'Temperature inversions' presentation slideshows

Meteorological Concepts for Soaring in the Western U.S.

Meteorological Concepts for Soaring in the Western U.S. Dan Gudgel Meteorologist/Towpilot/CFIG Presentation Points Weather Information Sources Meteorology Points Synoptic Scale Weather Patterns A Forecast Funnel Miscellaneous Info 1. Weather Information Sources Weather Data

1.56k views • 97 slides

WEATHER FRONTS AND AIR MASSES

WEATHER FRONTS AND AIR MASSES. Take notes as you go. These notes can be used to study for our next quiz. Ms. Augustyn - Mr. Swerin Sandpoint Middle School Lake Pend Oreille School District. Weather Fronts.

1.48k views • 47 slides

Propagation of Waves

Propagation of Waves. Ham Radio Class Week 5. Propagation of waves. Radio waves spread out from the antenna in straight lines (like light). The farther it travels the weaker it becomes, eventually becoming too weak to be received. The distance over which a transmission can be received is

1.05k views • 46 slides

LEADS Cross Sections Construction and Examples

LEADS Cross Sections Construction and Examples. Captain Brian Yates Training Flight Commander 25 th Operational Weather Squadron 22 April 2010. Outline. Introduction Basic concept review Cross Section Conceptual Model Cross Section Generation and Pattern Recognition Cold Fronts

602 views • 42 slides

Jun Li @ , Hui Liu # , Jinlong Li @ , and Tim Schmit &

Using water vapor measurements from hyperspectral advanced IR sounder (AIRS) for tropical cyclone forecast . Jun Li @ , Hui Liu # , Jinlong Li @ , and Tim Schmit &. UW-Madison. Impact of Satellite Data. 2007 ECMWF Numerical Weather forecasting system.

465 views • 31 slides

Air Pollution

Air Pollution. Indoor/Outdoor. The Atmosphere. Troposphere. 78% N, 21% O. Stratosphere. Ozone layer. Greenhouse effect. Outdoor Air Pollution. airborne particles and gasses concentrations that endanger: heath and well-being of organisms

327 views • 24 slides

Killer Smog

468 views • 16 slides

STEM-4 TH TERESA PUGMIRE/LINDA TYRRELL

STEM-4 TH TERESA PUGMIRE/LINDA TYRRELL. INVERSION AVERSION. COLD AIR IS HEAVIER. Cold air sinks because it is more dense, which means molecules are closer to together so there are more molecules in a space than molecules of warm air. . WARM AIR IS LIGHTER.

210 views • 13 slides

Temperature Inversions in Alaska ITEP Air Quality Training Lower Kalskag 2014

Temperature Inversions in Alaska ITEP Air Quality Training Lower Kalskag 2014. Barbara Trost/Bob Morgan Alaska Department of Environmental Conservation. Normal Conditions. Warm air rises | cold air sinks Temperature decreases as you go higher in atmosphere Warmer near ground, colder aloft

204 views • 8 slides

Smog

1.16k views • 8 slides