Barnes, G. M., E. J. Zipser, D. P. Jorgensen, and F. D. Marks Jr., 1983: Mesoscale and convective structure of a hurricane rainband. J. Atmos. Sci.,40, 2125–2137.
Browning, P., J. F. Weaver, and B. Connell, 1997: The Moberly, Missouri, tornado of 4 July 1995. Wea. Forecasting,12, 915–927.
Cione, J. J., P. G. Black, and S. H. Houston, 2000: Surface observations in the hurricane environment. Mon. Wea. Rev.,128, 1550–1561.
Fitzpatrick, P. J., 1996: Understanding and forecasting tropical cyclone intensity change. Department of Atmospheric Science Paper No. 598, Colorado State University, 346 pp. [Available from Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523.].
Johnson, R. H., and M. E. Nichols, 1983: A composite analysis of the boundary layer accompanying a tropical squall line. Mon. Wea. Rev.,111, 308–319.
Maddox, R. A., L. R. Hoxit, and C. F. Chappell, 1980: A study of tornadic thunderstorm interactions with thermal boundaries. Mon. Wea. Rev.,108, 322–336.
Magor, B. W., 1959: Mesoanalysis: Some operational analysis techniques utilized in tornado forecasting. Bull. Amer. Meteor. Soc.,40, 499–511.
Markowski, P. M., E. N. Rasmussen, and J. M. Straka, 1998: The occurrence of tornadoes in supercells interacting with boundaries during VORTEX-95. Wea. Forecasting,13, 852–859.
Powell, M. D., 1990: Boundary layer structure and dynamics in outer hurricane rainbands. Mon. Wea. Rev.,118, 918–938.
Przybylinski, R. W., T. J. Shea, D. L. Perry, E. H. Goetsch, R. R. Czys, and N. E. Wescott, 1993: Doppler radar observations of high-precipitation supercells over the mid Mississippi Valley region. Preprints, 17th Conf. on Severe Local Storms, St. Louis, MO, Amer. Meteor. Soc., 158–163.
Purdom, J. F. W., 1976: Some uses of high-resolution GOES imagery in the mesoscale forecasting of convection and its behavior. Mon. Wea. Rev.,104, 1474–1483.
Saxen, T. R., and S. A. Rutledge, 1998: Surface fluxes and boundary layer recovery in TOGA COARE: Sensitivity to convective organization. J. Atmos. Sci.,55, 2763–2781.
Simpson, R. H., 1974: The hurricane disaster potential scale. Weatherwise,27, 169 and 186.
——, and H. Riehl, 1958: Mid-tropospheric ventilation as a constraint on hurricane development and maintenance. Proc. Technical Conf. on Hurricanes, Miami Beach, FL, Amer. Meteor. Soc., D4-1–D4 -10.
Weaver, J. F., 1979: Storm motion as related to boundary-layer convergence. Mon. Wea. Rev.,107, 612–619.
——, and S. P. Nelson, 1982: Multiscale aspects of thunderstorm gust fronts and their effects on subsequent storm development. Mon. Wea. Rev.,110, 707–718.
——, and J. F. W. Purdom, 1995: An interesting mesoscale storm–environment interaction observed just prior to changes in severe storm behavior. Wea. Forecasting,10, 449–453.
——, ——, and E. J. Szoke, 1994: Some mesoscale aspects of the 6 June 1990 Limon, Colorado, tornado case. Wea. Forecasting,9, 45–61.
Willoughby, H. E., 1998: Tropical cyclone eye thermodynamics. Mon. Wea. Rev.,126, 3053–3067.
Wilson, J. W., G. B. Foote, N. A. Crook, J. C. Fankhauser, C. G. Wade, J. D. Tuttle, C. K. Mueller, and S. K. Krueger, 1992: The role of boundary-layer convergence zones and horizontal rolls in the initiation of thunderstorms. Mon. Wea. Rev.,120, 1785–1815.
Young, G. S., S. M. Perugini, and C. W. Fairall, 1995: Convective wakes in the equatorial western Pacific during TOGA. Mon. Wea. Rev.,123, 110–123.
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A large, low-level thunderstorm outflow boundary was observed as it exited from beneath the cirrus canopy of Hurricane Luis following a period of intense convection in the storm’s eyewall. A description of the feature and a short summary of its behavior are presented.
Corresponding author address: John Knaff, NOAA/CIRA, Colorado State University, Fort Collins, CO 80523.
Email: Knaff@cira.colostate.edu
A large, low-level thunderstorm outflow boundary was observed as it exited from beneath the cirrus canopy of Hurricane Luis following a period of intense convection in the storm’s eyewall. A description of the feature and a short summary of its behavior are presented.
