N: 60 S: -60 E: 180 W: -180
Description
These data originate from NOAA/NCEP.
The NOAA Climate Prediction Center/NCEP/NWS is making the data available originally in binary format, in a weekly rotating archive. The NASA GES DISC is acquiring the binary files as they become available, converts them into CF (Climate and Forecast) -convention compliant netCDF-4 format, and stores the product in a permanent archive. The original record started from February, 2000, but in June, 2025 it was extended back to January, 1998.
The leading edge of data availability is delayed by about 24 hours from real-time to abide by international data exchange agreements between NOAA and EUMETSAT (the METEOSAT data providers).
The data contain globally-merged (60°S-60°N) 4-km pixel-resolution IR brightness temperature data (equivalent blackbody temps), merged from the European, Japanese, and U.S. geostationary satellites over the period of record (GOES-8/9/10/11/12/13/14/15/16/17/18/19, METEOSAT-5/7/8/9/10/11, and GMS-5/MTSat-1R/2/Himawari-8/9).
The global geo-IR are dynamically calibrated to GOES East, using a 35 day trailing inter-calibration using time/space-matched IR Tb’s at the mid-point between sub-satellite positions. In the event of duplicate data in a grid box, the value with the smaller zenith angle is taken. The data have been corrected for "zenith angle dependence", in which IR temperatures for locations far from satellite nadir are erroneously cold due to a combination of geometric effects and radiometric path extinction effects (Joyce et al. 2001). Finally, the data are re-navigated for parallax, which shifts the geo-location of the GEO-IR footprints to approximately account for the cloud tops that the IR “sees” being displaced away from their actual geographic location when viewed along a slanted path. These corrections allow for the merging of the IR data from the various GEO-satellites with greatly reduced discontinuities at GEO-satellite data boundaries. In the event of duplicate data in a grid box, the value with the smaller zenith angle is taken.
The NASA GES DISC is curating these data in a self-documenting, CF-compliant, netCDF-4 format, which allows a broad range of applications to access the data directly, without the need to cope with the original binary data format. In addition to the direct download of netCDF-4 data, the GES DISC provides data download in binary, ASCII, and netCDF-3 formats using the OPeNDAP interface which also provides remote data access.
Similarities with the original
As in the original binaries, every netCDF-4 file covers one hour, and contains two half-hourly grids, at 4-km grid cell resolution.
Differences from the original
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The data in the netCDF-4 files are already converted to physical values of Brightness Temperatures in Kelvin. Because the original data values are round with no decimal precision, the data type in the netCDF-4 files has been changed to 2-byte signed integer, a transition that took place in mid-August, 2025. This reduces the file size and speeds up data download and remote access. There is no need to further scale these data. The netCDF-4 format is machine-independent and users need not worry about the endian-ness of their machines.
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To meet the requirements of collection spatial metadata, the grid is re-ordered from the original and now goes from -180 (West) to 180 (East). It is also starting from -60 (South).
The data and time units are reflected in the corresponding "units" attributes, and grid dimensions are described by longitude ("lon"), latitude ("lat") and "time" vectors. Thus, any CF-compliant tool should automatically understand the setup in the data files and the starting time for each half-hourly grid. Even without such tools, simple "ncdump" or "h5dump" command line tools will easily disclose the netCDF-4 files configuration.
Acknowledgements
The creation of the original data at NOAA/NCEP is supported by funding from the NOAA Office of Global Programs for the Global Precipitation Climatology Project (GPCP) and by NASA via the Tropical Rainfall Measuring Mission (TRMM).
The permanent archive at GES DISC is supported by NASA's HQ Earth Science Data Systems (ESDS) Program.
Product Summary
Citation
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.
