Data

Quality controlled wave attenuation and frequency dispersion products in landfast sea ice

Australian Ocean Data Network
Voermans, J. ; VOERMANS, JOEY
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=http://data.aad.gov.au/metadata/records/AAS_4593_attenuation_dispersion_profiles&rft.title=Quality controlled wave attenuation and frequency dispersion products in landfast sea ice&rft.identifier=http://data.aad.gov.au/metadata/records/AAS_4593_attenuation_dispersion_profiles&rft.publisher=Australian Antarctic Data Centre&rft.description=Data contains profiles of wave attenuation and frequency dispersion in landfast ice as derived from wave measurements in the Antarctic (October 2020, 66.2°S 110.6°E) and Arctic (March 2020, 78.0°N 14.2°E). Instruments used to measure ice motion are ice buoys (Rabault et al., 2020) using a high-accuracy internal motion unit (VectorNav VN-100). To assure quality of data, a signal to noise ratio equal or larger than 2 is used. Attenuation between instruments is then determined following the exponential decay of waves in sea ice. The typical direction of wave energy into the marginal ice zone is well aligned with the instruments deployed. The wavelength of waves in sea ice were determined for each instrument by using information of the spectra of heave, pitch and roll. We observe a bias of about 3% between the wave length and open water wave length for waves between 8 and 12 seconds. Details of data quality control and processing is given in Voermans et al. (2021).Progress Code: completed&rft.creator=Voermans, J. &rft.creator=VOERMANS, JOEY &rft.date=2023&rft.coverage=westlimit=110.6; southlimit=-66.2; eastlimit=110.6; northlimit=-66.2&rft.coverage=westlimit=110.6; southlimit=-66.2; eastlimit=110.6; northlimit=-66.2&rft_rights=This metadata record is publicly available.&rft_rights=These data are publicly available for download from the provided URL.&rft_rights= https://creativecommons.org/licenses/by/4.0/legalcode&rft_rights=This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4593_attenuation_dispersion_profiles when using these data. http://creativecommons.org/licenses/by/4.0/).&rft_rights=Portable Network Graphic&rft_rights=https://i.creativecommons.org/l/by/3.0/88x31.png&rft_rights=Creative Commons by Attribution logo&rft_rights=Attribution 4.0 International (CC BY 4.0)&rft_rights=Legal code for Creative Commons by Attribution 4.0 International license&rft_rights=Attribution 4.0 International (CC BY 4.0)&rft_rights= https://creativecommons.org/licenses/by/4.0/legalcode&rft_subject=oceans&rft_subject=EARTH SCIENCE > OCEANS > OCEAN WAVES > GRAVITY WAVES&rft_subject=EARTH SCIENCE > OCEANS > SEA ICE > SEA ICE MOTION&rft_subject=WAVE-ICE BUOY&rft_subject=DRIFTING BUOYS > DRIFTING BUOYS&rft_subject=FIELD SURVEYS > FIELD SURVEYS&rft_subject=AMD&rft_subject=AMD/AU&rft_subject=CEOS&rft_subject=GEOGRAPHIC REGION > POLAR&rft_subject=CONTINENT > ANTARCTICA > ANTARCTICA&rft.type=dataset&rft.language=English Access the data

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This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/).

Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4593_attenuation_dispersion_profiles when using these data.
http://creativecommons.org/licenses/by/4.0/).

Attribution 4.0 International (CC BY 4.0)

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This metadata record is publicly available.

These data are publicly available for download from the provided URL.

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Brief description

Data contains profiles of wave attenuation and frequency dispersion in landfast ice as derived from wave measurements in the Antarctic (October 2020, 66.2°S 110.6°E) and Arctic (March 2020, 78.0°N 14.2°E). Instruments used to measure ice motion are ice buoys (Rabault et al., 2020) using a high-accuracy internal motion unit (VectorNav VN-100). To assure quality of data, a signal to noise ratio equal or larger than 2 is used. Attenuation between instruments is then determined following the exponential decay of waves in sea ice. The typical direction of wave energy into the marginal ice zone is well aligned with the instruments deployed. The wavelength of waves in sea ice were determined for each instrument by using information of the spectra of heave, pitch and roll. We observe a bias of about 3% between the wave length and open water wave length for waves between 8 and 12 seconds. Details of data quality control and processing is given in Voermans et al. (2021).

Lineage

Progress Code: completed

Notes

Purpose
Dataset can be used to calibrate and validate wave-ice interaction parameterizations, and wave products in wave models.

Data time period: 2020-10-01 to 2020-10-31

This dataset is part of a larger collection

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110.6,-66.2

110.6,-66.2

text: westlimit=110.6; southlimit=-66.2; eastlimit=110.6; northlimit=-66.2

Other Information
Download the dataset. (GET DATA > DIRECT DOWNLOAD)

uri : https://data.aad.gov.au/eds/5591/download

Identifiers
  • global : AAS_4593_attenuation_dispersion_profiles