Fronts And Frontal Depression Flashcards
Cyclogenesis
Is the-name used to describe a development of low pressure
High level divergence is the main issue of low pressure
Jet streams forms due high level divergnce
Wave of polar fronts
(Travel to east)
Locationtion in the westerly ,can expect waves of rain (1-2 days breaks in between)
Polar air depression (over water)
Most polar air depressions are in»_space;norwegian sea, barents sea, sea of japan,gulf of alska
Because of the difference between cold air masses and warm seas
Frontogenesis
Frontolysis
FRONTOGENESIS»formation of a fronty
Frontolysis»decay /dissipation of a front
In. A polar front check the warm sector lines to see the direction of the front
~Warm front»warmer air advances on colder air
~cold front» cold air adavnces on warmer air
~occluded front» cold front rises or undercuts the warm fron
Warm front
Moves relatively slow (10kts)
Slope 1:150
CI,CS,AS,NS,ST
Warm fron t hazards
~freezing rain in winter ~low cloud over large area ~icing in cloud ~poor visibilty in heavy rain/low cloud/frontal fog ~aquaplanning on wet runways ~cat areound jet sttrream
Passage warm front
800km ahead of the surface front
~warm front approaches»pressure reduces ,lowering cloud with -ra
~warm front»RA/DZ,pressure minimum ,wind veers,increase in temperature
~after warm front»warm sectro ocnditions,pressure slight increase
WARM SECTOR
~LOW CLOUD,INTERMITTENT,DRIZZLE,POOR VISIBILTY
~TEMPERATURE IS OFTEN MILD
~IN SUMMER ,CLOUD MAY BURN OFF,POSSIBLE FORM OVER CONTINENTAL AREAS
~A DEPRESSION MOVES IN THE DIRECTION OF THE GEOSTROPHIC WIND BLOWING PARALLEL TO HE ISOBARS INSIDE THE WARM SECTOR
COLD SECTOR
~typical cumuls copuld develpment just ahead of cold front
~tyhe slope is steeper than the warm front. 1:50
~travels quicker 20-20kts
200/300km from the surface
St,cb,as,cs,ci.
Rememeber after cold front there a CU
Flying hazard in cold front
~severe turbulence in cb ~sevre icing in cb ~lightning from thnuderstorm ~abrupt change in wind direction passing through front ~windshear associated with gust ~poor visubity ~cat ~aquaplaning
Cold front approaches»_space;slight pressure reduction
At cold front»+RA with cb ,pressure minimum ,wind veers,decreases in temp
after cold front»pressure increase,good visibility but isolated TCU/CU
Warm occlusion
When the coldest air is in front,the warm air is aloft and the less cold air is behind.
More likely in winter
Cold occlusion
Cold air is in front and the warm air is aloft and the coldest air is behind.
More likely in summer
Stationary front
~caused by isobars being parallel to the warm /cold air boundary
~the weather can persist for several days
Passage warm front
Passage cold front
Warm front»
~warm front approches: pressure reduces from high (because replacing cold air with warm air),lowering clopud,
-RA
~at warm front:RA/DZ,pressure minimum,wind veers,increase in temp
~after warm front:warm sector conditions ,pressure slight increase
~warm sector:low cloud,intermittent drizzle,poor visibility,temp mild
COLD FRONT»
~cold front approaches slight pressure reduction
~+RA with CB,pressure minimum,wind vees,decrease in temp
~pressure increase ,good visibility but TCU/CU