The Diurnal Hysteresis of Snow Albedo

Abstract The appearance of a diurnal hysteresis in snow albedo is a widely reported phenomenon. This note discusses the relative importance of two separate effects: surface morphosis and surface irregularities (sastrugi). It is concluded that surface morphosis is the more important effect of the two...

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Published in:Journal of Glaciology
Main Authors: Mcguffie, K., Henderson-Sellers, A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1985
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000006456
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006456
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spelling crcambridgeupr:10.1017/s0022143000006456 2024-09-09T19:09:58+00:00 The Diurnal Hysteresis of Snow Albedo Mcguffie, K. Henderson-Sellers, A. 1985 http://dx.doi.org/10.1017/s0022143000006456 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006456 en eng Cambridge University Press (CUP) Journal of Glaciology volume 31, issue 108, page 188-189 ISSN 0022-1430 1727-5652 journal-article 1985 crcambridgeupr https://doi.org/10.1017/s0022143000006456 2024-08-21T04:04:46Z Abstract The appearance of a diurnal hysteresis in snow albedo is a widely reported phenomenon. This note discusses the relative importance of two separate effects: surface morphosis and surface irregularities (sastrugi). It is concluded that surface morphosis is the more important effect of the two in the region of the marginal cryosphere. Surface irregularities probably are the dominant influence only on permanent cryospheric areas such as the Greenland and Antarctic plateaux. Article in Journal/Newspaper Antarc* Antarctic Greenland Journal of Glaciology Cambridge University Press Antarctic Greenland Sastrugi ENVELOPE(163.683,163.683,-74.617,-74.617) Journal of Glaciology 31 108 188 189
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract The appearance of a diurnal hysteresis in snow albedo is a widely reported phenomenon. This note discusses the relative importance of two separate effects: surface morphosis and surface irregularities (sastrugi). It is concluded that surface morphosis is the more important effect of the two in the region of the marginal cryosphere. Surface irregularities probably are the dominant influence only on permanent cryospheric areas such as the Greenland and Antarctic plateaux.
format Article in Journal/Newspaper
author Mcguffie, K.
Henderson-Sellers, A.
spellingShingle Mcguffie, K.
Henderson-Sellers, A.
The Diurnal Hysteresis of Snow Albedo
author_facet Mcguffie, K.
Henderson-Sellers, A.
author_sort Mcguffie, K.
title The Diurnal Hysteresis of Snow Albedo
title_short The Diurnal Hysteresis of Snow Albedo
title_full The Diurnal Hysteresis of Snow Albedo
title_fullStr The Diurnal Hysteresis of Snow Albedo
title_full_unstemmed The Diurnal Hysteresis of Snow Albedo
title_sort diurnal hysteresis of snow albedo
publisher Cambridge University Press (CUP)
publishDate 1985
url http://dx.doi.org/10.1017/s0022143000006456
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000006456
long_lat ENVELOPE(163.683,163.683,-74.617,-74.617)
geographic Antarctic
Greenland
Sastrugi
geographic_facet Antarctic
Greenland
Sastrugi
genre Antarc*
Antarctic
Greenland
Journal of Glaciology
genre_facet Antarc*
Antarctic
Greenland
Journal of Glaciology
op_source Journal of Glaciology
volume 31, issue 108, page 188-189
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000006456
container_title Journal of Glaciology
container_volume 31
container_issue 108
container_start_page 188
op_container_end_page 189
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