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Cold drop

meteorological phenomenon blocking atmospheric circulation

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionSep 17, 2026
Entity authorityQ2735247
Source-derived summary

A cold drop is a term used in Spain and France that has commonly come to refer to any high impact rainfall event occurring in the autumn along the Spanish Mediterranean coast or across France. In Europe, cold drops belong to the characteristics of the Mediterranean climate.

The Spanish-language name of gota fría was directly adapted from the term Kaltlufttropfen introduced by German meteorologists, and became very popular in 1980s Spain as a blanket term to refer to any high-impact rainfall event.

In the eastern regions of the Iberian Peninsula, these events are typically caused by the interaction of upper-level low pressure systems strangled and ultimately detached from the zonal (eastward) circulation displaying stationary or retrograde (westward) circulation with humid warmer air masses that form over an overheated Mediterranean Sea in the Autumn. The Spanish equivalent of cut-off low is known as an "isolated depression at high levels" (depresión aislada en niveles altos) and is often abbreviated to the acronym DANA. Such recurring synoptic configurations are not necessarily associated to cold drop events.

Occurrence

Spain

If a sudden cut off in the jet stream takes place (particularly on the Atlantic Ocean), a pocket of cold air detaches from the main jet stream, moving southward over the Pyrenees into the warm air over Spain, causing its most dramatic effects in the southeast of Spain, particularly along the Spanish Mediterranean coast, especially in the Valencian Community. The torrential rain from a cold drop can result in devastation from torrents and flash floods.

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 layers of the atmosphere needs to be combined with a significant amount of moisture.

Disasters

The great Valencia flood on 14 October 1957 was the result of a three-day-long cold drop and caused the deaths of at least 81 people.

Editorial summary

Begin with the source’s own compact description: “Cold drop” is meteorological phenomenon blocking atmospheric circulation. The dossier treats that line as a proposition to test through Cold, drop and meteorological, not as a finished interpretation.

Editorial reviewA dependable orientation record for establishing vocabulary, names and a first evidence trail. The current lead gives the account dated anchors—1957—that can be checked directly. The selected authority fields contribute no independent date. For this dossier, Cold, drop and meteorological is the immediate research focus.
Editorial analysis

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Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Sep 17, 2026. The linked authority identifier is Q2735247. The first chronological checks are 1957.

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This entry incorporates text from Cold drop” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.