Lower-tropospheric height tendencies associated with the shearwise and transverse components of quasigeostrophic vertical motion

Monthly Weather Review

Volumn 135, Issue 7, 2007, Pages 2803-2809

  Martin, Jonathan E ^a  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC MOVEMENTS; ATMOSPHERIC PRESSURE; SEA LEVEL; TROPOSPHERE; VORTICITY;

CYCLOGENESIS; QUASIGEOSTROPHIC VERTICAL MOTION; SHEARWISE UPDRAFT; TRANSVERSE UPDRAFT;

METEOROLOGY;

CYCLOGENESIS; QUASI-GEOSTROPHIC FLOW; TROPOSPHERE; UPDRAFT;

EID: 34547678068     PISSN: 00270644     EISSN: None     Source Type: Journal    
DOI: 10.1175/MWR3416.1     Document Type: Article

References (6)

1. Hoskins, B. J., I. Draghici, and H. C. Davies, 1978: A new look at the ω-equation. Quart. J. Roy. Meteor. Soc., 104, 31-38.
2. Martin, J. E., 1998: On the deformation term in the quasigeostrophic omega equation. Mon. Wea. Rev., 126, 2000-2007.
3. Martin, J. E., 1999: Quasigeostrophic forcing for ascent in the occluded sector of cyclones and the trowal airstream. Mon. Wea. Rev., 127, 70-88.
4. Martin, J. E., 2006: The role of shearwise and transverse quasigeostrophic vertical motions in the midlatitude cyclone life cycle. Mon. Wea. Rev., 134, 1174-1193.
5. Sutcliffe, R. C., 1947: A contribution to the problem of development. Quart. J. Roy. Meteor. Soc., 73, 370-383.
6. Trenberth, K. E., 1978: On the interpretation of the diagnostic quasi-geostrophic omega equation. Mon. Wea. Rev., 106, 131-137.