Filed
Under: Baby
Activities, Crafts for Kids, Do (Activities by Subject), Elementary Activities, Family Activities (all ages), Indoor, Kids Activities (by Age), Kindergarten Activities, Preschool Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities, Crafts for Kids, Do (
Activities by Subject), Elementary Activities, Family Activities (all ages), Indoor, Kids Activities (by Age), Kindergarten Activities, Preschool Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities by Subject), Elementary
Activities, Family Activities (all ages), Indoor, Kids Activities (by Age), Kindergarten Activities, Preschool Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities, Family
Activities (all ages), Indoor, Kids Activities (by Age), Kindergarten Activities, Preschool Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities (all ages), Indoor, Kids
Activities (by Age), Kindergarten Activities, Preschool Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities (by Age), Kindergarten
Activities, Preschool Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities, Preschool
Activities, Toddlers Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities, Toddlers
Activities Tagged With: activities, frozen, ice, olaf, play dough, snowm
Activities Tagged With:
activities, frozen, ice, olaf, play dough, snowm
activities, frozen,
ice, olaf, play dough, snowman, winter
Other factors would include: — albedo shifts (both from
ice > water, and from increased biological
activity, and from edge melt revealing more land, and from more old dust coming to the surface...); — direct effect of CO2 on
ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on
ice; — «stuck» weather systems bringing more and more warm tropical air ever further toward the poles; — melting of sea
ice shelf increasing mobility of glaciers; — sea water getting
under parts of the
ice sheets where the base is below sea level; — melt water lubricating the
ice sheet base; — changes in ocean currents -LRB-?)