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Weather - PowerPoint PPT Presentation

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Weather. Weather is. The current state of the atmosphere...what is happening right now. Main points to remember as we learn about weather:. The sun warms the earth’s surface and therefore all the air above the surface The earth is warmed most at the equator and least at the poles.

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Presentation Transcript
weather is
Weather is....
  • The current state of the atmosphere...what is happening right now
main points to remember as we learn about weather
Main points to remember as we learn about weather:
  • The sun warms the earth’s surface and therefore all the air above the surface
  • The earth is warmed most at the equator and least at the poles.
  • The air above land is warmed more quickly than air above water.
  • Warm air expands and rises, creating an area of low pressure; cold air is dense and sinks, creating an area of high pressure
weather factors
Weather Factors
  • Weather: The state of the atmosphere at a specific time and place


the average motion of molecules

↑ TEMP= ↑movement of molecules= feels hot

↓ TEMP= ↓movement of molecules= feels cold

air pressure
Air Pressure
  • Warm air= expanding or rising air= leaves behind L pressure
  • Cold Air=sinking air= leaves an area of H pressure
wind movement
Wind Movement
  • Uneven heating of the earth’s surface causes some areas to be warmer than others.
  • As we know, warm always follows cold to share it’s warmth- when this happens in the atmosphere, wind happens!
what causes winds
What causes winds?
  • A wind is a horizontal movement of air from an area of high pressure to an area of low pressure
  • It is this difference in pressure that makes the air move=wind
  • Winds are measured by direction and speed
  • The anemometer is the tool we use to measure this
  • Wind chill=↑ cooling the wind causes
local winds
Local Winds
  • The land cools and heats faster than the ocean. Water holds heat longer than land, and takes longer to heat or cool.


During the day, the land gets hotter faster than the water. The heated air rises, leaving behind an area of low pressure. Wind from the cooler sea blows in to take the place of that warmer air. These happen during the day!

land breezes
Land Breezes

At night the land cools off faster than the sea. Cool air sinks creating an area of high pressure. Wind blows from the land to the sea.

global circulation and wind systems
Global Circulation and Wind Systems
  • Solar energy is at its greatest around the equator.
global winds
Global Winds:
  • Wind belts:

Horse Latitudes= 30°N and S of

equator =calm winds= worlds

desert areas

Jet Streams= 10km above the

surface blow from the west to the east

doldrums calm winds of the tropics
Doldrums – calm winds of the tropics
  • The Doldrums is an area of low pressure at the equator. Most of the air movement in the doldrums is upward, as the heated air rises.
  • Known also as the Equatorial Convergence Zone
intense heat powerful convection
Intense heat = Powerful CONVECTION
  • Warm, moist air rises and leaves behind an area of low pressure. This is why most rain forests are found along equatorial regions.
  • That air rises until it reaches the top of the troposphere, where it can’t rise any further.
  • It spreads out towards the polar regions HOT follows COLD wanting to share its warmth.
  • As it spreads it begins to cool and sink-usually 30°N and S of the equator- sinking air produces an area of H pressure with dry conditions= desert regions on earth
water in the atmosphere humidity
Water in the Atmosphere: Humidity
  • Humidity: measure of the amount of water vapor stuck between molecules in the air. The air’s ability to hold water depends on the air temp
  • The hotter the air, the more water the air can hold
  • Cold air: molecules move slower so droplets of water can start to stick together=condensation
  • Relative humidity: the amount of water vapor(%) compared to the amount the air can hold- tool used is a psychrometer.
  • 100%=air is saturated
cloud formation
Cloud Formation
  • Clouds form when water vapor condenses on dust, salt particles in the air
  • The temperature in which condensation begins is called the dew point
types of clouds
  • Cirrus Clouds: wispy, feathery clouds

Form only at high levels, therefore are made of ice crystals

types of clouds1
Types of Clouds
  • Cumulus Clouds: are puffy white cotton ball looking clouds
cumulonimbus clouds
Cumulonimbus Clouds
  • These are thunderstorm clouds
types of clouds2
Types of Clouds
  • Stratus Clouds: clouds that form in flat layers- cover all or most of the sky and are low level clouds
air masses
Air Masses
  • Air masses are masses of air that have the same characteristics of the surface over which it develops
  • Pressure Systems

descending (going down)=H pressure

ascending (going up)=L pressure

fronts the boundary between 2 air masses
Fronts: the boundary between 2 air masses

This is the symbol on a map for a warm front

  • Warm Front: warm air slides over departing cold air- large bands of precipitation form
cold fronts

This is the symbol for a cold front

Cold Fronts
  • Cold air pushes under a warm air mass. Warm air rises quickly=narrow bands of violent storms form
occluded front

This is the weather map symbol for an occluded front

Occluded Front
  • 2 air masses merge and force warm air between them to rise quickly. Strong winds and heavy precipitation will occur
stationary front

This is the weather map symbol for a stationary front

Stationary Front
  • Warm or cold front stops moving. Light wind and precipitation may occur across the front boundary
reading a weather map
Reading a weather map
  • ISOBAR= connects areas of equal pressure BAR comes from BARometric pressure
surface analysis
Surface Analysis

Shows cold fronts and warm fronts

Shows isobars connecting like pressures

reading a weather map1
Reading a weather map...
  • Isotherm: Connects areas of equal temperature; therm means temperature