Layer and crust development in a Central Sierra Nevada snowpack: some preliminary observations

TitleLayer and crust development in a Central Sierra Nevada snowpack: some preliminary observations
Publication TypeConference Proceedings
Year of Conference1982
AuthorsBerg, N. H.
Conference Name50th Annual Western Snow Conference
Series TitleProceedings of the 50th Annual Western Snow Conference
Date PublishedApril 1982
PublisherWestern Snow Conference
Conference LocationReno, Nevada
KeywordsCrusts, Ice layers, Snow hydrology, Snow stratigraphy
Abstract

Snow surface crusts and subsurface 'ice' layers densify exponentially. Crust thicknesses range form 4 to 10 cm; layer thicknesses are greater, ranging from 6 to 28 cm. Crusts exist on the majority of non-snowfall days and individually persist from 2 to 20 days. Layers may persist up to 50 days. All layers formed from burial of surface crusts under new snowfall. Pit studies show that layers can be discontinuous and that it is inappropriate to extrapolate point estimates of internal layer properties to wider areas.

URLsites/westernsnowconference.org/PDFs/1982Berg.pdf