mountainwatch.com

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Definitions (192)

1

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Absolutely Unstable Air


What we call it when the temperature in a section of the atmosphere is decreasing so quickly that any air parcel that rises will find itself warmer, lighter and more buoyant than its surrounds. The further it rises the bigger the difference and so it will keep on going until it hits a layer of stable air above. During summer the lower half of the a [..]
Source: mountainwatch.com

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atmosphere


The air stuck to the Earth by gravity.
Source: mountainwatch.com

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540 line


A depth of 5400 m between the 1000 hPa and the 500 hPa pressure levels in the atmosphere. The thickness of this 1000-500 hPa layer is largely dependent upon the average temperature in the layer and to a lesser extent on the moisture content. During a cold outbreak, the air is very dense and so this layer is thinner. When the thickness is less than [..]
Source: mountainwatch.com

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Ablation


The loss of snow by melting and evaporation. Ablation sucks.
Source: mountainwatch.com

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Absolutely Stable Air


What we call it when a section of the atmosphere is so stable (warm light air over cold dense air) that a parcel of air rising through it will always wind up cooler and heavier than its surroundings and want to sink again, even if condensation is occurring and releasing heat.
Source: mountainwatch.com

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ACCRETION


What happens when a drop of super-cooled liquid water collides with an ice particle and freezes on impact.
Source: mountainwatch.com

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adiabatic


A fancy term to describe changes in the temperature of air due to expansion or compression. Air sinks, it is compressed and warmed adiabatically, without any exchange of heat with the outside environment (although there's always some mixing around the edges). Air rises, it expands and cools.
Source: mountainwatch.com

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Advection


A fancy word for the wind blowing stuff around - usually cold or warm air, but also some other more complicated atmospheric variables like vorticity.
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Advection fog


Fog caused by warm moist air flowing over a cold surface and cooling until condensation occurs.
Source: mountainwatch.com

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aerosol


Little bits of stuff floating around in the air. Dirt, insects, sea salt, pollution. These are really important because water vapour needs them to start the process of forming rain and snow. Not enough, and precious water vapour can slip by the mountains without turning into rain. That's why Snowy Hydro seed clouds with extra aerosols.
Source: mountainwatch.com


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