19. Polar Front Depression Part 2 Flashcards
Polar Front Depression Pt 2
Refer to the following diagram. Numbered in order is the cloud formation with the passing of a polar front depression. What are each of the cloud types;
- [ ]
- [ ]
- [ ]
- [ ]
- [ ]
- [ ]
- [ ]
- [ ]
- [ ]
- [ ]
- [Ci]
- [As]
- [Ns]
- [St Fra]
- [St / Sc]
- [Ns]
- [Emb Cb]
- [As]
- [Ci]
- [Cu]
Polar Front Depression Pt 2
- The slope ratio of a warm front is 1:80 or 1:150
- The slope ratio of a cold front is 1:80 or 1:150
- 1:150
- 1:80
- REMEMBER warmer temperatures have higher degrees celcius
- Think of the slope ratios as temperatures, 80 and 150
- The warmer temperature (warm front) is 150, and the colder temperature (cold front) is 80
1
Polar Front Depression Pt 2
In the continuous moderate rain just ahead of the warm front, what type of cloud formation might form at the low level
FRACTOSTRATUS
(StFra)
Polar Front Depression Pt 2
At which point of a polar depression might you expect drizzle followed by continuous rain, possibly snow
[ ] 500 nm ahead of the warm front
[ ] 100 nm ahead of the warm front
[ ] At the warm front
[ ] Within the warm sector
[ ] At the cold front
[ ] 200 nm behind the cold front
[ ] 500 nm ahead of the warm front
[X] 100 nm ahead of the warm front
[ ] At the warm front
[ ] Within the warm sector
[ ] At the cold front
[ ] 200 nm behind the cold front
- Just ahead of the warm front
- Stable mTw is cooling on the colder air below
Polar Front Depression Pt 2
At which point of a polar depression might you expect heavy showers;
[ ] 500 nm ahead of the warm front
[ ] 100 nm ahead of the warm front
[ ] At the warm front
[ ] Within the warm sector
[ ] At the cold front
[ ] 200 nm behind the cold front
[ ] 500 nm ahead of the warm front
[ ] 100 nm ahead of the warm front
[ ] At the warm front
[ ] Within the warm sector
[X] At the cold front
[ ] 200 nm behind the cold front
- The cold front lifts warmer mTw air up
- This is convective lifting and NimboStratus clouds form as well as Embeded Cumulonimbus
- These bring heavy showers, and occur at the “nose” of the cold front
2
Polar Front Depression Pt 2
At which point of a polar depression might you expect advection fog in winter;
[ ] 500 nm ahead of the warm front
[ ] 100 nm ahead of the warm front
[ ] At the warm front
[ ] Within the warm sector
[ ] At the cold front
[ ] 200 nm behind the cold front
[ ] 500 nm ahead of the warm front
[ ] 100 nm ahead of the warm front
[X] At the warm front
[ ] Within the warm sector
[ ] At the cold front
[ ] 200 nm behind the cold front
- As the warm front approaches the ground is moist from precipitation and cold
- The air mass within the warm sector is mTw, so air is warm and moist
- The air is warmer and cooling so bringing on the onset of the dew point
- Advection fog in winter can be expected, and within the warm sector stratus cloud
2
Polar Front Depression Pt 2
- Wind speeds within the warm sector of a polar front depression are FASTER or SLOWER than the wind speeds within the cold air ahead of the warm front
- Wind speeds within teh warm sector of a polar front depression are FASTER or SLOWER than the wind speeds within the cold air behind the cold front
- SLOWER
- SLOWER
- In both cases, the wind within the warm sector is slower than the wind speeds within the cold and cool sectors
- We know that wind speeds in High pressure systems, also associated with warmer air, are slower
- Inlow pressure systems, the gradient wind is stronger and the isobars bend in towards the low
- Therefore in teh colder sectors, whcih are associated with the low pressure system, the wind speeds are greater
3
Polar Front Depression Pt 2
Refer to the following diagram. Completed each of the missing fields for WIND;
WIND
1. [ ]
2. [ ]
3. [ ]
4. [ ]
5. [ ]
=====
WIND
* VEERS
* VEERS
* W
* NW
* SW
- [SW]
- [VEERS]
- [W]
- [VEERS]
- [NW]
Polar Front Depression Pt 2
Refer to the following diagram. Completed each of the missing fields for PRESSURE;
PRESSURE
1. [ ]
2. [ ]
3. [ ]
4. [ ]
5. [ ]
====
PRESSURE
* FALLING
* FALLS
* STEADY
* RISING
* -
- [FALLING]
- [-]
- [STEADY]
- [FALLS]
- [RISING]
NOTE
* There is an exam question where it asks what will happen to pressure at point D in 1 hour
* Remember that the point itself is NOT MOVING with the passing of the front, but is stationary
* This is not clear in the question and it is meant to be inferred that the point is stationary
* Therefore, after 1 hour, the pressure will increase as point D is in effect in the position that point E is at in an hours time.
