Passage of a “typical” disturbance on the Brittany coasts #
Diagram of the passage of a disturbance #
For an observer placed on the right side of the diagram, the cloudy ceiling will sink and become darker and darker accompanied by heavy rain. Then, in a second time, it will clear and give way to a sky filled with stratocumulus or stratus clouds and a few showers. This respite will be short-lived and will give way to strong winds and violent showers as the cumulonimbus passes. Thunderstorms are possible. The situation will then improve to give way to a trailing sky with a few squalls and clearings.
The passage between the two air masses takes place over a long distance and it is sometimes difficult to note the exact moment of its passage. Once the warm front has passed, we enter the warm sector, the zone of mild air between the warm and cold fronts in a frontal low.
Reproduce the diagram of the arrival of a disturbance
Réponse
Several presentations are possible
View from above #
The clouds associated with the depression are in order:
- Cirrus (CI) and Cirostatus (CS)
- Altostratus (As)
- Nimbostratus (Ns)
- Stratocumulus (Sc) and Stratus (St)
- Cumulonimbus (Cb)
- Altocumulus (Ac) and Altostratus (As)
- Cumulus (Cu)
Satellite view of a depression #
Very often, the cloud structure of a disturbance allows you to distinguish several parts. The head is located in front of the disturbance. The body corresponds closely to the fronts. The warm sector is the warm air trapped between the warm and cold fronts.
Finally, the trail is located behind the cold front. Quite often, the low-pressure center can be isolated on satellite photographs, by a less important presence of cloudy masses.
For each letter indicate the corresponding element:
Answer
A: Warm front / B: Cold front / C: Triple point / D: Occluded front / E: Depression center