Use of dynamical concepts in weather forecasting

Meteorological Applications

Volumn 4, Issue 4, 1997, Pages 345-352

  Carroll, E B ^a  

^a MET OFFICE   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

ADVECTION;

INSTANTANEOUS PRESSURES; LOWER TROPOSPHERE; OPERATIONAL USE; QUASI-GEOSTROPHIC; THERMAL ADVECTION; TWO LAYER MODEL; VERTICAL VELOCITY; VORTICITY ADVECTION;

WEATHER FORECASTING;

ADVECTION; AGEOSTROPHIC FLOW; QUASI-GEOSTROPHIC FLOW; TROPOSPHERE; TWO-DIMENSIONAL MODELING; WEATHER FORECASTING;

EID: 0347827020     PISSN: 13504827     EISSN: None     Source Type: Journal    
DOI: 10.1017/S1350482797000583     Document Type: Article

References (6)

1. Carroll, E. B. (1995). Practical subjective application of the omega equation and Sutcliffe development theory. Meteorol. Appl., 2: 71-81.
2. Hoskins, B. J. (1997). A potential vorticity view of synoptic development. Meteorol. Appl., 4: 325-334.
3. Hoskins, B. J., Draghici, I. & Davies, H. C. (1978). A new look at the w-equation. Q. J. R. Meteorol. Soc., 104: 31-38.
4. Pedder, M. (1997). The omega equation: Q-G interpretations of simple circulation features. Meteorol. Appl., 4: 335-344.
5. Sutcliffe, R. C. (1947). A contribution to the problem of development. Q. J. R. Meteorol. 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.