Climate vs. Weather. Weather: Short term state of the atmosphere. Climate: The average weather conditions in an area over a long period of time

Transcription

1 Weather and Climate

2 Climate vs. Weather Weather: Short term state of the atmosphere. Temperature, humidity, cloud cover, precipitation, winds, visibility, air pressure, air pollution, etc Climate: The average weather conditions in an area over a long period of time Described by temperature and precipitation

3 Measurement Definition Instrument M E A S U R I N G Temperature Air Pressure Wind Speed How hot or cold the air is The weight of the air How fast the wind is blowing Thermometer Barometer Anemometer W E A T H E R Wind Direction Humidity Precipitation Where the wind is blowing from Amount of water vapor in the air Amount of rain or snow that falls Weather Vane Hygrometer Rain Gauge

4 Measuring Weather Instruments used in measuring weather in the upper atmosphere Radiosonde: a package of instruments that is carried aloft by balloons to measure upper atmospheric conditions, including temperature, dew point, and wind velocity sends measurements as radio waves to a receiver that records the information. When the balloon reaches a very high altitude, the balloon expands and bursts, and the radiosonde parachutes back to Earth. Radar: radio detection and ranging a system that uses reflected radio waves to determine the velocity and location of objects The newest Doppler radar can indicate the precise location, movement, and extent of a storm. It can also indicate the intensity of precipitation and wind patterns within a storm. Weather Satellites: Satellite images provide weather information for regions where observations cannot be made from ground. The direction and speed of the wind at the level of the clouds can also be measured by examining a continuous sequence of cloud images. Satellite instruments can also measure marine conditions. Computers Solving very difficult mathematical equations Store weather data Can provide information that is useful in forecasting weather changes

5 Measuring Weather Continue

6 Measuring Climate Methods of Studying Past Climates Method What is measured What is indicated Length of time measured Ice Core Concentrations of gases in ice and melt water High levels of CO 2 indicate warmer climate; ice ages follow decreases in CO 2 Hundreds of thousand of years Sea-floor Sediment Concentration of 18 O in shells of microorganisms High 18 O levels indicate cool water; lower 18 O levels indicate warm water. Hundreds of thousand of years Fossils Pollen types, leaf shapes, and animal body adaptations Flower pollens and broad leaves indicate warm climates; evergreen pollens and small, waxy leaves indicate cool climates. Animal fossils show adaptations to climate changes. Millions of years Tree Rings Ring width Thin rings indicate cool weather and less precipitation Hundreds to thousands of years

7 Measuring Climate Continue Long term weather measurements Satellites Geological Evidence Evidence of glaciation Rock layers

8 Climate Graph

9 Creation of Wind that eventually leads to weather and climate.

10 Flashlight Mini Lab Flashlight Demo: Predictions: Which will have the most energy per given area, the 90 degree or the 30 degree angle flashlight? Hold the flashlight at 90 degree angle and about 10 inches above your paper Draw an outline around the beam Count the number of squares: Hold the flashlight at 30 degree angle and about 10 inches above your paper Draw an outline around the beam Count the number of squares: Which has the most energy per given area? 90 degree

11 Direct vs. Indirect Sunlight Sun gives off the same amount of radiation and stays the same temperature! The tilt of the Earth (23 ½ degrees) determines the concentration of the sun in a given area Small area = large concentration Big area = less concentration

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14 HOW DIRECT AND INDIRECT RELATES TO CLIMATES

15 Winter in Northern Hemisphere Tilted away from the Sun Cooler Temperatures = Cooler Climates Higher latitudes Sun s rays hit Earth at a smaller angle Solar energy is spread out over a larger area windows2universe.org

16 Summer in Northern Hemisphere Tilted towards the Sun Higher Temperatures = Warmer Climates Lower latitudes Sun s rays hit Earth around 90 degrees Solar energy is more direct, smaller areas windows2universe.org

17 HOW DIRECT AND INDIRECT RELATE TO WIND

18 Uneven Heating of the Earth Is warm air more or less dense the cold air? Less Dense If you have cold air at the poles and warm air at the equator where do you think each air mass will want to move and why? Cold air mass will move toward the warm air mass and the warm air mass will move toward the cold air mass because of convection. Convection: the movement of matter due to differences in the density that are caused by temperature variations; can result in the transfer of energy as heat. Convection currents/density currents The convection of air is a key piece in creating wind.

19 Atmospheric Pressure(Air Pressure) atmospheric pressure: the force per unit area that is exerted on a surface by the weight of the atmosphere decreases as altitude increases changes as a result of differences in temperature and in the amount of water vapor in the air

20 Atmospheric Pressure Continue

21 Atmospheric Pressure Continue

22 Pressure Gradient Uneven heating of the Earth s surface creates pressure gradients. Cause air to move form high pressure areas to low pressure areas creating wind mation/atmosphere/pressure_gradient.gif

23 THE WIND S PATH

24 Question Why doesn t the wind blow straight to the North and South pole from the equator? Rotation of the Earth, which we call the Coriolis Effect

25 Coriolis Effect Coriolis effect: the curving of the path of a moving object from an otherwise straight path due to Earth s rotation Circulation of atmosphere and ocean currents are effected. elated Hold the spherical device in your hand and rotate it counterclockwise (West to East) and look at it from the top. Which way is it rotating? counterclockwise Now keep rotating it counterclockwise (West to East) and look from the bottom, which why is it rotating? Clockwise

26 Coriolis Effect Continue

27 High and Low Pressure Wind High pressure winds move outwards Low pressure winds move inwards Both are curved because of the Coriolis Effect Directions

28 Cyclones and Anticyclones The hole column of air around a high or low pressure. Cyclones: when air moves into low areas it collides or converges. The collision causes the air to lifted and then diverge. Part of how storms are created Anticyclones: air converges towards the surface and then once it reaches the surface it is forced out (divergence) Nice weather

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30 Global Wind Patterns trade wind: Blow from east to west Latitudes 30º latitude to the equator in both hemispheres Westerlies: Blow from west to east between 30º and 60º latitude in both hemispheres descending air moving toward the poles is deflected by the Coriolis effect Polar easterlies: Blow from east to west between 60 and 90 latitude in both hemispheres Surface winds created by the polar high pressure are deflected by the Coriolis effect Each of the three types of winds are affected by the High and Low pressures Both winds and pressure zones have an impacted on determining climates around the global. Dry air Sinking Dry air Sinking Moist air rising Moist air rising Dry air Sinking Moist air rising Dry air Sinking

31 Jet Stream a narrow band of strong winds that blow in the upper troposphere These wind exist in the Northern and Southern Hemisphere. Subtropical jet stream. Polar jet streams: reach speeds of 500 km/h can affect airline routes and the paths of storms.

32 HOW OCEAN ARE EFFECTED BY WIND

33 How Global Winds Effect Ocean Surface Currents Trade winds cause the ocean currents to be pushed westward across the tropical latitudes of all three major oceans. Westerlies cause the ocean currents to be pushed eastward in the higher latitudes.

34 Coriolis Effect on Oceans Cause gyre Huge circle of moving ocean water found above and below the equator Northern hemisphere they move clockwise Southern hemisphere they move counterclockwise

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36 El Nino Trade wind either weaken or switch direction Cause upwelling to weaken or stop off the coast of South America and the fish die from heat and lack of nutrient from the upwelling process. Causes flooding in South America (Peru) and droughts in Indonesia and Australia. Mess up the weather for the rest of the Global.

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