'Equal temperature' diaporamas de présentation

Mapping

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200

Clouds. Weather Terms I. Weather Terms II. Precipitation. Fronts and More. 100. 100. 100. 100. 100. 200. 200. 200. 200. 200. 300. 300. 300. 300. 300. 400. 400. 400. 400. 400. 500. 500. 500. 500. 500. Classroom-100 Answer. Cirro or cirrus clouds.

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Latitude and Longitude

572 views • 39 slides

Weather

557 views • 31 slides

Period 6 10/12/ 12

Period 6 10/12/ 12. 1. Attendance 2. Brainpop on weather 3 . New Notes - Weather 4 . Brainpop on the atmosphere 5. Lab # 8 Layers of the atm. Period 9 10/11/ 12. 1. Attendance 2. Test 3. Pass Back. Using your senses is called:. Observation.

375 views • 31 slides

Period 6 10/12/ 12

Period 6 10/12/ 12. 1. Attendance 2. Brainpop on weather 3 . New Notes - Weather 4 . Brainpop on the atmosphere 5. Lab # 8 Layers of the atm. Period 9 10/11/ 12. 1. Attendance 2. Test 3. Pass Back. Using your senses is called:. Observation.

313 views • 31 slides

Weather

427 views • 30 slides

Portraying the Earth

Portraying the Earth. Chapter 2. The Nature of Maps. How and why do we describe the earth using maps? When we need to understand the world around us we use maps.

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Chapter 3

Chapter 3. Water and the Environment. The Molecule That Supports All of Life. Can exist in 3 forms at once Main reason Earth is habitable Life on earth probably evolved in water Living organisms require water more than any other substance Most cells are surrounded by water

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Weather Maps

Weather Maps. Adapted from NOAA and www.metoffice.gov.uk/ by Ms. Shaw. Weather maps can graphically show either one feature, or multiple features of the weather. Isolines connect points of equal conditions on weather maps. Names of Isolines. Note the root words:

280 views • 7 slides

Graphical Weather Products

Graphical Weather Products. Chapter 9, Section D. Surface Analysis Chart. Surface Analysis chart is a good source for general information over a large area. Shows position of fronts, temperature, dewpoint, wind at valid time of the chart

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1. warmed. 2. cooled. 3. neither warmed nor cooled.

When evaporation of water occurs, the faster-moving (more energetic) water molecules escape the liquid and become molecules in the air. The average kinetic energy of molecules remaining in the liquid is lowered. The water is cooled. Normally, the air that receives the escaping molecules is.

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1. warmed. 2. cooled. 3. neither warmed nor cooled.

When evaporation of water occurs, the faster-moving (more energetic) water molecules escape the liquid and become molecules in the air. The average kinetic energy of molecules remaining in the liquid is lowered. The water is cooled. Normally, the air that receives the escaping molecules is.

42 views • 4 slides