Corresponding author address: John Knaff, NOAA/CIRA, Colorado State University, Fort Collins, CO 80523.
Email: Knaff@cira.colostate.edu
Barnes, G. M., E. J. Zipser, D. P. Jorgensen, and F. D. Marks Jr., 1983: Mesoscale and convective structure of a hurricane rainband. J. Atmos. Sci.,40, 2125–2137.
Browning, P., J. F. Weaver, and B. Connell, 1997: The Moberly, Missouri, tornado of 4 July 1995. Wea. Forecasting,12, 915–927.
Cione, J. J., P. G. Black, and S. H. Houston, 2000: Surface observations in the hurricane environment. Mon. Wea. Rev.,128, 1550–1561.
Fitzpatrick, P. J., 1996: Understanding and forecasting tropical cyclone intensity change. Department of Atmospheric Science Paper No. 598, Colorado State University, 346 pp. [Available from Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523.].
Johnson, R. H., and M. E. Nichols, 1983: A composite analysis of the boundary layer accompanying a tropical squall line. Mon. Wea. Rev.,111, 308–319.
Maddox, R. A., L. R. Hoxit, and C. F. Chappell, 1980: A study of tornadic thunderstorm interactions with thermal boundaries. Mon. Wea. Rev.,108, 322–336.
Magor, B. W., 1959: Mesoanalysis: Some operational analysis techniques utilized in tornado forecasting. Bull. Amer. Meteor. Soc.,40, 499–511.
Markowski, P. M., E. N. Rasmussen, and J. M. Straka, 1998: The occurrence of tornadoes in supercells interacting with boundaries during VORTEX-95. Wea. Forecasting,13, 852–859.
Powell, M. D., 1990: Boundary layer structure and dynamics in outer hurricane rainbands. Mon. Wea. Rev.,118, 918–938.
Przybylinski, R. W., T. J. Shea, D. L. Perry, E. H. Goetsch, R. R. Czys, and N. E. Wescott, 1993: Doppler radar observations of high-precipitation supercells over the mid Mississippi Valley region. Preprints, 17th Conf. on Severe Local Storms, St. Louis, MO, Amer. Meteor. Soc., 158–163.
Purdom, J. F. W., 1976: Some uses of high-resolution GOES imagery in the mesoscale forecasting of convection and its behavior. Mon. Wea. Rev.,104, 1474–1483.
Saxen, T. R., and S. A. Rutledge, 1998: Surface fluxes and boundary layer recovery in TOGA COARE: Sensitivity to convective organization. J. Atmos. Sci.,55, 2763–2781.
Simpson, R. H., 1974: The hurricane disaster potential scale. Weatherwise,27, 169 and 186.
——, and H. Riehl, 1958: Mid-tropospheric ventilation as a constraint on hurricane development and maintenance. Proc. Technical Conf. on Hurricanes, Miami Beach, FL, Amer. Meteor. Soc., D4-1–D4 -10.
Weaver, J. F., 1979: Storm motion as related to boundary-layer convergence. Mon. Wea. Rev.,107, 612–619.
——, and S. P. Nelson, 1982: Multiscale aspects of thunderstorm gust fronts and their effects on subsequent storm development. Mon. Wea. Rev.,110, 707–718.
——, and J. F. W. Purdom, 1995: An interesting mesoscale storm–environment interaction observed just prior to changes in severe storm behavior. Wea. Forecasting,10, 449–453.
——, ——, and E. J. Szoke, 1994: Some mesoscale aspects of the 6 June 1990 Limon, Colorado, tornado case. Wea. Forecasting,9, 45–61.
Willoughby, H. E., 1998: Tropical cyclone eye thermodynamics. Mon. Wea. Rev.,126, 3053–3067.
Wilson, J. W., G. B. Foote, N. A. Crook, J. C. Fankhauser, C. G. Wade, J. D. Tuttle, C. K. Mueller, and S. K. Krueger, 1992: The role of boundary-layer convergence zones and horizontal rolls in the initiation of thunderstorms. Mon. Wea. Rev.,120, 1785–1815.
Young, G. S., S. M. Perugini, and C. W. Fairall, 1995: Convective wakes in the equatorial western Pacific during TOGA. Mon. Wea. Rev.,123, 110–123.
| All Time | Past Year | Past 30 Days | |
|---|---|---|---|
| Abstract Views | 0 | 0 | 0 |
| Full Text Views | 92 | 24 | 2 |
| PDF Downloads | 52 | 16 | 0 |
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