Cryosphere glossary
A B C D E F G H I J K L M N O P R S T U V W Y Z
a surficial layer of angular shattered rocks formed in either modern or pleistocene periglacial environments.
opening through a snow bridge into a crevasse or system of crevasses which are otherwise sealed by snow bridges; a snowdrift usuallly forms on the lee side.
an ensemble of snow particles raised by the wind to moderate or great heights above the ground; the horizontal visibility at eye level is generally very poor.
a cold wind blowing down an incline; a kind of katabatic wind.
the forested region that adjoins the tundra along the arctic tree line, which has two main divisions: its northern portion is a belt of taiga or boreal woodland, while its southern portion is a belt of true forest, mainly conifers but with some hardwoods; on its southern boundary the boreal forest passes into “mixed forest” or “parkland,” prairie, or steppe, depending on the rainfall.
icebergs that originate from near the bottom of a glacier; the color is usually black from trapped rock material or dark blue because of old, coarse, bubble-free ice; they sit low in the water due to the weight of the embedded rocks.
temperature measured at the base of the snow cover during mid- to late-winter (February/March).
glacier that has one or more tributary glaciers that flow into it; distinguished from a simple valley glacier that has only a single tributary glacier.
Image
branched_valley_glacier.jpg

In this photograph from 1969, small glaciers flow into the larger Columbia Glacier from mountain valleys on both sides. Columbia Glacier flows out of the Chugach Mountains into Columbia Bay, Alaska.

United States Geological Survey. Archived at the World Data Center for Glaciology, Boulder, CO
accumulation of floating ice made up of fragments not more than 2 meters (6.6 feet) across, the wreckage of other forms of ice.
small droplets of highly saline water that form in pockets between ice crystals, as sea ice forms and expels salt into the underlying ocean water.
method to predict the presence or absence of permafrost in a mountain area, using measurements of the bottom temperature of snow cover mid- to late-winter.
smooth hills of ice that form on the bottom of sea ice from eroding keels, particularly during the summer melt.
a buoy, either fixed or floating, which carries instruments for sensing various meteorological elements and for transmitting the data by radio.
ice formed or deposited on the ground surface and later covered by sediments.
Meterological law which states that if you are standing with your back to the wind in the Northern Hemisphere, low pressure will be on your left, and high pressure will be on your right. Ballot was a 19th century Dutch climatalogist.