By Gert A. Schultz, Edwin T. Engman

ISBN-10: 3642595839

ISBN-13: 9783642595837

ISBN-10: 3642640362

ISBN-13: 9783642640360

The authors of this ebook were approached by way of consulting engineers: "You learn about distant sensing and therefore you could receive hydrological details the place no info exist, even with out flooring measurements, in order that i will be able to layout the mandatory ability of a consuming water provide reservoir in a constructing nation. " nevertheless, the authors were instructed: "Remote sensing isn't really of a lot use because it remains to be very unlikely to estimate floor water assets or floor water flows from distant sensing info. " the key objective of this e-book is to right such unjustified illusions in addition to exaggerated feedback through offering the reader with sound info at the power - and the restrictions - of distant sensing within the box of hydrology and water administration. The e-book is intended to be a reference and textual content; it isn't a suite of papers from a few assembly. The e-book is meant to supply how to aid the readers remedy their very own difficulties in hydrology and water administration. for that reason, medical concerns are awarded simply so far as they're priceless for the appliance of distant sensing. The reader will see that during a few fields, (e. g. evapotranspiration, soil moisture, hydrological modeling) the clinical improvement remains to be at the means, whereas in others operational options are already to be had (e. g. snow soften run­ off-model, land use class and detection of land use alterations, flood fore­ casting and control).

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The signal received at the antenna is compared with the signals of the reference sources by switching between the antenna input and the reference loads. According to Eq. 4 the microwave radiometric measurements can conveniently be expressed in terms of temperature. 25) where B = t111 is the bandwidth in Hz, t is the integration time in sec, and M is the radiometric figure of merit, which is a constant for a given receiver configuration, depending on its technical design. It is obvious that the radiometric resolution has to be traded off versus spectral resolution (given by B) and integration time.

R. Jensen Department of Geography, University of South Carolina, Columbia, SC 29208 Analog and digital remotely sensed data are used operationally in many hydrologic and water management applications. g. aerial photographs) are routinely analyzed visually using optical instruments such as stereoscopes. Digital remote sensor data are analyzed using a digital image processing system that consists of both hardware and software. 1 image processing system characteristics, image processing (and some GIS) software requirements, and commercial and public providers of digital image processing systems.

IEEE Trans. Geosc. Rem Sens. 33(4), 915 - 926 Elachi C. (1987) Spaceborne Radar Remote Sensing: Applications and Techniques. IEEE Press, New York Francois C. & Ottle C. (1996) Atmospheric corrections in the thermal infrared: Global and water vapor dependent split-window algorithms - applications to ATSR and AVHRR data. IEEE Trans. Geosc. Rem Sens. K. A. (1981) Spectral albedos of an alpine snowpack. E. (1994) Earthwatch, the Climate from Space. John Wiley and Sons, Chichester, New York Ishimaru A.

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Remote Sensing in Hydrology and Water Management by Gert A. Schultz, Edwin T. Engman


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