Arctic Blast Brightened the West Florida Shelf

January 24, 2026

February 3, 2026

Gulf waters off southwestern Florida appear dark blue, except for some lighter greenish areas along the coast and Florida Keys.

NASA Earth Observatory

Gulf waters off southwestern Florida appear bright blue due to suspended sediment. The water swirls into intricate patterns along the bright area’s western edge as it transitions to dark blue.

NASA Earth Observatory

January 24, 2026

February 3, 2026

In late January and early February 2026, surges of Arctic air funneled into eastern North America, causing cold and wintry conditions across much of the United States. Snow and ice blanketed large swaths of the country, stretching as far south as Georgia, in a layer of white. Meanwhile, waters off the west coast of Florida lit up in brilliant shades of blue.

In this rare outbreak of intense winter weather, cold air infiltrated Florida and drove temperatures below freezing in several counties at the start of February. This frigid intrusion not only caused beautiful phenomena in the atmosphere, forming cloud streets, but it also produced a colorful display in the shallow marine waters below, stirring up carbonate sediment from the seafloor.

On February 3, the MODIS (Moderate Resolution Imaging Spectroradiometer) on NASA’s Terra satellite captured this image (right) of brightened waters over the West Florida Shelf, a broad and shallow continental shelf region known as a carbonate ramp. The blue color comes from suspended calcium carbonate (CaCO₃) mud, which consists primarily of remnants of marine organisms that live on the shelf. For comparison, the left image shows the area on January 24, before the cold air arrived.

The mud was mostly kicked up by wind-stirred ocean waters during the cold air event, said James Acker, a data support scientist at the NASA Goddard Earth Sciences Data and Information Services Center. Sediment suspension events like this are more typically associated with hurricane winds that churn the water, as with Melissa in 2025, but the winds brought by strong cold fronts can have a similar, if less dramatic, effect.

“Another interesting aspect of these events is that the cold air cools off the shallow water on the banks and makes it denser than the surrounding warmer open ocean water,” Acker said. When this dense water sinks and flows offshore with the tides, it can carry some of the sediment out toward the shelf’s edge.

The water north of the Florida Keys appears bright blue to white. To the south, it is dark blue except for a long, narrow bright band running from west to east.

February 3, 2026

An area of bright blue swirling water includes a feature with a hammerhead-like shape, with eddies curling off either side of a narrow jet.

February 3, 2026

The detailed images above, acquired with the OLI (Operational Land Imager) on Landsat 9, offer a closer look at that process playing out. “Hammerhead” eddy features appeared along the slope of the West Florida Shelf, Acker noted. These can form when narrow streams of denser chilled seawater carry sediment offshore, encounter slower-moving Gulf waters, and curl into pairs of counterrotating eddies, he said. These types of features have been observed in other natural events—dust storms, for example—both on Earth and on Mars.

Other dynamics were at work near the Dry Tortugas on the southwestern side of the shelf, where the patch of bright water ends abruptly along a straight, sharp edge. Here, sediment-laden water exited the shelf area through channels to the south, said sedimentologist Jude Wilber, and was immediately swept east by the Loop Current. After Hurricane Ian stirred up sediment off Florida in 2022, Wilber and Acker noted a similar interaction between suspended material and the Loop Current. The researchers used that event to improve satellite-based methods for estimating sediment concentrations in these plumes.

Scientists are interested in studying carbonate sediment suspension events because of their role in the planet’s carbon cycle. They have shown that tropical cyclones are the primary mechanism by which carbon in shallow-water marine sediments is moved to deeper waters, where it can remain sequestered for a long time. However, the contribution of cold fronts is less well understood. Acker and Wilber hypothesize that they act on a more local scale: they influence ocean color by stirring sediments but do not transport significant amounts of material to the deep ocean.

NASA Earth Observatory images by Michala Garrison, using MODIS data from NASA EOSDIS LANCE and GIBS/Worldview, and Landsat data from the U.S. Geological Survey. Story by Lindsey Doermann.