Le cyclone tropical "Gafilo" cause une catastrophe majeure à
Madagascar le 6 Mars 2004.
Le cyclone tropical "Gafilo" cause une catastrophe
majeure à Madagascar le 6 Mars 2004.
The severe Tropical
Cyclone Gafilo was one of several
cyclones to affect Madagascar in the 2003-2004 season. With 1-minute averaged
windspeeds of about 250 km/h and gusts of up to 330 km/h, this cyclone struck
the northeast coast of Madagascar early on the morning of 7 March 2004, in particularly,
the city of Antalaha. There was massive distruction and 85% of the city was
destroyed). 237 lives were lost, with 181 missing persons and 879 injured (official
figures as of 30 March 2004). Of the total of 237 fatalities, more than 110
persons were killed on the ferry "Le Samson" from the nearby Comoro Islands
that was reported to have capsized in heavy seas. More than 304,000 people were
left homeless by the storm and more than six thousand hectares of agricultural
land were flooded, resulting in major crop losses. According to the Multi-Satellite
Precipitation Analysis (MPA) product from the NASA Goddard Space Flight Center,
total rainfall for the period 3-10 March 2004 reached values of up to 500 mm
in an area from the central Mozambique Channel eastward along the northwest
coastline of Madagascar.
The upper two Meteosat-8
images below show Tropical Cyclone Gafilo about 18 hours before it made landfall.
These two images have been reprojected into Mercator projection, which provides
a better presentation for images that are viewed at very large satellite viewing
angles.
The lower two images
are presented in the original satellite projection. The lower right Meteosat-8
image shows the Tropical Cyclone on 7 March 2004, after landfall and when it
had already weakened somewhat.
The Meteosat-8
images from 6 March show the marked spiral structure of Gafilo and a relatively
large eye, with the eyewall and the Central Dense Overcast (CDO) region. They
also show areas of small ice particles/intense precipitation (in yellow colour
on the RGB images) within the CDO region and the spiral bands. The Meteosat-8
visible and infrared images, however, do not reveal an eyewall replacement cycle,
which could only be observed in microwave imagery (e.g. AMSU on NOAA, TMI on
TRMM, AMSR on Acqua or SSMI on DMSP). The two examples from 6 March 20
04 that show the double eyewall
structure are also presented below.
Met-8,
06 March 2004, 09:00 UTC
Channel 12 (HRV)
Full Resolution (345 KB)
Met-8,
06 March 2004, 09:00 UTC
RGB Composite
NIR1.6, HRV, HRV Full Resolution(324 KB)
Met-8,
06 March 2004, 09:00 UTC
RGB Composite
WV6.2-WV7.3,
IR3.9-IR10.8, NIR1.6-VIS0.6 Full Resolution (125 KB)
Met-8, 07 March
2004, 09:00 UTC
RGB Composite
WV6.2-WV7.3,
IR3.9-IR10.8, NIR1.6-VIS0.6 Full Resolution (127 KB)
TMI
on TRMM, 06 March 2004, 08:01 UTC
85 GHz Channel
(HH) Full Resolution (339 KB)
Source:
Naval Research Laboratory, Monterey, CA
AMSU-B
on NOAA, 06 March 2004, 10:45 UTC
RGB Composite
150GHz, 89 GHz, 89 GHz Full Resolution (213 KB)
Source:
Naval Research Laboratory, Monterey, CA