Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q2678309> ?p ?o }
Showing triples 1 to 23 of
23
with 100 triples per page.
- Q2678309 subject Q7197713.
- Q2678309 abstract "Frontogenesis is a meteorological process of tightening of horizontal temperature gradients to produce fronts. In the end, two types of fronts form: cold fronts and warm fronts. A cold front is a narrow line where temperature decreases rapidly. A warm front is a narrow line of warmer temperatures and essentially where much of the precipitation occurs. Frontogenesis occurs as a result of a developing baroclinic wave. According to Hoskins & Bretherton (1972, p. 11), there are eight mechanisms that influence temperature gradients: horizontal deformation, horizontal shearing, vertical deformation, differential vertical motion, latent heat release, surface friction, turbulence and mixing, and radiation. Semigeostrophic frontogenesis theory focuses on the role of horizontal deformation and shear.".
- Q2678309 wikiPageWikiLink Q1027878.
- Q2678309 wikiPageWikiLink Q1063457.
- Q2678309 wikiPageWikiLink Q1207934.
- Q2678309 wikiPageWikiLink Q1548585.
- Q2678309 wikiPageWikiLink Q189000.
- Q2678309 wikiPageWikiLink Q189796.
- Q2678309 wikiPageWikiLink Q2046922.
- Q2678309 wikiPageWikiLink Q210316.
- Q2678309 wikiPageWikiLink Q21529466.
- Q2678309 wikiPageWikiLink Q217219.
- Q2678309 wikiPageWikiLink Q2721218.
- Q2678309 wikiPageWikiLink Q3027650.
- Q2678309 wikiPageWikiLink Q3433864.
- Q2678309 wikiPageWikiLink Q39552.
- Q2678309 wikiPageWikiLink Q537536.
- Q2678309 wikiPageWikiLink Q676622.
- Q2678309 wikiPageWikiLink Q7197713.
- Q2678309 wikiPageWikiLink Q7269452.
- Q2678309 wikiPageWikiLink Q929043.
- Q2678309 comment "Frontogenesis is a meteorological process of tightening of horizontal temperature gradients to produce fronts. In the end, two types of fronts form: cold fronts and warm fronts. A cold front is a narrow line where temperature decreases rapidly. A warm front is a narrow line of warmer temperatures and essentially where much of the precipitation occurs. Frontogenesis occurs as a result of a developing baroclinic wave. According to Hoskins & Bretherton (1972, p.".
- Q2678309 label "Frontogenesis".