Megatides in the Arctic Ocean under glacial conditions

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

5

Oceanography: Physical: Surface Waves And Tides (1222), Oceanography: General: Arctic And Antarctic Oceanography (9310, 9315), Oceanography: General: Numerical Modeling (0545, 0560), Paleoceanography: Abrupt/Rapid Climate Change (1605), Cryosphere: Ice Streams

Scientific paper

Over the history of the Earth, changes in ocean depth and coastal configuration have led to considerable variations in the pattern and amplitude of ocean tides. Here we perform global simulations of ocean tides for the Last Glacial Maximum, using new data sets for both ocean depth and density stratification. We show how the configuration of the Arctic Ocean, which was almost entirely enclosed by continents at that time, leads to the near-resonant excitation of large semi-diurnal tides. Under certain conditions, this previously unidentified Arctic tide is massively amplified in the Canadian Archipelago. Such tides may have played a role in destabilizing the coastal margins of North American ice sheets, with implications for rapid changes in the Earth's climate and ocean circulation.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Megatides in the Arctic Ocean under glacial conditions does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Megatides in the Arctic Ocean under glacial conditions, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Megatides in the Arctic Ocean under glacial conditions will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1343003

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.