Kleist, D.T., and M.C. Morgan, 2005:
Application of adjoint-derived forecast sensitivities to the 24-25
January 2000 U.S. east coast snowstorm. Mon.Wea. Rev., in press.
Kleist, D.T., and M.C. Morgan, 2005:
Interpretation of the structure and evolution of adjoint-derived
forecast sensitivity gradients. Mon.
Wea. Rev., 133, 467-485.
Kim, H. M., M. Morgan, and R. E. Morss, 2004: Evolution of analysis
error and adjoint-based sensitivities: Implications for adaptive
observations. J. Atmos. Sci., 61, 795-812.
Risbey, J., P. Lamb, R. Miller, M. Morgan, and G. Roe, 2002:
Exploring the structure of regional climate scenarios by combining
synoptic and dynamic guidance and GCM Output, J. Climate. 15,1036-1050.
Kim, H. M. and M. Morgan, 2002: Dependence of singular vector structure
and evolution on the choice of norm. J.
Atmos. Sci., 59,
3099-3116.
Morgan, M. and C. Chen, 2002: Diagnosis of optimal perturbation
evolution in the Eady model, J.
Atmos. Sci. 169–185.
Morgan, M C., 2001 A potential
vorticity and wave activity diagnosis of optimal perturbation evolution. J. Atmos. Sci., 58, 2518-2544.
Morgan, M. C., 1999 Using piecewise potential vorticity inversion to
diagnose frontogenesis, Part 1: A partitioning of the Q vector applied
to diagnosing surface frontogenesis and vertical motion. Mon. Wea. Rev., 127, 2796-2821.
Morgan, M. C. and J. W. Nielsen-Gammon, 1998: Using tropopause
maps to diagnose midlatitude weather systems. Mon. Wea. Rev., 126,
2555-2579.
Haines, K., P. Malanotte-Rizzoli,
and M. Morgan, 1993: Persistent jet stream intensifications: A
comparison between theory and data. J.
Atmos. Sci., 50, 146-154.