Determination of Snow Water Equivalent by the Atmospheric Beta-Background
| Parent link: | AIP Conference Proceedings Vol. 2101 : Isotopes: Technologies, Materials and Application (ITMA-2018).— 2019.— [020010, 8 p.] |
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| Corporate Author: | |
| Other Authors: | , , , |
| Summary: | Title screen The paper presents the results of the long-term monitoring of beta-radiation flux density in the background atmosphere in Tomsk Observatory of Radioactivity and Ionizing Radiation by using beta-radiation detectors installed at different heights up to 35 m from the earth's surface. Analysis of seasonal variations of beta-background and characteristics of snow revealed that the specific of decreasing of beta-radiation flux density is similar to specific of increasing the snow water equivalent. Seasonal minimums of beta-radiation flux density, regardless of the height of measurement, better correspond to the maximums of snow water equivalent then to snow cover thickness. As a result of investigation a BetaSnow method for estimating the moisture content of snow cover based on measurements of the atmospheric beta-background was developed and described in detail. Режим доступа: по договору с организацией-держателем ресурса |
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2019
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| Online Access: | https://doi.org/10.1063/1.5099602 |
| Format: | Electronic Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=660280 |
| Summary: | Title screen The paper presents the results of the long-term monitoring of beta-radiation flux density in the background atmosphere in Tomsk Observatory of Radioactivity and Ionizing Radiation by using beta-radiation detectors installed at different heights up to 35 m from the earth's surface. Analysis of seasonal variations of beta-background and characteristics of snow revealed that the specific of decreasing of beta-radiation flux density is similar to specific of increasing the snow water equivalent. Seasonal minimums of beta-radiation flux density, regardless of the height of measurement, better correspond to the maximums of snow water equivalent then to snow cover thickness. As a result of investigation a BetaSnow method for estimating the moisture content of snow cover based on measurements of the atmospheric beta-background was developed and described in detail. Режим доступа: по договору с организацией-держателем ресурса |
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| DOI: | 10.1063/1.5099602 |