Download e-book for iPad: Advances in Geoscience and Remote Sensing by GARY JEDLOVEC

By GARY JEDLOVEC

ISBN-10: 9533070056

ISBN-13: 9789533070056

Distant sensing is the purchase of data of an item or phenomenon, via both recording or real-time sensing device(s), that's not in actual or intimate touch with the article (such as in terms of airplane, spacecraft, satellite tv for pc, buoy, or ship). In perform, distant sensing is the stand-off assortment by using quite a few units for accumulating details on a given item or region. Human life relies on our skill to appreciate, make the most of, deal with and continue the surroundings we are living in - Geoscience is the technological know-how that seeks to accomplish those targets. This ebook is a suite of contributions from world-class scientists, engineers and educators engaged within the fields of geoscience and distant sensing.

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2000). Ice in the Ocean, Gordon and Breach Science Publishers, ISBN 90-5699296-1, Amsterdam, The Netherlands. ; Nakamura, K. & Nishio, F. (2004). Polarimetric characteristics of sea ice in the Sea of Okhotsk observed by airborne L-band SAR, IEEE Trans. Geosci. Remote Sensing, Vol. 42, No. 11, 2412-2425. ; Campbell, W. & Edgerton, A. (1972). Aircraft measurements of microwave emission from Arctic sea ice, Remote Sensing of Environment, Vol. 129-139. ; Wen, B & West, R. (1989). Sea ice characterization measurements needed for testing of microwave remote sensing models, IEEE J.

This system was also deployed in the Sea of Okhotsk in 1991. Monitoring of the ice thickness distribution in the southern Sea of Okhotsk has continued since then from the icebreaker P/V “Soya”, in collaboration with the Japan Coast Guard. Based on the data set obtained from 1991 to 2000, Toyota et al. (2004) showed that the thickness distribution follows a near Poisson distribution with an average of 33±10 cm, and proposed a stochastic rafting cycle model, referring to the layered structure. , 2003) and confirmed that the thickness distribution of these two methods matches well within the range of a few percent for non-ridged ice.

G. , 1984; Comiso, 1986). On the other hand, this has not necessarily been the case with ice thickness. , 1981; Grenfell and Comiso, 1986). Thus in a practical sense, the signals received by this sensor originate from the top few centimetres of sea ice and cannot include the direct information of ice thickness. Even so, if there are any surface dielectric properties of sea ice that do correlate well with ice thickness, they differentiate the emissivity and then allow the estimation of ice thickness.

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Advances in Geoscience and Remote Sensing by GARY JEDLOVEC


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