Katabatic wind
A local wind which develops due to cool, dense air flowing downhill. The cooler air is generally a result of night time radiational cooling in the lower layers of the atmosphere, but katabatic winds also occur over snow fields and glaciers. See also anabatic winds.
|
Katafront
A front where the warm air descends the frontal surface, except in the low layers.
|
Kelvin
Unit of thermodynamic temperature. Zero Kelvin is absolute zero (-273.15°C). Temperatures in Kelvin can be obtained from temperatures in Celsius by the formulae K=C+273.2.
|
Kelvin-Helmholtz billows
A phenomenon that occurs in a high-shear environment between two layers of fluid which are stably stratified (i.e. a denser fluid beneath a lighter fluid).
|
Kinetic energy
The energy a body possesses as a consequence of its motion. Defined as half the product of its mass and the square of its speed.
|
Knot
The unit of speed equal to 1 nautical mile/hour, or 1.85 km/h. The knot is commonly used to report wind speed and ocean current speed.
|
Knuckles
[Slang] Lumpy protrusions on the edges, and sometimes the underside, of a thunderstorm anvil. They usually appear on the upwind side of a back-sheared anvil, and indicate rapid expansion of the anvil due to the presence of a very strong updraft. They are not mammatus clouds. See also cumuliform anvil, anvil rollover.
|
Køppen's classification of climates
Classification of climate based on annual and monthly means of temperature and precipitation which also takes into account the vegetation limits. It is a tool for presenting the world pattern of climate and for identifying important deviations from this pattern.
|