ISS032-E-24687 Click the photo number to access all resolutions available and the database record.
Smaller fire “complexes” appear as tendrils of smoke near the sources—for example, the Halstead fires—and as major smoke plumes from fires in the densest forests—such as the Mustang fire complex. Mustang produced the largest plume in the region, with thick smoke blowing eastward over the Beaverhead Mountains (image bottom).
The linear shape of the smoke plumes gives a sense of the generally eastward smoke transport on September 3, 2012. (Note that the image is rotated so that north is to the right.) The smoke distribution also reveals another kind of transport. At night, when winds are weak, the cooling of the atmosphere near the ground causes cooler, denser air to drain down into the valleys. On September 3, this led to some smoke flowing west, down into the narrow Salmon and Lochsa River valleys—in the opposite direction from the higher winds and the thick smoke masses.
Beyond the fires, the bright yellow-tan areas at image top left and right are grasslands (including the Palouse Grasslands Ecoregion). Light green areas in many of the valleys are agricultural crops, including barley, alfalfa, and wheat. The largest single wilderness area in the contiguous United States, the Frank Church-River of No Return Wilderness, occupies the wooded zones of the Salmon River Mountains and the Clearwater Mountains—most of the area shown in the middle of the image. And the Continental Divide cuts through the bottom of the image—rivers on the eastern slopes of the Beaverhead Mountains drain to the Atlantic Ocean, while rivers in the rest of the area drain to the Pacific Ocean.
