Microwave estimates of rainfall from direct broadcast data on Guam
![](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2023/09/H9Band13-20230921_1010_1130_1530_1620step.gif)
The National Weather Service forecast office on Guam (at 13.4oN, 144.7oW) is paired with an L/X band satellite receiver that can download data from Polar Orbiting satellites, which data can subsequently be processed by Polar2Grid software to produce useful products. The animation above shows 4 different Himawari-9 Band 13 images on 21 September, a day when Guam was experiencing intermittent rains as a feature moved northward. When do you think the rain was heaviest? Did you choose 1130 UTC? That is what the microwave-derived rainrate suggests (see below). A side-by-side comparison of the Himawari Band 13 imagery and Microwave-derived rain rate is here. A meteorogram for Guam International airport is here: Heaviest observed rains were around 1200 UTC; rains ended around 1500 UTC. That is in agreement with the microwave diagnoses.
![](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2023/09/npp_atms_rain_rate_20230921_1013_161818step.gif)
What was the environment around Guam? Microwave estimates of Total Precipitable Water, below, (source), show Guam near the northern edge of a moisture-rich band of tropical origins. Advanced Scatterometer winds, at bottom, from MetopB and MetopC (times as noted in the caption), show a convergence line nearing Guam on 20 September (on 21 September, ASCAT did not sample over Guam).
![](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2023/09/mimictpw_wpac_24h_ending_2000_21September.gif)
![](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2023/09/MetopB_Descending_Ascending21Sept2023_0000_1107_1200UTCstepanim.gif)
Thanks to Douglas Schumacher, CIMSS, for supplying the imagery from the Guam Direct Broadcast antenna!