Weather Dynamics

1. Weather Dynamics

2. A Closer Look at Earth Section 13.1

3. The main components of Earth that influence weather are: • the atmosphere • land forms • water in various forms (solid, liquid, gas) • Earth’s surface area: • 70% covered by oceans • 30% forms continents

4. Weather vs. Climate • Weather: a set of environmental conditions encountered from day to day. • Today’s weather: sunny with a few clouds, -17 C, wind chill - 30 C, Winds from the West at 37 km/h. • Climate: a set of environmental conditions averaged over many years. • PEI’s climate in February: crisp and clean, temperature ranges from -3 to -11 C.

5. Assignment: • Read pages 500-503 and do questions 1-4 & 9 on page 503. • Accuracy of Advanced Weather Forecasts (handout) • Use the following website to do the “Weather Assignment”: http://www.weatheroffice.gc.ca/canada_e.html

6. Earth’s Energy Balance Section 13.2

7. There are four methods of energy transfer that help to maintain the Earth’s energy balance as well as distribute energy around the world. They all contribute to weather. • Radiation: transfer of energy by means of waves. • These waves are measured using the electromagnetic spectrum. • Conduction: transfer of energy through the collision of particles. • Occurs in metals (steel), rock, sand, soil and water. • Convection: vertical transfer of energy by the movement of particles in a fluid (liquid or gas). • Advection: horizontal transfer of energy by the movement of particles in a fluid (liquid or gas).

8. How does Earth receive energy through radiation? The Electromagnetic Spectrum – shows all types of radiation that can travel through space at the speed of light.

10. Reflection and Absorption of Energy • Energy from the Sun that reaches the Earth will undergo one of the following: • 27% is reflected off the atmosphere and clouds back into space. • 3 % passes through the atmosphere and bounce off the Earth’s surface and back into the atmosphere. • 20% is absorbed by the atmosphere. • 50% is absorbed by the ground or water at the surface.

11. The energy that is reflected back off the surfaces of the Earth depends on the albedo of the material. • Albedo: a percentage of light that an object reflects. • High albedo - reflects a lot of light (Eg. white snow). • Low albedo - reflects very little light (Eg. black soil). • An object which absorbs energy and becomes warmer is called a heat sink. • Good heat sinks: oceans and lakes. • Poor heat sinks: soil and rocks. • Heat Capacity: how much heat a substance requires to increase its temperature, or how much heat it releases as its temperature decreases. • high heat capacity: water (holds a lot of heat). • low heat capacity: soil and rocks.

12. Assignments: • Read pages 504-506 and do questions 1-10 on page 507. • How Much Do You Know? (handout BLM 13.2). • Video Response: Understanding Weather Concepts

13. The Hydrosphere Section 13.8

14. The Hydrosphere • All of Earth’s fresh and salt water. The Water Cycle • Water in our atmosphere is present in 3 states: liquid, vapour (gas) and solid. The energy from the Sun helps circulate this water and create our weather. • Water is essential for humans. People settle themselves near bodies of water (rivers, lakes, oceans) as they serve as a source of food, drinking water, and transportation. Weather systems near bodies of water affect a large number of people.

15. Water Distribution in the Hydrosphere 10% of the world’s fresh water supply is located in Canada.

16. Key Terms • Evaporation • changing from liquid to gas. • Sublimation • changing directly from solid to a gas. • Condensation • changing from gas to liquid. • Transpiration • movement of water from plants and bodies to the air. • Precipitation • water that falls to the ground (rain, snow, hail, dew, freezing rain, etc.)

17. Condensation Sublimation Transpiration Evaporation Precipitation

18. Assignment: • Read pages 522-524 and do questions 2, 3 & 4. Water Cycle Video

19. Clouds and Fog pages 530-534

20. The water cycle shows us that energy from the sun and surrounding environment cause water particles to heat up and turn to water vapour. • These particles rise in the less dense air until they reach lower temperatures in higher altitudes and lower pressure. • This is the formation of water droplets that are very small. Only when thousands of these droplets join together does a raindrop form which is carried to earth through precipitation.

21. Clouds are natures indicators of weather conditions and weather patterns. • Understanding the characteristics of clouds helps to predict the weather.

22. Cloud Formation is classified into three main categories: • Convective Clouds • Are produced when air near the ground absorbs energy from heated surfaces such as oceans, lakes, asphalt, concrete and dirt. • Frontal Clouds • Form when a front or large moving air mass meets another air mass of a different temperature. Warm air masses are usually less dense and contain more water vapour and will rise above the cold air mass. Clouds form due to the moisture cooling and condensing. • Orographic Clouds Form when air moves up a mountain, expands at the lower pressure and cools/condenses. • http://www.curriculumbits.com/prodimages/details/geography/rainfall.swf

23. Frontal Clouds

24. Animation

25. FOG • Fog is a cloud that forms near the ground. • The most common is produced on clear nights when the absence of clouds keeps the energy from the Earth from being reflected or kept near the surface. The air near the ground cools and water vapour turns to fog. • Fog also happens when warm air passes over snow-covered land, when moist sea air drifts over a seashore or a cold current, or when moist air rises up the mountains during the orographic lift.

