Multiple equilibria in β-plane thermohaline convection / Paola Cessi, William R. Young.

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035 ## ‡aSPRI-126167
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aCessi, Paola.
245 10 ‡aMultiple equilibria in β-plane thermohaline convection /‡cPaola Cessi, William R. Young.
260 ## ‡aBerlin :‡bSpringer,‡c1993.
300 ## ‡ap. 375-393 :‡bdiags.
490 0# ‡aNATO ASI Series. Series I, Global environmental change ;‡v12
500 ## ‡aIn: Ice in the climate system / W. Richard Peltier, ed.
520 3# ‡aBuoyancy-driven circulation on β-plane with density determined by heat and salt concentration is studied. Flow is forced by prescribed temperature and salinity surface fluxes and there is no wind forcing. Examines zonally averaged model using Wiright and Stocker's (1992) parameterization for pressure difference between east and west coast, In limit of weak surface forcing, equation of motion can be further simplified by exploiting extreme aspect ratio of domain. Coupled set of amplitude equations governs evolution of vertically averaged temperature, and they exhibit linearly stable, multiple equilibria.
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465.45 -- Water masses.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
700 1# ‡aYoung, William R.
773 0# ‡7nnam ‡aW. Richard Peltier, ed. ‡tIce in the climate system. ‡dBerlin : Springer, 1993. ‡wSPRI-126141
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231130