Abstract
Remote sensing, encompassing the study of satellite data and aerial photographs, is an extremely powerful technique for earth resources exploration, mapping and management. It involves measurements of electromagnetic (EM) radiation in the wavelength range of about 0.4 µm–1 m, from sensors flying on aerial or space platforms to characterize and infer properties of the terrain. Remote sensing has evolved primarily from the methods of aerial photography and photo-interpretation used extensively in 1950s–1960s. The technique has grown rapidly during the last four to five decades. In the context of groundwater studies, remote sensing is of great value as a very first reconnaissance tool, the usual sequence of investigations being: satellite images—aerial photographs—geophysical survey—drilling.
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Further Reading
Becker MW (2006) Potential for satellite remote sensing of ground water. Ground Water, Vol. 44(20), pp. 306–318.
Gupta RP (2003) Remote Sensing Geology. 2nd ed., Springer-Verlag, 655 p.
Lillesand T, Kiefer RW, Chipman J (2007) Remote Sensing and Image Interpretation. 6th ed., John Wiley, 1164 p.
Meijerink AMJ, Bannert D, Batelaan O, Lubcyznski MW, Pointet T (2007) Remote Sensing Applications to Groundwater. IHP-VI, Series on Groundwater No. 16, UNESCO, Paris, 312 p.
Waters P, Greenbaum D, Smart PL, Osmaston H (1990) Applications of remote sensing to groundwater hydrology. Remote Sensing Reviews. Vol. 4(2), pp. 223–264.
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Singhal, B.B.S., Gupta, R.P. (2010). Remote Sensing. In: Applied Hydrogeology of Fractured Rocks. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-8799-7_4
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DOI: https://doi.org/10.1007/978-90-481-8799-7_4
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