Changes in atmospheric forcing can affect the subsurface water column of the ocean by three different mechanisms. First, warmed mixed-layer water that is subducted into the ocean interior will cause subsurfce warming; second, the subducted surface water can be freshened through changes in evaporation and precipitation; and third, the properties at a given depth may be changed by the vertical displacement of isotherms and isohalines without changes of water masses. Linear relations are derived for the relative strength of each process in terms of the observed changes of potential temperature and salinity in two different coordinate frames: 1) constant density surfaces, and 2) isobaric surfaces. -from Authors
History
Publication title
Journal of Physical Oceanography
Volume
24
Issue
6
Pagination
1137-1152:16
ISSN
1520-0485
Department/School
Australian Antarctic Program Partnership
Publisher
AMER METEOROLOGICAL SOC
Publication status
Published
Rights statement
Copyright 1994 AMS. Article is freely accessible on the publisher's website https://doi.org/10.1175/1520-0485(1994)024<1137:DCCAOV>2.0.CO;2