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The distribution of these data sets is funded by NASA's
Earth Science Enterprise. The data are not copyrighted;
however, we request that when you
publish data or results using these data, please
acknowledge as follows:
The authors wish to thank Robert F. Contreras, Dept. of Atmospheric
Sciences, University of Washington, Seattle, WA for the production of these
data and the Distributed Active Archive Center(Code 610.2) at the Goddard Space
Flight Center, Greenbelt, MD, 20771, which archives and distributes them under
sponsorship of NASA's Earth Science Enterprise.
The Ku-band System and Data
The Ku-band (14 GHz) microwave system used on the RV Ronald H. Brown during
KWAJ EX was a continuous-wave, dual-polarized, coherent system. The one-way,
half-power, full beamwidths were:
- 6.4 Degrees (vertical V-pol),
- 6.4 Degrees
(vertical H-pol),
- 6.9 Degrees (horizontal V-pol)
- 6.8 Degrees (horizontal
H-Pol).
The system was downward looking from a height of 16.2 m above the
water surface and it stepped through incidence angles ranging from 12.5
Degrees to 76 Degrees.
HH and VV polarization returned powers were recorded at 2 Hz and from this
normalized radar cross sections (NRCS) were calculated; mean spectra were
recorded every 40 samples (20 seconds). The 20 second mean cross sections
were computed, and from these the scattering from rain was removed by
eliminating the component of the return with very large Doppler shifts.
Ancillary Data
- Rain Guage: The Hasse rain guage values for the rain rate were used
- Neutral Winds: The 10m neutral winds (speed and direction) were calculated
using Monin-Obhukov similarity theory. The wind speed and direction, and the
fluxes of momentum and heat used to compute the neutral winds were provided by
Dr. Jeff Hare and Dr. Chris Fairall (NOAA/ETL Air-Sea Interaction Group). The
wind speed, wind direction, heat flux, and momentum flux were provided as 10
minute averages; they were linearly interpolated to 20 second intervals and
the neutral winds were computed.
Problems
The transmitted power began to fluctuate August 25. The VV polorization NRCS
was completely corrected for this. The HH polarization was corrected for this
but there is an increase in the NRCS variance associated with this instrument error.
At incidence angles greater than 55 degrees separating the rain signal from the
surface signal was difficult; this should be kept in mind when using data at
these incident angles.
At incidence angles less than 13.5 degrees the system was seeing the ship
and this data should not be used.
The KU band radar dataset consists of a single 7MB ASCII file named kwaj_proc_ascii.dat, which is tabularly formatted as follows:
| Column | Description | Units |
| YYYY | year |
| MM | month |
| DD | day |
| HH | hour |
| MM | minute |
| SS | seconds |
| SIGMA0_H | Normalized radar cross section, HH polarization | unitless |
| SIGMA0_V | Normalized radar cross section, VV polarization | unitless |
| INCIDENCE | Incidence angle, angle from nadir | Degrees |
| RAIN_RATE | Rain rate | mm/hr |
| WIND_SPEED | Neutral wind speed at 10m | m/s |
| WIND_DIRECTION | Clockwise direction between system look direction and the direction from which the wind is blowing. | Degrees
| | NaN was used as the fill value |
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FTP Site
The KU band radar data from KWAJEX may be accessed from this page,
Radar Data Online
or directly via ftp:
ftp disc2.nascom.nasa.gov
logon: anonymous
passwd:
cd data/KWAJ/surface_data/rv_rhbrown/ku_band_radar/
The Principal Investigator for the KU band radar data is
Robert F. Contreras
Dept. of Atmospheric Sciences
University of Washington, Box 351640
Seattle, WA 98195-1640, USA
robb@apl.washington.edu
206-543-2480 (voice)
For additional information, please contact the GES DISC User Services:
Last update:Fri Dec 5 07:25:15 EST 2003
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