OCCLUSION: COLD CONVEYOR BELT TYPE - METEOROLOGICAL PHYSICAL BACKGROUND

by ZAMG


As has been explained in the general remarks the starting viewpoint for the conceptual model Occlusion: Cold Conveyor Belt Type is the typical configuration in the satellite imagery and its development up to an eventually longer lasting mature stage.

The classical Norwegian model

The classical development of an Occlusion is described in the well-known polar front theory after Bergeron as a development from a Wave stage (see Wave) with a well developed Cold Front (see Cold Front, Cold Front In Cold Advection, Cold Front In Warm Advection, Split Front and Arctic Cold Front) and Warm Front (see Warm Front Band, Warm Front Shield and Detached Warm Front). The basic idea is that the Cold Front moves faster than the Warm Front. Therefore the warm sector continously becomes more narrow until finally the Cold Front overtakes the Warm Front completely, thereby lifting the warm air. This is the typical situation for the Occlusion band which turns cyclonically around the core of the cyclone.
According to this classical theory of the Occlusion band, this front separates the cold air mass, which is situated in front of the former Warm Front, from that behind the former Cold Front with a tongue of warm air within the higher levels of the troposphere (see Typical appearance in vertical cross section ). Following the distribution of the temperature in front of and behind the occlusion, two sub-types can be separated:
Warm Occlusion
Cold Occlusion
During this process, the displacement of the low becomes smaller, until it becomes quasi-stationary.

Deviations between cloud configurations in satellite images and the classical Norwegian model

Very soon after the use and study of satellite images it became clear that this idealized theory cannot be observed in every step and detail in reality. In particular, the overtaking of the Warm Front by the Cold Front with very narrow warm sectors can never be seen (left schematic). Instead of this a mergence of Cold and Warm Front cloudiness in the centre of the surface low takes place followed by a westward extension of the Occlusion cloud spiral, while the Warm Front cloudiness becomes shorter (right schematic).
Beside this there are Occlusion spirals which contradict the overtaking mechanism completely. Those developments show a lower cloud spiral penetrating westward from below the Cold Front and Warm Front.
As already mentioned for Cold Fronts and Warm Fronts, those contradictions between the typical polar front theory and the appearance in the satellite imagery were also one reason for the conveyor belt theory.

Conveyor Belt model

This theory is not an independent new model, but allows a different insight into the same phenomena of the Occlusion process. It shows a much bigger variety of development possibilities and clearly indicates that the Occlusion development described by the Norwegian model represents only a special case.

The conveyor belt theory for the Cold Front deals predominantly with two relative streams: the warm conveyor belt and the dry intrusion. The warm front deals predominantly with the relative streams of the warm conveyor belt and the cold conveyor belt. For the Occlusion all three conveyor belts are relevant:

The vertical relation of these three conveyor belts to each other results in the different cloud types of the Occlusion: the multilayered Warm Conveyor Belt Type of the cloud spiral and the Cold Conveyor Belt Type.

The latter form of the Occlusion can much more often be observed in the satellite image than the Warm Conveyor Belt form of the Occlusion (see Occlusion: Warm Conveyor Belt Type ).It can only be explained with the help of the conveyor belt theory.

The dominant streams in this case are the cold conveyor belt and the warm conveyor belt.

The lower cloud spiral develops in the rising cold conveyor belt, while the higher cloud band of Warm Front and Cold Front are determined by the warm conveyor belt.

In literature different configurations of the cold conveyor belt are mentioned:

