@InProceedings{FigueroaTarBarBonSil:2006:ImCuRa,
author = "Figueroa, Silvio Nilo and Tarasova, Tatiana and Barbosa, Henrique
Melo Jorge and Bonatti, Jose Paulo and Silvia Dias, Pedro Leite",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)}",
title = "The impact of cumulus and radiation parameterization schemes on
Southern Hemisphere summer climate simulated by CPTEC Atmospheric
General Circulation Model",
booktitle = "Proceedings...",
year = "2006",
editor = "Vera, Carolina and Nobre, Carlos",
pages = "1037--1040",
organization = "International Conference on Southern Hemisphere Meteorology and
Oceanography, 8. (ICSHMO).",
publisher = "American Meteorological Society (AMS)",
address = "45 Beacon Hill Road, Boston, MA, USA",
keywords = "Atmospheric general circulation model, cumulus parameterization,
radiation parameterization, South Atlantic Convergence Zone, South
Pacific Convergence Zone.",
abstract = "The Southern Hemisphere summer climate is primarily influenced by
the Indonesian, African and Amazon intense convection; South
Pacific Convergence Zone (SPCZ) and South Atlantic Convergence
Zone (SACZ); low pressures over western Australia, southern South
America (Gran Chaco) and southern Africa. Numerical experiments
with different cumulus and solar radiation parameterization
schemes were performed using a CPTEC Atmospheric global
circulation model (CPTEC-AGCM) to study the impact of different
physical processes on Southern Hemisphere summer climate. The
CPTEC-AGCM in comparison with CPTEC/COLA-AGCM contains: a new
dynamic code, three cumulus schemes (KUO, Relaxed
Arakawa-Schubert, and Grell-ensemble modified by Figueroa, called
here Grell2), two shallow convection schemes (Tiedke and Souza)
and two solar radiation schemes (of Lacis and Hansen called here
Rad1 and Clirad-sw of Chou and Suarez and modified by Tarasova and
Fomin, called here Rad2). All remaining physical processes are
similar to CPTEC/COLA AGCM. The horizontal resolution of the model
is triangular 62 (T62), and vertical resolution is 28 levels
(L28).The surface temperature is prescribed, which is updated
daily by linear interpolation between monthly climatological
blended data sets. The initial conditions were obtained from NCEP
analysis. The integration is carried out for 5 years for each
experiment. The results for different summers are similar. These
results show the importance of convection scheme (deep and
shallow) for tropical convection and subtropical convergence
zones, and radiation scheme for subtropical low pressures. The
main impact of Rad2 in comparison with rad1 is the reduction of
downward solar radiation at the surface by approximately 50 W/m2
in the subtropical region. Our conclusion is that the better
simulation of Southern Hemisphere summer climate is by combination
Grell2 for deep convection, Souza for shallow convection and Rad2
for solar radiation.",
conference-location = "Foz do Igua{\c{c}}u",
conference-year = "24-28 Apr. 2006",
copyholder = "SID/SCD",
language = "en",
organisation = "American Meteorological Society (AMS)",
ibi = "cptec.inpe.br/adm_conf/2005/10.31.23.00",
url = "http://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/10.31.23.00",
targetfile = "1037-1040.pdf",
type = "Monsoon systems and continental rainfall",
urlaccessdate = "23 abr. 2024"
}