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Documents
Publications Citing This Dataset
| Title | Year Sort ascending | Author | Topic |
|---|---|---|---|
| Conditions for Convective Deep Inflow | Kuo, YiHung, Neelin, J. David | Precipitation, Brightness Temperature, Droplet Size, Precipitation Rate, Radar Reflectivity | |
| Diurnal Variations in Contraction of the Radius of Maximum Tangential Wind in Tropical Cyclones | Wu, Qiaoyan, Hong, Jiacheng | Precipitation, Brightness Temperature | |
| Crucial Role of Mesoscale Convective Systems in the Vertical Mass, Water, and Energy Transports of the South Asian Summer Monsoon | Precipitation, Brightness Temperature, Precipitation Amount, Precipitation Rate, Snow, Rain | ||
| Deep Convective Cloud Top Altitudes at High Temporal and Spatial Resolution | Pfister, L., Ueyama, R., Jensen, E. J., Schoeberl, M. R. | Precipitation, Precipitation Amount, Precipitation Rate, Snow, Rain, Total Surface Precipitation Rate, Brightness Temperature | |
| Exploratory precipitation metrics: spatiotemporal characteristics, process-oriented, and phenomena-based | Leung, L. Ruby, Boos, William R., Catto, Jennifer L., A. DeMott, Charlotte, Martin, Gill M., Neelin, J. David, OBrien, Travis A., Xie, Shaocheng, Feng, Zhe, Klingaman, Nicholas P., Kuo, Yi-Hung, Lee, Robert W., Martinez-Villalobos, Cristian, Vishnu, S., Priestley, Matthew D. K., Tao, Cheng, Zhou, Yang | Precipitation, Brightness Temperature | |
| Global Tropical Precipitation Relationships to Free-Tropospheric Water Vapor Using Radio Occultations | Padulles, Ramon, Kuo, Yi-Hung, Neelin, J. David, Turk, F. Joseph, Ao, Chi O., de la Torre Juarez, Manuel | Precipitation, Brightness Temperature, Precipitation Amount, Precipitation Rate, Snow, Rain | |
| PrecipitationMoisture Coupling Over Tropical Oceans: Sequential Roles of Shallow, Deep, and Mesoscale Convective Systems | Chen, Xingchao, Leung, L. Ruby, Feng, Zhe, Yang, Qiu | Precipitation, Brightness Temperature, Precipitation Amount, Precipitation Rate, Snow, Rain | |
| Mesoscale Convective Systems Simulated by a HighResolution Global Nonhydrostatic Model Over the United States and China | Na, Ying, Fu, Qiang, Leung, L. Ruby, Kodama, Chihiro, Lu, Riyu | Precipitation, Brightness Temperature, Precipitation Amount, Precipitation Rate, Snow, Rain | |
| Significant Ionospheric Hole and Equatorial Plasma Bubbles After the | Aa, Ercha, Zhang, ShunRong, Erickson, Philip J., Vierinen, Juha, Coster, Anthea J., Goncharenko, Larisa P., Spicher, Andres, Rideout, William | Precipitation, Brightness Temperature | |
| Relationship between Size and Intensity in North Atlantic Tropical Cyclones with Steady Radii of Maximum Wind | Ruan, Zhenxin, Wu, Qiaoyan | Precipitation, Brightness Temperature | |
| The Influence of Shallow Cloud Populations on Transitions to Deep Convection in the Amazon | Barber, Katelyn A., Burleyson, Casey D., Feng, Zhe, Hagos, Samson M. | Precipitation, Brightness Temperature, Total Surface Precipitation Rate, Clouds, Cloud Properties, Cloud Fraction, Cloud Frequency, Cloud Height, Cloud Top Height, Cloud Top Temperature, Cloud Emissivity, Infrared Radiance, REFLECTED INFRARED, Visible Radiance | |
| The Behaviors of Intraseasonal Cloud Organization During DYNAMO/AMIE | Sakaeda, Naoko, Torri, Giuseppe | Precipitation, Brightness Temperature | |
