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Weather.

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Presentation on theme: "Weather."— Presentation transcript:

1 Weather

2 Precipitation Rain & Drizzle- most common type of precipitation.
Freezing Rain- drizzle from stratus clouds. Freezing Rain- raindrops freeze when they hit the ground. Sleet- raindrops that freeze before they hit the ground. Waters 3 States Video 6:52

3 Precipitation snow- as ice grows and merges into clouds they form snowflakes. hail- is the largest type of precipitation. Lumps or balls of ice that fall from cumulonimbus clouds in warm weather. 5th

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5 Let’s take a look at the weather picture and why we have weather!

6 What is Weather? State of the atmosphere at a specific time and place
Includes such conditions as air pressure, wind, temperature, and moisture in the air Temperature is a measure of air molecule movement Sun’s energy causes air molecules to move rapidly; temperatures are high and it feels warm When less of the Sun’s energy reaches air molecules, they move less rapidly and it feels cold

7 What is Weather? Energy is transferred between fast-moving molecules and slower-moving molecules CONDUCTION – transfer of energy when molecules collide CONVECTION – occurs when warm air rises and cool air sinks; it’s the transfer of heat, usually in liquids or gases

8 You might pick heat or sun….but another good choice would be
If 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

9 After 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, it’s 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

10 Take a look at this!

11 Notice the band of clouds around the equator ?
This is the ITCZ or inter tropical convergence zone

12 Why do you think there is this band of clouds near the equator?

13 Did you figure it out? Warm, moist air in the tropics rises
Cold air can hold less moisture than warm air As the moist air rises, it condenses and forms clouds!

14 Now 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?

15 Let’s take another look at the weather map
Notice that there are H’s and L’s on the map There are also blue lines with spikes and red lines with half circles Let’s take a closer look! 6th

16 AIR PRESSURE Air weight that varies over Earth’s surface
Warmer air is less dense and exerts less pressure Cooler air is more dense and exerts more pressure

17 High 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

18 Low 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

19 So, if you see a big H on the weather map over the area you live, you can expect fair weather

20 When you see a big L in your area, there will probably be stormy weather

21 These highs and lows move or less along the jet stream and bring us our weather changes

22 Humidity The amount of water vapor in the air
Temperature affects how much moisture is in the air - warmer air can hold more water vapor, tending to make it more humid Relative humidity – the amount of water vapor in the air compared to what it can hold at a specific temperature When air cools, it can’t hold as much water vapor, so the water vapor condenses to liquid or forms ice crystals Dew point – the temperature at which air is saturated and condensation forms

23 Global Winds Wind patterns, caused by convection currents combined with the Coriolis effect, of Earth that affect the world’s weather Near equator, very little wind and daily rain patterns called the doldrums Surface winds: Between equator and 30 degrees N and S latitude are steady trade winds Between 30 and 60 degrees N and S latitude, the westerlies blow in opposite direction from the trade winds. The polar easterlies blow from northeast to southwest near the north pole and from southeast to northwest near the south pole

24 Global Winds TRADEWINDS Equatorial doldrums TRADEWINDS

25 The 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

26 The 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?

27 Fronts and Air Masses Because air and moisture move in the atmosphere, weather is constantly changing Air pressure – measured by barometer An air mass is a large body of air whose temperature and moisture are fairly similar at a given altitude; properties like the part of Earth’s surface over which it formed Fronts are boundaries separating different air masses – clouds, precipitation, and storms occur at frontal boundaries There are four different air masses that affect the United States

28 The 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

29 This map shows the air mass source regions and there paths

30 Warm Fronts A warm front is warm air displacing cool air
Shallow leading edge warm air must “overrun” cold air These are usually slow moving Widespread precipitation develops!

31 Warm Front 2. Warm Front: The zone where warm air is replacing colder air In U.S., warm fronts usually move from southwest to northeast Air gets more humid after a warm front moves through

32 Cold 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 Temperature drops; narrow band of violent storms!

33 Cold Front 1. Cold Front: The zone where cold air is replacing warmer air 3rd In U.S., cold fronts usually move from northwest to southeast Air gets drier after a cold front moves through

34 Stationary Fronts Surface positions of the front do not move
Often a region of clouds and precipitation

35 Stationary Front 3. Stationary Front: When either a cold or warm front stops moving When the front starts moving again it returns to either being a cold or warm front

36 Occluded Fronts Cold front overtakes warm front
Involves three air masses of different temperatures Often found close to the low pressure center Cloudy weather with precipitation!

37 Occluded Front 4. Occluded Front: Formed when a cold front overtakes a warm front This occurrence usually results in storms over an area In U.S., the colder air usually lies to the west MENU

38 Weather Tools Anemometer- A tool used to measure
wind speed in miles per hour. Wind vane · A tool used to measure wind direction. · Sometimes referred to as a wind-weather vane or a wind sock. · Wind direction is described by the direction from which the wind is blowing. Thermometer - A tool used to measure air temperature in degrees Fahrenheit or Celsius.

39 Weather Instruments Video 1 15:01 Weather Instruments Video 2 19:41
Weather Tools Sling Psychrometer- A two-thermometer instrument also referred to as a wet-dry bulb used to measure relative humidity (the amount of water vapor in the air). Temperatures readings are converted using a relative humidity table. Weather Instruments Video 1 15:01 Weather Instruments Video 2 19:41

40 Weather Tools Barometer- A tool used to measure air pressure in inches of mercury or millibars (mb). Rain gauge- A tool used for measuring the amount of precipitation in inches or centimeters.

41 Weather Map Symbols

42 MENU

43 Reading a weather map ISOBAR= connects areas of equal pressure BAR comes from BARometric pressure

44 Reading a weather map... Isotherm: Connects areas of equal temperature; therm means temperature

45 Satellites & Radar Satellites
· Satellite images are used for seeing cloud patterns and movements. · For example, hurricane clouds and movement can be observed using satellite images. Radar · Radar images can be used to detect cloud cover, rainfall or storm location, intensity, and movement, as well as the potential for severe weather (for example, hurricanes or tornadoes).

46 Severe Weather Thunderstorms occur inside warm, moist air masses and at fronts Warm, moist air is forced rapidly upward, where it cools and condenses Strong updrafts of warm air and sinking, rain-cooled air cause strong winds

47 Lightning Movement of air inside a storm cloud causes parts of the cloud to become oppositely charged Current flows between the regions of opposite electrical charge, forming a lightning bolt Thunder – lightning superheats the air, causing it to expand rapidly and then contract, forming sound waves

48 Tornado Violent, whirling wind that moves in a narrow path over land

49 Blizzard A winter storm with strong winds, cold temperatures, and low visibility, that lasts more than three hours

50 Hurricane Large, swirling, low-pressure system that forms over tropical oceans Heat energy from moist air is converted to wind that can reach speeds of 250 km/h

51 Severe Weather Safety A National Weather Service WATCH means conditions are favorable for severe weather to develop A warning means that severe weather conditions already exist Meteorologists study and predict weather National Weather Service makes weather maps and issues watches and warnings


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