An eddy-permitting 2-1/2-layer Reduced Gravity Ocean (RGO) model is
developed. Compared with the conventional 2-1/2-layer RGO models, the new model
has improvements in subsurface thermodynamics, vertical mixing scheme and open
boundary conditions. Using this new 2-1/2-layer RGO model as a dynamical tool, a
systematic investigation of the role of oceanic processes in controlling tropical Atlantic
sea-surface temperature (SST) response to Atlantic Meridional Overturning Circulation
(AMOC) changes is carried out by varying the strength of northward mass transport at
the open boundaries. It is found that the North Brazil Undercurrent (NBUC) reverses its
direction in response to a shut-down of the AMOC. Such circulation change allows
warm waters of the northern subtropical gyre enter the equatorial zone, giving rise to a
prominent warming in the Gulf of Guinea and off the coast of Africa. Sensitivity
experiments further show that the SST response behaves nonlinearly to AMOC changes.
The rate of SST changes increases dramatically when the AMOC strength is below a
threshold value. This nonlinear threshold behavior depends on the position of
subsurface temperature gradient. The new RGO is coupled to an atmosphere general
circulation model (AGCM) (CCM3.6). The coupled model is capable of capturing major
features of tropical Atlantic variability. With the aid of this coupled model, a series of
experiments with different combinations of oceanic and atmospheric processes are
carried out to elucidate the relative importance of the oceanic processes and atmospheric
processes in AMOC-induced tropical Atlantic variability/change. It is found that the oceanic processes are a primary factor contributing to the warming at and south of the
equator and the precipitation increase over the Gulf of Guinea, while atmospheric
processes are responsible for the surface cooling of the tropical north Atlantic and
southward displacement of ITCZ. The sensitivity of the coupled system to different
strength of the AMOC is further investigated. It is found that equatorial SST and
precipitation response also behaves nonlinearly to AMOC changes. The impact of
AMOC changes on Tropical Instability Waves (TIWs) is assessed. It is found that the
activity of TIWs is reduced in response to the AMOC-induced equatorial SST warming.
Correlation analysis suggests that AMOC may affect TIW activities by modifying SST
gradient north of the equator.
| Identifer | oai:union.ndltd.org:tamu.edu/oai:repository.tamu.edu:1969.1/ETD-TAMU-2009-08-2920 |
| Date | 2009 August 1900 |
| Creators | Wen, Caihong |
| Contributors | Chang, Ping |
| Source Sets | Texas A and M University |
| Language | en_US |
| Detected Language | English |
| Type | Book, Thesis, Electronic Dissertation, text |
| Format | application/pdf |
Page generated in 0.0025 seconds