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Volumn 17, Issue 4, 2002, Pages 723-738

Formation of a sharp snow gradient in a midwestern heavy snow event

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION; SNOW; STORMS;

EID: 0036694315     PISSN: 08828156     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0434(2002)017<0723:FOASSG>2.0.CO;2     Document Type: Article
Times cited : (15)

References (33)
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    • Emanuel, K.A.1
  • 15
    • 3643092705 scopus 로고    scopus 로고
    • The structure and evolution of a continental winter cyclone. Part II: Frontal forcing for an extreme snow event
    • (1998) Mon. Wea. Rev , vol.126 , pp. 329-348
    • Martin, J.E.1
  • 16
    • 0032599673 scopus 로고    scopus 로고
    • Quasigeostropic forcing of ascent in the occluded sector of cyclones and the trowal airstream
    • (1999) Mon. Wea. Rev , vol.127 , pp. 70-88
    • Martin, J.E.1
  • 17
    • 0033399966 scopus 로고    scopus 로고
    • The separate roles of geostropic vorticity and deformation in the midlatitude occlusion process
    • (1999) Mon. Wea. Rev , vol.127 , pp. 2404-2418
    • Martin, J.E.1
  • 18
    • 0024191537 scopus 로고
    • The role of frontogenetical forcing and conditional symmetric instability in the Midwest snowstorm of 30-31 January 1982
    • (1988) Mon. Wea. Rev , vol.116 , pp. 2155-2171
    • Moore, J.T.1    Blakely, P.D.2
  • 27
    • 0022171987 scopus 로고
    • Mesoscale structure in the megalopolitan snowstorm of 11-12 February 1983. Part I: Frontogenetical forcing and symmetric instability
    • (1985) J. Atmos. Sci , vol.42 , pp. 1050-1061
    • Sanders, F.1    Bosart, L.F.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.