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Record #165338:

Diagnosis of the katabatic wind influence on the wintertime Antarctic surface wind field from numerical simulations / Thomas R. Parish, John J. Cassano.

Title: Diagnosis of the katabatic wind influence on the wintertime Antarctic surface wind field from numerical simulations / Thomas R. Parish, John J. Cassano.
Author(s): Parish, Thomas R.
Cassano, John J.
Date: 2003.
Abstract: Presents results of two numerical simulations of low-level wind field over Antarctica, with daily numerical simulations for midwinter month July 2001. Analyses of katabatic forcing showed it was significant component of total horizontal pressure gradient force over interior of continent, though near coast and extending several hundred kilometres inland effects of ambient pressure gradient force were typically comparable to katabatic forcing and often considerably more important. This suggests that role of topography in shaping Antarctic boundary layer wind through blocking and subsequent adjustment is critical to establishment of low-level wintertime Antarctic wind field.
Notes:

Offprint: Monthly Weather Review. Vol. 131(6) :1128-1139.

Keywords: 551.5 -- Meteorology.
551.55 -- Wind and air turbulence.
551.555.4 -- Katabatic winds, cold.
551.54 -- Atmospheric pressure.
551.555 -- Winds of special localities.
551.4 -- Geomorphology.
519.673 -- Modelling.
91(08) -- Expeditions: 1955- US Antarctic Program.
D -- Atmospheric sciences.
(*7) -- Antarctic regions.
Location(s): SCO: SPRI-PAM: (*7) : 551.555.4
SPRI record no.: 165338

MARCXML

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100 1# ‡aParish, Thomas R.
245 10 ‡aDiagnosis of the katabatic wind influence on the wintertime Antarctic surface wind field from numerical simulations /‡cThomas R. Parish, John J. Cassano.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2003.
300 ## ‡ap. 1128-1139 :‡bdiags., maps.
500 ## ‡aOffprint: Monthly Weather Review. Vol. 131(6) :1128-1139.
520 3# ‡aPresents results of two numerical simulations of low-level wind field over Antarctica, with daily numerical simulations for midwinter month July 2001. Analyses of katabatic forcing showed it was significant component of total horizontal pressure gradient force over interior of continent, though near coast and extending several hundred kilometres inland effects of ambient pressure gradient force were typically comparable to katabatic forcing and often considerably more important. This suggests that role of topography in shaping Antarctic boundary layer wind through blocking and subsequent adjustment is critical to establishment of low-level wintertime Antarctic wind field.
541 0# ‡aParish, T.R. (gift)‡5UkCU-P
650 07 ‡a551.5 -- Meteorology.‡2udc
650 07 ‡a551.55 -- Wind and air turbulence.‡2udc
650 07 ‡a551.555.4 -- Katabatic winds, cold.‡2udc
650 07 ‡a551.54 -- Atmospheric pressure.‡2udc
650 07 ‡a551.555 -- Winds of special localities.‡2udc
650 07 ‡a551.4 -- Geomorphology.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a91(08) -- Expeditions: 1955- US Antarctic Program.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
700 1# ‡aCassano, John J.
852 7# ‡2camdept‡bSCO‡cSPRI-PAM‡h(*7) : 551.555.4‡9Create 1 item record‡0Migrate
916 ## ‡a129026 -- 2003/07/29 -- HS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231001 ‡bHS