@Article{PezziCataChal:2006:SaObPa,
author = "Pezzi, Luciano Ponzi and Catalbiano, A. C. and Chalenor, P.",
affiliation = "Instituto Nacional de Pesquisas Espaciais (INPE), Centro de
Previs{\~a}o de Tempo e Estudos Clim{\'a}ticos (CPTEC)",
title = "Satellite observations of the Pacific tropical instability waves
characteristics and their interannual variability",
journal = "International Journal of Remote Sensing",
year = "2006",
volume = "27",
number = "08",
pages = "1581--1599",
month = "Apr.",
keywords = "tropical Instability waves, satellite, tropical Pacific, sea
surface temperature.",
abstract = "Descriptions of tropical instability wave (TIW) characteristics in
the tropical Pacific Ocean as a function of the large-scale
climate conditions and interannual variability, such as the El
Niņo southern oscillation, are made based on satellite data. As
others have found, the TIW ocean atmosphere coupling is caused by
atmospheric boundary layer instability and mixing. Our
observational investigation extends some of these previous
findings and suggests that this mechanism of coupled variability
of the wind and sea surface temperature may occur not only during
La Nina years, when TIWs are more active, but whenever the TIWs
are active. The sea surface temperature and height anomaly
covariability phase shift might occur also independent of the TIW
season activity. There is evidence that TIW activity increases
when under strengthened wind stress conditions either in La Nina
years or, by analogy, when oceanic numerical simulations are
carried out with stronger wind stress. Observational results show
larger TIW wavelengths and shorter periods when the ocean is under
the action of strengthened wind stress. On this observational
study this occurs when La Nina conditions prevail on the
equatorial Pacific.",
copyholder = "SID/SCD",
issn = "0143-1161",
language = "en",
targetfile = "Pezzi. satellite.pdf",
urlaccessdate = "11 maio 2024"
}