Ocean Surface Winds -- SSMI and AMI Microwave Sensors
SSMI
The SSMI derived ocean surface winds are calculated at a height of 19.5m
for the previous days ascending and
descending satellite passes.
The wind speed algorithm used was developed by
Goodberlet et al.,
and expresses the wind speed, WS, in meters/second as
WS=147.90+1.0969*TB16v-0.4555*TB22v-1.7600*TB37v+0.7860*TB37h
where, TB is the radiometric brightness temperature at the
frequencies and polarizations indicated. All data where
TB37v-TB37hr < 50 or TB19h > 165 was rain flagged (Rain Flag 0) yielding
wind speeds with an accuracy of 2m/s.
ERS-1 (AMI)
The ERS-1(AMI) derived ocean surface winds are calculated at a
height of 10m for the previous days satellite passes as
provided by ESA in
their fast delivery product data. The
current empirically derived model function being used by
ESA to relate normalized
radar cross-section with wind speed and direction is referred to as CMOD4.
This data is considered to be
of research quality, and the presented wind speed
quantities should not be considered absolute. In storms
with high wind gradients, the wind speed values will be underestimated.
For the SSMI data, the presence of liquid water not detected with rain flag 0 will tend to add a positive bias in the estimated wind speeds.
Merged F10, F11 and F13 SSMI Orbits (Previous Day's)
-- Archived ascending pass - wind speeds, water vapor
Ascending pass - Water vapor
Ascending pass - Global water vapor
Rain rate algorithm
AMI - ERS-1 Orbits
Previous Day's Orbits
Today's current Orbits, Updated at 06:00, 12:00, 18:00 and 24:00 GMT
Note: Any requests, comments or suggestions are welcome and
desired.

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paul.s.chang@noaa.gov
Paul Chang
NOAA/NESDIS/Office of Research and Applications
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