Rain and ice profiles inside storms (TRMM)
What it measures. Estimates of rainfall at the surface and vertical profiles of water and ice inside storms - cloud water, rain, cloud ice, falling ice, and the heat released as rain forms - layer by layer through the atmosphere.
How it's made. Derived from microwave brightness measurements by the TRMM Microwave Imager, using the Goddard Profiling algorithm to match each pixel to one of 100 typical storm structures.
How & where you'd use it. Useful for studying tropical storms and the inner workings of rainfall, though note this version has been superseded by a newer GPM-format product.
What's measured
Coverage & cadence
- Time span1997-12-31 → 2015-04-08
- Measured byTRMM (TMI)
- Processing levelLevel 2
- Spatial extent-180, -38, 180, 38
- StatusCOMPLETE
What you can do with it
- Map air pollutants — NO₂, aerosols, ozone
- Track greenhouse gases and Earth's energy budget
- Feed weather and air-quality analysis
Official description
The new version of these data is in GPM-like format and can be found under the name GPM_2AGPROFTRMMTMI_CLIM. This dataset, 2A12, ”TMI Profiling”, generates surface rainfall and vertical hydrometeor profiles on a pixel by pixel basis from the TRMM Microwave Imager (TMI) brightness temperature data using the Goddard Profiling algorithm GPROF2010. Because the vertical information comes from a radiometer, it is not written out in independent vertical layers like the TRMM Precipitation Radar. Instead, the output is referenced to one of 100 typical structures for each hydrometeor or heating profile. These vertical structures are referenced as clusters in the output structure. Vertical hydrometeor profiles can be reconstructed to 28 layers by knowing the cluster number (i.e. shape) of the profile and a scale factor that is written for each pixel. This product contains hydrometeor profiles of cloud liquid water, precipitation water, cloud ice water, precipitation ice, rainfall type, and latent heating in 28 atmospheric layers. Changes in horizontal resolution resulting from the TRMM boost that occurred on 24 August 2001: Pre-Boost (before 7 August 2001): Temporal Resolution: 91.5 min/orbit ~ 16 orbits/day; Swath Width: 760 km; Horizontal Resolution: 4.4 km Post-Boost (after 24 August 2001): Temporal Resolution: 92.5 min/orbit ~ 16 orbits/day; Swath Width: 878 km; Horizontal Resolution: 5.1 km
Get the data
import earthaccess
earthaccess.login(strategy="netrc") # free Earthdata Login
results = earthaccess.search_data(
short_name="TRMM_2A12",
version="7",
bounding_box=(-122.5, 37.2, -121.8, 37.9), # your area (W,S,E,N)
temporal=("2024-01-01", "2024-12-31"), # your dates
)
files = earthaccess.open(results) # stream straight from GES_DISC Browsing CMR needs no login. Downloading or streaming bytes needs a free Earthdata Login + the earthaccess package. Official links
- Access the data via HTTPS GET DATA
- Use the Earthdata Search to find and retrieve data sets across multiple data centers. GET DATA
- File specification document. VIEW RELATED INFORMATION
- Comparison between TRMM versions 6 and 7. VIEW RELATED INFORMATION
- README Document VIEW RELATED INFORMATION
- Access the data via the OPeNDAP protocol. USE SERVICE API
- TRMM Data Gaps VIEW RELATED INFORMATION
- TRMM File Naming Convention VIEW RELATED INFORMATION