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Further observations on sastrugi, snow dunes and the pattern of surface winds in Antarctica

Datos Bibliográficos

ID9219145
AutoresK B Mather (autor de correspondencia)
Año1962
Volumen11
Número71
Páginas158-171
Fecha de publicación1962-05-01
Open AccessSí
TipoARTICLE
RevistaPolar Record (JOURNAL)
Identificadores de la revistaISSN: 0032-2474 • E-ISSN: 1475-3057
EditorialCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0032247400052888
OpenAlexW2009963325
IdiomaEN
Citas recibidas1
Referencias citadas3

Surface winds are responsible for the two main types of feature observed on the Antarctic plateau: ( a ) sastrugi, produced by katabatic (gravity) winds, and ( b ) snow dunes, which are raised by blizzard winds. The two are often associated in the sense that the severest patches of sastrugi seem to be eroded out of dunes deposited by a previous blizzard. However, sastrugi are by no means limited to this; they may occur more or less continuously, merging one into the next over a wide area of plateau

Climatology · Geography · Geomorphology · Katabatic wind · Physical geography · Plateau (mathematics) · Prevailing winds · Sand dune stabilization · Snow · Snowmelt · Aeolian processes and effects · Geology · Geology and Paleoclimatology Research · Oceanography · Polar Research and Ecology

  • Experiences of Scott's Northern Party

    Open Access•David H Bromwich, Dennis D Kurtz•Polar Record•1982

  • Australian Antarctic Ice Thickness Measurements and Sastrugi Observations, Mac-Robertson Land, 1957–58

    Open Access•K B Mather, M J Goodspeed et al.•Polar Record•1959

Citas por año0,02
Intervalo de citas1982 - 1982 (1)
Altamente citadoNo

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