WARM FRONT BAND - SPECIAL INVESTIGATION: DIFFERENT KINDS OF WF DEVELOPMENT

by ZAMG


Warm Front Bands are described in this chapter as CMs standing alone. But it is especially interesting to look at the development of such weather systems.

The most common development of a Warm Front Band is connected to classical Norwegian Model of the polar front theory; that means that Cold Fronts and Warm Fronts develop if a disturbance is superimposed on the (in the beginning stationary) polar front (see also Occlusion: Warm Conveyor Belt Type).

09 August 2001/15.00 UTC - Meteosat IR image
09 August 2001/18.00 UTC - Meteosat IR image
10 August 2001/06.00 UTC - Meteosat IR image
10 August 2001/12.00 UTC - Meteosat IR image
But there are also other developments which lead to cloud configurations as well as to distributions of relative streams and key parameters which are fully comparable to that kind of Warm Fronts which have developed in the classical way. Those developments are warm air outbreaks from the Sahara or from the Black Sea area very often diagnosed as "Warm Conveyor Belt" in the initial stages of development.

There are two examples in the "Case Study" part of this manual:

  1. The case from 13 - 15 March 1998 which shows the development of a very pronounced Warm Front cloud band over the Eastern Mediterranean/Turkey. Its initial stages can be followed backwards to the Sahara where cloudiness in the typical form of a Warm Conveyor Belt can be observed.
    13 March 2001/06.00 UTC - Meteosat IR image
    13 March 2001/18.00 UTC - Meteosat IR image
    14 March 2001/06.00 UTC - Meteosat IR image
    14 March 2001/12.00 UTC - Meteosat IR image
    15 March 1998/06 UTC - IR image; SatRep overlay: names of conceptual models; symbols: weather events (green: rain and showers, blue: drizzle, cyan: snow, purple: freezing rain, red: thunderstorm with precipitation, orange: hail, yellow: fog, black: no actual precipitation or thunderstorm with precipitation); lines: magenta: relative streams on 308 K, yellow: isobars, system velocity 273° 7 m/s
  2. The case from 14 - 15 June 1998 (see Case Study 14 - 15 June 1998 ) which shows a Warm Front cloud band moving from SE Europe across Finland and the Scandinavian countries westward. The initial stages of cloudiness can be found over the Balkan Peninsula within a warm air mass.
    13 June 1998/06.00 UTC - Meteosat IR image
    13 June 1998/18.00 UTC - Meteosat IR image
    14 June 1998/06.00 UTC - Meteosat IR image
    14 June 1998/12.00 UTC - Meteosat IR image
    15 June 1998/06 UTC - IR image; isobars (yellow) and relative streams (magenta) on 324K

SUB-MENU OF WARM FRONT BAND