Springtime Precipitation and Water Vapor Flux over Southeastern South America

Wang and Paegle (1996) found that primarily due to large uncertainties in wind analyses, and consequently in the moisture flux convergence, estimates of moisture budgets from different global analysis datasets have considerable disagreement. [...]the uncertainty is not reduced by using the more rece...

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Published in:Monthly weather review 2000-05, Vol.128 (5), p.1328-1346
Main Authors: Berbery, Ernesto H, Collini, Estela A
Format: Article
Language:English
Subjects:
Agricultural production
Budgets
Climate studies
Hydrologic cycle
Mesoscale convective complexes
Meteorology
Mountains
Orography
Precipitation
South America
Studies
Water vapor
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Collini, Estela A
description Wang and Paegle (1996) found that primarily due to large uncertainties in wind analyses, and consequently in the moisture flux convergence, estimates of moisture budgets from different global analysis datasets have considerable disagreement. [...]the uncertainty is not reduced by using the more recent reanalysis products, as noted by Higgins et al. Orography can then be defined as ''steps'' that are particularly well suited to reproduce sharp slopes like those of the Andes Mountains. [...]it is not unexpected that an adapted version of NCEP's Eta Model is currently being used operationally at the Brazilian Center forWeather Forecasts and Climate Studies.\n The lack of precipitation over the Atlantic may be due to the proximity of the northern and eastern model boundary, which in turn may also relate to precipitation overprediction over northeast Brazil.
doi_str_mv 10.1175/1520-0493(2000)128<1328:SPAWVF>2.0.CO;2
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subjects Agricultural production
Budgets
Climate studies
Hydrologic cycle
Mesoscale convective complexes
Meteorology
Mountains
Orography
Precipitation
South America
Studies
Water vapor
title Springtime Precipitation and Water Vapor Flux over Southeastern South America
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