Visibility
Tule fog is a thick ground fog that settles in valley areas of California during the late autumn and winter after the first significant rainfall. The official time frame for tule fog to form is from November 1 to March 31, California’s rainy season. This phenomenon is named after the tule grass wetlands of the Central Valley.
Radiation fog is formed by the cooling of land after sunset by thermal radiation in calm conditions with clear sky. The cool ground produces condensation in the nearby air by heat conduction. In perfect calm the fog layer can be less than a meter deep but turbulence can promote a thicker layer. Radiation fogs occur at night, and usually do not last long after sunrise.
In California, tule fog can extend from Bakersfield to Red Bluff. Tule fog occasionally drifts as far west as the San Francisco Bay Area, even drifting westward out the Golden Gate, opposite to the usual course of summertime ocean fog. The nights are longer in the winter months, which creates rapid ground cooling, and thereby a pronounced temperature inversion at a low altitude.
The fog forms when cold mountain air flows downslope into the valley during the night, pooling in the low areas until it fills the valleys. This occurs because most areas in the valley has little or no air drainage below the level of mountains. Because of the density of the cold air in the winter, winds are not able to dislodge the fog and the high pressure of the warmer air above the mountaintops presses down on the cold air trapped in the valley, resulting in a dense fog..
In the California’s Central Valley, Tule fog is a low cloud, usually below 1,000 feet in altitude that can be seen from above by driving up into the foothills of the Sierra Nevada to the east or the Coast Ranges to the west. Above the cold, foggy layer, the air is typically warm, dry and clear. Once tule fog is formed, turbulent air is necessary to break through the temperature inversion layer. Daytime heating sometimes evaporates the fog in some areas, although the air remains chilly and hazy below the inversion. Tule fog usually remains longer in the southern and eastern parts of the Central Valley.
Visibility in tule fog is usually less than an eighth of a mile, but can be less than 10 feet. Visibility can vary rapidly. In only a few feet visibility can go from 10 feet to near zero. Satellite and overhead photos of the San Joaquin Valley may show the fog where agriculture and cities like Sacramento can be seen.
Lack of visibility in tule fog is hazardous enough, but these fog events are often accompanied by drizzle and freezing drizzle. Because of the lack of sunlight penetrating the fog layer, temperatures may struggle to climb above freezing, and episodes of freezing drizzle occasionally accompany tule fog events during winter. Such events can leave an invisible glaze of black ice on roadways, making travel especially treacherous.
Accidents caused by the tule fog are the leading cause of weather-related casualties in California.

Sebastopol, California