Divergent Circulations Associated with the Presidents’ Day (1979) Storm 19 February 2019.

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Presentation transcript:

Divergent Circulations Associated with the Presidents’ Day (1979) Storm 19 February 2019

The Sawyer–Eliassen Circulation Equation The Sawyer (1956)–Eliassen (1962) Circulation Equation provides a way to diagnose the transverse circulations associated with active fronts. Arnt Eliassen Norwegian Encyclopedia

Sawyer–Eliassen Circulation Equation Where: X Y

Sawyer–Eliassen Circulation Equation Where: X Y

Sawyer–Eliassen Circulation Equation Uccellini and Kocin (1987)

Sawyer–Eliassen Circulation Equation Where: X Y

Sawyer–Eliassen Circulation Equation Static Stability Where: X Y

Sawyer–Eliassen Circulation Equation Static Stability Across-Front Baroclinicity Where: X Y

Sawyer–Eliassen Circulation Equation Static Stability Across-Front Baroclinicity Geo. Absolute Vorticity Where: X Y

Sawyer–Eliassen Circulation Equation Static Stability Across-Front Baroclinicity Geo. Absolute Vorticity Frontal Characteristics Where: X Y

Sawyer–Eliassen Circulation Equation Abs. Vorticity Baroclinicity Hakim and Keyser (2001) How do the coefficients of the Sawyer–Eliassen Equation modulate the resultant circulation? Static Stability Near Boundary

Sawyer–Eliassen Circulation Equation Static Stability Across-Front Baroclinicity Geo. Absolute Vorticity Geostrophic and Diabatic Forcing Frontal Characteristics Where: X Y Shearing Confluence

Overview –312 K Surface A A A’ A’ Uccellini et al. (1985)

Wind Perpendicular to Cross Section CFSR A A’ Uccellini et al. (1985)

Wind Parallel to Cross Section CFSR Uccellini et al. (1985)

Full Sawyer–Eliassen Circulation CFSR Uccellini et al. (1985)

Contribution from Horizontal Shear Term CFSR Uccellini et al. (1985)

Contribution from Confluence Term A’ A A A’ CFSR Uccellini et al. (1985)

Full Sawyer–Eliassen Circulation CFSR Uccellini et al. (1985)

The Psi Vector Keyser et al. (1989)

500-hPa Psi Vectors – 12Z 18 Feb 1979

References Eliassen, A., 1962: On the vertical circulation in frontal zones. Geophys. Publ., 24, 147-160. Hakim, G. J., and D. Keyser, 2001: Canonical frontal circulation patterns in terms of Green’s functions for the Sawyer–Eliassen equation. Quart. J. Roy. Meteor. Soc., 127, 1795–1814. Keyser, D., B. D. Schmidt, and D. G. Duffy, 1989: A technique for representing three-dimensional vertical circulations in baroclinic disturbances. Mon. Wea. Rev., 117, 2463–2494. Sawyer, J. S., 1956: The vertical circulation at meteorological fronts and its relation to frontogenesis. Proc. Roy. Soc. London, 234A, 346-362. Uccellini, L. W., D. Keyser, K. F. Brill, and C. H. Wash, 1985: The Presidents’ Day cyclone of 18-19 February 1979: Influence of upstream trough amplification and associated tropopause folding on rapid cyclogenesis. Mon. Wea. Rev., 113, 962-988. ________, and P. J. Kocin, 1987: The interaction of jet streak circulations during heavy snow events along the East Coast of the United States. Wea. Forecasting, 2, 289-308.