The forcing of anomalous divergent wind and transient vorticity fluxes to the anomaly of stationary waves

Acta Meteorologica Sinica

Volumn 11, Issue 1, 1997, Pages

  Geng, Quanzhen ^a   Huang, Ronghui ^b  

^a China Meteorological Administration   (China)

^b INSTITUTE OF ATMOSPHERIC PHYSICS   (China)

Author keywords

Anomaly; Divergent wind; Forcing; Stationary wave; Transient vorticity flux

Indexed keywords

ANOMALIES; ATMOSPHERIC CIRCULATION; DIVERGENT WIND; FORCING; STANDING WAVES 00003; STATIONARY WAVE; TELECONNECTION; TELECONNECTIONS; TRANSIENT VORTICITY FLUX; VORTEX;

NORTH AMERICA; PACIFIC;

EID: 0030921965     PISSN: 08940525     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (14)

1. Branstator, G. (1985), Analysis of general circulation model sea-surface temperature anomaly simulations using a linear model. Part I: Forced solutions, J. Atmos. Sci., 42: 2225-2241.
2. Haarsma, R. J. and Opsteegh, J. D. (1989), Nonlinear response to anomalous tropical forcing, J. Atmos. Sci., 46, 3240-3255.
3. Held, I. M. and Kang, I. S. (1987), Barotropic models of the extratropical response to El Nino, J. Atmos. Sci., 44: 3576-3586.
4. Holopainen, E. O. and Oort, A. H. (1981), On the role of large-scale transient eddies in the time-mean atmospheric flow, J. Atmos. Sci., 38: 270-280.
5. Horel, J. D. and Wallace, J. M. (1981), Planetary-scale atmospheric phenomena associated with the Southern Oscillation, Mon. Wea. Rev., 109: 813-829.
6. Hoskins, B. J. and Karoly, D. (1981), The steady linear response of a spherical atmosphere to thermal and orographic forcing, J. Atmos. Sci., 38: 1179-1196.
7. Kang, I.-S. and Held, I. M. (1986), Linear and nonlinear diagnostic models of stationary eddies in the upper troposphere during Northern Summer, J. Atmos. Sci., 43: 3045-3057.
8. Lau, K.-M. and Peng, L. (1992), Dynamics of atmospheric teleconnections during the Northern Summer, J. Climate, 5: 140-158.
9. Lau, N.-C. and Nath, M. J. (1991), Variability of the baroclinic and barotropic transient eddy forcing associated with monthly changes in the midlatitude storm tracks, J. Atmos. Sci., 48: 2589-2631.
10. Qin, J.-C. and Robinson, W. A. (1993), On the Rossby wave source and steady linear response to tropical forcing, J. Atmos. Sci., 50: 1819-1823.
11. Sardeshmukh, P. D. and Hoskins, B. J. (1988), The generation of global rotational flow by steady idealized tropical divergence, J. Atmos. Sci., 45: 1228-1251.
12. Simmons, A. J. (1982), The forcing of stationary wave motion by tropical diabatic heating, Quart. J. Roy. Meteor. Soc., 108: 503-534.
13. Valdes, P. J. and Hoskins, B. J. (1989), Linear stationary wave simulations of the time-mean climatological flow, J. Atmos. Sci., 46: 2509-2527.
14. Wallace, J. M. and Gutzler, D. S. (1981), Teleconnection patterns in the geopotential height field during the Northern Hemisphere winter, Mon. Wea. Rev., 109: 758-812.