The mp4 animation above (produced using CSPP Geosphere‘s latest beta version) shows strong convection over Oklahoma and the eastern Texas panhandle, with lower clouds (in a bluish hue) over the northwestern Texas panhandle. With time, the Night Microphysics RGB acquires a reddish hue (as cloud tops cool), and then convection develops. A nowcaster can use changes in the colors of this RGB to anticipate initiation. (A similar recent example is shown here).

The AWIPS imagery from 0701 UTC below shows the RGB with Level 2 Products: Cloud Top Phase — showing liquid water clouds over Texas where the RGB suggests low clouds, and Cloud Top Temperature — where values of 7-8^oC are common. The default color table Cloud Top Temperature has been changed. Recall also that the Level 2 Cloud Top Temperature product is not produced for the CONUS sector, so Full-Disk values are shown. Surface winds suggest low-level convergence: winds are northeasterly over the NW Texas panhandle, and southeasterly to easterly over the southern portions of the Texas panhandle. GOES-16 Cloud Top Heights (not shown) show cloud heights around 12000 feet over the NW Texas panhandle.

Fifty minutes later, at 0751, the band of low clouds over the northeastern Texas panhandle has reddened somewhat (click here for a toggle between 0701 and 0751). Cloud top temperatures in that cloud band have dropped to between 1^o and 4^oC, and cloud top heights have increased to 14000 feet. Cloud-top phase is still liquid however (except over northern New Mexico, as might be inferred by the yellower tinge to those low clouds in the RGB). There is also a red tint to the RGB just north of the obvious east-west band of clouds near the Hereford TX airport (where the temperature and dewpoint are 65 and 60, respectively, and no wind is reported). Convective initiation is likely occurring in these regions.

From 0801 to 0816 UTC, shown below, supercooled clouds are noted, as the Night Microphysics RGB continues to redden. By 0816 UTC, mixed phase clouds are noted in the line developing near Hereford. Cloud-top heights increase from 15000 to 21000 feet between 0811 and 0816 UTC.

By 0826 UTC, Cloud Tops are shown to include ice over the line developing over the east-central part of the Texas panhandle.

A rocking animation of the 4-panels above, from 0801 to 0901 (and back) is here. If convection is expected overnight, and low clouds are present, use the Night Time Microphysics RGB to monitor when convection might initiate. Color changes in the low clouds give important information.

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1-minute Mesoscale Domain Sector GOES-16 (GOES-East) “Red” Visible (0.64 µm) images (above) include time-matched SPC Storm Reports — and showed the development severe thunderstorms across parts of the Upper Midwest during the afternoon and early evening hours on 30 May 2022. These storms produced several tornadoes, hail as large as 2.00 inches in diameter and damaging winds as strong as 90 mph.

In the corresponding 1-minute GOES-16 “Clean” Infrared Window (10.35 µm) images (below), pulsing overshooting tops exhibited infrared brightness temperatures as cold as -70ºC (darker black enhancement).

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1-minute Mesoscale Domain Sector GOES-17 (GOES-West) — and GOES-16 (GOES-East) after 1621 UTC — “Clean” Infrared Window (10.35 µm) and “Red” Visible (0.64 µm) images (above) showed Hurricane Agatha after the tropical storm reached hurricane intensity at 1200 UTC on 29 May 2022. Overshooting tops near the storm center exhibited infrared brightness temperatures as cold as -90 to -95ºC at times.

GOES-16 Infrared Window (11.2 µm) images from the CIMSS Tropical Cyclones site (below) include contours of deep-layer wind shear at 12 UTC and 21 UTC — which indicated that Agatha was moving through an environment of relatively low shear, one factor that favored its phase of rapid intensification (ADT | SATCON).

Agatha was also moving across warm water, with high Sea Surface Temperature and modest Ocean Heat Content values.

===== 30 May Update =====

Hurricane Agatha made landfall along the southern coast of Mexico — between Puerto Escondido MMPS and Bohias De Huatulco MMBT —  around 2040 UTC on 30 May, as seen in 1-minute GOES-16 Visible and Infrared images (above).

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A sequence of GOES-16 (GOES-East) Day Land Cloud RGB images and radar-estimated Storm Total Precipitation (above) revealed a west-to-east oriented swath of wet soil (darker shades of brown) created by thunderstorms that moved across central Iowa on 28 May 2022. Radar-estimated precipitation associated with the swath was generally 1 inch or less.

Given the fairly light precipitation amounts, the swath of wet soil dried rather quickly due to warm and windy conditions across the area (below).

Comparisons of GOES-16 Day Land Cloud RGB, Land Surface Temperature (LST) and radar-estimated Storm Total Precipitation at 1601 UTC and 1701 UTC (below) showed that the swath of moist soil exhibited LST values in the upper 60s to low 70s F (shades of green), in contrast to upper 80s to low 90s F (shades of orange) across adjacent areas of dry soil.

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