Satellite images captured a dramatic change on Oahu
NASA Earth Observatory has published a stark before-and-after view of flooding on Oahu following two powerful March storms that brought some of Hawaii’s worst flooding in decades. The imagery, acquired by the Operational Land Imager on Landsat 9, compares conditions on January 25, 2026, with those on March 14, 2026, after the first and more destructive of the two storm systems struck the island.
In the earlier image, coastal towns and green farmland between Mokuleia and Waialua appear largely unaffected, and the nearby ocean is mostly blue. In the later scene, floodwaters spread across neighborhoods and farmland, while a red-brown sediment plume extends into coastal waters around Kaiaka Bay. The side-by-side contrast makes the scale of the flooding legible in a way that rainfall totals alone often do not.
NASA says the flooding followed back-to-back low-pressure systems that struck Hawaii in March 2026. Near the islands, these subtropical weather systems are known as kona lows.
What made the storms so destructive
According to NASA Earth Observatory, the kona lows siphoned moisture from the tropics and fueled slow-moving thunderstorms with torrential, destructive rains. That combination is important. Storms do not need to move quickly to be dangerous; in many flood events, persistence is the key variable. When heavy rain lingers over the same areas, runoff accumulates, drainage systems are overwhelmed, and floodwaters spread far beyond streams and channels.
The National Weather Service reported rainfall totals of 5 to 10 inches across the state between March 11 and March 15. Some areas saw more than 30 inches. Weather stations in Honolulu, Hilo, Lihue, and Kahului all broke daily rainfall records during the period.
Those figures help explain why the flood signal in the satellite image is so extensive. The March 14 image does not show an isolated patch of standing water. It shows a landscape reorganized by runoff, with swamped neighborhoods, inundated farmland, and visible discoloration of nearshore waters from suspended sediment.








