@Article{RaoGiarEspiFran:2008:CoSuWi,
author = "Rao, Vadlamudi Brahmananda and Giarolla, Emanuel and Espirito
Santo, Clovis Monteiro do and Franchito, Sergio Henrique",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)} and
{Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)} and
{Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)} and
{Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)}",
title = "Comparison of surface wind stress characteristics over the
tropical Atlantic (10 degrees N-40 degrees S) in fields derived
from the UWM/COADS, NCEP/NCAR and QuikSCAT datasets",
journal = "Journal of Oceanography",
year = "2008",
volume = "64",
number = "4",
pages = "551--560",
month = "AUG.",
keywords = "wind stress,,ocean modeling, intertropical convergence zone,
UWM/COADS, NCEP/NCAR reanalysis, QuikSCAT dataset, climatology.",
abstract = "A comparison of monthly wind stress derived from winds of
NCEP/NCAR (National Centers for Environmental Prediction/National
Center for Atmospheric Research) reanalysis and UWM/COADS (The
University of Wisconsin -Milwaukee/Comprehensive Ocean-Atmosphere
Data Set) dataset (1950-1993), and of NCEP/NCAR reanalysis and
satellite-based QuikSCAT dataset (2000-2006), is made over the
South Atlantic (10 degrees N-40 degrees S). On a mean seasonal
scale, the comparison shows that these three wind stress datasets
have qualitatively similar patterns. Quantitatively, in general,
from about the equator to 20 degrees S in the mid-Atlantic the
wind stress values are stronger in NCEP/NCAR data than those in
UWM/COADS data. On the other hand, in the Intertropical
Convergence Zone (ITCZ) area the wind stress values in NCEP/NCAR
data are slightly weaker than those in UWM/COADS data. In the
South Atlantic, between 20 degrees S-40 degrees S, the QuikSCAT
dataset presents complex circulation structures which are not
present in NCEP/NCAR and UWM/COADS data. The wind stress is used
in a numerical ocean model to simulate ocean currents, which are
compared to a drifting-buoy observed climatology. The modeled
South Equatorial Current agrees better with observations between
March-May and June-August. Between December-February, the South
Equatorial Current from UWM/COADS and QuikSCAT experiments is
stronger and more developed than that from NCEP/NCAR experiment.
The Brazil Current, in turn, is better represented in the QuikSCAT
experiment. Comparison of the annual migration of ITCZ at 20
degrees and 30 degrees W in UWM/COADS and NCEP/NCAR data sources
show that the southernmost position of ITCZ at 30 degrees W in
February, March and April coincides with the rainy season in NE
Brazil, while the northernmost position of ITCZ at 20 degrees W in
August coincides with the maximum rainfall of Northwest Africa.",
copyholder = "SID/SCD",
issn = "0916-8370",
language = "en",
targetfile = "Rao_comparison.pdf",
urlaccessdate = "02 maio 2024"
}