WARM FRONT BAND - METEOROLOGICAL PHYSICAL BACKGROUND

by ZAMG


In the case of a Warm Front, warm air (moist air) moves against colder air (dry air). At the boundary of these two air masses the warm air tends to glide up over the wedge of colder air (see Typical appearance in vertical cross section). This process causes the frontal cloud band, and therefore also the precipitation, to be found in front of the surface front (or the TFP) (see Weather events).
The idealized structure and physical background of a Warm Front can be explained with the conveyor belt theory as follows:

Discussion

In addition to this idealized structure, the experience from a series of case studies carried out at ZAMG differs somewhat from the one described above, allowing more differentiation. In the case of a band type the Warm Conveyor Belt can be observed within the warm sector up to the Cold and Warm Front line. If there is high cloudiness in front of and parallel to the Warm Front line, it is situated within an (at least in the area of the fronts) ascending conveyor belt from the rear side of the Cold Front extending from south-west to north-east, the so-called upper relative stream. While the high cloudiness can thus be explained, the Warm Front cloudiness in the lower levels of the troposphere develops, as in the ideal case described above, within the Cold Conveyor Belt.

The conveyor belt situation, especially of the Warm Conveyor Belt and the upper relative stream, described above can be found in a thick layer of isentropic surfaces, but there is some tendency that the Warm Conveyor Belt in lower layers overruns the surface Warm Front to a small extent. The ascending Warm Conveyor Belt in the warm sector is not accompanied by appreciable cloudiness either because of too dry air masses or/and too little lifting. But it can be observed that in the ascending Warm Conveyor Belt cloudiness may develop leading to a second Warm Front type, the Warm Front Shield.

Very often a transition from the Warm Front Band to the Warm Front Shield type can be observed by the development of cloudiness within the warm sector. This is described in detail in the chapter of the Warm Front Shield (see Warm Front Shield - Meteorological physical background ).
01 March 1995/12.00 UTC - Vertical cross section; black: isentropes (ThetaE), orange thin: IR pixel values, orange thick: WV pixel values
The 300 K isentropic surface chosen for the relative streams in the figure below is very close to the upper boundary of the crowded, inclined Warm Front zone.
01 March 1995/12.00 UTC - Meteosat IR image; blue: relative streams 300K - system velocity: 262° 16 m/s, green: isobars 300K, red: wind vectors 300K, position of vertical cross section indicated
The analysis shows two Conveyor Belts: there is one from eastern directions across Romania, Hungary and Austria turning northward across Germany and further on north-eastward across the Baltic Sea and the Baltic countries. This is a typical example of a Warm Conveyor Belt extending across the warm sector to the leading edge of the Cold Front and the rear edge of the Warm Front cloudiness. A second relative stream originates from the cold air mass over the Atlantic behind the Cold Front and approaches the Warm Conveyor Belt over the Benelux countries, extending from there on across Denmark and south Norway parallel to the Warm Conveyor Belt. Generally speaking, the Warm Conveyor Belt rises from about 700 hPa over the Alps up to its culmination point at 550 hPa (although it has to be taken into account that there is a lack of radiosonde measurements in the Ukraine and Russia). The relative stream from the Atlantic exists in a higher layer rising from about 600 to 450 hPa. The high cloudiness of the Warm Front exists in this latter relative stream.
12 June 1996/00.00 UTC - Vertical cross section; black: isentropes (ThetaE), orange thin: IR pixel values, orange thick: WV pixel values
The isentropic surfaces which are used for the relative streams are 306K, which represents the situation within the lower levels of the troposphere, and 318K which is characteristic of the upper levels.
12 June 1996/00.00 UTC - Meteosat IR image; magenta: relative streams 306K - system velocity: 207° 11 m/s, yellow: isobars 306K, red: wind vectors 306K, position of vertical cross section indicated
12 June 1996/00.00 UTC - Meteosat IR image; magenta: relative streams 318K - system velocity: 207° 11 m/s, yellow: isobars 318K, red: wind vectors 318K, position of vertical cross section indicated
The analysis shows in the lower layers of the troposphere a Cold Conveyor Belt (left) originating from northern directions. As described above, the Cold Conveyor Belt approaches the warm front with a descending component (from approximately 650 hPa to approximately 750 hPa). In front of the surface front line it turns to a direction parallel to the front where it starts ascending (from approximately 750 hPa to approximately 700 hPa).

The upper levels of the troposphere are as described in the case before within the ascending relative stream of the upper relative stream (right), which originates from the western side of the trough. The Warm Conveyor Belt can only be found within the warm sector in front of the cloud band of the Cold Front.


SUB-MENU OF WARM FRONT BAND
CLOUD STRUCTURE IN SATELLITE IMAGES
KEY PARAMETERS