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.
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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.

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3
Q
  1. before the warm front
A
  • cirrus clouds
  • dry and cold
  • wind is light southerly
  • air pressure falling high (1002)
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4
Q
  1. at the warm front
A
  • nimbostratus clouds
  • consistent rain
  • warm
  • wind is strong and more westerly
  • air pressure falling
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5
Q
  1. at warm sector
A
  • dull, low, flat, stratus
  • relatively dry
  • warm
  • winds moderate and westerly
  • air pressure steady
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6
Q
  1. as cold front passes
A
  • cumulonimbus
  • heavy downpour
  • temp falls rapidly
  • wind is more northernly
  • air pressure rising
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7
Q
  1. after cold front
A
  • cumulus
  • showers cold temperature
  • wind north or north west
  • air pressure rising
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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
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