Thermal

From Wikipedia, the free encyclopedia Thermal Thermal then said to be unstable. If there is a warm layer of air higher up, an inversion can prevent thermals from rising high and the air is said to be stable. Thermals on the Sun typically form hexagonal prisms (Bénard cells). Thermals are often indicated by the presence of visible cumulus clouds. When a steady wind is present thermals and their respective cumulus clouds can align in rows oriented with wind direction. Cumulus clouds formed by the rising air in a thermal as it cools and ascends, until the water vapor in the air begins to condense into visible droplets. The condensing water releases latent heat energy allowing the air to rise higher. Very unstable air can reach the level of free convection (LFC) and thus rise to great heights condensing large quantities of water and so forming showers or even thunderstorms. Thermals are one of the many sources of lift used by soaring birds and gliders to soar. A similar phenomenon can be seen in a lava lamp. Example of a thermal column between the ground and a cumulus A thermal column (or thermal) is a column of rising air in the lower altitudes of the Earth’s atmosphere. Thermals are created by the uneven heating of the Earth’s surface from solar radiation, and an example of convection. The Sun warms the ground, which in turn warms the air directly above it.[1] The warmer air expands, becoming less dense than the surrounding air mass. The mass of lighter air rises, and as it does, it cools due to its expansion at lower high-altitude pressures. It stops rising when it has cooled to the same temperature as the surrounding air. Associated with a thermal is a downward flow surrounding the thermal column. The downward moving exterior is caused by colder air being displaced at the top of the thermal. The size and strength of thermals are influenced by the properties of the lower atmosphere (the troposphere). Generally, when the air is cold, bubbles of warm air are formed by the ground heating the air above it and can rise like a hot air balloon. The air is External links • What do thermals look like? - Thermal Structure and Behavior by Wayne M. Angevine • Time-lapse video of clouds caused by thermals forming and decaying References [1] Bradbury, Tom (2000). Meteorology and Flight: Pilot’s Guide to Weather (Flying & Gliding). A & C Black. ISBN 0-7136-4226-2. Retrieved from "http://en.wikipedia.org/wiki/Thermal" Categories: Aviation terminology, Aeronautics, Weather, Convection This page was last modified on 18 May 2009, at 19:19 (UTC). All text is available under the terms of the GNU Free Documentation License. (See Copyrights for details.) Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a U.S. registered 501(c)(3) taxdeductible nonprofit charity. Privacy policy About Wikipedia Disclaimers 1