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Vertical distribution of brine and volume structure thin one year ice Amur bay on base NMR and MRT dates
Author(s) -
N. A. Mel’nichenko,
N. A. Mel’nichenko,
Anton Viktorovich Tyuveev,
А В Тювеев,
A. Yu. Lazaryuk,
А Ю Лазарюк,
V. E. Savchenko,
V. E. Savchenko,
Elena Kustova,
Elena Kustova
Publication year - 2019
Publication title -
okeanologiâ
Language(s) - English
Resource type - Journals
ISSN - 0030-1574
DOI - 10.31857/s0030-1574595859-869
Subject(s) - sea ice thickness , sea ice , arctic ice pack , snow , brine , geology , bay , arctic , cryosphere , spatial distribution , snow cover , sea ice growth processes , fast ice , oceanography , physical geography , climatology , atmospheric sciences , geomorphology , chemistry , geography , remote sensing , organic chemistry
It was studying distribution of liquid and solid phases in pores one year sea ice on Amur Bay with using NMR and MRT methods in period 20132016. According to findings predominant factor in ice structure formation is snow cover. The patterns of brine content and solid phase distribution are considered in interdependence with air temperature and corresponding ice layer temperatures in compliance with preceding weather conditions. Differences in vertical profiles for temperature and salinity for winter and spring periods was marked. The main features of spatial phase dictribution in thin ice in comparision Arctic ice are presented. Just snow cover effects on ice parameters was demonstrated using data 20132016. The relationship of interlayings number in ice with its thickness, air temperature, and snow cover thickness is discussed. The main features of spatial phase dictribution in thin ice in comparision Arctic ice are presented. The empirical relation for calculations thin sea ice thickness was suggested.

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