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  2. Measurement of sea ice - Wikipedia

    en.wikipedia.org/wiki/Measurement_of_sea_ice

    Sea ice mass balance is the balance of how much the ice grows in the winter and melts in the summer. For Arctic sea ice virtually all of the growth occurs on the bottom of the ice. Melting occurs on both the top and the bottom of the ice. In the vast majority of cases all of the snow melts during the summer, typically in just a couple of weeks.

  3. Past sea level - Wikipedia

    en.wikipedia.org/wiki/Past_sea_level

    The main factors affecting sea level are the amount and volume of available water and the shape and volume of the ocean basins. The primary influences on water volume are the temperature of the seawater, which affects density, and the amounts of water retained in other reservoirs like rivers, aquifers, lakes, glaciers, polar ice caps and sea ice.

  4. Sea ice - Wikipedia

    en.wikipedia.org/wiki/Sea_ice

    Satellite study of sea ice began in 1979 and became a much more reliable measure of long-term changes in sea ice. In comparison to the extended record, the sea-ice extent in the polar region by September 2007 was only half the recorded mass that had been estimated to exist within the 1950–1970 period. [23]

  5. Sea ice is thinning. Here’s how Boise State researchers are ...

    www.aol.com/news/sea-ice-thinning-boise-state...

    Researchers hope the new tool that measures sea ice depth will help them understand the Arctic environment. Sea ice is thinning. Here’s how Boise State researchers are measuring its change

  6. Geologic temperature record - Wikipedia

    en.wikipedia.org/wiki/Geologic_temperature_record

    Reconstruction of the past 5 million years of climate history, based on oxygen isotope fractionation in deep sea sediment cores (serving as a proxy for the total global mass of glacial ice sheets), fitted to a model of orbital forcing (Lisiecki and Raymo 2005) [2] and to the temperature scale derived from Vostok ice cores following Petit et al. (1999).

  7. Sea ice thickness - Wikipedia

    en.wikipedia.org/wiki/Sea_ice_thickness

    Sea ice freeboard is the difference between the height of the surface of sea ice and the water in open leads. Since 85–95% of snow-free sea ice is usually located below the waterline, the computation of the thickness is fairly simple; [ 3 ] however, accurate measurement of ice freeboard is hindered by several factors including snow cover, and ...

  8. Stone Age megastructure found submerged in the Baltic Sea ...

    www.aol.com/underwater-may-one-oldest-known...

    Sea levels rose significantly after the end of the last ice age about 8,500 years ago, which would have led to the wall and large parts of the landscape being flooded, according to the study ...

  9. From Ice Age to Modern Day: How Reindeer Thrive in ... - AOL

    www.aol.com/ice-age-modern-day-reindeer...

    Reindeer evolved during the last ice age to withstand temperatures as low as minus 94°F (minus 70° C. Yes, you read that right. This is an amazing feat, accomplished only by a select group of ...