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Meteorology study of atmosphere & weather events.

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Presentation on theme: "Meteorology study of atmosphere & weather events."— Presentation transcript:

1 Meteorology study of atmosphere & weather events

2 Atmosphere Gases 78% = Nitrogen 21% = Oxygen <1% = Argon, Carbon
Dioxide, & others As seen on p. 477 % 78% 21% 1% gas Nitrogen Oxygen Ozone Carbon Dioxide Argon Hydrogen atom(s) N O C & O Ar H molecule N2 O2 O3 CO2 -- H2

3 Atmosphere Layers

4

5 Temperature Heat Conduction Convection Radiation
measurement of how rapidly or slowly molecules move around transfer of energy that occurs because of a difference in temperature between substances Transfer of Energy: Conduction Convection Radiation Transfer of heat from one object to another through touch Transfer of heat from one place to another through circulation Transfer of energy in the form of waves A spatula warms up after sitting in a hot pan. In the ocean, warm currents move heat from the equator to higher latitudes. Radiant heat energy that is emitted by an oven.

6 N. Hemisphere = right. S. Hemisphere = left.
The Coriolis Effect As Earth spins, anything (planes, boats, water, wind, & molecules) moving in a straight line will be deflected. N. Hemisphere = right. S. Hemisphere = left.

7 Air Pressure Force exerted on an object by the air (molecules).
Occurs in all directions → up, down, & sideways Barometer = instrument used to measure air pressure. Units = mmHg (millimeters of Mercury) or atm (atmospheres) Sea Level = 1 atmosphere As seen on p. 533

8 Air Pressure (continued)
Isobars = lines on a weather map that connect areas of equal pressure “H” = high pressure cell “L” = low pressure cell How does air move? air moves from High to Low

9 High & Low Pressure Cells
clear skies outward sinking air C.W. cloudy skies inward rising air C.C.W.

10 Airflow of cyclones & anticyclones
aloft = high in the atmosphere p. 539

11 HIGH pressure cell :) Anticyclone
Center of HIGH pressure (“H” in BLUE) Pressure increases toward the center Winds associated with an anticyclone: Outward (divergence) C.W. = Clockwise (opposite in the Southern Hemisphere) subsiding (sinking) air Usually bring "fair" (clear) weather

12 LOW pressure cell :( Cyclone rising air Bring clouds & precipitation
Center of LOW pressure (“L” in RED) Pressure decreases toward the center Winds associated with a cyclone: Inward (convergence) C.C.W. = Counterclockwise (opposite in the Southern Hemisphere) rising air Bring clouds & precipitation

13 Winds in the N. Hemisphere

14 Caused by horizontal air pressure differences (pressure gradients)
Wind Caused by horizontal air pressure differences (pressure gradients) Uneven heating of the Earth creates pressure differences. What part of the Earth heats up the most? How does air pressure relate to density?

15 Factors that affect wind:
If the Earth didn’t rotate how would global winds move? from the poles to the equator As seen on p. 540 …but the earth DOES rotate so that creates some craziness Factors that affect wind: Pressure differences = cause air to move Coriolis Effect = cause winds to be deflected Friction = slows down air, changes wind direction

16 Global Winds p. 541 both poles are high pressure

17 hot air forms near Equator
Air masses Large body of air that takes on the characteristics of the area over which it forms. It’s source region determines temperature & humidity. p. 559 Air Masses forms over Land (dry) forms over Water (humid) hot air forms near Equator Continental Tropical (cT) Maritime Tropical (mT) cold air forms near Poles Continental Polar (cP) Maritime Polar (mP)

18 As seen on p. 560

19 Fronts Boundary that separates air masses of different densities
Air masses retain their identities Warm, less dense air forced to move up Cold, dense air acts as wedge, moving down 4 types: p. 564

20 Warm Front Warm air replaces cooler air
Front is very gentle slope & moves slowly Light-to-moderate precipitation p. 565

21 Cold Front Twice as steep and moves faster than warm front
Violent weather, very intense, & short duration Weather behind front is cold, sinking air, & clear conditions p. 566

22 Stationary Front When 2 air masses meet but don’t advance
Flow of air on both sides of front is parallel Rarely any clouds or heavy precipitation

