Us. Bhatt et al., ATMOSPHERE-OCEAN INTERACTION IN THE NORTH-ATLANTIC - NEAR-SURFACE CLIMATE VARIABILITY, Journal of climate, 11(7), 1998, pp. 1615-1632
The impact of an interactive ocean on the midlatitude atmosphere is ex
amined using a 31-yr integration of a variable depth mixed layer ocean
model of the North Atlantic (between 20 degrees and 60 degrees N) cou
pled to the NCAR Community Climate model (CCM1). Coupled model results
are compared with a 31-yr control simulation where the annual cycle o
f sea surface temperatures is prescribed. The analysis focuses on the
northern fall and winter months. Coupling does not change the mean win
tertime model climatology (December-February); however, it does have a
significant impact on model variance. Air temperature and mixing rati
o variance increase while total surface heat flux variance decreases.
In addition, it is found that air-sea interaction has a greater impact
on seasonally averaged variance than monthly variance. There is an en
hancement in the persistence of air temperature anomalies on interannu
al timescales as a result of coupling. In the North Atlantic sector, s
urface air and ocean temperature anomalies during late winter are unco
rrelated with the following summer but are significantly correlated (0
.4-0.6) with anomalies during the following winter. These autocorrelat
ions are consistent with the ''re-emergence'' mechanism, where late wi
nter ocean temperature anomalies are sequestered beneath the shallow s
ummer mixed layer and are reincorporated into the deepening fall mixed
layer. The elimination of temperature anomalies from below the mixed
layer in a series of uncoupled sensitivity experiments notably reduces
the persistence of year-to-year anomalies. The persistence of air tem
perature anomalies on monthly timescales also increases with coupling
and is likely associated with ''decreased thermal damping.'' When coup
led to the atmosphere, the ocean is able to adjust to the overlying at
mosphere so that the negative feedback associated with anomalous heat
fluxes decreases, and air temperature anomalies decay more slowly.