1979
DOI: 10.1175/1520-0450(1979)018<1275:tfomfa>2.0.co;2
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The Formation of Marine Fog and the Development of Fog-Stratus Systems along the California Coast

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Cited by 116 publications
(77 citation statements)
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“…California marine stratus and fog have been studied primarily on daily time scales (3,(26)(27)(28)(29) with aims toward forecasting for aviation and maritime activities.…”
Section: Resultsmentioning
confidence: 99%
“…California marine stratus and fog have been studied primarily on daily time scales (3,(26)(27)(28)(29) with aims toward forecasting for aviation and maritime activities.…”
Section: Resultsmentioning
confidence: 99%
“…Figure 6b shows that the period was characterized by multiple events of cloud-base lowering followed by cloud-base rising with a stratus-fog layer ranging in depth from 200 to 1,000 m. Cloud radar reflectivity profiles up to 12 km (not shown) indicate that there were no clouds above the stratus deck during the entire period. Several processes have been suggested to explain variations in near-surface stratus cloud-base heights (e.g., Oliver et al 1978;Pilié et al 1979). ParisFog observations show that several processes were at play during the period.…”
Section: Stratus-fog Events: 23-29 December 2006mentioning
confidence: 99%
“…It is expected that the combination of these two datasets can be sufficient for investigating the roles of large-scale environmental changes in long-term sea-fog variation in the near surface layer. In particular, a temperature difference between the atmosphere and ocean has been often adopted for estimating sea-fog generation over the ocean (Pili e et al 1979;Dorman et al 1998;Cho et al 2000;Koracin et al 2001;Lewis et al 2003). Reanalysis-based temperature difference is easily calculated and suggests a possibility for generating sea fog over the ocean; this value is insufficient for discussing fog frequency observed in coastal land areas, however.…”
Section: Introductionmentioning
confidence: 99%