depressions Flashcards
1
Q
how does a depression form
A
- a mid-latitude depressions forms when warm tropical maritime air mass from the North Atlantic meets a cold polar maritime air mass along the front between 30 degrees and 60 degrees in latitude
- the westerly flowing jet stream in the upper atmosphere plays a vital role in the anticlockwise uplift of air which produces a well-defined warm front, warm sector and a cold front
- as the upper air jet moves upwards, from a trough to a ridge it accelerates, diverges and draws air upwards creating low pressure centre at the ground surface with an anticlockwise pattern of winds
- the path of the depression follows the westerly movement of the jet stream and is associated with a sequence of weather with the passage of a the warm front, warm sector and the cold front.
2
Q
general weather conditions associated with depressions
A
RAINFALL
- Area of low pressure, Tropical maritime air rising, cools, reaches dew point (RH 100%) and condenses = cloud formation.
WINDY
- isobars close together= steep pressure gradient
-Therefore, winds quickly move from high to low pressure
-Air accelerates as it moves from trough to ridge (sharp uplift of air molecules)
LOW/MILD TEMPERATURES
-Clouds, restrict the level of solar radiation the therefore temperatures may be cooler.
3
Q
- before the warm front
A
- cirrus clouds
- dry and cold
- wind is light southerly
- air pressure falling high (1002)
4
Q
- at the warm front
A
- nimbostratus clouds
- consistent rain
- warm
- wind is strong and more westerly
- air pressure falling
5
Q
- at warm sector
A
- dull, low, flat, stratus
- relatively dry
- warm
- winds moderate and westerly
- air pressure steady
6
Q
- as cold front passes
A
- cumulonimbus
- heavy downpour
- temp falls rapidly
- wind is more northernly
- air pressure rising
7
Q
- after cold front
A
- cumulus
- showers cold temperature
- wind north or north west
- air pressure rising
8
Q
how does a depression end?
A
- the cold front has a steeper pressure gradient and moves faster than the warm front
- when the cold front catches up with the warm front it forms an occluded front
- the tropical air by this stage will have been squeezed upwards leaving no warm sector at ground level
- as uplift of air is reduced, so too is the amount of condensation and cloud formation
- air pressure begins to rise, and wind speeds decrease.
- the colder air replaces the uplifted air and infills the depression