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Titlebook: Remote Sensing with Imaging Radar; John A. Richards Book 2009 Springer-Verlag Berlin Heidelberg 2009 Backscattering.Cultural Structures.In

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发表于 2025-3-21 18:12:13 | 显示全部楼层 |阅读模式
书目名称Remote Sensing with Imaging Radar
编辑John A. Richards
视频video
概述Develops the technology of radar imaging in a manner suited to the mathematical background of most earth scientists – no deep knowledge.Emphasises the application of imaging radar in the context of re
丛书名称Signals and Communication Technology
图书封面Titlebook: Remote Sensing with Imaging Radar;  John A. Richards Book 2009 Springer-Verlag Berlin Heidelberg 2009 Backscattering.Cultural Structures.In
描述This book is concerned with remote sensing based on the technology of imaging radar. It assumes no prior knowledge of radar on the part of the reader, commencing with a treatment of the essential concepts of microwave imaging and progressing through to the development of multipolarisation and interferometric radar, modes which underpin contemporary applications of the technology. The use of radar for imaging the earth’s surface and its resources is not recent. Aircraft-based microwave systems were operating in the 1960s, ahead of optical systems that image in the visible and infrared regions of the spectrum. Optical remote sensing was given a strong impetus with the launch of the first of the Landsat series of satellites in the mid 1970s. Although the Seasat satellite launched in the same era (1978) carried an imaging radar, it operated only for about 12 months and there were not nearly so many microwave systems as optical platforms in service during the 1980s. As a result, the remote sensing community globally tended to develop strongly around optical imaging until Shuttle missions in the early to mid 1980s and free-flying imaging radar satellites in the early to mid 1990s became
出版日期Book 2009
关键词Backscattering; Cultural Structures; Interferometry; Natural Media; Polarimetry; SAR; remote sensing; ecoto
版次1
doihttps://doi.org/10.1007/978-3-642-02020-9
isbn_softcover978-3-642-26113-8
isbn_ebook978-3-642-02020-9Series ISSN 1860-4862 Series E-ISSN 1860-4870
issn_series 1860-4862
copyrightSpringer-Verlag Berlin Heidelberg 2009
The information of publication is updating

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发表于 2025-3-21 23:55:20 | 显示全部楼层
John A. Richardsdem Menschen ist heute – im Zeitalter der zunehmenden Verschmelzung von Mensch und Technik (Cyborgisierung), der Genom-Editierung und der fortgeschrittenen Naturalisierung des Menschenbildes – aktueller denn je. Der Autor präsentiert hier erstmals eine systematische und prägnante Darstellung der Ide
发表于 2025-3-22 02:39:33 | 显示全部楼层
John A. Richardsikation mit seinem ersten öffentlichen Funknetz im Jahr 1958, dem sog. .(vgl. Gerum et al. 2005, S. 10). Diese erste Mobilfunkgeneration (kurz: 1G) arbeitete ausschließlich analog und bot lediglich einfache Sprachübertragung. Datenübertragung bzw. der Zugang zum Internet über ein mobiles Endgerät, w
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Correcting and Calibrating Radar Imagery,ortions and treat methods for removing, or at least minimising, them. We commence with errors in geometry..Closely related to distortions in brightness is the need to calibrate data, including the need to ensure that polarimetric responses are cross-calibrated. Calibration methods are also treated in this Chapter.
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Book 2009 commencing with a treatment of the essential concepts of microwave imaging and progressing through to the development of multipolarisation and interferometric radar, modes which underpin contemporary applications of the technology. The use of radar for imaging the earth’s surface and its resources
发表于 2025-3-22 23:36:57 | 显示全部楼层
The Imaging Radar System,the image data recorded is more varied. Since there are so many concepts and techniques to be assimilated, this chapter provides an overview of the topic as a framework for the later chapters. It also draws attention to the knowledge assumed on the part of the reader..First, we should establish why
发表于 2025-3-23 03:35:22 | 显示全部楼层
The Radiation Framework,ion of interest so that an image can be formed. The energy can originate from the earth itself, as a result of its finite temperature, or it can be the reflection of energy incident on the earth‘s surface from an external source such as the sun. It could also come from an artificial source such as a
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