N: 79 S: -80 E: 180 W: 64
N: 79 S: -80 E: -134 W: -180
Multi-functional Transport Satellites (MTSAT) are a series of geostationary weather satellites operated by the Japan Meteorological Agency (JMA). MTSAT carries an aeronautical mission to assist air navigation, plus a meteorological mission to provide imagery over the Asia-Pacific region for the hemisphere centered on 140 East. The meteorological mission includes an imager giving nominal hourly full Earth disk images in five spectral bands (one visible, four infrared). MTSAT are spin stabilized satellites. With this system images are built up by scanning with a mirror that is tilted in small successive steps from the north pole to south pole at a rate such that on each rotation of the satellite an adjacent strip of the Earth is scanned. It takes about 25 minutes to scan the full Earth's disk. This builds a picture 10,000 pixels for the visible images (1.25 km resolution) and 2,500 pixels (4 km resolution) for the infrared images. The MTSAT-2 (also known as Himawari 7) and its radiometer (MTSAT-2 Imager) was successfully launched on 18 February 2006. For this Group for High Resolution Sea Surface Temperature (GHRSST) dataset, skin sea surface temperature (SST) measurements are calculated from the IR channels of the MTSAT-2 Imager full resolution data in satellite projection on a hourly basis by using Bayesian Cloud Mask algorithm at the Office of Satellite and Product Operations (OSPO). L2P datasets including Single Sensor Error Statistics (SSES) are then derived following the GHRSST Data Processing Specification (GDS) version 2.0.
Citation is critically important for dataset documentation and discovery. This dataset is openly shared, without restriction, in accordance with the EOSDIS Data Use and Citation Guidance.
The table below lists the variables contained within a single granule for this dataset. Variables often contain observed or derived geophysical measurements collected from a variety of sources, including remote sensing instruments on satellite and airborne platforms, field campaigns, in situ measurements, and model outputs. The terms variable, parameter, scientific data set, layer, and band have been used across NASA’s Earth science disciplines; however, variable is the designated nomenclature in NASA’s Common Metadata Repository (CMR). Variable metadata attributes such as Name, Description, Units, Data Type, Fill Value, Valid Range, and Scale Factor allow users to efficiently process and analyze the data. The full range of attributes may not be applicable to all variables. Additional information on variable attributes is typically available in the data, user guide, and/or other product documentation.
For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor | Offset |
|---|---|---|---|---|---|---|---|
| adi_dtime_from_sst | Difference in hours between the ADI and SST data | hour | byte | -128 | -127 to 127 | 1 | 127 |
| aerosol_dynamic_indicator | Estimate of the potential for aerosol contamination | count | byte | -128 | -127 to 127 | 0.01 | 1.27 |
| diurnal_warming | Estimate of diurnal warming using Gentemann (2003) diurnal warming parameterization | Kelvin | byte | -128 | -127 to 127 | 0.05 | N/A |
| dt_analysis | Analysis used is NOAAs Real-time Global SST analysis at high resolution (0.083 degree) | kelvin | byte | -128 | -127 to 127 | 0.1 | N/A |
| l2p_flags | The flags are important to preperly use the data. | N/A | short | 127 | 127 to -128 | -128 | -128 |
| lat | latitude from McIDAS derived data | degrees_north | float | -3.4028235E+38 | -90 to 90 | 1 | N/A |
| lon | longitude from McIDAS derived data | degrees_east | float | -3.4028235E+38 | -180 to 180 | 1 | N/A |
| probability_of_clear_sky | Clear sky probability from Bayesian analysis; non-standard L2P field | probability | byte | -128 | -127 to 127 | 0.0002 | 0.975 |
| quality_level | Proximity code defined as : 0 = unprocessed 1 = Cloudy (Clear sky probability < 0.800) 2 = Bad (0.800 <= Clear sky probability < 0.950) 3 = Suspect (0.950 <= Clear sky probability < 0.990) 4 = Acceptable (0.990 <= Clear sky probability < 0.999) 5 = Excellent (0.999 <= Clear sky probability) | N/A | byte | 0 | 0 to 5 | 1 | N/A |
| satellite_zenith_angle | The satellite zenith angle at the time of the SST observation | angular_degree | byte | -128 | -90 to 90 | 1 | N/A |
| sea_ice_fraction | Fractional sea ice cover from NCEP GFS estimate | fraction | byte | -128 | 0 to 1 | 0.01 | N/A |
| sea_surface_temperature | Skin temperature of the ocean | kelvin | short | -32768 | -5000 to 5000 | 0.01 | 273.15 |
| solar_zenith_angle | The solar zenith angle at the time of the SST observation | angular_degree | byte | -128 | 0 to -76 | 1 | N/A |
| sses_bias | Estimated bias based on NOAA bias scheme (contact Andy.Harris@noaa.gov) | kelvin | byte | -128 | -127 to 127 | 0.02 | N/A |
| sses_standard_deviation | Estimated standard deviation based on NOAA bias scheme (contact Andy.Harris@noaa.gov) | kelvin | byte | -128 | -127 to 127 | 0.01 | 1 |
| sst_dtime | time plus sst_dtime gives seconds after 00:00:00 UTC January 1, 1981 | second | short | -32768 | -32767 to 32767 | 1 | N/A |
| time | time in seconds since 1981-01-01 00:00:00 | seconds since 1981-01-01 00:00:00 | int | N/A | N/A | 1 | N/A |
| wind_speed | These wind speeds were created by NCEP and represent windows at 10 metres above the sea surface | m s-1 | byte | -128 | -127 to 127 | 1 | N/A |