23 Occluded Front Occurs when a cold air mass overtakes a warm front
Warm air is wedged upward Weather is often complex...at mature stage p. 567

24 Humidity = amount of water vapor in the air
Condensation gas → liquid Humidity = amount of water vapor in the air

25 Cloud Formation Saturation depends on the temperature of air: cold air
room temperature hot air less capacity to hold water vapor holds about 1% of greater capacity to hold water vapor atmosphere molecules moving slowly - less space between them atmosphere molecules moving quickly - more space between them Relative Humidity = ratio of water vapor in air relative to how much it can hold Dew point = temperature to which air must be cooled to reach saturation

26 Saturation = point at which air holds as much water vapor as it can
Cloud Formation Saturation = point at which air holds as much water vapor as it can Not saturated Saturated Beyond Saturated it could hold more it can’t hold this much

27 Cloud Classification Cloud Shapes Shape Feature Nimbus
Low, gray rain clouds Cumulus Flat Base, rising dome = Califlower Stratus Sheets or layers Cirrus Thin, wispy, ice crystals = high

28 Cloud Project Name of Cloud
Explanation of the Root words within the name Characteristics of the Shape of the Cloud Location of the Cloud in the Atmosphere Does the Cloud Produce Precipitation? Creative Rendering of the Cloud - Color, Materials, etc. Picture of You Interacting with Cloud - Airplane, Hot Air Ballon, Superhero...etc Cloud Shapes Shape Feature Nimbus Low, gray rain clouds Cumulus Puffy or lumpy Stratus Sheets or layers Cirrus Thin, wispy, or stringy

29 Cloud Formation Condensation nuclei = small particles (dust, particles, spores, aerosols) around which cloud droplets can form if density is high enough it becomes visible air cools as it rises it becomes precipitation if gravity overtakes

30 Processes that lift air
1. Orographic Lifting 2. Frontal Wedging When mountains block the flow of air forcing it up. When warm air is lifted at a front, two different densities 3. Convergence 4. Convective Lifting When air flows together and rises, similar densities When unequal surface heating causes pockets of air to rise, parking lot next to park

31 Severe Storms Cyclone = generic term for an organized system of winds rotating inward to an area of low pressure

32 Thunderstorms Storm that produces thunder,
lightning, heavy rain, gusty winds, & possibly hail. Can be local, single cloud storms, or multiple cells along a cold front. Storm Hazards: Lightning Hail Floods

33 3 stages of a thunderstorm:
p. 572 warm, moist air is moved upward (about 1 hour later) heavy precipitation begins with gusty winds, lightning, and hail. cooling of the air → the storm to dies down.

34 Tornadoes Violent windstorms that form a rotating column of air (vortex) that extends downward from a cumulonimbus cloud. Most form during thunderstorms. Intensity of a tornado is based on the wind speed & the estimated damage. (p. 574) also known as a “Twister”

35 Hurricanes Tropical cyclone that produces winds of at least 74 mph.
Intensity is based on wind speeds. Energy that drives it comes from warm ocean water. Power dies down when it moves over land.

36 Hurricanes (stages) Tropical Depression (disturbance) – first stage with several thunderstorm clusters and little or no cloud rotation. Tropical Storm – winds begin to rotate & thunderstorms progress. p. 577

37 Hurricanes (intensity)
p. 577 Category 3 is considered a major hurricane.

38 Hurricanes (structure)
p. 577 Eye – center of the hurricane where air is subsiding (sinking) & being warmed. Eye Wall – layer of clouds that surrounds the eye, where winds are fastest & rainfall is greatest. Rain Bands – clouds that extend outward from the eye wall, circulates, & rotates around the storm cell. Storm Surge – dome of water directly underneath the eye which can cause severe flooding as the storm hits land.

39 What is the temperature in Charlotte, NC ?
Isotherms = lines that connect areas of equal temperature What is the temperature in Charlotte, NC ?

40 Gathering Weather Data
Thermometer = temperature Barometer = air pressure Anemometer = Wind Speed Hygrometer = relative humidity Doppler Radar tracks precipitation & measures wind speeds in storms uses the Doppler Effect (change in wave frequency) Satellites Detects thermal (heat) energy Gives an image of cloud cover Determines cloud temperature

41 a record of weather data for a specific location and time
Station Model a record of weather data for a specific location and time


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