@Article{MachadoLiViMoAnLa:2006:TeApSa,
author = "Machado, Luiz Augusto Toledo and Lima, Wagner Flauber Araujo and
Vila, Daniel and Morales, C. R. and Angelis, Carlos Frederico and
Laurent, H.",
affiliation = "Instituto Nacional de Pesquisas Espaciais (INPE), Centro de
Previs{\~a}o de Tempo e Estudos Clim{\'a}ticos (CPTEC) and
Instituto Nacional de Pesquisas Espaciais (INPE), Centro de
Previs{\~a}o de Tempo e Estudos Clim{\'a}ticos (CPTEC) and
Instituto Nacional del Agua, INA, Argentina and Instituto
Astron{\^o}mico e Geof{\'{\i}}sico, IAG/USP and Instituto
Nacional de Pesquisas Espaciais (INPE), Centro de Previs{\~a}o de
Tempo e Estudos Clim{\'a}ticos (CPTEC) and Institut de Recherche
pour le D{\'e}veloppement IRD, France",
title = "Forecasting and tracking of the evolution of cloud cluster
(ForTraCC): The technique applied to satellite and the integration
with radar and lightning data",
journal = "Geophysical Research Abstracts",
year = "2006",
volume = "8",
pages = "SRef-ID: 1607--7962/gra/EGU06--A-01512",
month = "Apr.",
keywords = "meteorology satellite, FORTRACC, radar, electrical activity,
cycle.",
abstract = "The relationship between convective system area expansion, at the
initiation stage, and the life cycle duration allows this
parameter to be used as a tool for nowcasting. The area expansion
reaches its maximum value during the initiation stage of the
convec- tive systems and later, the upper level wind divergence
reaches its maximum, at or just before to the mature stage. The
maximum area expansion occurs close to the time of maximum
precipitation and about 4 hours before the maximum cold cloud
fraction at the same threshold. Also, the area expansion can be
used to determine the convective system life stage and to supply
information about the condensation processes and the upper level
wind divergence. The average area expansion at the initiation
stage varies exponentially with the life cycle duration. This work
introduces the operational prod- uct FORTRACC (FORecasting and
TRAcking of the evolution of Cloud Clusters) used to describe the
convective systems life cycle and its nowcasting. The results
using GOES IR image and radar CAPPI 3 km are presented to describe
the performance of this technique. Finally, it presents the
preliminary results of different techniques used by CPTEC for
nowcasting, as for example: the combination of IR and WV channel
to predict lightning activity, the application of ascend/descend
cloud top rate, using weather radar, to forecast the convection
intensity and duration of convective cells and the combination of
FORTRACC with the information of lightning activity, allowing to
describe the evolution of electrical activity during the
convective system life cycle.",
copyholder = "SID/SCD",
issn = "1029-7006",
language = "en",
targetfile = "Machado.forecasting.pdf",
urlaccessdate = "16 jun. 2024"
}