Atmospheric Temperature, Humidity, and Pressure Profile
The atmospheric temperature, humidity, and pressure profile is derived through inversion of atmospheric bending angle and refractive index data. This expands the data sources from a space-based perspective, deeply empowering atmospheric detection efforts.
High-coverage, high-precision data
The satellite limb scanning method ensures high temporal and spatial accuracy of the data. Combined with the latest data processing capabilities, it creates exceptional atmospheric data products, opening new perspectives for atmospheric detection.
Application
text-iconInsurance innovators
Utilize Atmospheric data for accurate premium calculation and innovative parametric insurance schemes, transforming how industry risks are managed.
text-iconTourism
Combining atmospheric data with attraction heat maps and other information, we provide travel recommendations to tourists, minimizing the impact of adverse weather on their plans, helping them catch the best moments at tourist sites, and enhancing the travel experience.
text-iconWeather Forecasting
By providing high-precision vertical atmospheric profiles, occultation data significantly improve the accuracy of numerical weather prediction models through more accurate initial fields and verification data. Tianmu occultation data, compared to other occultation data, have shown significant positive contributions to weather forecasting in various regions, including the Northern Hemisphere, Southern Hemisphere, East Asia, and the tropics.
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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.
text-iconScientific Research
Occultation data, with their global coverage, all-weather observation capabilities, and high precision and vertical resolution, are indispensable in providing valuable insights into the atmosphere and ionosphere. These data find broad applications in Earth and space sciences. Notably, Tianmu occultation data stand out with their smaller mean deviation and standard deviation, suggesting a higher level of data reliability.
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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
Data Sheets
L2Dry AtmosphereMoist Atmosphere
ContentsThe dry atmospheric profile product provides atmospheric profiles and auxiliary data from a single occultation event. The product content includes time, satellite number of occultation GPS/BDS/GALILEO/GLONASS, tangent point location, bending angle, refractive index, atmospheric density, dry temperature, and dry pressure.The moist atmospheric profile product provides atmospheric profiles of moisture and auxiliary data from a single occultation event. The product content includes time, satellite number of occultation GPS/BDS/GALILEO/GLONASS, tangent point location, temperature, pressure, and specific humidity.
File Naming
atmPrf_GNOS.LLL.YYYYMMDD_HHMM_GGG.nc
atmBufr_GNOS.LLL.YYYYMMDD_HHMM_GGG.bufr
wetPrf_GNOS.LLL.YYYYMMDD_HHMM_GGG.nc
File Format
NETCDF
BUFR
NETCDF
Technical Specifications
Vertical Resolution: <1KM
Average Refractive Index Deviation: ≤1%(Near the surface~5km) ≤0.5%(5~30km)
Average Temperature Deviation: ≤1K(Near the surface~5km) ≤0.5K(5km~30km)
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单星日增量
atmPrf: about 250MB
atmBufr: about 22MB
About 5MB
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Quality Assessment Results
Assessment of the Altitude Range for Atmospheric Occultation Detection
Indicator Requirements: Altitude range from 0.2 to 60 kilometers.
Test Method: Statistically analyze the altitude range of L2 occultation events generated by the business system over 3 days.
Test conditions:
1) Data source: January 13th to 15th, 2023.
2) Test Results:
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3) Test Conclusion: The altitude range of atmospheric occultation detection for Tianmu 01/02 satellites meets the test requirements.
Accuracy assessment of Atmospheric Occultation Refractive Index
Indicator Requirements: A mean deviation of less than 1% (between 5km and 35km) is considered acceptable
Test Method: A statistical analysis will be conducted to evaluate the accuracy of atmospheric occultation refractivity by comparing near real-time L2 dry atmospheric profiles generated operationally with analysis or reanalysis model data over a three-day period.
Test conditions:
1) Data source: April 2nd to 4th, 2023.
2) Test Results:
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3) Test Conclusion:
Testing has confirmed that the atmospheric occultation refractivity obtained from Tianmu 01/02 satellites meets the required accuracy.
Accuracy assessment of Atmospheric Occultation Temperature
Indicator Requirements: A mean deviation of less than 1K (between 5km and 35km) is considered acceptable.
Test Method: A statistical analysis will be conducted to evaluate the accuracy of atmospheric occultation temperature by comparing near real-time L2 moist atmospheric profiles generated operationally with analysis or reanalysis model data over a three-day period.
Test conditions:
1) Data source: April 2nd to 4th, 2023.
2) Test Results:
TM01:
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TM02:
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3) Test Conclusion: Testing has confirmed that the atmospheric occultation temperature accuracy of Tianmmu 01/02 satellites meets the test requirements.
L1bPrecise orbit and clock data for LEO satellitesAtmospheric Excess Phase data file
Contents
Precise orbit product data for LEO satellites
Precise clock product data for LEO satellites
The Global Navigation Satellite System Occultation (GNOS) Level 1 atmospheric excess phase data provides detailed measurements for each occultation event, including time, GNSS satellite and LEO satellite positions and velocities, signal-to-noise ratio, and occultation flag.
File Naming
leoSp3_LLL_YYYY.DDD.SSSSS.UUUUU_sys.sp3
leoClk_LLL_YYYY.DDD.SSSSS.UUUUU_sys.clk
atmPhs_GNOS.LLL.YYYY_DDD_HH_MM_GGG.nc
File Format
sp3
clk
NETCDF
Daily data growth from a single satellite
sp3: about 1.5MB
clk: about 1.5MB
about 1.7GB
L1aGNSS satellite positioning observation dataLEO satellite positioning observation dataAtmospheric occultation data
ContentsPositioning observation data, including carrier phase and pseudorange measurements from GNSS satellites received by the positioning channel.Including LEO satellite orientation data and real-time location data.
Occultation packet data consists of GNSS occultation carrier phase and pseudorange observations.
Occultation packets are divided into atmospheric and ionospheric occultation.
File NamingpodObs_LLL_AD_YYYY.DDD.SSSSS.UUUUU_SYS.rnx2
leoAtt_LLL_YYYY.DDD.SSSSS.UUUUU_txt
leoPos_LLL_YYYY.DDD.SSSSS.UUUUU_txt
occAtm_GNOS.LLL.GGG.RR.YYYY.DDD.SSSSS.UUUUU.AD.ROX
File Format
RINEX(Receiver Independent Exchange Format V2.10)
txtROEX(GNSS Radio Occultation Data Independent Exchange Format)
Daily data growth from a single satelliteAbout 500MB
leoAtt:about 6MB
leoPos:about 13MB
About 1GB
L0Raw payload data packet
ContentsRaw occultation payload observation data, including positioning and occultation data.
File NamingLEOX_GNOSO_L0_YYYYMMDD_hhmmss_UUUUU.DAT
File FormatBIN
Daily data growth from a single satelliteAbout 3GB