Using NOAA/AVHRR Products to Monitor El Nio Impacts: Focus on Indonesia in 199798

Using NOAA/AVHRR Products to Monitor El Nio Impacts: Focus on Indonesia in 199798 The development of the El Nio-Southern Oscillation (ENSO) in 199798, the most intense in this century, has been monitored by space- and ground-based observations. In this study, the authors present the signatures of ENSO impacts on the surfaceatmosphere system, as detected in satellite products that are routinely derived at NOAA from measurements by a single instrument on board NOAA polar-orbiting satellitesthe Advanced Very High Resolution Radiometer (AVHRR). The Indonesian archipelago was selected to demonstrate how AVHRR products can be synergistically used to monitor interannual variability, such as caused by ENSO, on regional and global scales. The authors examined month-to-month changes in surfaceatmosphere conditions over the region during July 1997June 1998.The major ENSO impact over the Indonesian archipelago was a prolonged dry period with anomalously low amounts of cloud, precipitation, and water vapor. The net effect of these changes was a significant increase in the absorbed shortwave and outgoing longwave radiation fluxes. ENSO-induced drought coincided with the slash-and-burn agricultural season, which resulted in persistent fires and smoke from biomass burning, covering larger areas, producing more smoke, remaining longer than during most dry seasons, and causing health hazards for millions of people in Southeast Asia. Analysis of the impact of fires on cloud microphysics confirms earlier suggestions that the effective cloud droplet size decreases due to smoke aerosols and cloud reflectivity increases due to higher concentration of small droplets. Analysis of areas with active fires showed a decrease in both surface albedo and fractional green vegetation as a result of intensive burning. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Bulletin of the American Meteorological Society American Meteorological Society

Using NOAA/AVHRR Products to Monitor El Nio Impacts: Focus on Indonesia in 199798

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1520-0477
D.O.I.
10.1175/1520-0477(2000)081<1189:UNPTME>2.3.CO;2
Publisher site
See Article on Publisher Site

Abstract

The development of the El Nio-Southern Oscillation (ENSO) in 199798, the most intense in this century, has been monitored by space- and ground-based observations. In this study, the authors present the signatures of ENSO impacts on the surfaceatmosphere system, as detected in satellite products that are routinely derived at NOAA from measurements by a single instrument on board NOAA polar-orbiting satellitesthe Advanced Very High Resolution Radiometer (AVHRR). The Indonesian archipelago was selected to demonstrate how AVHRR products can be synergistically used to monitor interannual variability, such as caused by ENSO, on regional and global scales. The authors examined month-to-month changes in surfaceatmosphere conditions over the region during July 1997June 1998.The major ENSO impact over the Indonesian archipelago was a prolonged dry period with anomalously low amounts of cloud, precipitation, and water vapor. The net effect of these changes was a significant increase in the absorbed shortwave and outgoing longwave radiation fluxes. ENSO-induced drought coincided with the slash-and-burn agricultural season, which resulted in persistent fires and smoke from biomass burning, covering larger areas, producing more smoke, remaining longer than during most dry seasons, and causing health hazards for millions of people in Southeast Asia. Analysis of the impact of fires on cloud microphysics confirms earlier suggestions that the effective cloud droplet size decreases due to smoke aerosols and cloud reflectivity increases due to higher concentration of small droplets. Analysis of areas with active fires showed a decrease in both surface albedo and fractional green vegetation as a result of intensive burning.

Journal

Bulletin of the American Meteorological SocietyAmerican Meteorological Society

Published: Jun 22, 2000

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