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.