ІЛЕ АЛАТАУЫНЫҢ СОЛТҮСТІК БАУРАЙЫНДАҒЫ ОРТАЛЫҚ ТҰЙЫҚСУ МҰЗДЫҒЫ МАССАСЫНЫҢ БАЛАНСЫ МЕН КИНЕМАТИКАСЫ
DOI:
https://doi.org/10.54668/2789-6323-2024-115-4-91-110Кілт сөздер:
Солтүстік Тянь-Шань, Орталық Тұйықсу мұздығы, мұздық кинематикасы, мұздың қозғалу жылдамдығы, мұздық массасының балансыАңдатпа
2006...2023 жылдар аралығында Орталық Тұйықсу мұздығында тікелей бақылаулар жүргізіліп, соның негізінде сыртқы және ішкі масса алмасу компоненттерінің есептеулері жасалынды, осы есептеулер 1958...1972 және 1977...1992 жылдардағы алынған мәндермен салыстырылды. Масса балансының кинематикалық компоненттерін анықтау үшін жергілікті жерге геодезиялық байланысы бар мұзға бұрғыланған рейкалар қолданылды. Қарастырылып отырған кезеңде мұздық 420 метрге шегінген, масса балансы орта есеппен -0,54 м. с.э., құраса, барлық бақылау кезеңінде, яғни 1958 жылдан бастап, мұздық 1190 м-ге шегінді, ал 1956...2023 жылдардағы масса балансының орташа мәні -0,42 м. с.э. 2006...2023 жылдар кезеңінде кинематикалық қоректену аймағындағы (КҚА) жылдық масса балансы + 0,13 м құрады, сол кезеңде осы аймақтағы абляцияның кинематикалық аймағындағы мұзды шығару -1,24 м құрады, ал КҚА ауданы 17 % - ға өсті, ал абляцияның кинематикалық аймағы (АКА) 46,3 % - ға қысқарды. КҚА мұздың түсуі 1977/78...1991/92 жылдар аралығында АКА-дағы шығындардың жартысының ғана (49,5 %) орнын толтырса, 2006/07...2022/23 жылдар аралығында 75,9 % - ға дейін орнын толтырды. Орталық Тұйықсу мұздығындағы мұз қозғалысының максималды жылдамдығы 1956...65 жылдарда байқалды, ол жылдары жылдамдық жылына 22...24 м\ж құрады, ал 1977...1992 жылдар аралығында 16 м/ж дейін төмендеді, ал 2006...2023 жылдар кезеңінде 12,8 м/ж құрады.
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