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Record #185778:

Antarctic bottom water variability in a coupled climate model / Agus Santoso, Matthew H. England.

Title: Antarctic bottom water variability in a coupled climate model / Agus Santoso, Matthew H. England.
Author(s): Santoso, Agus.
England, Matthew H.
Date: 2008.
In: Journal of Physical Oceanography. (2008.), Vol. 38(9) (2008)
Abstract: Provides extensive analysis of Antarctic Bottom Water (AABW) overturning and temperature-salinity variability on interannual to centennial times scales in long-term integration of coupled climate model, with particular reference to how variability in AABW overturning and properties is influenced by surface temperature-salinity conditions. Maximum rate of Atlantic sector Antarctic overturning is shown to represent outflow of Weddell Sea deep and bottom waters and compensating inflow of warm deep water (WDW). Variability of overturning is driven by surface density variability, which is in turn controlled by sea surface salinity (SSS), suggesting that SSS is better proxy than sea surface temperature for post-Holocene paleoclimate reconstructions of AABW overturning rate.
Notes:

Journal of Physical Oceanography. Vol. 38(9) :1870-1893 (2008).

Keywords: 551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
551.465.45 -- Water masses.
551.464.5 -- Salinity.
551.58 -- Climatology.
551.583 -- Climatic changes.
551.794 -- Holocene.
C -- Oceanography, hydrography and hydrology.
(*7) -- Antarctic regions.
(*80) -- Southern Ocean.
(*82) -- South Atlantic Ocean.
(*826) -- Weddell Sea.
SPRI record no.: 185778

MARCXML

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100 1# ‡aSantoso, Agus.
245 10 ‡aAntarctic bottom water variability in a coupled climate model /‡cAgus Santoso, Matthew H. England.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2008.
300 ## ‡ap. 1870-1893 :‡bill., diags., tables.
500 ## ‡aJournal of Physical Oceanography. Vol. 38(9) :1870-1893 (2008).
520 3# ‡aProvides extensive analysis of Antarctic Bottom Water (AABW) overturning and temperature-salinity variability on interannual to centennial times scales in long-term integration of coupled climate model, with particular reference to how variability in AABW overturning and properties is influenced by surface temperature-salinity conditions. Maximum rate of Atlantic sector Antarctic overturning is shown to represent outflow of Weddell Sea deep and bottom waters and compensating inflow of warm deep water (WDW). Variability of overturning is driven by surface density variability, which is in turn controlled by sea surface salinity (SSS), suggesting that SSS is better proxy than sea surface temperature for post-Holocene paleoclimate reconstructions of AABW overturning rate.
530 ## ‡aAlso issued online ‡uurn:doi:10.1175/2008JPO3741.1‡uhttps://dx.doi.org/10.1175/2008JPO3741.1
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.45 -- Water masses.‡2udc
650 07 ‡a551.464.5 -- Salinity.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*80) -- Southern Ocean.‡2udc
651 #7 ‡a(*82) -- South Atlantic Ocean.‡2udc
651 #7 ‡a(*826) -- Weddell Sea.‡2udc
700 1# ‡aEngland, Matthew H.
773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 38(9) (2008) ‡wSPRI-78712
916 ## ‡aHS
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220927 ‡bHS