The low, sharp inversion can lead to areas of persistent stratocumulus or stratus cloud, colloquially known as anticyclonic gloom.
2.
For example, extensions of the Azores high pressure may bring about anticyclonic gloom during the winter because they are warmed at the base and trap moisture as they move over the warmer oceans.
3.
For example, extensions of the Azores high pressure may bring about anticyclonic gloom during the winter, as they are warmed at the base and will trap moisture as they move over the warmer oceans.
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