Tuesday, November 27, 2012

Summary- Atmosphere Power Point

Solar energy as radiation is nearly 150 million kilometers separate the sun and earth and it drives earth’s weather. Earth’s atmosphere is 99% atmospheric gases, including water vapor, extend only 30 kilometers (km) above earth’s surface. Atmosphere gases include nitrogen, oxygen, argon, water vapor, and carbon dioxide are invisible. Variable and increasing gases; nitrogen and oxygen concentrations experience little change but carbon dioxide methane and oxides of nitrogen are greenhouse gases experiencing increasing in concentrations C02 have raised more than 18%. Atmospheric Greenhouse affects the warming of the atmosphere by absorbing and emitting infrared radiation and allowing shortwave infrared radiation to pass through. The main gases responsible for the greenhouse effect are water vapor and carbon dioxide. Aerosols are human and natural activities displace tiny soil salt and ash particles as suspended aerosols. Pollution are sulfur and nitrogen oxides, and hydrocarbons are emitted as pollution. Lapse rate is the rate at which air temperature decreases with height. In average lapse rate in the lower atmosphere is about 6.5 degrees (*) per 1 km or 3.6 *f per 1000ft. Urban heat island effect occurs when a metropolitan area is warmer than the surrounding rural areas. UHI effect is caused primarily by modification of land surfaces in developments that use materials that retain heat. The cloud triangle: Clouds can be defined by: Their shape & form: The cloud base altitude: If they are precipitating. Air pressure: Warm air-expanding or rising: Air-leaves behind L pressure: Cold air-sinking air=leaves an H pressure. Wind movement uneven heat of the earth’s surface causes some areas to be warmer than others.  Warm always follows cold to share its warmth- when this happens in the atmosphere, wind happens. Pressure, wind and weather, the winds are horizontal flows of air; winds blow from areas of high pressure to areas of low pressure. Pressure describes the tendency of the air to rise or to sink at any given place or time. Humidity measure of the amount of water vapor stuck between molecules in the air and the airs ability to hold water depends on the air temperature. Relative humidity amount of water vapor (%) compared to the amount the air can hold and 100%= air is saturated.