Cold drop

Source: Wikipedia, the free encyclopedia.
A stationary cold low, in which a cold drop is found.

A cold drop (from the Spanish "gota fría") is a term used in Spain that has commonly come to refer to any high impact rainfall events occurring in the autumn along the Spanish Mediterranean coast.[1] In Europe, cold drops belong to the characteristics of the Mediterranean climate.[2][3] It is also termed a cut-off low.

Occurrence

Spain

If a sudden cut off in the stream takes place (particularly in the

flash floods. For instance, the great Valencia flood of 1957
was the result of a 3-day-long cold drop.

This phenomenon is associated with extremely violent downpours and storms, but not always accompanied by significant rainfall. For this, high atmospheric instability in the lower air layers needs to combine with a significant amount of moisture.[4]

Other areas

Cut-off lows are apparent near the

and the northeast Atlantic.

See also

References

  1. ^ Martín León, Francisco (2003). "LAS GOTAS FRÍAS / DANAS IDEAS Y CONCEPTOS BÁSICOS" (PDF). Servicio de Técnicas de Análisis y Predicción, INM (in Spanish). Retrieved 13 September 2019.
  2. ^ "Los episodios de lluvias intensas otoñales en Francia: el cévenol". Tiempo.com (in European Spanish). 14 October 2016. Retrieved 13 September 2019.
  3. ^ Cold drop meteorologiaenred.com
  4. ^ Cut-Off Lows and Extreme Precipitation in Eastern Spain: Current and Future Climate by Rosana Nieto Ferreira from Department of Geography, Planning and Environment, East Carolina University. 28 June 2021. Retrieved 6 April 2022.