Data Acquisition
Tianmu 1 is equipped with "GNSS Occultation Reflection Detector" and "Atmospheric Density Detector", continuously collecting data on land, ocean, atmosphere, and ionosphere 24/7.
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Certification of data availability
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The China Meteorological Administration's assessment indicates that Tianmu occultation data offer higher accuracy, with smaller mean deviation and standard deviation compared to other occultation data.
Accuracy assessment of occultation data
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Forecast performance metric card
Legend: Red: Assimilated occultation data improved the forecast. Green: Assimilated occultation data worsened the forecast. Triangle size represents the magnitude of the effect.
Based on the forecast scorecard from the Numerical Prediction Center of the China Meteorological Administration, the assimilation of Tianmu occultation data into the CMA-GFS4.0 system has shown significant positive impacts on forecasts in all regions (Northern Hemisphere, Southern Hemisphere, East Asia, and the tropics), outperforming other occultation data sources.
About data products
Atmospheric Temperature, Humidity, and Pressure Profile
With limb scanning technique, we capture real-time atmospheric bending angles and refractive indices globally. Through inversion processing, it provides high-vertical-resolution, high-accuracy atmospheric profiles of temperature, humidity, and pressure.
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Electron Density
Utilizing limb scanning, we obtain global 24/7 total electron content (TEC) from the ionosphere. Through inversion processing, high-vertical-resolution and high-accuracy vertical profiles of ionospheric electron density are derived.
Soil Moisture
By using GNSS reflection signal remote sensing, the reflectivity of signals from the land surface is obtained. Through inversion processing, this data enables real-time determination of global 24/7 soil moisture levels.
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Ocean wind speed
Using GNSS reflection signal remote sensing, sea surface roughness is determined from the reflectance power spectrum of signals reflected off the ocean surface. This data, through inversion processing, enables the global 24/7 calculation of ocean wind speeds.
Atmospheric Density
The spatial and temporal distribution of atmospheric density at approximately 500 km in a sun-synchronous orbit enables the simultaneous retrieval of atmospheric density at different spatial locations at the same altitude. Level I products include sensor pressure and temperature information, while Level II products provide atmospheric density data at orbital altitude.
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