The development of the Fl Nino-Southern Oscillation (ENSO) in 1997-98, 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 im
pacts on the surface-atmosphere system, as detected in satellite products t
hat are routinely derived at NOAA from measurements by a single instrument
on board NOAA polar-orbiting satellites-the Advanced Very High Resolution R
adiometer (AVHRR). The Indonesian archipelago was selected to demonstrate h
ow AVHRR products can be synergistically used to monitor interannual variab
ility, such as caused by ENSO, on regional and global scales. The authors e
xamined month-to-month changes in surface-atmosphere conditions over the re
gion during July 1997-June 1998.
The major ENSO impact over the Indonesian archipelago was a prolonged dry p
eriod with anomalously low amounts of cloud, precipitation, and water vapor
. The net effect of these changes was a significant increase in the absorbe
d shortwave and outgoing longwave radiation fluxes. ENSO-induced drought co
incided with the slash-and-burn agricultural season, which resulted in pers
istent fires and smoke from biomass burning, covering larger areas, produci
ng more smoke, remaining longer than during most dry seasons, and causing h
ealth hazards for millions of people in Southeast Asia. Analysis of the imp
act of fires on cloud microphysics confirms earlier suggestions that the ef
fective cloud droplet size decreases due to smoke aerosols and cloud reflec
tivity increases due to higher concentration of small droplets. Analysis of
areas with active fires showed a decrease in both surface albedo and fract
ional green vegetation as a result of intensive burning.