The omega equation: Q-G interpretations of simple circulation features

Meteorological Applications

Volumn 4, Issue 4, 1997, Pages 335-344

  Pedder, Mike A ^a  

^a UNIVERSITY OF READING   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

FORCING FUNCTION; GEOPOTENTIALS; PARTICULAR DISTRIBUTION; PRESSURE AND TEMPERATURE; QUASI-GEOSTROPHIC; SUBJECTIVE ANALYSIS; SURFACE DEVELOPMENT; VERTICAL CIRCULATION;

DETECTION METHOD; GEOSTROPHIC FLOW; SYNOPTIC METEOROLOGY; TEMPERATURE EFFECT;

EID: 0041978521     PISSN: 13504827     EISSN: None     Source Type: Journal    
DOI: 10.1017/S1350482797000595     Document Type: Article

References (5)

1. Carlson, T. N. (1991). Mid-latitude weather systems. Harper Collins Academic, 507 pp.
2. Carroll, E. B. (1995). Practical subjective applications of the omega equation and Sutcliffe development theory. Meteorol. Appl., 2: 71-81.
3. Hoskins, B. J. (1997). A potential vorticity view of synoptic development. Meteorol. Appl., 4: 325-334.
4. Hoskins, B. J. & Pedder, M. A. (1980). The diagnosis of middle latitude synoptic development. Q. J. R. Meteorol. Soc., 106: 707-719.
5. Kurz, M. (1994). The role of diagnostic tools in modern weather forecasting. Meteorol. Appl., 1: 45-68.