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- Q747330 subject Q8151534.
- Q747330 abstract "An occluded front is formed during the process of cyclogenesis when a cold front overtakes a warm front. When this occurs, the warm air is separated (occluded) from the cyclone center at the Earth's surface. The point where the warm front and the occluded front meet (and consequently the nearest location of warm air to the center of the cyclone) is called the triple point.The trowal (short for TROugh of Warm air ALoft) is the projection on the Earth's surface of the trough of warm air aloft formed during the occlusion process of the depression.".
- Q747330 thumbnail Occluded_cyclone.svg?width=300.
- Q747330 wikiPageExternalLink ofdef.rxml.
- Q747330 wikiPageExternalLink 2010BAMS3057.1.
- Q747330 wikiPageWikiLink Q1063457.
- Q747330 wikiPageWikiLink Q11157129.
- Q747330 wikiPageWikiLink Q1194255.
- Q747330 wikiPageWikiLink Q1757780.
- Q747330 wikiPageWikiLink Q189796.
- Q747330 wikiPageWikiLink Q2.
- Q747330 wikiPageWikiLink Q209190.
- Q747330 wikiPageWikiLink Q210316.
- Q747330 wikiPageWikiLink Q245472.
- Q747330 wikiPageWikiLink Q537536.
- Q747330 wikiPageWikiLink Q8151534.
- Q747330 wikiPageWikiLink Q865144.
- Q747330 comment "An occluded front is formed during the process of cyclogenesis when a cold front overtakes a warm front. When this occurs, the warm air is separated (occluded) from the cyclone center at the Earth's surface.".
- Q747330 label "Occluded front".
- Q747330 depiction Occluded_cyclone.svg.