1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Visible and Infrared images (above) showed Category 5 Hurricane Melissa as it made landfall along the far southwest coast of Jamaica around 1700 UTC on 28 October 2025. Low-altitude mesovortices were evident within the eye — and GLM Flash Points revealed abundant lightning activity within the inner eyewall region.

1-minute GOES-19 Infrared images displayed using RealEarth (below) indicated that the center of the eye of Melissa passed over White House, Jamaica during landfall — with the right-front quadrant of the inner eyewall (where wind damage and storm surge is often highest) passing over Black River.

Shortly after Melissa made landfall, the eye quickly became cloud-filled as the hurricane moved inland and interacted with topography across the western part of Jamaica (below).

A larger-scale view of GOES-19 CIMSS True Color RGB images created using Geo2Grid (below) indicated that after landfall, the eye of Melissa remained cloud-filled as the hurricane finished crossing the island and eventually emerged over water north of Jamaica around 2100 UTC. 

A larger-scale view of 1-minute GOES-19 Infrared images during the 5 hours leading up to landfall is shown below — which revealed a continual series of cloud-top gravity waves propagating radially outward from the eye of Melissa. The radius of hurricane-force winds appeared to be rather small, since surface wind speeds at the Kingston METAR site in eastern Jamaica were only in the 20-40 kt range during that time period.

A GMI Microwave image (below) displayed the compact eye and eyewall of Melissa about 3 hours prior to landfall.

Just prior to landfall, Melissa was moving through an environment characterized by fairly low values of deep-layer wind shear (below).

A Synthetic Aperture Radar (SAR) image (source) at 1110 UTC (below) retrieved a maximum wind velocity value of 143 kts in the NW quadrant of Melissa.

It is noteworthy that the Advanced Dvorak Technique (ADT) satellite-derived intensity estimate peaked at 185 kts for Melissa (below) — which according to the developer at CIMSS is the highest value on record for any tropical cyclone since the ADT was implemented.

219-kt peak wind would be the highest wind value a dropsonde has ever recorded, ahead of 215-kt value in Super Typhoon Megi in 2010 & the 210 kt recorded just yesterday in #Hurricane #Melissa.Still needs to be validated… so this data is preliminary.

— Philippe Papin (@pppapin.bsky.social) 2025-10-28T15:48:47.358Z

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1-minute Mesoscale Domain Sector GOES-19 (GOES-East) Infrared images (above) showed Tropical Storm Melissa in the Caribbean Sea as it began to rapidly intensify during the afternoon and evening hours on 25 October 2025 — reaching Category 1 intensity at 1800 UTC on 25 October and Category 3 intensity at 0300 UTC on 26 October. A series of convective bursts (exhibiting cloud-top infrared brightness temperatures as cold as -90 to -96C, denoted by darker shades of purple) rotated around the storm center — and GLM Flash Points highlighted intermittent lightning activity within some of those convective bursts. Some semblance of a ragged eye occasionally appeared as Melissa neared and attained Category 3 intensity, but an eye was never well organized in the infrared imagery.

Melissa then reached Category 4 intensity south of Jamaica at 1200 UTC on 26 October — and by that time the eye was well defined in both Infrared and Visible imagery (below). Low-altitude mesovortices were apparent within the eye in the Visible images.

The eye of Category 4 Melissa was exhibiting a “stadium effect”, with a small surface eye having walls that sloped outward with height (below).

Melissa was moving through an environment of relatively light deep-layer wind shear, and was traversing warm water — two factors that favored intensification (below).

===== 27 October Update =====

Post-sunrise 1-minute GOES-19 Visible and Infrared images on 27 October (above) again showed a nice “stadium effect” with the eye of Melissa, which reached Category 5 intensity south of Jamaica at 0900 UTC. Visible images continued to display low-altitude mesovortices within the 10-mile diameter eye — and GLM Flash Points highlighted abundant lightning activity within the inner eyewall.

The maximum sustained wind speed of Melissa was increased to 150 kts at 2100 UTC (SATCON | ADT).

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5-minute PACUS Sector GOES-18 (GOES-West) Mid-level Water Vapor and Upper-level Water Vapor images (above) displayed orographic waves downwind (southwest) of the Hawaiian Islands on 23 October 2025. With a ridge of high pressure north of Hawai’i (surface analyses), boundary layer flow from the northeast interacted with the topography of the island chain — generating vertically-propagating waves that were apparent in Mid-level (and to a lesser extent, even Upper-level) Water Vapor imagery (below).

