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Product Description


Ridges form when sea ice is deforming and fracturing due to forces from winds and currents. Ridges are elongated accumulations of broken ice resulting from deformation of sea ice. Rafting is another form of deformed ice occurring when one ice sheet overrides another ice sheet. Ridging and corresponding ice keels represent the thickest part of the sea ice cover. Detection and monitoring of ridges is therefore an important part of met-ice-ocean services to support operations in ice-covered seas. On large scale ridges can be observed by laser and radar altimeter data through a surface roughness parameter that is defined by standard deviation of the surface elevation measurements along the satellite orbit (as ICESAT laser altimeter). On regional and local scale, SAR images have been used for ridge detection and sea ice processes in the Baltic Sea, the Barents Sea and Svalbard area, in the Russian Arctic and in Canadian waters. SAR image cannot provide any quantitative estimate of the height of ridges. Use of SAR images with alternating polarization and high spatial resolution (better than 10 m) is expected to improve the classification of rough ice and detection of ridges.

Product Specifications


OF GEOINFORMATION Ice  ice Temporal Resolution update

BUSINESS PROCESS

SD, SC, IN

DESCRIPTION

Ice ridges refer to elongated and elevated formations of ice that develop in ice-covered seas. These ridges are typically created through the interaction of drifting sea ice and external forces such as wind, currents, and collisions between ice floes.

EO INFORMATION OF INTEREST

Wind and current velocity components (u, v) deforming and fracturing ice

drift fields, SIT

MAIN PROCESS STEPS

Sea ice deformation derived from models

INPUT DATA SOURCE

SAR and in situ measurements used for assimilation/validation

SPATIAL RESOLUTION AND COVERAGE

Coverage of the model domain (an enclosed sea, a bay), spatial resolution based on the model grid

ACCURACY / CONSTRAINS

Not specified

LIMMITATIONS

Not specified

LIMITATIONS

Limited availability of ground truth.

The interpretation of data can indeed be challenging, especially when handled by personnel without extensive experience in the field. 

TEMPORAL RESOLUTION

Same as SIUV

FREQUENCY

UPDATE

Very high (model time-steps) from hourly to days

DELIVERY / OUTPUT FORMAT

NetCDF-3, NetCDF-4, Raster (geo-located) and shape formats

ACCESSIBILITY

Copernicus marine service and Artic hub


Business Process Challenges


Ship Design (SD) Challenges

SD-1 Environmental Conditions

Ship Construction (SC) Challenges

  • SC-1 Lifting Operations 
  • SC-2 Tow Operations
  • SC-3 Planning of Sea Trials Outside of Ice Season

    Ship Certification (SCE) Challenges

    Insurance (IN) Challenges

    Ship Operation (SO) Challenges 

    End of Life Vessel Disposal (ELD) Challenges