Project 7628. AD0707824 (from http://www.dtic.mil). "May 1970." The parts of the electromagnetic spectrum are discussed, with the type(s) of sensor(s) required to record energy in each part. A review is given of the classes of airborne (and satellite) remote sensor data which are available to geoscientists. Different types of remote sensor data are described and examples provided, including panchromatic, infrared, color, and color infrared aerial photography (Kullaberg, Sweden); multispectral aerial photography (with importance of optimum film/filter combination for specific phenomena); airborne thermal infrared imagery (Kullaberg, Sweden and Surtsey, Iceland); side-looking airborne radar (Tuskahoma Syncline, Oklahoma); and radio sounding of glacial ice (Antarctica). The projected future increase in amount of remote sensor data will require computer processing techniques, although man will serve the most important role in the analysis and use of remote sensor information of the earth's surface. Mode of access: Internet. Text Antarc* Antarctica Iceland Surtsey Hathi Trust Digital Library Somerville ENVELOPE(-64.307,-64.307,-65.376,-65.376) Surtsey ENVELOPE(-20.608,-20.608,63.301,63.301) |
institution |
Open Polar |
collection |
Hathi Trust Digital Library |
op_collection_id |
ftumichgbhathi |
language |
English |
topic |
Remote sensing Natural resources Aerial reconnaissance |
spellingShingle |
Remote sensing Natural resources Aerial reconnaissance Svensson, Harald. Air Force Cambridge Research Laboratories (U.S.) Remote sensing / |
topic_facet |
Remote sensing Natural resources Aerial reconnaissance |
description |
The parts of the electromagnetic spectrum are discussed, with the type(s) of sensor(s) required to record energy in each part. A review is given of the classes of airborne (and satellite) remote sensor data which are available to geoscientists. Different types of remote sensor data are described and examples provided, including panchromatic, infrared, color, and color infrared aerial photography (Kullaberg, Sweden); multispectral aerial photography (with importance of optimum film/filter combination for specific phenomena); airborne thermal infrared imagery (Kullaberg, Sweden and Surtsey, Iceland); side-looking airborne radar (Tuskahoma Syncline, Oklahoma); and radio sounding of glacial ice (Antarctica). The projected future increase in amount of remote sensor data will require computer processing techniques, although man will serve the most important role in the analysis and use of remote sensor information of the earth's surface. Translation supported by the Air Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force (L.G. Hanscom Field, Mass.), and translated by the Translation Center of New England, Somerville, Massachusetts. Translated from Forskaning och Fromsteg, No. 5, pp. 10-19, 1969. AFCRL Research Laboratory Project 7628. AD0707824 (from http://www.dtic.mil). "May 1970." The parts of the electromagnetic spectrum are discussed, with the type(s) of sensor(s) required to record energy in each part. A review is given of the classes of airborne (and satellite) remote sensor data which are available to geoscientists. Different types of remote sensor data are described and examples provided, including panchromatic, infrared, color, and color infrared aerial photography (Kullaberg, Sweden); multispectral aerial photography (with importance of optimum film/filter combination for specific phenomena); airborne thermal infrared imagery (Kullaberg, Sweden and Surtsey, Iceland); side-looking airborne radar (Tuskahoma Syncline, Oklahoma); and radio sounding of glacial ice (Antarctica). The projected future increase in amount of remote sensor data will require computer processing techniques, although man will serve the most important role in the analysis and use of remote sensor information of the earth's surface. Mode of access: Internet. |
format |
Text |
author |
Svensson, Harald. Air Force Cambridge Research Laboratories (U.S.) |
author_facet |
Svensson, Harald. Air Force Cambridge Research Laboratories (U.S.) |
author_sort |
Svensson, Harald. |
title |
Remote sensing / |
title_short |
Remote sensing / |
title_full |
Remote sensing / |
title_fullStr |
Remote sensing / |
title_full_unstemmed |
Remote sensing / |
title_sort |
remote sensing / |
url |
http://hdl.handle.net/2027/mdp.39015095133784 |
long_lat |
ENVELOPE(-64.307,-64.307,-65.376,-65.376) ENVELOPE(-20.608,-20.608,63.301,63.301) |
geographic |
Somerville Surtsey |
geographic_facet |
Somerville Surtsey |
genre |
Antarc* Antarctica Iceland Surtsey |
genre_facet |
Antarc* Antarctica Iceland Surtsey |
op_relation |
http://hdl.handle.net/2027/mdp.39015095133784 |
op_rights |
Items in this record are available as Public Domain, Google-digitized. View access and use profile at http://www.hathitrust.org/access_use#pd-google. Please see individual items for rights and use statements. |
op_rightsnorm |
PDM |
_version_ |
1766255968132268032 |