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Titlebook: Remote Sensing of Ice and Snow; Dorothy K. Hall,Jaroslav Martinec Book 1985 Chapman and Hall Ltd and J. Martinec 1985 remote sensing

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书目名称Remote Sensing of Ice and Snow
编辑Dorothy K. Hall,Jaroslav Martinec
视频video
丛书名称Remote Sensing Applications
图书封面Titlebook: Remote Sensing of Ice and Snow;  Dorothy K. Hall,Jaroslav Martinec Book 1985 Chapman and Hall Ltd and J. Martinec 1985 remote sensing
描述Remote sensing using aircraft and satellites has helped to open up to intensified scientific scrutiny the cold and remote regions in which snow and ice are prevalent. In this book, the utility of remote sensing for identifying, mapping and analyzing surface and subsurface properties of worldwide ice and snow features is described. Emphasis is placed on the use of remote sensing for developing an improved understanding of the physical properties of ice and snow and understanding the interrelationships of cryospheric processes with atmospheric, hydrospheric and oceanic processes. Current and potential applications of remotely sensed data are also stressed. At present, all-weather, day and night observations of the polar regions can be obtained from sensors operating in different portions of the electromagnetic spectrum. Because the approaches for analysis of remotely sensed data are not straightforward, Chapter 1 serves to introduce the reader to some of the optical, thermal and electrical properties of ice and snow as they pertain to remote sensing. In Chapter 2 we briefly describe many of the sensors and platforms that are referred to in the rest of the book. The remaining chapters
出版日期Book 1985
关键词remote sensing
版次1
doihttps://doi.org/10.1007/978-94-009-4842-6
isbn_softcover978-94-010-8647-9
isbn_ebook978-94-009-4842-6
copyrightChapman and Hall Ltd and J. Martinec 1985
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Remote Sensing Applicationshttp://image.papertrans.cn/r/image/826932.jpg
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now and ice are prevalent. In this book, the utility of remote sensing for identifying, mapping and analyzing surface and subsurface properties of worldwide ice and snow features is described. Emphasis is placed on the use of remote sensing for developing an improved understanding of the physical pr
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Permafrost,hemisphere permafrost covers an estimated 2.3 . 10. km. in area (Fujii and Higuchi, 1978). The occurrence of permafrost is either continuous, or discontinuous in which large masses of unfrozen ground may be interspersed with masses of permafrost.
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