Факторы формирования поверхностного притока к озерам антарктического оазиса Холмы Ларсеманн
https://doi.org/10.30758/0555-2648-2021-67-3-293-309
Аннотация
Объектами исследования являются 11 водоемов антарктического оазиса Холмы Ларсеманн. Работа выполнена по материалам сезонных работ 63 — 65-й РАЭ: используются наблюдения за уровнем воды озер, аэрофотосъемки БПЛА, маршрутные обследования, приведены результаты выделения границ водосборных площадей озер. Наиболее значимыми выявленными факторами, определяющими формирование притока воды к озерам, являются метеорологические условия (количество твердых осадков, ветровой режим, температура воздуха), наличие многолетних снежников и ледниковых участков на водосборах, прорыв верхнего в системе озера. Сезонно-талый слой рыхлых отложений регулирует склоновый сток по мере протаивания и промерзания. Особенностью оазиса является то, что на формирование стока практически не влияют растительный покров и антропогенная деятельность.
Ключевые слова
Об авторах
М. Р. КузнецоваРоссия
Санкт-Петербург
Г. В. Пряхина
Россия
Санкт-Петербург
С. Д. Григорьева
Россия
Санкт-Петербург
Э. Р. Киньябаева
Россия
Санкт-Петербург
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Рецензия
Для цитирования:
Кузнецова М.Р., Пряхина Г.В., Григорьева С.Д., Киньябаева Э.Р. Факторы формирования поверхностного притока к озерам антарктического оазиса Холмы Ларсеманн. Проблемы Арктики и Антарктики. 2021;67(3):293-309. https://doi.org/10.30758/0555-2648-2021-67-3-293-309
For citation:
Kuznetsova M.R., Priakhina G.V., Grigoreva S.D., Kiniabaeva E.R. Formation factors of surface inflow to antarctic lakes of the Larsemann Hills oasis. Arctic and Antarctic Research. 2021;67(3):293-309. (In Russ.) https://doi.org/10.30758/0555-2648-2021-67-3-293-309