Water vapor in the pore space of snow

Sokratov, S.A.; Sato, A.; Kamata, Y.

Информация о цитировании статьи получена из Web of Science, Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 18 июля 2013 г.

Авторы: Sokratov S.A., Sato A., Kamata Y.
Журнал: Annals of Glaciology
Том: 32
Год издания: 2001
Издательство: International Glaciological Society
Местоположение издательства: United Kingdom
Первая страница: 51
Последняя страница: 58
DOI: 10.3189/172756401781819111
Аннотация: Water vapor in snow is responsible for two main processes connected to almost all studies where snow cover is involved: the snow-density change with time and snow recrystallization. Both processes are the result of a balance between evaporation and condensation on individual snow-crystal surfaces. However, such micro-scale mass balance has rarely been considered as a component of "macro-" heat and mass transfer in snow cover. The present work is an attempt to find a way of combining these two mass-exchange processes, as occurs in Nature. Density change and snow recrystallization rates are analyzed based on recently published temperature field observations around individual snow crystals, combined with experimental data on temperature distributions and recrystallization rates in snow under applied temperature gradients.
Добавил в систему: Сократов Сергей Альфредович

	ИСТИНА	Войти в систему Регистрация
	ИСТИНА ЦЭМИ РАН
	Главная Поиск Статистика О проекте Помощь

ИСТИНА

ИСТИНА ЦЭМИ РАН

Water vapor in the pore space of snowстатья

Прикрепленные файлы