Climate

1. Climate P. Lobosco

2. Chapter 17-1What is climate? • Objectives: • To describe what determines climate. • To explain how latitude, oceans and other factors affect the climate of a region.

3. What Causes Climate? • Climate is the name for the general conditions of temperature and precipitation for an area over a long period of time. • It determines the types of plants or animals that can survive and it influences how people live.

4. Factors that Affect Climate • Latitude • Large Bodies of Water • Ocean Currents • Mountains • Rain Shadows • Cities

5. Latitude • Latitude is the measure of the distance north and south of the equator. Latitude is measured in degrees. Areas close to the equator, or 0 degrees latitude, receive the direct rays of the sun. These direct rays provide the most radiant energy. Areas near the equator have a warm climate. Polar regions have a cold climate.

6. Latitude Zones • The tropics extend from the equator to 23.5º north and south. They receive the most direct solar radiation. • The temperate zones extend from 23.5º to 66.5. These areas receive moderate amounts of solar radiation. • The polar zones from 66.5 º to the Poles receive very little solar radiation.

7. Tropical Zones • The tropical zones, which extend from 23.5º north and south latitude to the equator, have high temperatures and high humidity. Tropical zones are also known as low-latitude climates. The average temperature during the coldest month of the year does not fall below 18 degrees C. Many deserts are located on the western coasts of the continents. This is because the prevailing winds, the trades, blow from east to west.

8. Temperate Zones • In each hemisphere, the temperate zone is found between 66.5ºand 23.5º latitude. In the areas of the temperate zones farther from the equator, snow is common in the winter. • In the areas of the temperate zones closer to the equator, rain normally falls all year round. The average amount of precipitation is about the same throughout. The average temperatures range from 5 º C to 20 ºC.

9. Deserts in the Temperate Zone • Deserts in the temperate zones are usually located in land, far away from the oceans. The winds that blow across these inland deserts carry little moisture. • Although very hot during the day, temperatures at night can drop to below freezing. Inland deserts are found in Australia (the Great Sandy Desert) and Central Asia ( the Gobi Desert).

10. Polar Zones • In each hemisphere, the polar zone extends from the pole to about 60 degrees latitude. In polar zones, the average yearly temperature is below freezing. There are some areas in the polar zones, such as the northern coasts of Canada and Alaska and the southern tip of South America, where the snow melts during the warmest part of the year.

11. Large Bodies of Water • The surface temperature of water affects the temperature of the water above it. Warm water warms the air and cold water tends to cool it.

12. Marine and Continental Climates • Within each of the three major climate zones, there are marine and continental climates. Areas near an ocean or other large body of water have a marine climate. Areas located within a large landmass have a continental climate. • Areas with a marine climate receive more precipitation and have more moderate temperatures. A continental climate has less precipitation and a greater range in temperature.

13. Ocean Currents • Land areas near warm ocean currents have warm temperatures. • The Gulf Stream is an ocean current that carries warm water along the eastern coast of the United States. • The California Current travels toward the equator carrying cold water along the west coast of the United States.

14. Elevation • Elevation, or altitude, is the distance above sea level. As elevation increases, the air becomes less dense. This means there are fewer gas molecules in the air and they are spread far apart. Less- dense air cannot hold as much heat as denser air. So as elevation increases, temperature decreases.

15. Rain Shadows • Mountains also affect regional climates. • On the windward side of a mountain range air rises and cold, and drops its moisture. • On the leeward side the dry air descends and dries the land. • Deserts are common on the leeward side of the mountain ranges.

16. Cities • Large cities affect local climate. • Streets, parking lots and building heat up and in turn, heat the air. • Air pollution heats up traps the heat, creating the heat-island effect. • Temperatures are at least 5º higher than the surrounding areas.

17. Chapter 17-2Climate Types • Objectives: • To describe a climate classification system. • To explain how organisms adapt to a particular climate.

18. Koppen Classification • Koppen classified world climates by using the annual and monthly averages of temperature and precipitation. • He then related the types and distribution of native vegetation to the various climates. • It separates into six groups, tropical, mild, dry, continental, polar and high elevation.

19. Classifying Climate

20. Adaptations • The climate determines the vegetation in the area. • Organisms adapt to their environment. • An adaptation is any structure or behavior that helps an organism survive its environment. • Structural adaptations are inherited and develop in a population over a long period of time.

21. Structural Adaptation • Some organisms have body structures that help them certain in climates. • The fur of mammals is really hair that insulates against the cold. • Cacti have a thick, fleshy stem that hold water, • Cacti also have spiny needles that also reduce water loss.

22. Behavioral Adaptations • Some behaviors help organisms survive in certain climates. • Rodents and certain mammals undergo a period of decreased activity called hibernation. • They have a lower body temperature and lowered body processes.

23. Other Behavioral Adaptations • Bees huddle together during cold weather. • On hot days, snakes hide under rocks. • Desert turtles and lizards obtain water from their food.

