How is the intensity of precipitation distributed within a given data value in IMERG?
In the previous TMPA data set, each data value provided a precipitation rate based on one (or perhaps two) satellite snapshots during the TMPA’s 3-hour analysis period. IMERG values are based on a single microwave snapshot during its half-hour analysis period, or a morphed/Kalman filter interpolation if no microwave values are available. The values are expressed in the intensive units mm/hr; it is usually best to assume that this rate applies for the entire half-hour period.
How important are surface precipitation gauges in combined satellite-gauge data sets?
Q1: How closely should the monthly satellite-gauge combined precipitation datasets follow the gauge analysis?
What is the difference between the global (90°N-S) and full (60°N-S) coverage for IMERG?
Compared to previous versions, Version 06 IMERG introduces additional coverage at the high latitudes for the precipitation fields in all Runs -- Early, Late, and Final. IMERG continues to use a merged geosynchronous infrared brightness temperature analysis to provide IR-based precipitation estimates. The requisite analysis (provided by NOAA/NWS/Climate Prediction Center) covers the latitude band 60°N-S, so a "full" IMERG analysis is possible there.
What are the IMERG variables in Giovanni?
The following table provides a quick reference for the IMERG variables that can be visualized using Giovanni.
Product |
Variable and Description |
---|---|
GPM_3IMERGHHE 30-min averaged data |
Merged microwave-only precipitation estimate [Final] Precipitation estimates from combining microwave data from the GMI, TMI, and other partner instruments. |