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Description of SSM/I Data Products |

Version-6 SSM/I Ocean Products
The entire SSM/I ocean data set has been completely reprocessed. As of September 13, 2006, all SSM/I data files have been updated from Version-5 to Version-6. Version-5 SSM/I data have been archived off-line and are no longer available except by special request.
The byte map folder has changed from "bmaps_v05" to "bmaps_v06".
The final file designation has changed from "v5" to "v6".
No changes were made to the data file format.
More details on SSM/I Version-6 improvements:
The September 2006 Update to RSS Climate Data Records
 
Introduction
These Special Sensor Microwave/Imager (SSM/I) data products are produced as part of NASA's Pathfinder Program. Remote Sensing Systems generates SSM/I data products using a unified, physically based algorithm to simultaneously retrieve ocean wind speed (at 10 meters), water vapor, cloud water, and rain rate. This algorithm is a product of 15 years of refinements, improvements, and verifications. While the algorithms have evolved over time, a substantial background to the radiative transfer function used to derive the geophysical parameters is described in the following two papers:
The above two articles are in the postscript and PDF formats. You will need a postscript viewer such as GSview, or PDF viewer such as Adobe Acrobat Reader in order to view the files online. These articles have been published in the following journals:
Wentz F. J. 1997, "A well-calibrated ocean algorithm for SSM/I", J. Geophys. Res., Vol. 102, No. C4, pg. 8703-8718.
Wentz, Frank J. and Roy W. Spencer, May 1, 1998, "SSM/I Rain Retrievals within a Unified
All-Weather Ocean Algorithm", Journal of the Atmospheric Sciences, Vol. 55, pg. 1613-1627.
 
SSM/I Data
The RSS SSM/I geophysical dataset consists of data derived from observations collected by SSM/I instruments carried onboard the DMSP series of polar orbiting satellites. These satellite are numbered:
F08 SSM/I | Jul 1987 | to | Dec 1991 |
F10 SSM/I | Dec 1990 | to | Nov 1997 |
F11 SSM/I | Dec 1991 | to | May 2000 |
F13 SSM/I | May 1995 | to | present |
F14 SSM/I | May 1997 | to | present |
F15 SSM/I | Dec 1999 | to | Aug 2006 |
There are gaps within these data. If you select a date for which no data is available, either a list of acceptable dates will appear, or a blank map with text stating "Data not available" will be posted.
Remote Sensing Systems performs a detailed processing of SSM/I instrument data in two stages.
The first stage produces an interim product (identified by "rt" within the file name) which we make available as soon as possible, generally within hours of when the data are recorded. This product can contain geolocation errors and erroneous brightness temperatures inherent in the data supplied to us.
These errors are removed and better ice flagging is performed by the final processing stage, usually completed within 15 days of the intial product. The final product replaces the interim product automatically, with the "rt" designation in the file name changing to "v6".
The SSM/I Pathfinder data products include the daily geophysical data and time-averaged data as follows:
daily | orbital data mapped to 0.25 degree grid, data overwritten by later data |
3-day | average of 3 days ending on file date |
weekly | average of 7 days ending on the Saturday file date |
monthly | average of all data within month |
Geophysical graphic images can be viewed on our web page and binary data files can be downloaded from our ftp server: ftp.ssmi.com/ssmi
 
Graphic Image Maps
Each daily, 3-day, weekly and monthly graphic image map displays one geophysical parameter, 10 meter Surface Wind Speed (W), Columnar Water Vapor (V), Cloud Liquid Water (L), or Rain Rate (R). The daily maps display the local morning or evening satellite passes separately. The date of the data displayed is the date at Greenwich Mean Time when each orbit occured and the data were collected (See the following section on Map dates and Times). The scale for each map is located next to the map for reference. The scale bar extends between zero and the defined maximum listed below:
| |
Daily |
3-Day |
Weekly |
Monthly |
Units |
| Surface Wind Speed: |
15 |
15 |
15 |
12 |
meters/second |
| Atmospheric Water Vapor: |
60 |
60 |
60 |
60 |
millimeters |
| Cloud Liquid Water: |
0.3 |
0.3 |
0.3 |
0.24 |
millimeters |
| Rain Rate: |
20 |
10 |
5.0 |
2.0 |
millimeters/hour |
White areas on the daily map represent regions of ice (greater than 0% sea ice) as determined by the SSM/I instrument. In the time-averaged maps, ice is shown when ice is present over 50% of the time, or when the number of times a cell is identified as containing ice is greater than the number of times the cell contains data. Land regions are colored gray. Those areas where SSM/I data are not available are black. For the daily maps, the black color includes areas where the satellite did not pass over and no data were collected, areas where data were collected but were determined to be bad, coastal areas, areas affected by sun glint, areas of rain on the surface wind speed map, and areas of heavy rain on the water vapor map.
 
