Cryosphere Glossary
- albedo
- a measure of the reflectivity of a surface ranging from 0 to 1; albedo is calculated by taking the ratio of reflected radiation to incoming radiation, such that a surface that reflects 100% of light hitting it has an albedo of 1, and a surface that absorbs 100% of the light hitting it has an albedo of 0.
- anomaly
- irregularity or deviation from normal.
- anthropogenic
- of, relating to, or resulting from the influence of human beings on nature.
- brine
- water with a high salt content.
- cryosphere
- the set of all locations on or beneath Earth's surface where frozen water exists.
- fast ice
- ice that is anchored to the shore or ocean bottom, typically over shallow ocean shelves at continental margins; fast ice is defined by the fact that it does not move with the winds or currents.
- feedback
- exchange between the input and the output of a system.
- first-year ice
- floating ice of no more than one year's growth developing from young ice; thickness ranges from 0.3 to 2 meters (1 to 6.6 feet); first-year ice is characteristically level (flat) where it is undisturbed by pressure, but can be rough and angular where ridges occur.
- glacier
- a mass of ice that originates on land, usually having an area larger than one tenth of a square kilometer; many believe that a glacier must show some type of movement; others believe that a glacier can show evidence of past or present movement.
- greenhouse gas
- any gas, including carbon dioxide, water vapor, ozone and methane, that traps heat in the Earth's atmosphere.
- iceberg
- a piece of ice that has broken off from the end of a glacier that ends in water.
- ice sheet
- a dome-shaped mass of glacier ice that covers surrounding terrain and is greater than 50,000 square kilometers (12 million acres) (e.g., the Greenland and Antarctic ice sheets).
- ice shelf
- portion of an ice sheet that spreads out over water.
- land ice
- any part of Earth's ice cover that formed over land primarily from freezing precipitation, as opposed to sea ice formed by the freezing of seawater.
- multiyear ice
- ice that has survived at least one melt season; it is typically 2 to 4 meters (6.6 to 13.1 feet) thick and thickens as more ice grows on its underside.
- new ice
- a general category of ice representing the earliest stages of sea ice growth.
- permafrost
- layer of soil or rock, at some depth beneath the surface, in which the temperature has been continuously below 0°C for at least several years; it exists where summer heating fails to reach the base of the layer of frozen ground.
- salinity
- measurement of salt content.
- sea ice
- any form of ice found at sea which formed from the freezing of sea water.
- sea ice concentration
- the fraction of an area that is covered by sea ice.
- sea ice extent
- the total area covered by some amount of ice, including open water between ice floes; sea ice extent is typically measured in square kilometers.
- thermodynamic equilibrium
- the state of a system in which its energy distribution is such that all parts of the system have the same temperature and no heat flows.
- thermodynamics
- the study of conversions between heat and other forms of energy.
- thermohaline circulation
- deep-ocean currents driven by differences in the water's density, which is controlled by temperature (thermo) and salinity (haline).
- young ice
- a general category of ice that is less than one year old and about 10 to 30 centimeters (4 to 12 inches) thick.



