Antarctica is a 'game of two halves'. East Antarctica is a mile thick ice sheet on top of solid bedrock. But the ice on West Antarctica sits precariously above and below the sea line on a series of islands. The country sized glaciers on it's outer edges, that keep the ice flow at bay, have been receding for years, but now new research has shown the disintegration of Thwaites, or Doomsday, Glacier is accelerating fast.

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Interested in mastering and remembering the concepts that I present in my videos? Check out the FREE Dive Deeper mini-courses offered by the Center for Behavior and Climate. These mini-courses teach the main concepts in select JHAT videos and go beyond to help you learn additional scientific or conservation concepts. The courses are great for teachers to use or for individual learning.[ Ссылка ]

Check out other YouTube Climate Communicators

zentouro:
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Climate Adam:
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Kurtis Baute:
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Levi Hildebrand:
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Simon Clark:
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Sarah Karvner:
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Rollie Williams / ClimateTown: [ Ссылка ]

Jack Harries:
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Beckisphere: [ Ссылка ]

Our Changing Climate :
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Research Links

ITGC Press Conference Video
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ITGC Press Release
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CIRES Article
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