Observations of the annual cycle of sea ice temperature and mass balance

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

12

Oceanography: Physical: Ice Mechanics And Air/Sea/Ice Exchange Processes, Oceanography: General: Arctic And Antarctic Oceanography

Scientific paper

A vertical array of thermistors coupled with an autonomous data-logging system was used to obtain a 15-month record of ice temperature profiles in a multiyear floe in the Beaufort Sea. This record was used to monitor atmosphere, ice, and ocean temperatures, determine changes in the ice mass balance, and infer estimates of the ocean heat flux and the snow thermal conductivity. Ablation during the summer melt season consisted of approximately 0.3 m of snow melt, 0.67 m of ice surface ablation, and 0.25 m of bottom ablation. There was 0.45 m of bottom accretion during the growth season. The annually averaged ocean heat flux was 4Wm-2, with a summertime value of 9Wm-2. Comparing these results to earlier studies conducted in the same region showed considerable interannual variability in summer melting. The thermal conductivity of snow cover was approximately 0.3Wm-1K-1 during winter.

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

Observations of the annual cycle of sea ice temperature and mass balance 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 Observations of the annual cycle of sea ice temperature and mass balance, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Observations of the annual cycle of sea ice temperature and mass balance will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-1860211

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