NOAA GOES-8 Satellite Soundings
Analysis of Central Florida Tornado Event - 2/22/98 - 2/23/98
Overview of Event
During the evening of February 22, 1998
and the early morning of February 23, 1998, severe thunderstorms, which
spawned numerous tornadoes developed in Central Florida, from Kissimmee
eastward to near Daytona Beach, resulting in numerous deaths and injuries,
as well as extensive property damage.
NOAA GOES-8 Lifted Index Fields
GOES-8 satellite soundings of
atmospheric temperature, humidity and stability are generated at NOAA's
National Environmental Satellite, Data, and Information Service (NESDIS)
on an hourly basis, using data collected by the 'sounder' instrument. Each
sounding is representative of an area approximately 30 km x 30 km in size.
Shown below are GOES-8
Lifted Index (LI) values (Degrees Celsius) for 1700 UTC - 2100 UTC 2/22/98,
plotted over the corresponding NOAA GOES-8 visible satellite image, followed
by the NWS numerical forecast model (ETA)
LI estimates at the same sounding locations. Different colors represent
ranges of LI values. LI's greater than 0 correspond to stable atmospheric
conditions, less than 0 unstable. LI values less than -5C indicate extremely
unstable conditions. The GOES-8 soundings indicated an area of increasing
instability during this time period in Central Florida, with LI values
decreasing from -1C to -8C. The corresponding numerical model forecast
(ETA) estimates did not indicate this rapid de-stabilization. It is important
to note that NOAA GOES-8 satellite soundings are available only in clear
or partly cloudy conditions. As such they can be used to diagnose atmospheric
conditions, such as stability, prior to severe weather outbreaks in the
clear or partly cloudy conditions that typically occur during the morning
and early afternoon. However, once severe weather develops, the associated
cloudiness generally prevents the use of this data source.
NOAA GOES-8 Satellite Lifted Index at 1702 UTC (12:02PM EST),
2/22/98.
NOAA GOES-8 Lifted Index at 1802UTC (1:02PM EST), 2/22/98.
NOAA GOES-8 Lifted Index at 1902UTC (2:02PM EST), 2/22/98.
NOAA GOES-8 Lifted Index at 2002UTC (3:02PM EST), 2/22/98.
NOAA GOES-8 Lifted Index at 2102UTC (4:02PM EST), 2/22/98.
NOAA ETA Forecast Lifted Index Fields
NOAA ETA Forecast Lifted Index at 1702UTC (12:02PM EST),
2/22/98.
NOAA ETA Forecast Lifted Index at 1802UTC (1:02PM EST),
2/22/98.
NOAA ETA Forecast Lifted Index at 1902UTC (2:02PM EST),
2/22/98.
NOAA ETA Forecast Lifted Index at 2002UTC (3:02PM EST),
2/22/98.
NOAA ETA Forecast Lifted Index at 2102UTC (4:02PM EST),
2/22/98.
Conclusions
The NOAA/NESDIS GOES-8
soundings over Central Florida on February 22, 1998 accurately identified
a region of maximum atmospheric de-stabilization, between 1700 UTC and
2000 UTC, associated with the outbreak of severe weather later that evening.
The ETA forecast stability fields depicted a larger area of moderate instability
over Central and Southern Florida, but failed to identify the zone of maximum
instability associated with the tornadoes. Although the GOES-8 soundings
helped localize the area of likely severe weather, their utility in this
case was limited by high level cloudiness which moved over the area after
2000 UTC (3PM EST). The tornado outbreak occurred 8 - 10 hours later. Satellite
soundings in cloudy areas are possible using microwave sounding technology,
but this is not available on the current GOES satellite series. This capability
would significantly improve the ability to monitor atmospheric stability
changes prior to severe weather development in cloudy conditions. Further
study is planned by NOAA/NESDIS scientists, and additional case studies
will be made available in the future.
Comments are greatly appreciated. For more information contact:
Additional
information on the Central Florida tornado event is available at the
Cooperative Institute for Meteorological Satellite Studies (CIMSS) at the
University of Wisconsin.
Web Page Last Updated: 02/01/99