Изотопный состав и регионы-источники зимних атмосферных осадков в Надымской низменности

Изотопный состав и регионы-источники зимних атмосферных осадков в Надымской низменности

Наталья Малыгина

Abstract

Приведены результаты изотопного анализа атмосферных осадков, отобранных в Надымской низменности (холодный период 2016-2017 г.), которые показали их значимые изменения (для δ¹⁸О на 21 ‰, для δD на 167 ‰). Локальная линия метеорных вод осадков описывается уравнением: δ²D=7,86×δ¹⁸О+2,4 (R²=0,99), а уравнение изотопно-температурной зависимости при использовании в расчетах значений температуры точки росы в момент выпадения осадков имеет вид: δ¹⁸O=0,67×Т_тр–15,2 (R²=0,67). На основе совместного анализа синоптических, траекторных и изотопных данных были определены основные регионы-источники поступления атмосферной влаги, выпавшей в виде осадков в Надымской низменности. Наибольший вклад внесли Атлантика (35,7%) и Северная Атлантика и Северный Ледовитый океан (30,4%); одну пятую часть определил Черноморско-Каспийский регион, а внутриконтинентальные регионы внесли наименьший вклад в поступление осадков (чуть более 10%).

Keywords

: зимние атмосферные осадки, Надымская низменность, стабильные изотопы кислорода и водорода,

About the Author

Наталья Малыгина

Федеральное государственное бюджетное учреждение науки Институт водных и экологических проблем Сибирского отделения РАН
Russian Federation

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