Estimation of the age of ice hummocks in the freezing seas

A method of estimating the ice ridge age proposed in the 1990s was analyzed and some disadvantages of this method were shown. Analysis of the ice thickness distribution in the ice ridges demonstrated that in many cases the average value of the thickness used in the above mentioned method did not cor...

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Main Authors: E. U. Mironov, V. S. Porubaev
Format: Article
Language:Russian
Published: Nauka 2019-09-01
Series:Лëд и снег
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Online Access:https://ice-snow.igras.ru/jour/article/view/579
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author E. U. Mironov
V. S. Porubaev
author_facet E. U. Mironov
V. S. Porubaev
author_sort E. U. Mironov
collection DOAJ
description A method of estimating the ice ridge age proposed in the 1990s was analyzed and some disadvantages of this method were shown. Analysis of the ice thickness distribution in the ice ridges demonstrated that in many cases the average value of the thickness used in the above mentioned method did not correspond to the thickness of an ice floe of which the ice blocks were formed. The ice floe thickness is characterized by the modal value of the ice thicknesses. After the ice ridge has been formed the ice block thickness in its above-water part does not change while the thickness of the ice floe on which the ice ridge is located continues to increase. Our study has shown that the difference between thickness of the plane ice and the modal value of the ice block thickness may be used as a characteristic of the ice growth for the period of the ice ridge existence. This period can be determined by one of the calculation formulas at the known initial and final ice thickness. Calculation by formula of the ice growth thickness make possible to derive the date of ice ridge formation based on the average air temperatures. The updated method of estimating the time of ice ridge formation can be used for the ice-covered seas. Analysis of the estimated ice ridge ages showed a significant dependence of thickness of the minimal consolidated layer on the time of the ice ridge formation. A comparative analysis of (the) ages of ice ridges and the flexural strength of ice samples made it possible to determine important tendency - the increased ice strength in ice ridges of early formation. This allows us in further studies to derive a formula of relationship between an ice ridge age and a strength of its ice. In some cases the ice strength measurement in ice ridges can be replaced by a less laborious estimating of strength basing on data of the age.
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spelling doaj-art-cea495c5962a42f09bd0549335ccf66b2025-08-20T03:00:45ZrusNaukaЛëд и снег2076-67342412-37652019-09-0159335536210.15356/2076-6734-2019-3-385428Estimation of the age of ice hummocks in the freezing seasE. U. Mironov0V. S. Porubaev1Arctic and Antarctic Research InstituteArctic and Antarctic Research InstituteA method of estimating the ice ridge age proposed in the 1990s was analyzed and some disadvantages of this method were shown. Analysis of the ice thickness distribution in the ice ridges demonstrated that in many cases the average value of the thickness used in the above mentioned method did not correspond to the thickness of an ice floe of which the ice blocks were formed. The ice floe thickness is characterized by the modal value of the ice thicknesses. After the ice ridge has been formed the ice block thickness in its above-water part does not change while the thickness of the ice floe on which the ice ridge is located continues to increase. Our study has shown that the difference between thickness of the plane ice and the modal value of the ice block thickness may be used as a characteristic of the ice growth for the period of the ice ridge existence. This period can be determined by one of the calculation formulas at the known initial and final ice thickness. Calculation by formula of the ice growth thickness make possible to derive the date of ice ridge formation based on the average air temperatures. The updated method of estimating the time of ice ridge formation can be used for the ice-covered seas. Analysis of the estimated ice ridge ages showed a significant dependence of thickness of the minimal consolidated layer on the time of the ice ridge formation. A comparative analysis of (the) ages of ice ridges and the flexural strength of ice samples made it possible to determine important tendency - the increased ice strength in ice ridges of early formation. This allows us in further studies to derive a formula of relationship between an ice ridge age and a strength of its ice. In some cases the ice strength measurement in ice ridges can be replaced by a less laborious estimating of strength basing on data of the age.https://ice-snow.igras.ru/jour/article/view/579arctic seasconsolidated layerice-covered seasice regimeice ridges
spellingShingle E. U. Mironov
V. S. Porubaev
Estimation of the age of ice hummocks in the freezing seas
Лëд и снег
arctic seas
consolidated layer
ice-covered seas
ice regime
ice ridges
title Estimation of the age of ice hummocks in the freezing seas
title_full Estimation of the age of ice hummocks in the freezing seas
title_fullStr Estimation of the age of ice hummocks in the freezing seas
title_full_unstemmed Estimation of the age of ice hummocks in the freezing seas
title_short Estimation of the age of ice hummocks in the freezing seas
title_sort estimation of the age of ice hummocks in the freezing seas
topic arctic seas
consolidated layer
ice-covered seas
ice regime
ice ridges
url https://ice-snow.igras.ru/jour/article/view/579
work_keys_str_mv AT eumironov estimationoftheageoficehummocksinthefreezingseas
AT vsporubaev estimationoftheageoficehummocksinthefreezingseas