In this section
@article{Czaja:2004:10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2,
author = {Czaja, A},
doi = {10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2},
journal = {Journal of Climate},
pages = {3017--3025},
title = {Why is north tropical Atlantic SST variability stronger in boreal spring?},
url = {http://dx.doi.org/10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2},
volume = {17},
year = {2004}
}
TY - JOUR
AB - It is suggested that the seasonal dependence of interannual variability displayed by observed sea surface temperature (SST) over the north tropical Atlantic primarily reflects the seasonality of the remote forcing associated with the North Atlantic and Southern Oscillations and is controlled by the mean damping time scale of SST anomaly. A stochastic model including a seasonally dependent forcing is used to test this hypothesis against observations. © 2004 American Meteorological Society.
AU - Czaja,A
DO - 10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2
EP - 3025
PY - 2004///
SN - 0894-8755
SP - 3017
TI - Why is north tropical Atlantic SST variability stronger in boreal spring?
T2 - Journal of Climate
UR - http://dx.doi.org/10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2
VL - 17
ER -