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Inter-comparison of the solar UVB,UVA and global radiation clearness and UV indices for Beer Sheva and Neve Zohar (Dead Sea), Israel
Affiliation:1. SINTEF Building and Infrastructure, Trondheim Norway;2. Norwegian University of Science and Technology, Trondheim Norway;1. Research Institute of Basic Sciences, Chungnam National University, Daejeon, Republic of Korea;2. Department of Physics, University of Toronto, Toronto, Ontario, Canada;3. Department of Atmospheric Sciences, Yonsei University, Seoul, Republic of Korea;1. Masaryk University, Faculty of Science, Department of Geography, Kotlá?ská 2, 611 37 Brno, Czech Republic;2. Czech Geological Survey, Brno Branch, Leitnerova 22, 658 69 Brno, Czech Republic;1. University of Latvia, Raina blvd. 19, Riga, Latvia
Abstract:An inter-comparison of the clearness indices for the solar UVB, UVA and global radiation for Beer Sheva and Neve Zohar (Dead Sea) are presented utilizing radiation data measured from January 1995 through December 2001 for which there is a one-to-one correspondence between the measurements, viz., any day for which a hourly value for one of the sites was missing is rejected and not included in the analysis for that particular radiation type. Beer Sheva is located ca. 65 km to the west and is approximately 700 m above Neve Zohar, which is located on the western shore of the Dead Sea. The Dead Sea is the lowest terrestrial point on the earth, approximately 400 m below mean sea level. The relative magnitudes of the global, UVB and UVA radiation intensities at the two sites can be attributed to the enhanced scattering at the Dead Sea due to the longer optical path length the solar radiation must traverse at the Dead Sea. The degree of attenuation due to scattering phenomena is inversely proportional to the wavelength raised to some power and, consequently, it is greatest for UVB and very small for global radiation. The UVB and UVA solar constants were determined from the extraterrestrial radiation values tabulated by Fröhlich and Wehrli Spectral distribution of solar irradiance from 25000 nm to 250nm, in: M. Iqbal, An introduction to solar radiation, Academic Press, New York, 1981, Appendix C, pp. 380–381]. The clearness indices for global and UVA radiation were of similar magnitude, whereas those for UVB radiation were of two orders of magnitude smaller. In addition, the monthly average hourly UV Index at both sites has also been determined and an inter-comparison of the values has been performed for all available hourly values from January 1995 through August 2002 for both sites. It is observed that the monthly average hourly UV Index values at the Dead Sea are never in the extreme range.
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