Northwest of the Big Island of Hawai’i, there was one Pilot Report of continuous light turbulence between the altitudes of 18000-20000 ft (below).

One item of interest was the diurnal change in thermal signatures of the Mauna Kea and Mauna Loa summits — transitioning from cooler (darker shades of blue) during the nighttime at 1201 UTC to warmer (brighter shades of yellow) during the daytime at 0001 UTC (below).

Plots of Weighting Functions for the GOES-18 Mid-level and Upper-level Water Vapor spectral bands — derived using rawinsonde data from Hilo (PHTO) — showed the profiles of Band 08 and Band 09 weighting functions at 1200 UTC on 23 October to 0000 UTC on 24 October (below). The summits of Mauna Kea and Mauna Loa extend upward to near the 600 hPa pressure level — close to the level of strong weighting function contributions for Water Vapor spectral band 09 at each of those 2 times.

This diurnal variability of Mauna Kea and Mauna Loa thermal signatures in Water Vapor imagery has been discussed in previous blog posts here, here and here.

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In a sign that the seasons are changing, the lake effect is now clearly visible over the Great Lakes. While most commonly associated with heavy snowfalls downwind of the Great Lakes, in these early pre-freezing times of the year it can be associated with the enhancement of rainfall as well. The lake effect has two principal causes: colder air that originated over land is advected over warmer lake water causing latent heat transfer into the cold air mass, while the topographical lift and sudden increase in friction at the opposite shore forces additional upward motion, leading to precipitation enhancement. Lake effect clouds are generally shallow compared to more synoptically-forced precipitation systems.

The lake effect is easily detectable via satellite as parallel bands of clouds oriented along the direction of the wind flow. However, advanced tools allow us to gain some additional insight about the lake effect and its underlying processes from satellites. For example, here is the Day Cloud Phase Distinction RGB from GOES-19. In this product, three GOES ABI channels with various cloud microphysical characteristics are assigned the red, green, or blue color in the animation to help highlight various characteristics of the clouds. In this product, low level liquid-phase clouds are lavender or cyan, thicker liquid clouds are yellow, glaciating clouds are green, and thin cirrus are salmon.

To begin with, the ASOS observations plotted on the above animation show northeasterly winds on either side of the Lake Michigan shore, being driven by a large midlatitude cyclone centered over northern Quebec (see the surface map here to know more about the synoptic situation). Bands of shallow convection are visible from the central axis of Lake Michigan streaming to the southeast. These clouds are a light cyan to periwinkle in color in this RGB, which indicates that they are likely low-level liquid clouds. This is consistent with what we’d expect for lake effect precipitaiton, especially in mid-October.

As the clouds propagate toward the Michigan shore, they become more congested and are changing to a greenish-yellow. This color shift indicates that they clouds are deepening and changing phase to ice at their tops. In fact, these clouds are growing deep enough to precipitate. Since surface temperatures on the western edge of the lower peninsula of Michigan are well into the mid 40s, this takes the form of rain. A contemporaneous view of the NEXRAD radar mosaic is seen below.

Of course, the key factor in the development of lake effect precipitation is a difference in the temperature of the air that originated over the land relative to the temperature of the water surface. The Great Lakes Surface Enivronmental Analysis produced by our colleagues at NOAA’s Great Lakes Environmental Research Laboratory shows that mid-lake temperatures are in the low-to-mid 60s.

However, the surface temperatures over Wisconsin depicted in the initial animation show that the airmass likely has a temperature in the mid 40s. That is a substantial difference between the lake and the air that is advecting over it, and so it should not be a surprise that this is having an impact on the precipitation patterns.

As noted above, lake effect precipitation is shallow. One way to illustrate this is by looking at two adjacent radars. The minimum elevation angle for a NEXRAD weather radar is typically set to 0.5 degrees above the horizon while the surface of the earth is curving away from the beam. This means the further away from a radar one goes, the farther above the surface the bottommost radar beam is. While deep precipitation systems are tall enough to be easily visible from multiple radars, shallow systems can often sneak below the minimum beam height. Here, contemporaneous radar images from Grand Rapids, Michigan(left), and Detroit (right), are shown. Note how the Detroit radar is unable to detect the rain in the western half of the state: it’s just too shallow to appear on that radar.

The lake effect will likely be contributing to rain and snow over the next few months as the large thermal mass of the lake generally means it remains warmer than the surrounding land for much of the fall and winter. (In the spring, the temperature gradient reverses and lake breezes are born instead).

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