TY - JOUR
T1 - Rectified effects of tropical instability wave (TIW)-induced atmospheric wind feedback in the tropical Pacific
AU - Zhang, Rong Hua
AU - Busalacchi, Antonio J.
PY - 2008/3/16
Y1 - 2008/3/16
N2 - Recent high-resolution space-based observations reveal significant two-way air-sea interactions associated with tropical instability waves (TIWs) in the tropical oceans. But in most large-scale climate modeling studies, the atmospheric wind response to TIW-induced sea surface temperature (SSTTTW) anomalies has not been taken into account realistically and thus the corresponding feedbacks to the ocean are not known. Here we apply a singular value decomposition (SVD) analysis to satellite data to derive an empirical model for the SSTTTW induced wind stress (ΤTIW) variability in the eastern tropical Pacific. The derived SSTTIW-ΤTIW relationship is then nested into a basin-scale ocean and a hybrid coupled ocean-atmosphere model of the tropical Pacific to take into account the TIW-induced wind-SST coupling. It is demonstrated that TIW-induced wind feedback to the ocean can have a rectified effect on large-scale mean ocean state and interannual variability, with an asymmetric difference in SST (a cooling) and a significant modulation of ENSO amplitude.
AB - Recent high-resolution space-based observations reveal significant two-way air-sea interactions associated with tropical instability waves (TIWs) in the tropical oceans. But in most large-scale climate modeling studies, the atmospheric wind response to TIW-induced sea surface temperature (SSTTTW) anomalies has not been taken into account realistically and thus the corresponding feedbacks to the ocean are not known. Here we apply a singular value decomposition (SVD) analysis to satellite data to derive an empirical model for the SSTTTW induced wind stress (ΤTIW) variability in the eastern tropical Pacific. The derived SSTTIW-ΤTIW relationship is then nested into a basin-scale ocean and a hybrid coupled ocean-atmosphere model of the tropical Pacific to take into account the TIW-induced wind-SST coupling. It is demonstrated that TIW-induced wind feedback to the ocean can have a rectified effect on large-scale mean ocean state and interannual variability, with an asymmetric difference in SST (a cooling) and a significant modulation of ENSO amplitude.
UR - https://www.scopus.com/pages/publications/43549093331
U2 - 10.1029/2007GL033028
DO - 10.1029/2007GL033028
M3 - Article
AN - SCOPUS:43549093331
SN - 0094-8276
VL - 35
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 5
M1 - L05608
ER -