3
Polar Front Depression Pt 2
Refer to the following diagram. Completed each of the missing fields for TEMPERATURE;
TEMPERATURE
1. [ ]
2. [ ]
3. [ ]
4. [ ]
5. [ ]
=====
TEMPERATURE
* STEADY WARM
* STEADY, COOL
* STEADY, COOL
* FALLS
* INCREASES
- [STEADY, COOL]
- [INCREASES]
- [STEADY, WARM]
- [FALLS]
- [STEADY, COOL]
Polar Front Depression Pt 2
Warm Fronts
- Warm fronts on average move at ____kts
- Radiational cooling at night cerates cool dense surface air behind the front. This will inhibit what 2 things
- The average width of a precipitation zone on a warm front is ____ miles (____km)
- Turbulence is typically STRONG or WEAK apart from the frontal layer where it will be MODERATE or MODERATE TO STRONG
- Severe icing can be anticipated in Nimbostratus if temperatures are around ____℃ to ____℃
- The transition zone depicted on the surface of a weather chart as a line with red semicircles is a band ____ to ____ miles wide
- 10 KTS
- LIFTING and FORWARD PROGRESS
- 185 Miles (300 KM)
- WEAK / MODERATE TO STRONG
- -7℃ to -10℃
- 30 to 60 miles
Polar Front Depression Pt 2
Cold Fronts;
- The transition zone depicted on the surface of a weather chart as a line with blue triangles is a band ____ to ____ miles wide
- Active cold fronts (slow moving) average speed of ____ kts
- Inactive cold fronts (fast moving) have an average speed of ____kts
- Given an equal pressure gradient, the rate of movement of a cold front is ____% greater than that of a warm front
- The cloud mass is around ____ miles wide
- In winter, cloud types will usually be ____ and ____
- In summer, cloud types will be ____
- Icing and turbulence associated with thunderstorms, especially in summer, will be ____
- 30 to 60 miles
- 15 kts
- 25 kts
- 50%
- 120 miles
- NIMBOSTRATUS and ALTOSTRATUS
- EMBEDDED CUMULONIMBUS
- SEVERE
Polar Front Depression Pt 2
Warm Sectors;
- Consists of a ____ air mass
- What might be expected in coastal regions in winter
- Visibility is typically ____ at best, with it possibly being poor in winter
- TROPICAL MARITIME
- FOG
- MODERATE
Polar Front Depression Pt 2
- The high level wind (jet stream) associated with a polar front depression when viewed from above on a weather chart, will be BEHIND or INFRONT of and CLOSE TO or FAR FROM from the cold front line.
- The high level wind (jet stream) associated with a polar front depression when viewed from above on a weather chart, will be BEHIND or INFRONT of and CLOSE TO or FAR FROM from the warm front line.
- BEHIND / CLOSE TO
- INFRONT / FAR FROM
- When seen from above the jetstream appears to be situated in the cold air ahead of the warm front and behind front
- In reality, we have to remember that the fronts are sloped, and as such, the jetstream is actually in the warm sector aloft
- Compare the overhead view to the side profile view below
- The reason the jetstream is clsoer to the cold front is that the gradient of the slope is steeper
Polar Front Depression Pt 2
- When a warm front crosses over a mountain range, it is possible for warm air to get trapped on the UPSTREAM or LEESIDE of the mountain
- When a cold front crosses a mountain, precipitation and fully developed clouds are anticipated on the UPSTREAM or LEESIDE of the mountain
- UPSTREAM
- UPSTREAM
- As he warm front crosses the mountain, some warm air can get trapped on the windward (upstream) side of the mountain
- When the cold front approaches, the trapped warm air is forced upwards as a result of both orographic lifting and the cold air forcing its way underneath the warm air
- The warm air will want to rise as it is lighter than the cold air
- As a result, this triggers lifting and convective cloud formation and intensive presipitation