Sea state and boundary layer physics of the emerging arctic ocean
The Office of Naval Research initiated a Department Research Initiative (DRI) titled Sea State and Boundary Layer Physics of the Emerging Arctic Ocean. The central hypothesis of the 'Sea State' DRI is that surface waves now have a much greater role in the contemporary Arctic Ocean. Indeed,...
Main Authors: | , , , , , , , , , , , , , , , , , , , |
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Other Authors: | |
Format: | Report |
Language: | unknown |
Published: |
2013
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Subjects: | |
Online Access: | http://elib.dlr.de/93641/ http://www.apl.washington.edu/research/downloads/publications/tr_1306.pdf |
Summary: | The Office of Naval Research initiated a Department Research Initiative (DRI) titled Sea State and Boundary Layer Physics of the Emerging Arctic Ocean. The central hypothesis of the 'Sea State' DRI is that surface waves now have a much greater role in the contemporary Arctic Ocean. Indeed, the entire Arctic Ocean in summer may soon resemble a marginal ice zone (MIZ). The Sea State DRI will use a combination of modeling, in situ observations, and remote sensing to address the following science objectives: 1. Develop a sea state climatology for the Arctic Ocean 2. Improve wave forecasting in the presence of sea ice 3. Improve theory of wave attenuation/scattering in the sea ice cover 4. Apply wave-ice interactions directly in integrated arctic system models 5. Understand heat and mass fluxes in the air-sea-ice system |
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