Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q2882177> ?p ?o }
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- Q2882177 subject Q7139097.
- Q2882177 subject Q7213751.
- Q2882177 subject Q8432456.
- Q2882177 subject Q9041898.
- Q2882177 subject Q9382390.
- Q2882177 abstract "A rainband is a cloud and precipitation structure associated with an area of rainfall which is significantly elongated. Rainbands can be stratiform or convective, and are generated by differences in temperature. When noted on weather radar imagery, this precipitation elongation is referred to as banded structure. Rainbands within tropical cyclones are curved in orientation. Tropical cyclone rainbands contain showers and thunderstorms that, together with the eyewall and the eye, constitute a hurricane or tropical storm. The extent of rainbands around a tropical cyclone can help determine the cyclone's intensity.Rainbands spawned near and ahead of cold fronts can be squall lines which are able to produce tornadoes. Rainbands associated with cold fronts can be warped by mountain barriers perpendicular to the front's orientation due to the formation of a low-level barrier jet. Bands of thunderstorms can form with sea breeze and land breeze boundaries, if enough moisture is present. If sea breeze rainbands become active enough just ahead of a cold front, they can mask the location of the cold front itself. Banding within the comma head precipitation pattern of an extratropical cyclone can yield significant amounts of rain or snow. Behind extratropical cyclones, rainbands can form downwind of relative warm bodies of water such as the Great Lakes. If the atmosphere is cold enough, these rainbands can yield heavy snow.".
- Q2882177 thumbnail Sturmfront_auf_Doppler-Radar-Schirm.jpg?width=300.
- Q2882177 wikiPageWikiLink Q1027878.
- Q2882177 wikiPageWikiLink Q1063457.
- Q2882177 wikiPageWikiLink Q1114042.
- Q2882177 wikiPageWikiLink Q1268345.
- Q2882177 wikiPageWikiLink Q129558.
- Q2882177 wikiPageWikiLink Q198782.
- Q2882177 wikiPageWikiLink Q202325.
- Q2882177 wikiPageWikiLink Q209190.
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- Q2882177 wikiPageWikiLink Q2399824.
- Q2882177 wikiPageWikiLink Q25257.
- Q2882177 wikiPageWikiLink Q2857578.
- Q2882177 wikiPageWikiLink Q338346.
- Q2882177 wikiPageWikiLink Q372001.
- Q2882177 wikiPageWikiLink Q40526.
- Q2882177 wikiPageWikiLink Q537536.
- Q2882177 wikiPageWikiLink Q640404.
- Q2882177 wikiPageWikiLink Q6795923.
- Q2882177 wikiPageWikiLink Q7139097.
- Q2882177 wikiPageWikiLink Q7213751.
- Q2882177 wikiPageWikiLink Q7347.
- Q2882177 wikiPageWikiLink Q747330.
- Q2882177 wikiPageWikiLink Q7561.
- Q2882177 wikiPageWikiLink Q7925.
- Q2882177 wikiPageWikiLink Q79602.
- Q2882177 wikiPageWikiLink Q8074.
- Q2882177 wikiPageWikiLink Q8081.
- Q2882177 wikiPageWikiLink Q8092.
- Q2882177 wikiPageWikiLink Q81242.
- Q2882177 wikiPageWikiLink Q81809.
- Q2882177 wikiPageWikiLink Q841225.
- Q2882177 wikiPageWikiLink Q8432456.
- Q2882177 wikiPageWikiLink Q853213.
- Q2882177 wikiPageWikiLink Q863343.
- Q2882177 wikiPageWikiLink Q9041898.
- Q2882177 wikiPageWikiLink Q931652.
- Q2882177 wikiPageWikiLink Q9382390.
- Q2882177 wikiPageWikiLink Q99.
- Q2882177 type Thing.
- Q2882177 comment "A rainband is a cloud and precipitation structure associated with an area of rainfall which is significantly elongated. Rainbands can be stratiform or convective, and are generated by differences in temperature. When noted on weather radar imagery, this precipitation elongation is referred to as banded structure. Rainbands within tropical cyclones are curved in orientation.".
- Q2882177 label "Rainband".
- Q2882177 seeAlso Q1063457.
- Q2882177 seeAlso Q1268345.
- Q2882177 depiction Sturmfront_auf_Doppler-Radar-Schirm.jpg.