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Record #162981:

Momentum budget of the East Antarctic atmospheric boundary layer: results of a regional climate model / Michiel R. van den Broeke, N.P.M. van Lipzig, E. van Meijgaard.

Title: Momentum budget of the East Antarctic atmospheric boundary layer: results of a regional climate model / Michiel R. van den Broeke, N.P.M. van Lipzig, E. van Meijgaard.
Author(s): Broeke, Michiel R. van den.
Lipzig, N. P. M. van.
Meijgaard, E. van.
Date: 2002.
Abstract: Uses output of regional atmospheric climate model to quantify average January and July momentum budget of atmospheric boundary layer (ABL) over East Antarctic ice sheet and surrounding oceans. In January surface cooling is weak and large-scale pressure gradient force dominates ABL momentum budget. In July under conditions of strong surface cooling shallow katabatic jet develops over gentle slopes of interior ice sheet and strong, deep jet develops over steep coastal slopes. ABL thickens considerably in coastal regions due to piling up of cold air over adjacent sea ice and ice shelves, which represents main opposing force for katabatic winds. Horizontal and vertical advection are generally small. In cross-slope direction momentum budget represents simple balance between surface drag and Coriolis turning. Discusses intra-seasonal variability of large-scale wind field in ABL in relation to strength of polar vortex, background baroclinicity, and topography of ice sheet. Subsidence is found over interior ice sheet and rising motion in coastal zone, reflecting acceleration and deceleration of katabatic circulation. However, vertical velocities are generally small because downslope mass flux in ABL is confined to shallow layer below wind speed maximum.
Notes:

Offprint: Journal of the Atmospheric Sciences. Vol. 59(21) :3117-3129.

Keywords: 551.5 -- Meteorology.
551.55 -- Wind and air turbulence.
551.555.4 -- Katabatic winds, cold.
551.54 -- Atmospheric pressure.
519.673 -- Modelling.
D -- Atmospheric sciences.
(*7) -- Antarctic regions.
(*7.3) -- East Antarctica.
Location(s): SCO: SPRI-PAM: (*7) : 551.555.4
SPRI record no.: 162981

MARCXML

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005 20240329100319.0
007 ta
008 240329s2002####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-162981
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aBroeke, Michiel R. van den.
245 10 ‡aMomentum budget of the East Antarctic atmospheric boundary layer :‡bresults of a regional climate model /‡cMichiel R. van den Broeke, N.P.M. van Lipzig, E. van Meijgaard.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2002.
300 ## ‡ap. 3117-3129 :‡bdiags., table, maps.
500 ## ‡aOffprint: Journal of the Atmospheric Sciences. Vol. 59(21) :3117-3129.
520 3# ‡aUses output of regional atmospheric climate model to quantify average January and July momentum budget of atmospheric boundary layer (ABL) over East Antarctic ice sheet and surrounding oceans. In January surface cooling is weak and large-scale pressure gradient force dominates ABL momentum budget. In July under conditions of strong surface cooling shallow katabatic jet develops over gentle slopes of interior ice sheet and strong, deep jet develops over steep coastal slopes. ABL thickens considerably in coastal regions due to piling up of cold air over adjacent sea ice and ice shelves, which represents main opposing force for katabatic winds. Horizontal and vertical advection are generally small. In cross-slope direction momentum budget represents simple balance between surface drag and Coriolis turning. Discusses intra-seasonal variability of large-scale wind field in ABL in relation to strength of polar vortex, background baroclinicity, and topography of ice sheet. Subsidence is found over interior ice sheet and rising motion in coastal zone, reflecting acceleration and deceleration of katabatic circulation. However, vertical velocities are generally small because downslope mass flux in ABL is confined to shallow layer below wind speed maximum.
541 0# ‡aBroeke, M.R. van der (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 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aD -- Atmospheric sciences.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*7.3) -- East Antarctica.‡2udc
700 1# ‡aLipzig, N. P. M. van.
700 1# ‡aMeijgaard, E. van.
852 7# ‡2camdept‡bSCO‡cSPRI-PAM‡h(*7) : 551.555.4‡9Create 1 item record‡0Migrate
916 ## ‡a128232 -- 2003/02/21 -- HS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329 ‡bHS