Determination of Snow Water Equivalent by the Atmospheric Beta-Background

Bibliographic Details
Parent link:AIP Conference Proceedings
Vol. 2101 : Isotopes: Technologies, Materials and Application (ITMA-2018).— 2019.— [020010, 8 p.]
Corporate Author: Национальный исследовательский Томский политехнический университет Инженерная школа ядерных технологий Отделение ядерно-топливного цикла
Other Authors: Belyaeva I. Irina, Yakovlev G. Grigorii, Zelinskiy A. Aleksey, Yakovleva V. S. Valentina Stanislavovna
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
Published: 2019
Subjects:
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

MARC

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330 |a 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. 
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