Title: Why Do We Have Weather
1Why Do We Have Weather?
2An Introduction
- Take good notes! There will be a quiz at the end
of this presentation.
3WHY DO WE HAVE THE WEATHER ?
- Just think about it!
- Why is there wind? Why does it blow from one
direction one day and another the next? - Why is it rainy one day and dry the next?
- How come its cold in the winter?
- How can we have hail in the summer?
- What causes snow and freezing rain?
4Lets take a look at the weather picture and why
we have weather!
5If we were to pick one term to help explain why
we have weather, what do you think would be a
good word?
- You might pick heat or sun.but another good
choice would be - Convection
6Convection is the transfer of heat,usually in
gases or liquids.
7After the atmosphere is warmed by radiation and
conduction, the heat is transferred throughout
the atmosphere by convection.
- Since warmed air has more space between the
molecules, its less dense and rises - Cooled air is more dense and tends to sink
- In general, air near the equator tends to rise
and air near the poles tends to sink
8Take a look at this!
9Notice the band of clouds around the equator ?
- This is the ITCZ or inter tropical convergence
zone
10Why do you think there is this band of clouds
near the equator?
11Did you figure it out?
- Warm, moist air in the topics rises
- Cold air can hold less moisture than warm air
- As the moist air rises, it condenses and forms
clouds! - More on this later
12Consequences of Rotation the Coriolis effect
13The Weather Highways
- The rotation of the earth creates the Coriolis
effect. - The Coriolis effect causes the air and water to
be deflected to the right north of the equator. - This creates global weather highways
14The Westerlies
- Because of our latitude, most of our weather
comes from the west - Looking at the weather map, what type of weather
might we expect? - What type of weather might we expect in a few
days?
15Lets break for a short review
- 1.Transfer of heat in liquids or gases_____
- 2. _____ air is dense and tends to sink.
- 3. Band of clouds found around the equator______
- 4. Cold air holds _____ moisture than warm air
- 5. The Coriolis effect causes the air and water
to be deflected to the _____ of the equator
16How did you do?
- 1. CONVECTION
- 2. COLD
- 3. ITCZ
- 4. LESS
- 5. RIGHT
17Now What?
- Ok, so we know that the weather moves around on
these highways and that warm air rises and cold
air sinks. - But why is it sunny one day, and rainy the next?
18Lets take another look at the weather map
- Notice that there are Hs and Ls on the map
- There are also blue lines with spikes and red
lines with half circles - Lets take a closer look!
19High Pressure Areas
- When cooler air sinks and is warmed, the air can
hold more moisture - This usually means sunny skies
- Winds tend to move clockwise around a high
20Low Pressure Areas
- When warm air rises and is cooled, the air can
not hold as much moisture - Often, these areas are associated with
precipitation and stormy weather - Winds tend to move counter clockwise around the
low
21So, if you see a big H on the weather map over
the area you live, you can expect fair weather
22When you see a big L in your area, there will
probably be stormy weather
23These highs and lows move or less along the jet
stream and bring us our weather changes
24Fronts and Air Masses
- An air mass is a large body of air whose
temperature and moisture are fairly similar at a
given altitude - Fronts are boundaries separating different air
masses - There are four different air masses that affect
the United States
25The Air Masses
- cP( continental polar) cold, dry stable
- cT( continental tropical) hot, dry, stable air
aloft, unstable at the surface - mP( maritime polar) cool, moist, unstable
- mT( maritime tropical) warm, moist, unstable
26This map shows the air mass source regions and
there paths
27Ok, now we see the difference in the air masses
- Lets look at the different fronts and their
impact on weather - Can you see the four different types of fronts on
the map?
28Warm Fronts
- A warm front is warm air displacing cool air
diagram - Shallow leading edge warm air must overrun cold
air - These are usually slow moving
29Cold Fronts
- Cold air advances into region of warm air
- Intensity of precipitation greater, but short
lived - Clearing conditions after front passes
- Usually approaches from W or NW
30Stationary Fronts
- Surface positions of the front do not move
- Often a region of clouds
31Occluded Fronts
- Cold front overtakes warm front
- Often found close to the low pressure center
32Ready for a little quiz?Youll need a sheet of
paper
- Write your answers as we go
- Here we go!
331.
- Winds in a low pressure system move _____ around
the low
342.
- What type of front can be found close to point D ?
353.
- Which of these fronts would you expect to have
greater precipitation, but be short lived as the
front passes?
364.
- Give the name of the air mass that would have the
following characteristics - cool, moist, unstable
375.That important weather word that refers to the
transfer of heat
386.In general, air near the equator tend to_____
( rise or fall )
397.
- It causes air and water to be deflected to the
right north of the equator
408.Which of the weather highways usuallycontrols
our weather
419.
- Warm air holds ( more or less ) moisture than
cold air
4210.
- If there is a big H on the weather map where you
live, would you expect fair or stormy weather
43How did you do?
44Answers
- 1. Counterclockwise 8.
Westerlies - 2. Cold 9.
More - 3. Cold 10.
Fair - 4. Maritime polar (mP)
- 5. Convection
- 6. Rise
- 7. Coriolis