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Heat Release from Stagnant Deep Sea Helped End Last Ice Age

The build-up and subsequent release of warm, stagnant water from the deep Arctic Ocean and Nordic Seas played a role in ending the last Ice Age within the Arctic region, according to new research led by an international team of scientists.

Accelerated Warming of the Continental Shelf Off Northeast Coast

Water temperatures along the continental shelf off New Jersey have experienced unprecedented warming over the last 13 years.

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