26. Section 13.11 Classifying Clouds A. Clouds are classified using two general shapes: • Cumulus Clouds – meaning “heap” which have a billowing rounded shape. They tend to grow vertically and often indicate unstable weather. • They tend to form as a result of: • Convection currents • Cold air pushing into warm air masses. • Orographic lifting • Stratus Clouds – meaning “spread out” which have a layered, flat shape. They tend to grow horizontally and often indicate stable weather. • They form when: • Warm air takes over a cold air mass.

27. B. Clouds are classified by their height (altitude) in the atmosphere. • Low-level clouds keep their simple names. • Example: Cummulus or Stratus • Medium-level clouds start with the prefix alto (which means higher) • Example: Altostratus • High-level clouds start with the prefix cirrus (which means curly lock of hair) • Example: Cirrostratus C. Clouds are subclassified by whether or not they hold rain. • True rain clouds are called nimbus clouds. • Example: Nimbostratus

28. There are 10 major classifications of clouds. • Use your textbook to answer the rest of the sheet (handout). • Water Cycle and Clouds Song

30. cirrus cirro-stratus

31. Assignment: Questions • 1. Describe the three main ways that clouds form? • 2. Why doesn’t rain or snow fall from all clouds? Read pages 522-524 and answer questions 1, 3, 4, and 5 on page 534. Handout: *Rain or Shine Quiz/Clouds and Precipitation

32. North American Weather Systems Section 14.2

33. A weather system is a set of temperature, wind, pressure, and moisture conditions for a certain region that moves as a unit for a period of days. • An air mass is a large body of air that has the same temperature and moisture throughout.

34. North America is affected by four major types of air masses: • Maritime Polar • These air masses come from the Pacific and Atlantic Ocean and bring: • fog and cooler temperatures in the summer. • heavy snow and very cold temperatures in the winter. • Continental Polar • These air masses come from the North and bring: • cold, dry air in both summer and winter. • Maritime Tropical • These air masses come from the Pacific and Atlantic Ocean and bring: • warm, moist air in the summer • rain or snow in the winter • Continental Tropical • These air masses come from over Mexico and bring: • hot, dry air in the summer

36. These air masses help keep the balance of Earth’s energy. Convection and dominant winds move warm air northward, and cold air southward. When these air masses meet, they create interesting and unpredictable weather. • When two air masses meet, the differences in temperature and humidity cause a boundary, or front, to form between them. The weather at a front is usually stormy and unsettled.

37. Four Kinds of Fronts: Cold Front • forms when a cold air mass moves under a warm air mass • violent storms, followed by fair, cool weather. Warm Front • forms when warm air moves up and over a cold air mass • rain showers followed by hot, humid weather. Occluded Front (Cut Off) • forms when a fast moving cold air mass catches up with a slow moving air mass • weakens the weather caused by cold or warm fronts. Stationary Front • forms when 2 slow moving air masses collide • long periods of rain or other precipitation that lasts for days.

41. Assignment: • Read pages 546-548 and do questions 1-3.

42. Chapter 15 Extreme Weather Events Section 15.2 Weather in the News • Watch - conditions are present for extreme weather to occur in your area. • Advisory - severe weather, likely to cause local problems and inconveniences, is predicted for your area. • Warning - extreme weather is highly likely to arrive in your area or may already be happening. Take necessary precautions.

43. Thunderstorms and Tornadoes Section 15.3 http://news.bbc.co.uk/2/hi/5328524.stm

44. Thunderstorm • a storm with lightening, thunder, heavy rain, and sometimes hail. • In order for a thunderstorm to occur you need: • Moisture to form clouds and precipitation • Very strong lifting of air (uplift) to produce clouds which reach high in the atmosphere. • Thunderstorms form in 3 stages:

45. Cummulus Stage • The sun warms the surface of the Earth and the air. This warm air rises in an updraft. This air will condense into a cumulus cloud, which will continue to grow as long as there is warm air rising below it.

46. Mature Stage • When the cumulus cloud is very large it starts to rain. Also cool air starts to enter the cloud. Because this air is heavier it starts to descend in a downdraft pulling lots of water with it. The updraft and downdraft cause thunder, lightening and heavy rain.

47. Dissipating Stage • After a while the downdrafts in the cloud dominates the updrafts stopping water drops from forming. The storm begins to die out with light rain. * This process normally last about 1 hour.

48. Lightning occurs when clouds become positively charged at the top and negatively charged at the bottom. The charge builds up until it is strong enough to cause lightning. • To protect yourself: • Stay in a car • Avoid open areas like fields, open water, tops of hills. • Never stand near or under a tree, or utility pole

49. Tornado • a severe component of a thunderstorm in which a rotating funnel of air extends from the base of a thunderstorm cloud to the ground. • http://esminfo.prenhall.com/science/geoanimations/animations/Tornadoes.html

50. In order for a Tornado to occur you need: • Fast rising air in a thunderstorm sometimes begins spinning, forming a funnel of air and moisture. As more rising air is replaced by cooler air at the surface, the rotation becomes faster and faster. This rising air causes a pressure difference that increases speed. • Because of its shape, the rotating tornado is called a funnel cloud. • At the centre, the wind speeds can be as high as 500 km/h.