Late spring 2018 land-fast sea ice and sub-ice platelet layer thicknesses from electromagnetic induction soundings along transect West-East-EM-Transect_20181113 in McMurdo Sound, Antarctica

doi:doi:10.1594/PANGAEA.968707

Late spring 2018 land-fast sea ice and sub-ice platelet layer thicknesses from electromagnetic induction soundings along transect West-East-EM-Transect_20181113 in McMurdo Sound, Antarctica

Ground-based electromagnetic induction (EM) measurements of land-fast sea ice and sub-ice platelet layer (SIPL) thickness distributions were carried out in McMurdo Sound, Antarctica in late spring (November 1-19) of 2018. Repeated west to east EM transects were carried out across McMurdo Sound along latitude 77.767°S. The EM data was acquired using a frequency-domain Geonics Ltd EM31-MK2 instrument mounted on a sledge and towed by skidoo. The thicknesses of consolidated ice (sea ice plus the snow layer) and the sub-ice platelet layer were simultaneously retrieved from the EM31 measured response using forward modelling and inversion methods of Irvin (2018). Variability in EM thicknesses detected significant growth of sub-ice platelet layer over the 18-day survey period (Brett et al., 2024).

BibTex:

@dataset{Brett_Gemma_Marie_and_Leonard_Gregory_H_and_Rack_Wolfgang_and_Irvin_Anne_and_Haas_Christian_and_Langhorne_Patricia_J_2024,
    abstract = {Ground-based electromagnetic induction (EM) measurements of land-fast sea ice and sub-ice platelet layer (SIPL) thickness distributions were carried out in McMurdo Sound, Antarctica in late spring (November 1-19) of 2018. Repeated west to east EM transects were carried out across McMurdo Sound along latitude 77.767°S. The EM data was acquired using a frequency-domain Geonics Ltd EM31-MK2 instrument mounted on a sledge and towed by skidoo. The thicknesses of consolidated ice (sea ice plus the snow layer) and the sub-ice platelet layer were simultaneously retrieved from the EM31 measured response using forward modelling and inversion methods of Irvin (2018). Variability in EM thicknesses detected significant growth of sub-ice platelet layer over the 18-day survey period (Brett et al., 2024).},
    author = {Brett, Gemma Marie and Leonard, Gregory H and Rack, Wolfgang and Irvin, Anne and Haas, Christian and Langhorne, Patricia J},
    doi = {10.1594/PANGAEA.968707},
    institution = {PANGAEA (Ecology)},
    keyword = {'Antarctic sea ice', 'Ice thickness', 'Sub', 'electromagnetic induction', 'ice', 'ice platelet layer', 'ocean interaction'},
    title = {Late spring 2018 land-fast sea ice and sub-ice platelet layer thicknesses from electromagnetic induction soundings along transect West-East-EM-Transect_20181113 in McMurdo Sound, Antarctica},
    url = {https://service.tib.eu/ldmservice/vdataset/png-doi-10-1594-pangaea-968707},
    year = {2024}
}