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Water in the Atmosphere

Water in the Atmosphere

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Water in the Atmosphere

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  1. Water in the Atmosphere

  2. The Water Cycle

  3. The Water Cycle • The movement of water between the atmosphere and Earth’s surface is called the water cycle. • Three steps of the water cycle: • Evaporation • Condensation • Precipitation

  4. How Does the Water Cycle Work? • Density makes the water cycle work. • Water is more dense than air in its liquid form so it collects together via gravity into bodies of water such as the oceans and lakes etc. • As it is heated by the sun (driving energy source) and evaporates, it becomes a gas and that gas is less dense than air. • As it rises to very high altitudes in the troposphere, it cools due to lower temperatures and becomes more dense than air again. • Once enough water vapor has condensed into clouds and the clouds move away from the source of water, the water vapor will eventually condense enough that the cloud is more dense than the air. • Precipitation will fall in the form of rain, sleet, snow or hail.

  5. Density of Air in the Atmosphere

  6. Phase Change Diagram Review

  7. Evaporation • Evaporation is the process by which water molecules in liquid water escape into the air as water vapor. • Water molecules. • Water molecules i a liquid state are more dense than air. • When water is heated by the sun, the liquid moves faster and becomes less dense causing it to rise into the atmosphere.

  8. Examples of Evaporation • Humidity-the measure of the amount of water vapor in the air • Humidity depends upon temperature.

  9. Examples of Evaporation • Relative Humidity-the percentage of water vapor that is actually in the air compared to the maximum amount of water vapor the air can hold. • Warm air is less dense and can “hold” more water than cold air that is more dense. Warm air has more space to fit water vapor Cold air has less space to fit water vapor

  10. Measuring Relative Humidity • Psychrometer-Instrument used to measure relative humidity • Made of 2 thermometers • Wet-bulb thermometer • Dry-bulb thermometer

  11. Measuring Relative Humidity • Wet-bulb thermometer-bulb has a cloth covering that is moistened with water • Psychrometer is spun by the handle and air blows over both thermometers • Wet-bulb thermometer is cooled by evaporation • Compare readings on the two thermometers

  12. How to Determine Relative Humidity • Measure the dry bulb temperature. • Measure the wet bulb temperature. • Calculate the difference between the dry bulb and wet bulb temperatures. • Find the dry bulb temperature on the table. • Find the difference between the wet and dry bulb temperatures on the table. • The relative humidity will be at the intersection of the row and column.

  13. Relative Humidity Table Examples • Example #1: • Suppose the relative humidity of the air is 51% and the reading of the dry-bulb thermometer is 200C. What is the reading of the wet-bulb thermometer? • Answer: 14 oC

  14. Relative Humidity Table Examples • Example #2: • The readings on a sling psychrometer are 14 0C for the dry-bulb thermometer and 12 0C for the wet-bulb thermometer. What is the relative humidity? • Answer: 79%

  15. Example of Evaporation • Sweatis your body’s natural way of cooling down. • When sweat reaches the surface of our skin, it then evaporates, which cools us down! • Heat is transferred from your skin to the water which makes you feel cooler.

  16. Example of Evaporation • Outdoor drying: When you hang socks outside to dry, you're using energy from the Sun and the wind to evaporate and disperse the water they contain.

  17. Condensation Condensation

  18. Condensation • As warm, moist air rises in the atmosphere, its temperature begins to decrease. • Molecules of water vapor in the air become liquid water in the process of condensation.

  19. How Clouds Form • Clouds form when water vapor in the air condenses to form liquid water or ice crystals • Two conditions required for condensation: • Cooling of the air • Presence of particles in the air

  20. The Role of Cooling • Cold air holds less water vapor than warm air • Dew Point-the temperature at which condensation begins • Dew point abovefreezing=water vapor forms water droplets • Dew point below freezing=water vapor may change into ice crystals

  21. Dew Point and Humidity • The higher the dew point, the more moisture in the air • Example: Key West, Florida has high dew points so it feels “sticky” or humid • The lower the dew point, the less moisture in the air • Example: Death Valley, California has low dew points so it feels dry

  22. The Role of Particles • For water vapor to condense, tiny particles must be present so the water has a surface on which to condense • In cloud formation, most of these particles are salt crystals, dust from soil, and smoke • Water vapor also condenses onto solid surfaces, such as blades of grass or window panes

  23. The Role of Particles continued • Liquid water that condenses from the air onto a cooler surface is called dew • Ice that has been deposited on a surface that is below freezing is called frost

  24. Fog • Clouds are classified by their shape and their altitude • Different types of clouds are associated with different types of weather • Clouds that form at or near the ground are called fog • Fog often forms when the ground cools at night after a warm, humid day • The ground cools the air just above the ground to the air’s dew point • The next day the heat of the morning sun “burns” the fog off as its water droplets evaporate

  25. Cloud Seeding • During drought conditions, a method called cloudseeding is used to produce precipitation. • Tiny crystals of silveriodide and dryice are sprinkled into clouds from airplanes. • Water vapor can condense on the particles of silver iodide and dry ice cools the water vapor from the air. • As a result, clouds form.

  26. Precipitation • Precipitation is any form of water that falls from clouds and reaches Earth’s surface • Not all clouds produce precipitation • For precipitation to occur, cloud droplets or ice crystals must grown dense enough to fall through the air

  27. Types of Precipitation • Common types of precipitation include: • Rain • Sleet • Freezing rain • Snow • Hail

  28. Rain • Most common form of precipitation • Drops of water 0.5 mm in diameter • Drizzle-drops of water less than 0.5 mm • Mist- drops of water smaller than drizzle

  29. Sleet • Raindrops fall through a layer of air that is below 0oC • Ice particles smaller than 5 mm in diameter

  30. Freezing Rain • Raindrops falling through cold air near the ground do not freeze in the air, instead they freeze on a cold surface

  31. Snow • Water vapor in a cloud that is converted directly to ice crystals is called a snowflake

  32. Hail • Round pellets of ice larger than 5 mm in diameter • Form during thunderstorms • Difference between sleet and hail is the size of the ice pellets and where the ice pellets formed

  33. Measuring Precipitation • Rain gauges- open-ended can or tube that collects rainfall • The amount of rainfall is measured by dipping a ruler into the water or by reading a marked scale • Measuring sticks