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*Earth & Space Science - Ch.13 "The Nature of Storms" Games

AB
air-mass thunderstormtype of thunderstorm in which air rises because of unequal heating of Earth's surface within a single air mass and is most common during the afternoon and evening.
mountain thunderstormoccurs when an air mass rises from orographic lifting, which involves air moving up the side of a mountain
sea-breeze thunderstormlocal air-mass thunderstorm that commonly occurs along a coastal area because land and water store and release thermal energy diffferently
frontal thunderstormtype of thunderstorm usually produced by an advancing cold front, which can result in a line of thunderstorms hundreds of kilometers long, or, more rarely, an advancing warm front, which can result in a relatively mild thunderstorm
stepped leaderThe channel of partially charged air; the breakdown in charges in between positive and negative regions
return strokea branch channel of positively charged ions that rushes upward from the ground to meet the stepped leader
supercellextremely powerful, self-sustaining thunderstorm characterized by intense, rotating updrafts
downburstviolent downdrafts that are concentrated in a local area
tornadoviolent, whirling column of air in contact with the ground that forms when wind direction and speed suddenly change with height, is often associated with a supercell, and can be extremely damaging
Fujita tornado intensity scaleclassifies tornadoes according to the wind speed, duration, and path of destruction on a scale ranging from F0 to F5
tropical cyclonelarge, low-pressure, rotating tropical storm that gets its energy from the evaporation of warm ocean water and the release of heat
eyecalm center of a tropical cyclone that develops when the winds around its center reach at least 120 km/h
eyewallband where the strongest winds in a hurricane are usually concentrated, surrounding the eye
Saffir-Simpson hurricane scaleclassifies hurricanes according to wind speed, potential for property damage, and potential for flooding in terms of the effect on the height of sea level on a scale ranging from Catagory 1 to Catagory 5
storm surgeoccurs when powerful, hurricane-force winds drive a mound of ocean water toward the shore, where it washes over the land, often causing enormous damage
droughtextended period of well-below-average rainfall, usually caused by shifts in global wind petterns, allowing high-pressure systems to remain for weeks or months over continental areas
heat waveextended period of above-average temperatures caused by large, high-pressure systems that warm by compression and block cooler air masses
cold waveextended period of below-average temperatures caused by large, high-pressure systems of continental polar or arctic origin
windchill indexmeasures the windchill factor, by estimating the heat loss from human skin caused by a combination of wind and cold air

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