N: 90 S: -90 E: 180 W: -180
Description
The Global Precipitation Measurement (GPM) satellite was launched on February 27th, 2014 with the GPM Microwave Imager (GMI) instrument on board. The GPM mission is a joint effort between NASA, the Japan Aerospace Exploration Agency (JAXA) and other international partners. In march 2005, NASA has chosen the Ball Aerospace and Technologies Corp., Boulder, Colorado to build the GMI instrument on the continued success of the Tropical Rainfall Measuring Mission (TRMM) satellite by expanding current coverage of precipitation from the tropics to the entire world. GMI is a dual-polarization, multi-channel, conical-scanning, passive microwave radiometer with frequent revisit times. One of the primary differences between GPM and other satellites with microwave radiometers is the orbit, which is inclined 65 degrees, allowing a full sampling of all local Earth times repeated approximately every 2 weeks. The GPM platform undergoes yaw maneuvers approximately every 40 days to compensate for the sun's changing position and prevent the side of the spacecraft facing the sun from overheating. Today, the GMI instrument plays an essential role in the worldwide measurement of precipitation and environmental forecasting. Sea Surface Temperature (SST) is one of its major products. The GMI data from the Remote Sensing System (REMSS) have been produced using an updated RTM, Version-8. The V8 brightness temperatures from GMI are slightly different from the V7 brightness temperatures; The SST datasets are available in near-real time (NRT) as they arrive, with a delay of about 3 to 6 hours, including the Daily, 3-Day, Weekly, and Monthly time series products.
Product Summary
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Variables
Variables are a set of physical properties whose values determine the characteristics or behavior of something. For example, temperature and pressure are variables of the atmosphere. Parameters and variables can be used interchangeably. Variable level attributes provide individual information for each variable.
The Name in this table is the variable name. Fill value indicates missing or undefined data points in a variable. Valid range is the range of values the variable can store. Scale factor is used to increase or decrease the size of an object and can be used to correct for distortion. For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor |
|---|---|---|---|---|---|---|
| cloud_liquid_water | non L3U core field | kg m-2 | byte | -128 | -127 to 127 | 0.01 |
| confidence_flag | b0:1=within 50km rain, 0.6 dif mwoisst;b1:1=within 100km rain, 0.8 dif mwoisst;b2:1=within 150km ice, 0.6 dif mwoisst;b3:1=more than 5deg dif mwoisst;b4:1=3-sigma test;b5:1=(tmi only) within 150 km of land and 0.6 warmer than mwoisst;b6:1=diurnal estimate > 0.3 warming;b7:1=diurnal estimate > 1.0 warming | N/A | byte | N/A | N/A | 1 |
| cool_skin | non L3U core field | K | byte | -128 | -127 to 127 | 0.01 |
| diurnal_amplitude | non L3U core field | K | byte | -128 | -127 to 127 | 0.02 |
| dt_analysis | delta SST | K | byte | -128 | -127 to 127 | 0.1 |
| l2p_flags | These flags can help use the data | N/A | short | N/A | 0 to 2047 | 1 |
| lat | Latitude of retrievals | degrees_north | float | -32768 | -89.875 to 89.875 | 1 |
| lon | Longitude of retrievals | degrees_east | float | -32768 | -179.875 to 179.875 | 1 |
| proximity_confidence | 1=Bad, data rejected;2=Suspected Bad, data that has any confidence flags bit 0-5 thrown;3=Unprocessed proximity confidence flag, should be Good data;4=Good data | N/A | byte | N/A | N/A | 1 |
| quality_level | This flag can help use the data | N/A | byte | -128 | 0 to 5 | 1 |
| rain_rate | non L3U core field | mm hr-1 | byte | -128 | -127 to 127 | 0.1 |
| rejection_flag | b0:1=rain;b1:1=high wind/sunglint;b2:1=ice;b3:1=near land;b4:1=no data;b5:1=land; | N/A | byte | N/A | N/A | 1 |
| sea_ice_fraction | ftp://eclipse.ncdc.noaa.gov/pub/OI-daily-v2/IEEE/YYYY/AVHRR/avhrr-only-v2.YYYYMMDD.gz | 1 | byte | -128 | -127 to 127 | 0.01 |
| sea_surface_temperature | Microwave SST = approximately the top 1 milimeter | K | short | -32768 | -5000 to 5000 | 0.01 |
| sses_bias | Sensor Specific Bias from in situ SSTs | K | byte | -128 | -127 to 127 | 0.01 |
| sses_standard_deviation | Sensor Specific STD from in situ SSTs | K | byte | -128 | -127 to 127 | 0.01 |
| sst_dtime | relative time of SST observations | second | int | -32768 | 0 to 10000 | 10 |
| time | useful to help interpret sst_dtime | seconds since 1981-01-01 00:00:00 | int | N/A | N/A | 1 |
| water_vapor | non L3U core field | kg m-2 | byte | -128 | -127 to 127 | 0.3 |
| wind_speed | non L3U core field; wind_speed_lf | m s-1 | byte | -128 | -127 to 127 | 0.2 |