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Environmental Science 11/10/14

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Presentation on theme: "Environmental Science 11/10/14"— Presentation transcript:

1 Environmental Science 11/10/14
SEV3a: Explain how abiotic factors affect natural fluctuations in ecosystems Environmental Science /10/14 ES: What is the difference between weather and climate? Warm up: Draw and label picture of earth on pg 353; Label trade winds, easterlies, westerlies, Arctic, Antarctic, Equator; draw and label the picture of sun’s rays striking earth, pg 352. Classwork: Notes on weather and climate

2 Environmental Science 11/11/14
SEV3a: Explain how abiotic factors affect natural fluctuations in ecosystems Environmental Science /11/14 ES: What is the difference between weather and climate? Warm up: Draw and label the 4 seasons diagram on page 358 and the rain shadow effect diagram on page 357. Classwork: Finish the notes on weather and climate; Closing: quick quiz on weather and climate

3 Environmental Science 11/12/14
SEV3a: Explain how abiotic factors affect natural fluctuations in ecosystems Environmental Science /12/14 ES: What evidence is there of climate change? Warm up: video Classwork: Climate web quest: go to South Paulding home page-teacher websites-Cook-Environmental – Climate Web quest-click on blue link-follow instructions on worksheet-due today Closing: Write a summary explaining global warming, the evidence of global warming, green house gases, and how humans have affected this process.

4 Objectives Explain the difference between weather and climate.
Identify four factors that determine climate. Explain why different parts of the Earth have different climates. Explain what causes the seasons

5 Climate Weather is the day to day temperature and precipitation in an area. Climate is the average weather conditions in an area over a long period of time.

6 Climate is determined by a variety of factors that include latitude, atmospheric circulation patterns, oceanic circulation patterns, the local geography of an area, solar activity, and volcanic activity. The most important of these factors is Latitude distance from the equator.

7 Latitude Latitude is the distance north or south from the equator and is expressed in degrees. The area between 0 and 30 degrees N and S is Tropical The area between 30 and 60 degrees N and S is Temperate, with seasons The area between 60 and 90 degrees N is Arctic and S is Antarctic

8 Low and High Latitudes

9 Latitude strongly affects climate because the amount of sunlight an area of the Earth receives depends on the type of rays that strike the location. More solar energy falls on areas near the equator than on areas closer to the poles.

10 Low Latitudes In regions near the equator, night and day are both about 12 hours long throughout the year; temperatures are high year-round, and there are no summers or winters. In regions closer the poles, the sun is lower in the sky, reducing the amount of energy arriving at the surface. In the northern and southern latitudes, sunlight hits the Earth at an angle and spreads over a larger surface area than it does at the equator.

11 High Latitudes At 45° north and south latitude, there is as much as 16 hours of daylight each day during the summer and as little as 8 hours of sunlight each day in the winter. Near the poles, the sun sets for only a few hours each day during the summer and rises for only a few hours each day during the winter. Thus, the yearly temperature range near the poles is very large.

12 Atmospheric Circulation
Three important properties of air illustrate how air circulation affects climate. Cold air sinks because it is denser than warm air. As the air sinks, it compresses and warms. Warm air rises. It expands and cools as it rises. Warm air can hold more water vapor than cold air can. when warm air cools, it condenses into liquid water to form rain, snow, or fog.

13 Atmospheric Circulation

14 Prevailing Winds Winds that blow predominantly in one direction throughout the year are called prevailing winds. The trade winds blow from the northeast in the Northern Hemisphere and from the southeast in the Southern Hemisphere.

15 Prevailing Winds In the Northern Hemisphere, westerlies are southwest winds, and in the Southern Hemisphere, these winds are northwest winds. The polar easterlies blow from the poles to 60º north and south latitude.

16 Oceanic Circulation Ocean surface currents redistribute warm and cool masses of water around the world and in doing so, they affect the climate in many parts of the world.

17 El Niño–Southern Oscillation
El Niño is the warm phase of the El Niño–Southern Oscillation. It is the periodic occurrence in the eastern Pacific Ocean in which the surface-water temperature becomes unusually warm. Rainfall follows this warm water eastward and produces increased rainfall in the southern half on the U.S., but drought in Australia.

18 El Niño–Southern Oscillation
La Niña is the cool phase of the El Niño–Southern oscillation. It is the periodic occurrence in the eastern Pacific Ocean in which the surface water temperature becomes unusually cool. This cool water creates drought in the Southern US and excessive rainfall in Australia El Niño and La Niña are opposite phases of the El Niño–Southern Oscillation (ENSO) cycle.

19 Pacific Decadal Oscillation
The Pacific Decadal Oscillation (PDO) is a long-term, 20 to 30 year change in the location of warm and cold water masses in the Pacific Ocean. PDO influences the climate in the northern Pacific Ocean and North America. It affects ocean surface temperatures, air temperatures, and precipitation patterns.

20 Topography Height above sea level (elevation) has an important effect on climate. Temperatures fall by about 6°C (about 11°F) for every 1,000 m increase in elevation. Mountain ranges also influence the distribution of precipitation. For example, warm air from the ocean blows east, hits the mountains, and rises. As the air rises, it cools, causing it to rain on the western side of the mountain. When the air reaches the eastern side of the mountain it is dry. This effect is known as a rain shadow.

21 Topography

22 Seasonal Changes in Climate
The seasons result from the tilt of the Earth’s axis, which is about 23.5° relative to the plane of its orbit. Because of this tilt the angle at which the sun’s rays strike the Earth changes as the Earth moves around the sun.

23 Seasonal Changes in Climate

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