Снежный покров как фактор роста годичных колец деревьев в контрастных природных условиях Западно-Сибирской равнины

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Проанализирована зависимость ширины годичных колец древесных растений зоны лесотундры и подзон северной тайги (лесная зона), южной лесостепи (лесостепная зона) и сухой степи (степная зона) от таких показателей снежного покрова, как максимальная толщина и водозапас, даты установления, разрушения и продолжительность залегания устойчивого снежного покрова. Для анализа применены данные государственных метеорологических станций Росгидромета (далее – МС) за 1966–2020 гг. (по лесотундре и северной тайге); 1966–2018 гг. (по лесостепи и сухой степи); материалы собственных дендрохронологических работ.

Об авторах

Н. И. Быков

Институт водных и экологических проблем СО РАН

Автор, ответственный за переписку.
Email: nikolai_bykov@mail.ru
Россия, Барнаул

А. А. Шигимага

Институт водных и экологических проблем СО РАН

Email: nikolai_bykov@mail.ru
Россия, Барнаул

Н. В. Рыгалова

Институт водных и экологических проблем СО РАН

Email: nikolai_bykov@mail.ru
Россия, Барнаул

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