Answers are grounded in this paper and cite their sources.
The meteorological conditions associated with the high-inversion fog episode on 23–28 December 1978 near Chico, California, are described. In general, the meteorological conditions throughout the fog and inversion layers were characterized by wind speeds ≤3.5 m s−1, wind speed shear <1.0 m s−1 (100 m)−1, and wind directional shear of 10–20°(100 m)−1. Diurnal temperature variations at the earth's surface were 2°C or less. The fog layer had a near moist adiabatic lapse rate and a maximum height of 530 m. Pilot reports of the fog top (inversion base) suggest slight spatial and temporal variations in the fog-layer thickness during the 6-day episode. The inversion above the fog was moderately stable with low relative humidity and a thickness ranging from 200 to 1000 m. These meteorological conditions also were typical of other high-inversion episodes from 1954–80 in the Central Valley.
No takes yet. Share an insight, caveat, or question.
Holets et al. (1981) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: