Difference between revisions of "Mei-yu front"

From Glossary of Meteorology
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<div class="definition"><div class="short_definition">(''Also called'' baiu front). A quasi-persistent, nearly stationary, east&ndash;west-oriented weak  [[baroclinic]] zone in the lower [[troposphere]] that typically stretches from the east China coast, across  Taiwan, and eastward into the Pacific, south of Japan. The term "mei-yu" is the Chinese expression  for "plum rains."</div><br/> <div class="paragraph">The mei-yu front generally occurs from mid- to late spring through early to midsummer. This  low-level baroclinic zone typically lies beneath a confluent [[jet]] entrance region aloft situated [[downstream]]  of the Tibetan Plateau. The mei-yu/baiu front is very significant in the weather and [[climate]]  of southeast Asia as it serves as the focus for persistent heavy convective [[rainfall]] associated with  [[mesoscale convective complexes]] (MCCs) or [[mesoscale convective systems]] (MCSs) that propagate  eastward along the baroclinic zone. The moisture source is typically the South China Sea  and sometimes the Bay of Bengal. The usual lifting mechanism is low-level warm-air [[advection]]  in association with a [[low-level jet]] on the equatorward flank of the baroclinic zone. Deep ascent  and resulting organized MCCs/MCSs are especially favored when the low-level warm-air advection  is situated beneath the favorable equatorward jet entrance region aloft.</div><br/> </div>
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<div class="definition"><div class="short_definition">(''Also called'' baiu front). A quasi-persistent, nearly stationary, east&ndash;west-oriented weak  [[baroclinic]] zone in the lower [[troposphere]] that typically stretches from the east China coast, across  Taiwan, and eastward into the Pacific, south of Japan. The term "mei-yu" is the Chinese expression  for "plum rains."</div><br/> <div class="paragraph">The mei-yu front generally occurs from mid- to late spring through early to midsummer. This  low-level baroclinic zone typically lies beneath a confluent [[jet]] entrance region aloft situated [[downstream]]  of the Tibetan Plateau. The mei-yu/baiu front is very significant in the weather and [[climate]]  of southeast Asia as it serves as the focus for persistent heavy convective [[rainfall]] associated with  [[mesoscale convective complex|mesoscale convective complexes]] (MCCs) or [[mesoscale convective systems]] (MCSs) that propagate  eastward along the baroclinic zone. The moisture source is typically the South China Sea  and sometimes the Bay of Bengal. The usual lifting mechanism is low-level warm-air [[advection]]  in association with a [[low-level jet]] on the equatorward flank of the baroclinic zone. Deep ascent  and resulting organized MCCs/MCSs are especially favored when the low-level warm-air advection  is situated beneath the favorable equatorward jet entrance region aloft.</div><br/> </div>
 
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Latest revision as of 17:24, 25 April 2012



mei-yu front

(Also called baiu front). A quasi-persistent, nearly stationary, east–west-oriented weak baroclinic zone in the lower troposphere that typically stretches from the east China coast, across Taiwan, and eastward into the Pacific, south of Japan. The term "mei-yu" is the Chinese expression for "plum rains."

The mei-yu front generally occurs from mid- to late spring through early to midsummer. This low-level baroclinic zone typically lies beneath a confluent jet entrance region aloft situated downstream of the Tibetan Plateau. The mei-yu/baiu front is very significant in the weather and climate of southeast Asia as it serves as the focus for persistent heavy convective rainfall associated with mesoscale convective complexes (MCCs) or mesoscale convective systems (MCSs) that propagate eastward along the baroclinic zone. The moisture source is typically the South China Sea and sometimes the Bay of Bengal. The usual lifting mechanism is low-level warm-air advection in association with a low-level jet on the equatorward flank of the baroclinic zone. Deep ascent and resulting organized MCCs/MCSs are especially favored when the low-level warm-air advection is situated beneath the favorable equatorward jet entrance region aloft.