Pembrokeshire Dangler
id:
pembrokeshire-dangler-182-14315199
title:
Pembrokeshire Dangler
text:
The Pembrokeshire Dangler is a convergence zone which forms a line of continuous showers aligned north-south across the Irish Sea; often as snow occurring during late autumn and winter, since the environmental factors required for its formation such as warm sea temperatures and cold Arctic air aloft are usually only met at this time of year. It is initiated as a northerly flow is forced between the Rhins of Galloway and the Antrim Plateau. This is then augmented by land breeze effects producing
brand slug:
wiki
category slug:
encyclopedia
description:
Meteorological phenomenon over the Irish Sea
original url:
https://en.wikipedia.org/wiki/Pembrokeshire_Dangler
date created:
2006-02-04T21:03:02Z
date modified:
2024-09-06T12:01:16Z
main entity:
{"identifier":"Q7161993","url":"https://www.wikidata.org/entity/Q7161993"}
image:
fields total:
13
integrity:
15