24. Estivation • Lungfish survive periods of intense heat by entering an inactive state called estivation. • As the weather gets hot and water evaporates, the fish will burrow into mud and cover itseld in mucus and mud and wait until the weather improves.

25. Human Behavioral Adaptations • Humans also exhibit behavioral adaptations. • We shiver when we are cold because the rapid muscle movement produces heat. • We sweat when we a re hot because as the water evaporates, it takes some heat with it.

26. Chapter 17-3Climatic Changes • Objectives: • Explain what causes seasons • Describe how EL Nino affects climate • Explore the possible causes of climatic change.

27. Seasons • Seasons are short periods of climatic change. • Because the Earth is tilted, certain areas of Earth receive changing amounts of radiation throughout the year.

28. High Latitudes • During the year, the high latitudes near the poles have great differences in temperature and daylight hours.

29. Short Term Changes in Climate • Some short-term changes may be the result of changes in ocean currents and global winds. • Ocean currents help transfer heat to the atmosphere. This process generates global winds. The global winds help move ocean currents. • Any major change in an ocean current can cause a change in climate. El Nino is an example.

30. Peru Current • A cold current that flows from west to east across the southern part of the Pacific Ocean turns toward the equator along the coast of South America and flows north along the coast of Chile and Peru. It is known as the Peru Current.

31. El Nino • Occasionally the Peru Current is covered by a thin sheet of warm water. Every 2 to 10 years, strong winds spread the warm water over a large area resulting in droughts in some areas and flooding in others.

32. La Nina • The opposite of el Nino is La Nina. • During La Nina, the winds blowing across the Pacific are stronger than normal and warm water accumulates in the western Pacific. The water near Peru is colder. • This causes droughts in the southern United states and excess rainfall in the northwestern Untied States.

33. Changes in Climate • The natural factors responsible for long term climate changes are the slow drifting of the continents, changes in the sun’s energy output , natural catastrophic events and variations in the position of the Earth relative to the sun. • These natural factors are not related to human activity. The results of the human activity of the burning of fossil fuels may also lead to changes in climate.

34. Variations in Radiant Energy • During periods of high energy output, the Earth’s temperature would rise. The temperature would drop during periods of low energy output. • Scientists have found a link between sunspots activity and climate change. During very cold periods there are very few sunspots.

35. Catastrophic Events • Catastrophic events such as meteorite collisions and volcanic eruptions can put tremendous amount of dust ash and other particles into the atmosphere. • This in turn blocks sunlight and cools the planet. • Cities can also put up pollution that increases cloud cover downwind from the city. It also reduces rainfall in these areas.

36. Changes in Earth Movement in Space • The shape of the Earth’s orbit can change. Sometimes it is more circular, sometimes more elliptical. • The Earth’s tilt has varied from 21.5º to 24.5º. The tilt changes about every 41,000 years. • The Earth’s axis also wobbles like a top.

37. Ice Ages • Periods when much of the Earth’s surface has been covered with enormous sheets of ice are called ice ages or major glaciations. • Scientists have found evidence of four major ice ages during the last 2 million years each lasting between 60,000-100,000 years. The average temperature was 10-15ºC. • The causes are not known but they are probably associated with variations in the tilt of the Earth’s axis and/or the shape of the Earth’s orbit around the sun.

38. Interglacials • Interglacials are the time periods between major glaciations. Interglacials are warm periods. During an interglacial, the average temperature was about 4 to 6 degrees higher than the average temperature during a major glaciation. A cold period called the Little Ice Age lasted from 1500 to 1900.

39. Drifting Continents • About 230 million years ago, all the Earth’s landmasses were joined in one super continent, Pangaea. As the continents moved toward their present-day locations, the sea level dropped, volcanoes erupted, and much of the Earth’s surface was pushed upward. The combined effect was a drop in temperature and precipitation all over the Earth. These changes were gradual.

40. Extinction of the Dinosaurs • The climate change caused by the drifting of the continents may have resulted in the extinction of the dinosaur. Many types of plants also became extinct. Dinosaurs that depended on these plants died. Meat-eating dinosaurs that depended on plant-eating dinosaurs died. Other scientists believe that dinosaurs became extinct as the result of a giant asteroid striking the Earth 65 million years ago.

41. Greenhouse • The greenhouse effect is a natural process that occurs when certain gases in Earth’s atmosphere trap heat and serve to warm the earth. • When the Earth’s climate changes, the amount of carbon dioxide that cycles among the atmosphere, ocean and land can also change. • Greenhouse gases include water vapor, carbon dioxide and methane.

42. Global Warming • In the mid-nineteenth century industrialization led to the increased burning of fossil fuels, including coal, oil and natural gas. Then these fuels are burned they release carbon dioxide that traps heat. Carbon dioxide has increased by 20% in the last 100 years. As a result, the atmosphere becomes warmer, increasing 0.6º C in the last 100 years. • Deforestation may also contributes to global warming.

43. Carbon Cycle