Open AccessOverview of atmospheric conditions during the Smoke, Clouds, and Radiation‐Brazil (SCAR‐B) field experiment
Author(s) -
Nobre Carlos A.,
Mattos Luiz F.,
Dereczynski Claudine P.,
Tarasova Tatiana A.,
Trosnikov Igor V.
Publication year - 1998
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/98jd00992
Subject(s) - environmental science , atmospheric sciences , dryness , aerosol , atmosphere (unit) , cloud cover , climatology , haze , overcast , single scattering albedo , albedo (alchemy) , meteorology , sky , geology , geography , medicine , art , surgery , performance art , computer science , operating system , cloud computing , art history
The Smoke, Clouds, and Radiation‐Brazil (SCAR‐B) field experiment was conducted in central Brazil and southern Amazonia during the period August 15 to September 20, 1995. This paper presents an overview of atmospheric conditions during the SCAR‐B period. A meteorological office was established in Brasília to support the mission flights and field activities. All the meteorological data collected during the SCAR‐B have been archived and are available to the scientific community. The meteorological conditions throughout the SCAR‐B period of August and September 1995 were near climatological conditions. Few synoptic‐scale waves traveling from southeastern Pacific reached Brazil, therefore the SCAR‐B period was characterized by long periods of low humidity, dryness, little cloudiness, or rain, and haze events. The stable situation was interrupted due to the penetration of a frontal system on September 20, 1995, and a second and more rain‐producing one on September 28, 1995. Those two frontal systems in a period of 10 days brought an end to the dry season. Air particle trajectories show that most of the smoke below 4 km from Amazonia was transported to the south and then to the east exiting the continent at 25°S–30°S. Radiative transfer calculations carried out for the clear sky gaseous and aerosol atmosphere show the decrease of the solar radiation absorption in the atmosphere‐surface system due to smoke aerosol loading at the value from 5 to 50 W m −2 depending on the aerosol optical thickness, single‐scattering albedo, and solar zenith angle.