intro, dynamic nature, climate influence, distribution, glossary , references
QUIZ
Try answering these questions to help solidify your understanding of sea ice:
 
Q:  Fast ice usually moves with the following speed:
            A. the speed of sound
            B. 10-20 km/day
            C. 10-20 km/hour
            D.  none at all

Q:  Scientists refer to the concentrations of sea ice at the Earth's poles as:
            A. polar ice caps
            B. polar ice cubes
            C. polar ice cover
            D. cool
 
Q:  What is an ice floe?
            A. a fragment of sheetlike sea ice
            B. glacial ice flowing out of mountainous terrain
            C. a frosty dessert
            D. sea ice that has melted 

Q:  What does sea ice restrict the flow of between the atmosphere and ocean?
            A.  fish, water, salt
            B.  salt, heat, light
            C.  matter, momentum, heat
            D.  all of the above
 
Q:  How does sea ice moderate the temperature extremes of ice-forming regions?
            A.  ice releases heat when it forms, absorbs heat when it melts
            B.  ice absorbs heat when it forms, releases heat when it melts
            C.  sea ice traps heat inside tiny air bubbles
            D.  none of the above

Q:  What are two ways that density decreases as seawater changes its state from liquid to solid?
        A.  increasing volume, increasing mass
        B.  increasing mass, decreasing volume
        C.  increasing volume, decreasing mass
        D.  decreasing volume, decreasing mass

Q:  Name the two usual ways by which sea ice thickness increases to be greater than 3 meters:
            A. wrinkling and rafting
            B. crunching and smashing
            C. ridging and rafting
            D. piling and crashing

Q:  Why is sea ice formation the primary component of the polar hydrologic cycle?
            A.  it distills seawater
            B.  evaporation and precipitation rates are very low
            C.  it rejects salt and sea ice drifts
            D.  all of the above
 
Q:  Why is there a transfer of heat during sea ice formation and decay?
            A.  ice releases heat when it melts
            B.  there are different energy requirements for different states of water
            C.  heat must be absorbed when water freezes
            D.  solid water is more energetic than liquid water
 
Q:  Dynamic processes have what defining characteristic?
        A.  they do not change
        B.  they are constantly changing
        C.  they are always static
        D.  they do not exhibit perceptible variation

Q:  What type of electromagnetic radiation is currently the most effective for the satellite detection of sea ice?
        A.  visible light
        B.  infrared 
        C.  microwave
        D.  ultraviolet

Q:  The transpolar drift stream is a sea ice spatial phenomenon of what scale?
        A.  megascopic
        B.  mesoscopic
        C.  microscopic
        D.  macroscopic

Q:  The term, temporal, refers to what type of scale?
        A.  one that is temporary
        B.  one based upon size
        C.  one based upon time
        D.  macroscopic

Q:  What is the most important factor controlling the formation and decay of sea ice?
        A.  the distance from the Earth to the Sun
        B.  the position of land masses 
        C.  the position of the Gulf Stream
        D.  the angle of incoming sunlight

Q:  Which hemisphere is characterized as having land bordering its poleward sea ice extent?
        A.  Eastern
        B.  Southern 
        C.  Northern
        D.  Western

Q:  Why does north polar sea ice extend into the middle latitudes?
        A.  the influence of the Gulf Stream
        B.  the influence of land masses 
        C.  an absence of the effect of continentality
        D.  sea ice drift
 
 
 

intro, dynamic nature, climate influence, distribution, glossary
 
 
 
 
 
 
 
 
 
 
 
 

 
 
 

                  
                   
 
 
 
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NOT QUITE....
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D.  YES!  Ice that is attached to the land is known as "fast" ice, because it is 'fastened' to it.  Fast ice is the slowest of all the types of sea ice...it does not move much at all.
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C.   YES! Winds and waves cause ice floes to collide sharply with one another.  This causes floes to pile up or become deformed at the edges.  Sea ice can become significantly thicker as a result, sometimes as much as 20 or more meters thick! Ridging and rafting are the two typical ways that sea ice thicknesses increase to greater than 3 meters.
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C.  YES!  Many scientists that study sea ice phenomena refer to sea ice as ice "cover" rather than as an ice "cap" to better reflect the dynamic nature of sea ice.
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A.  YES! The constant motion of sea ice keeps it broken into large fragments called floes.  Floes can be less than a meter to over a kilometer wide and are usually only 2-3 meters thick.
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D.  YES! The distribution of sea ice varies throughout the year depending primarily upon the angle of incoming solar radiation reaching the higher latitudes.
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B.  YES! The southern ice cover has its equatorward extent unrestrained by land and is bounded by land poleward.
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B.  YES! The effects of land upon sea ice formation allow northern sea ice to extend well into the middle latitudes.  This is because land cools more quickly than water and influences the temperatures of the surrounding atmosphere and seas, an effect known as "continentality".
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C. YES! Sea ice distribution in the polar regions became much better understood with the successful remote sensing of the polar regions by satellites using passive microwave radiometers.
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TRUE...but not the best answer
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D.  YES!  Sea ice restricts the flow of all of the items listed.
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A. YES! Sea ice formation releases heat during freezing conditions, and the melting of sea ice absorbs heat. This results in a moderation of temperature extremes.
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C.  Yes!  If the water increases its volume or if the mass decreases as it changes state from liquid to solid, then its density must decrease also. Seawater undergoes both changes:
less density = (less mass)/(more volume)
 
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A.  Yes!  The transpolar drift stream transports ice from the shallow Eurasian continental shelves, over the North Pole, to the Nordic Seas.  Sea ice drifting at this scale involves several years and thousands of kilometers: the megascopic scale.

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B.  YES!  Dynamic processes are characterized by continuous change and activity.
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C.  YES!  Temporal scales are those that are based upon divisions in time.
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D. YES! Salt rejection during the formation of sea ice is a distillation process.  It acts as a seawater filter, allowing only a fraction of the initial salt content to become captured within the ice.  Since evaporation and precipitation rates in the polar regions are very small, the formation and redistribution of sea ice is the only effective way that freshwater is created and distributed in the polar regions [Aagard and Carmack, 1989]. 
 
 
 
 
 
 
 
 
 
 
 
 
 

 
 
 
 
 
 
 
 
 
 

 
 
 
B. YES! As water changes its state from a liquid to solid, the energy requirements necessary to maintain the new solid form are decreased.  The extra energy that was needed for the liquid state is then released into the cold. Conversely, sea ice absorbs heat as it melts.