ATS 735: Mesoscale Dynamics

Web-based list of articles

Bryan, G. H., J. C. Wyngaard, and J. M. Fritsch, 2003: Resolution requirements for the simulation of deep moist convection. Mon. Wea. Rev., 131, 2394—2416.

Crook, N. A., and M. W. Moncrieff, 1988: The effect of large—scale convergence on the generation and maintenance of deep moist convection. J. Atmos. Sci., 45, 3606—3624.

Davies-Jones, R., 2002: Linear and nonlinear propagation of supercell storms. J. Atmos. Sci., 59, 3178—3205, doi:10.1175/1520-0469(2003)059<3178:LANPOS>2.0.CO;2.

Davies-Jones, R., 2003: Reply. J. Atmos. Sci., 60, 2420—2426, doi:10.1175/1520-0469(2003) 060<2420:R>2.0.CO;2.

Doswell, C. A., III, and P. M. Markowski, 2004: Is buoyancy a relative quantity? Mon. Wea. Rev., 132, 853—863, doi:10.1175/1520-0493(2004)132<0853:IBARQ>2.0.CO;2.

Durran, D. R., 1993: Comments on "On the Richardson number dependence of nonlinear critical-layer flow over localized topography". J. Atmos. Sci., 50, 3029—3033.

Durran, D. R., and M. Gingrich, 2014: Atmospheric predictability: Why butterflies are not of practical importance. J. Atmos. Sci., 71, 2476—2488, doi:10.1175/JAS-D-14-0007.1.

Fujita, T. T., 1955: Results of detailed synoptic studies of squall lines. Tellus, 4, 405—436.

Haertel, P. T., R. H. Johnson, and S. N. Tulich, 2001: Some simple simulations of thunderstorm outflows. J. Atmos. Sci., 58, 504—516.

Markowski, P. M., and Y. P. Richardson, 2014: The influence of environmental low-level shear and cold pools on tornadogenesis: Insights from idealized simulations. J. Atmos. Sci., 71, 243—275, doi:10.1175/JAS-D-13-0159.1.

Miglietta, M. M., and R. Rotunno, 2009: Numerical simulations of conditionally unstable flows over a mountain ridge. J. Atmos. Sci., 66, 1865—1885, doi:10.1175/2009JAS2902.1; Corrigendum,3746--3748,doi:10.1175/2009JAS3304.1.

Miglietta, M. M., and R. Rotunno, 2012: Application of theory to simulations of observed cases of orographically forced convective rainfall. Mon. Wea. Rev., 140, 3039—3053, doi:10.1175/MWR-D-11-00253.1.

Parker, M. D., 2008: Response of simulated squall lines to low-level cooling. J. Atmos. Sci., 65, 1323–1341, doi:10.1175/2007JAS2507.1.

Peltier, W. R., 1993: Reply. J. Atmos. Sci., 50, 3034—3040.

Raymond, D. J., and H. Jiang, 1990: A theory for long-lived mesoscale convective systems. J. Atmos. Sci., 47, 3067—3077.

Rotunno, R., and M. L. Weisman, 2003: Comment on "Linear and nonlinear propagation of supercell storms". J. Atmos. Sci., 60, 2413—2419, doi:10.1175/1520-0469(2003)060<2413: COLANP>2.0.CO;2.

Schultz, D. M., and P. N. Schumacher, 1999: The use and misuse of conditional symmetric instability. Mon. Wea. Rev., 127, 2709—2732; Corrigendum, 128, 1573.

Schultz, D. M., P. N. Schumacher, and C. A. Doswell, III, 2000: The intricacies of instabilities. Mon. Wea. Rev., 128, 4143—4148.

Schultz, D. M., 2010: How to Research and Write Effective Case Studies in Meteorology. Electronic J. Severe Storms Meteor., 5 (2), 1-18.

Scinocca, J. F., and W. R. Peltier, 1991: On the Richardson number dependence of nonlinear critical-layer flow over localized topography. J. Atmos. Sci., 48, 1560—1572.

Sherwood, S. C., 2000: On moist instability. Mon. Wea. Rev., 128, 4139—4142.

Sun, Y. Q., and F. Zhang, 2016: Intrinsic versus practical limits of atmospheric predictability and the significance of the butterfly effect. J. Atmos. Sci., 73, 1419—1438, doi:10.1175/JAS-D-15-0142.1.

Trier, S. B., C. A. Davis, and J. D. Tuttle, 2000: Long-lived mesoconvective vortices and their environment. Part I: Observations from the central United States during the 1998 warm season. Mon. Wea. Rev., 128, 3376—3395.

Weisman, M. L., and R. Rotunno, 2004: "A theory for strong long-lived squall lines" revisited. J. Atmos. Sci., 61, 361—382.

Weisman, M. L., and R. Rotunno, 2005: Reply. J. Atmos. Sci., 62, 2997—3002.