메뉴 건너뛰기




Volumn 5, Issue 4, 1998, Pages 373-384

Heavy precipitation associated with elevated thunderstorms formed in a convectively unstable layer aloft

Author keywords

[No Author keywords available]

Indexed keywords

STABILITY;

EID: 0000598143     PISSN: 13504827     EISSN: None     Source Type: Journal    
DOI: 10.1017/S1350482798000863     Document Type: Article
Times cited : (23)

References (14)
  • 1
    • 0003820443 scopus 로고
    • Mesoscale objective analysis using weighted time-series observations
    • Available from NOAA/ERL, 325 Broadway, Boulder, CO 80303
    • Barnes, S. L. (1973). Mesoscale objective analysis using weighted time-series observations. NOAA Tech. Memo. ERL NSSL-62, 1-9. (Available from NOAA/ERL, 325 Broadway, Boulder, CO 80303.)
    • (1973) NOAA Tech. Memo. ERL NSSL-62 , pp. 1-9
    • Barnes, S.L.1
  • 2
    • 0018667525 scopus 로고
    • Conditional symmetric instability - A possible explanation for frontal rainbands
    • Bennetts, D. A. & Hoskins, B. J. (1979). Conditional symmetric instability - a possible explanation for frontal rainbands. Q. J. R. Meteorol. Soc., 105: 945-62.
    • (1979) Q. J. R. Meteorol. Soc. , vol.105 , pp. 945-962
    • Bennetts, D.A.1    Hoskins, B.J.2
  • 3
    • 0025662241 scopus 로고
    • Thunderstorms above frontal surfaces in environments without positive CAPE. Part I: A climatology
    • Colman, B. R. (1990a). Thunderstorms above frontal surfaces in environments without positive CAPE. Part I: A climatology. Mon. Wea. Rev., 118: 1103-21.
    • (1990) Mon. Wea. Rev. , vol.118 , pp. 1103-1121
    • Colman, B.R.1
  • 4
    • 0025662242 scopus 로고
    • Thunderstorms above frontal surfaces in environments without positive CAPE. Part II: Organization and instability mechanisms
    • Colman, B. R. (1990b). Thunderstorms above frontal surfaces in environments without positive CAPE. Part II: Organization and instability mechanisms. Mon. Wea. Rev., 118: 1123-44.
    • (1990) Mon. Wea. Rev. , vol.118 , pp. 1123-1144
    • Colman, B.R.1
  • 5
    • 0028576685 scopus 로고
    • The effect of neglecting the virtual temperature correction on CAPE calculations
    • Doswell, C. A., III & Rasmussen, E. N. (1994). The effect of neglecting the virtual temperature correction on CAPE calculations. Wea. Forecasting, 9: 625-9.
    • (1994) Wea. Forecasting , vol.9 , pp. 625-629
    • Doswell III, C.A.1    Rasmussen, E.N.2
  • 6
    • 0022170032 scopus 로고
    • Frontal circulations in the presence of small moist symmetric stability
    • Emanuel, K. A. (1985). Frontal circulations in the presence of small moist symmetric stability. J. Atmos. Sci., 42: 1062-71.
    • (1985) J. Atmos. Sci. , vol.42 , pp. 1062-1071
    • Emanuel, K.A.1
  • 7
    • 0342625641 scopus 로고
    • Elevated cold-sector severe thunderstorms: A preliminary study
    • Grant, B. N. (1995). Elevated cold-sector severe thunderstorms: a preliminary study. Nat. Wea. Dig., 19 (4): 25-31.
    • (1995) Nat. Wea. Dig. , vol.19 , Issue.4 , pp. 25-31
    • Grant, B.N.1
  • 8
    • 0020970640 scopus 로고
    • An interactive Barnes objective map analysis scheme for use with satellite and conventional data
    • Koch, S. E., Desjardins, M. & Kocin, P. J. (1983). An interactive Barnes objective map analysis scheme for use with satellite and conventional data. J. Climate Appl. Meteorol., 22: 1487-1503.
    • (1983) J. Climate Appl. Meteorol. , vol.22 , pp. 1487-1503
    • Koch, S.E.1    Desjardins, M.2    Kocin, P.J.3
  • 9
    • 1542733165 scopus 로고
    • Diagnosis of anafronts and katafronts
    • Moore, J. T. & Smith, K. F. (1989). Diagnosis of anafronts and katafronts. Wea. Forecasting, 4: 61-72.
    • (1989) Wea. Forecasting , vol.4 , pp. 61-72
    • Moore, J.T.1    Smith, K.F.2
  • 10
    • 0027786392 scopus 로고
    • The use of equivalent potential vorticity to diagnose regions of conditional symmetric instability
    • Moore, J. T. & Lambert, T. E. (1993). The use of equivalent potential vorticity to diagnose regions of conditional symmetric instability. Wea. Forecasting, 8: 301-8.
    • (1993) Wea. Forecasting , vol.8 , pp. 301-308
    • Moore, J.T.1    Lambert, T.E.2
  • 11
    • 1542733169 scopus 로고
    • National Climatic Data Center (1993). Storm Data, 38 (2): 74 pp.
    • (1993) Storm Data , vol.38 , Issue.2
  • 12
    • 0014767728 scopus 로고
    • Alternate solution to the classical vertical velocity problem
    • O'Brien, J. J. (1970). Alternate solution to the classical vertical velocity problem. J. Appl. Meteorol., 9: 197-203.
    • (1970) J. Appl. Meteorol. , vol.9 , pp. 197-203
    • O'Brien, J.J.1
  • 13
    • 0030411226 scopus 로고    scopus 로고
    • Initiation of an elevated mesoscale convective system associated with heavy rainfall
    • Rochette, S. M. & Moore, J. T. (1996). Initiation of an elevated mesoscale convective system associated with heavy rainfall. Wea. Forecasting, 11: 443-57.
    • (1996) Wea. Forecasting , vol.11 , pp. 443-457
    • Rochette, S.M.1    Moore, J.T.2
  • 14
    • 0040126356 scopus 로고
    • Comments on thunderstorms above frontal surfaces in environments without positive CAPE. Part I: A climatology
    • Williams, R. (1991). Comments on thunderstorms above frontal surfaces in environments without positive CAPE. Part I: A climatology. Mon. Wea. Rev., 119: 2511-13.
    • (1991) Mon. Wea. Rev. , vol.119 , pp. 2511-2513
    • Williams, R.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.