Because of warmer Arctic temperatures, little
multiyear ice forms to replace what's lost.
Not exact matches
The
ice is mapped by age: first year
ice that's
formed this year, 2 year old
ice (survived the last summer's melt), and so on up to «5 +» (which is very thick
multiyear ice that has survived five or more summer melt seasons).
the avalanche studies tell us the layers
formed in the snow are indicative of the type of avalanche expected, is there any reason not to believe that so called fractured
multiyear ice won't behave in the same style (breaks laterally)?