Investigations at ZAMG on all Occlusion events of one year clarified and contributed to these ideas.
There is an intensive upward inclination in the cross section of the isentropic surfaces, which leads to the fact that an isentropic surface which reaches the ground in the cross section A1-B1 (schematic bottom left) is already within the middle level Occlusion part in the cross section A2-B2 (schematic bottom right). Consequently in the schematics at the bottom left both relative streams can be seen: the cold conveyor belt which is only in the lowest layers and below the warm conveyor belt. It cuts the cross section perpendicularly, while the warm conveyor belt rises on the isentropic surface above. In the cross section above at the bottom right only the cold conveyor belt can be observed.
The cold conveyor belt described in this chapter develops if the absolute topography within the lower levels of the troposphere shows a closed cyclonic circulation. The mid- and upper levels of the troposphere are characterized by an upper level trough. During the lifetime of such a cloud spiral the trough within the mid- and upper levels of the troposphere might get more and more pronounced ending up in a closed cyclonic circulation. As a consequence of this process the development of high cloudiness within the cloud spiral immediately downstream of the point of the Occlusion can be observed (see cloud structure in satellite image ).
26 February 1997/06.00 UTC - Vertical cross section A; black: isentropes (ThetaE), blue: relative humidity, orange thin: IR pixel values, orange thick: WV pixel values
26 February 1997/06.00 UTC - Vertical cross section B; black: isentropes (ThetaE), blue: relative humidity, orange thin: IR pixel values, orange thick: WV pixel values
In cross section A, extending over the Atlantic from approximately 45N/45W to approximately 61N/45W, only the cold conveyor belt on both isentropic surfaces crosses the cross section perpendicularly. Humidity maxima and IR peaks contribute to the cold conveyor belt.
In cross section B, extending over the Atlantic from approximately 43N/42W to approximately 58N/41W, relative streams cut the cross section perpendicularly on the isentropic surface of 280 K at a height between 700 and 800 hPa. On the higher isentropic surface of 284 K a warm conveyor belt rises between 800 and 600 hPa. The cold conveyor belt can be found below 800 hPa and again cuts the cross section perpendicularly.
26 February 1997/06.00 UTC - Meteosat IR image; magenta: relative streams 280K - system velocity: 224° 13 m/s, yellow: isobars 280K, position of vertical cross section indicated
26 February 1997/06.00 UTC - Meteosat IR image; magenta: relative streams 284K - system velocity: 224° 13 m/s, yellow: isobars 284K, position of vertical cross section indicated
On the isentropic surface of 280K a rising cold conveyor belt can be observed.
On the isentropic surface of 284K the splittting of the conveyor belt into an eastward and a westward branch can be observed.
26 February 1997/06.00 UTC - Vertical cross section; black: isentropes (ThetaE), blue: relative humidity, orange thin: IR pixel values, orange thick: WV pixel values
26 February 1997/06.00 UTC - Meteosat IR image; magenta: relative streams 290K - system velocity: 224° 13 m/s, yellow: isobars 290K, position of vertical cross section indicated
In the cross section extending over the Atlantic from approximately 54N/26W to approximately 51N/53W, isentropes and relative humidity show a very similar distribution to the above mentioned schematics. On the isentropic surface of 284K the cold conveyor belt rises from 800 up to 500 hPa and is accompanied by a backward bend of the relative humidity. On the isentropic surface of 290K a strongly ascending warm conveyor belt cuts the cross section perpendicularly as well as the upper relative stream more to the west, both accompanied by a humidity maximum. On the same isentropic surface higher than 500 hPa the dry intrusion characterized by a strong humidity gradient restricts the wet air of the cold conveyor belt from above.
The figure including the relative streams on the isentropic surface of 290K shows a strongly rising warm conveyor belt above the Atlantic from approximately 50N/35W to approximately 56N/32W. Eastward of approximately 56N/32W the warm conveyor belt descends, accompanied in the satellite image by a dissolution of cloudiness. The upper relative stream, which like the warm conveyor belt also ascends, can be found in the image above the Atlantic from approximately 49N/40W to approximately 58N/31W. The limiting stream line between the warm conveyor belt and the upper relative stream can be found within the area of the cloudiness at approximately 50N/40W - 53N/41W - 56N/40W - 57N/32W.
28 March 1997/12.00 UTC - Vertical cross section; black: isentropes (ThetaE), blue: relative humidity, orange thin: IR pixel values, orange thick: WV pixel values
28 March 1997/12.00 UTC - Meteosat IR image; magenta: relative streams 294K - system velocity: 295° 14 m/s, yellow: isobars 294K, position of vertical cross section indicated
28 March 1997/12.00 UTC - Meteosat IR image; magenta: relative streams 306K - system velocity: 295° 14 m/s, yellow: isobars 306K, position of vertical cross section indicated, blue: zero line of shear vorticity 300 hPa (indicative for model jet axis), orange: transition between white and dark WV signals (indicative for jet axis)
Two isentropic surfaces which are representative of the explanation for the analysis of the conveyor belts have been chosen. The isentropic surface of 294K is typical for the situation on a lower isentropic surface, and the isentropic surface of 306K is typical for a higher isentropic surface.
On the isentropic surface of 294K the figure shows a strongly rising cold conveyor belt with the brightest tops above Lithuania in the area of geatest ascent.
On this isentropic surface (306K) all relevant streams for the higher levels can be observed: the warm conveyor belt in the southernmost cloud part, the upper relative stream from behind within the Cold Front, and the Warm Front cloudiness and the dry intrusion crossing the Occlusion immediately northward. But it has to be mentioned that there is a discrepancy between the model jet axis (dashed blue line) and the jet axis as localized by the satellite image (solid orange line). A northward shift of about three degrees in the area of the western Ukraine would be necessary.
28 March 1997/12.00 UTC - Meteosat IR image; yellow: isotachs 300 hPa, red: positive vorticity advection (PVA) 300 hPa
The satellite image shows cellular cloudiness embedded within the rear area of the Cold Conveyor Celt Type Occlusion at the border of Poland and White Russia at approximately 52N/24E. The embedded convective cloudiness is situated within the left exit region of the jet streak, which is a predestined area for such developments.

SUB-MENU OF OCCLUSION: COLD CONVEYOR BELT TYPE
CLOUD STRUCTURE IN SATELLITE IMAGES
KEY PARAMETERS