Map Dates and Times
It is currently 4 pm in New York City on August 18th and you see on our web page the daily map of data shown below.
August 18th Evening Passes F14 Data
The F14 satellite passes overhead at approximately 8:30 pm each evening, local time. How can there be data shown in the map for a time that hasn't occurred yet??? Did we make an error???
Each map shown on this web page is for morning or evening passes of a satellite on that date at Greenwich, England. For example, the data you see in the above map were collected near 8:30 pm local time. 8:30 pm in New York City is 1:30 am in Greenwich, England (8:30 + 5 hour time difference). Since it must be August 18th in Greenwich (the date of the map), then the data you see were collected on Aug 17th, local time.
Similar time "problems" occur for each of the satellites. The table below demonstrates another example, this time for data collected by the F13 satellite. F13 crosses the equator at approximately 5:30 am.
Location |
Lat/Lon |
F13 local Time/Date |
F13 GMT Time/Date |
Map Date |
| New Guinea |
0 / 133 |
5:30 AM 20-Sep |
8:30 PM 19-Sep |
19-Sep |
| Jarvis Island |
0 / 203 |
5:30 AM 19-Sep |
4:30 PM 19-Sep |
19-Sep |
| Ecuador |
0 / 280 |
5:30 AM 19-Sep |
10:30 AM 19-Sep |
19-Sep |
Here, the F13 morning pass time of 5:30 (local time) is used to determine the GMT (Greenwich Mean Time) of the map date. The corresponding GMT time and date are then used to determine the date at the given location. When the September 19th F13 morning pass was collected, it was actually September 20th in New Guinea, a location that is 8 hours ahead of Greenwich.
The best way to determine the time for scientific comparisons is to use the time data set in the daily binary data files. Each pixel location of an ocean parameter map has a specific GMT minute of day listed in the time array. Use of time in this manner will keep your data processing in the correct order.
 
Binary Data Files
We produce Daily binary data files and Time-Averaged (3-day, weekly and monthly) data files. The daily files consist of SSM/I geophysical products mapped to a regular grid complete with data gaps between orbits. Two maps exist for each parameter, one of ascending orbit segments and the other of descending orbit segments. Data on each of the segment maps are overwritten at both the high latitudes where successive orbits cross and at the "seam" or region where the last orbit of the day overlaps the first orbit of the day. Daily data files contain a time data set consisting of the time (in minutes UTC) of the data within that cell. Time-Averaged data files do not contain any time information.
Each binary data file available from our ftp site consists of ten (daily) or four (averaged) 0.25 x 0.25 degree grid (1440,720) byte maps. For daily files, five local morning (descending, except F08) maps in the following order, Time (T), 10 meter Surface Wind Speed (W), Atmospheric Water Vapor (V), Cloud Liquid Water (L), and Rain Rate (R), are followed by five local evening (ascending, except F08) maps in the same order. Time-Averaged files contain just the geophysical layers in the same order [W,V,L,R]. The daily, 3-day and monthly maps are stored by instrument in appropriate year and month subdirectories. The weekly data files are stored by instrument in the /weeks directory.
The file names have the following naming conventions:
| Daily |
fss_yyyymmddvv.gz |
| 3-Day |
fss_yyyymmddvv_d3d.gz |
| Weekly |
fss_yyyymmddv6.gz |
| Monthly |
fss_yyyymmv6.gz |
Where ss, yyyy, mm, dd, and vv stand for:
| ss |
satellite number |
08, 10 ,11, 13, 14, 15 |
| yyyy |
year |
1996, 1997, 2000, etc. |
| mm |
month |
01 (Jan), 02 (Feb), etc. |
| dd |
day |
01, 02,...31 |
| vv |
version |
rt = real time (daily and 3-day interim product) v6 = version 6 (final product) |
The center of the first cell of the 1440 column and 720 row map is at 0.125 E longitude and -89.875 latitude. The center of the second cell is 0.375 E longitude, -89.875 latitude.
The data values fall between 0 and 255. Specific values have been reserved:
| 0 to 250 |
= |
valid geophysical data |
| 251 |
= |
missing wind speed due to rain, or missing water vapor due to heavy rain |
| 252 |
= |
sea ice |
| 253 |
= |
SSM/I observations exist, but are bad (not used in composite maps) |
| 254 |
= |
no SSM/I observations |
| 255 |
= |
land mass |
The data values between 0 and 250 need to be scaled to obtain meaningful geophysical data. To scale the data, multiply by the scale factors listed below:
| T: |
multiply by |
6.0 |
to get |
time |
between |
0 and 1440 minutes |
| W: |
multiply by |
0.2 |
to get |
10 m winds |
between |
0 and 50.0 m/sec |
| V: |
multiply by |
0.3 |
to get |
water vapor |
between |
0 and 75 mm |
| L: |
multiply by |
0.01 |
to get |
cloud liquid water |
between |
0 and 2.5 mm |
| R: |
multiply by |
0.1 |
to get |
rain rate |
between |
0 and 25 mm/hr |
 
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SSM/I data are produced by Remote Sensing Systems and sponsored by the NASA Earth Science REASoN DISCOVER Project. Data are available at www.remss.com. |
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