Contribution Number Xxxx of Lamont D O H Erty E a R T H Observatory. 2

Numerical experiments are performed to examine the causes of variability of Atlantic Ocean SST during the period covered by the NCEP reanalysis (1958-1998). We use three ocean models. Two are mixed layer models, one with a 75m deep mixed layer and the other with a variable depth mixed layer. For both mixed layer models the ocean heat transports are assumed to remain at their diagnosed climatological values. The third model is a full dynamical ocean general circulation model (GCM). All models are coupled to a model of the subcloud atmosphericmixed layer (AML). The AMLmodel computes the air temperature and humidity by balancing surface uxes, radiative cooling, entrainment at cloud base, advection and eddy heat and moisture transports. The models are forced with NCEP monthly mean winds from 1958 to 1998. The ocean mixed layer models adequately reproduce the dominant pattern of Atlantic Ocean climate variability in both its spatial pattern and time dependence. This pattern is the familiar tripole of alternating zonal bands of SST anomalies stretching between the subpolar gyre and the subtropics. This SST pattern goes along with a wind pattern that corresponds to the North Atlantic Oscillation. Analysis of the results reveal that changes in wind speed create the subtropical SST anomalies while at higher latitudes changes in advection of temperature and humidity and changes in atmospheric eddy uxes are important. An observational analysis of the boundary layer energy balance is also performed. Anomalous atmospheric eddy heat uxes are very closely tied to the SST anomalies. Anomalous horizontal eddy uxes damp the SST anomalies while anomalous vertical eddy uxes tend to cool the entire mid-latitude North Atlantic during the NAO's high index phase with the maximum cooling exactly where the SST gradient is strengthened the most.