| A global highresolution mesoscale convective system database using satellitederived cloud tops, surface precipitation, and tracking | Feng, Zhe, Leung, L. Ruby, Liu, Nana, Wang, Jingyu, Houze, Robert A., Li, Jianfeng, Hardin, Joseph C., Chen, Dandan, Guo, Jianping | Precipitation, Brightness Temperature, Precipitation Amount, Precipitation Rate, Snow, Rain | |
| A high-resolution unified observational data product of mesoscale convective systems and isolated deep convection in the United States for 20042017 | Li, Jianfeng, Feng, Zhe, Qian, Yun, Leung, L. Ruby | Precipitation, Brightness Temperature | |
| A Satellite-Based Remote-Sensing Framework to Quantify the Upwelling | Nguyen, Kien T., Hu, Liang, Alenin, Andrey S., Ritchie, Elizabeth A., Tyo, J. Scott | Precipitation, Brightness Temperature | |
| Implications of GNSS-Inferred Tropopause Altitude Associated with Terrestrial Gamma-ray Flashes | Xian, Tao, Lu, Gaopeng, Zhang, Hongbo, Wang, Yongping, Xiong, Shaolin, Yi, Qibin, Yang, Jing, Lyu, Fanchao | Precipitation, Brightness Temperature | |
| Diagnostics of Convective Transport over the Tropical Western Pacific from Trajectory Analyses | Smith, W. P., Pan, L. L., Honomichl, S. B., Chelpon, S. M., Ueyama, R., Pfister, L. | Precipitation, Brightness Temperature | |
| Diurnal Cycle of Tropical Oceanic Mesoscale Cold Pools | Garg, Piyush, Nesbitt, Stephen W., Lang, Timothy J., Priftis, George | Precipitation, Brightness Temperature, Total Surface Precipitation Rate, Surface Winds | |
| Crucial roles of eastward propagating environments in the summer MCS initiation over the US Great Plains | Song, Fengfei, Feng, Zhe, Leung, L. Ruby, Pokharel, Binod, Wang, S.Y. Simon, Chen, Xingchao, Sakaguchi, Koichi, Wang, Chichia | Precipitation, Brightness Temperature | |
| CYGNSS ocean surface wind validation in the tropics | Asharaf, Shakeel, Waliser, Duane E., Posselt, Derek J., Ruf, Christopher S., Zhang, Chidong, Putra, Agie W. | Precipitation, Brightness Temperature | |
| Equatorial Waves, Diurnal Tides and SmallScale Thermal Variability in the Tropical Lower Stratosphere From COSMIC2 Radio Occultation | Randel, William J., Wu, Fei, Podglajen, Aurelien | Precipitation, Brightness Temperature | |
| Examining the Capacity of Hurricane Matthew (2016) in Spawning Halo/SpriteProducible Lightning Strokes During Its Lifetime | Huang, Anjing, Yang, Jing, Cummer, Steven A., Lyu, Fanchao, Liu, Ningyu | Precipitation, Brightness Temperature | |
| Observation of gravity waves at the tropical Tropopause using superpressure balloons | Corcos, Milena, Hertzog, Albert, Plougonven, Riwal, Podglajen, Aurelien | Precipitation, Brightness Temperature | |
| Sensing Horizontally Oriented Frozen Particles With Polarimetric Radio Occultations Aboard PAZ: Validation Using GMI Coincident Observations and Cloudsat a Priori ... | Padulles, Ramon, Cardellach, Estel, Turk, F. Joseph, Ao, Chi O., de la Torre Juarez, Manuel, Gong, Jie, Wu, Dong L. | Precipitation, Brightness Temperature | |
| Sensitivity of Summertime Convection to Aerosol Loading and Properties | Fonseca, Ricardo, Francis, Diana, Weston, Michael, Nelli, Narendra, Farah, Sufian, Wehbe, Youssef, AlHosari, Taha, Teixido, Oriol, Mohamed, Ruqaya | Precipitation, Brightness Temperature |