@InProceedings{FischMacSilLyrDol:2004:CoBoLa,
author = "Fisch, Gilberto and Machado, Luiz Augusto Toledo and Silva Dias,
Maria Assuncao Faus da and Lyra, Roberto F. da Fonseca and Dolman,
Anton J.",
affiliation = "{CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil} and
{CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil} and
{CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil} and {} and
{}",
title = "The convective boundary layer over pasture in Amazonia during the
LBA Dry-to-Wet Experiment 2002",
booktitle = "Anais...",
year = "2004",
organization = "Conferencia Cientifica do LBA, 3.",
abstract = "The coupling between a typical ranchland and the Convective
Boundary Layer (CBL) has been investigated using radiosoundings at
8, 11, 14 and 17 Local Time (- 4 hours from GMT), as a part of
LBA/DRY-TO-WET 2002 experiment. The field campaign held from Sept
15 up to Oct 30, 2002, extending from the end of the dry season
(Sept) to the onset of the wet period (Oct). The profiles of
potential temperature and specific humidity have been used to
compute the mean properties of the CBL, as well as the height of
the CBL. The CBL height varied from a typical value around
2000-2200 m during the end of the dry season (Sept 18-20,2002) to
a figure around 1600-1800 m in the beginning of the wet period
(20-28,Oct). The potential temperature and humidity profiles did
not changed remarkable during this period, oscillating from 307 -
308 K and 12 - 14 g/kg. During the beginning of the wet season,
some local showers have occurred and produced a remarkable change
in the structure of the CBL. Some events have been analyzed. For
instance, on Sept 28,2002, the height of the CBL was around
1400-1500 m at 14 LT with a average potential temperature (q)
around 306 K and specific humidity (q) of 13.5 g/kg. After a very
strong rainfall (38 mm/3 hours) at afternoon, the CBL has been
destroyed (height around 500 m) with q of 300 K and q around 15-16
g/kg. There was also a nocturnal jet case (night from Sept 23-24)
with strong wind of 11 m/s at 500 m. This strong windshear created
an unexpected shallow mixed layer (height of 400 m) during the
night instead of the nocturnal/stable pattern. This data-set will
provide opportunity for modeling studies of the growing of the CBL
and coupling with aerosols and/or clouds.",
conference-location = "Brasilia",
conference-year = "27-29 jul.",
language = "en",
organisation = "LBA",
targetfile = "Fisch_Machado_LBA.pdf",
urlaccessdate = "19 abr. 2024"
}