Marginal ice zone drift prediction model

• Other Authors: AADC (owner), AADC, DATA OFFICER (distributor), AADC, DATA OFFICER (custodian), ALBERELLO, ALBERTO (collaborator), ALBERELLO, ALBERTO (hasPrincipalInvestigator), ALBERELLO, ALBERTO (author), AU/AADC > Australian Antarctic Data Centre, Australia (hasAssociationWith), Alberello, A., Bennetts, L. and Toffoli, A. (originator), Australian Antarctic Data Centre (publisher), Australian Antarctic Division (sponsor), BENNETTS, LUKE (hasPrincipalInvestigator), TOFFOLI, ALESSANDRO (hasPrincipalInvestigator)
• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: oceans; EARTH SCIENCE > CRYOSPHERE > SEA ICE; OCEANS > SEA ICE > SEA ICE MOTION; MARGINAL ICE ZONE; LAGRANGIAN; PANCAKE ICE; SEA ICE DRIFT; Computer > Computer; MODELS; AMD/AU; AMD; CEOS; CONTINENT > ANTARCTICA; OCEAN > SOUTHERN OCEAN; GEOGRAPHIC REGION > POLAR; Antarc*; Antarctic; Antarctica; Sea ice; Southern Ocean
• Online Access: https://researchdata.edu.au/marginal-ice-zone-prediction-model/2819991

Progress Code: completed Purpose Modelling sea ice drift based on dedicated field observations A Langrangian free drift model is developed, including a term for geostrophic currents that reproduces the 13 h period signature in the ice motion observed in the data (CLSC_WIIOS_2017; parent data). The calibrated model is shown to provide accurate predictions of the ice drift for up to 2 days, and the calibrated parameters provide estimates of wind and ocean drag for pancake floes under storm conditions. Model setup is described in "Drift of pancake ice floes in the winter Antarctic marginal ice zone during polar cyclones", Alberello et. al [https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019JC015418; pre-print https://arxiv.org/pdf/1906.10839.pdf]. The dataset includes model data. Six model outputs are included. (i) "full_t00" includes the full 10 days simulation, with all the forcing switched on (ii) "noge_t00" includes the full 10 days simulation, but the geostrophic current is suppressed (iii) "full_t25_noup" includes the simulation with start at 2.5 days, all the forcing switched on, no update of the drag coefficients (iv) "full_t25_newn" includes the simulation with start at 2.5 days, all the forcing switched on, the drag coefficients are recalibrated (v) "full_t50_noup" includes the simulation with start at 5 days, all the forcing switched on, no update of the drag coefficients (vi) "full_t50_newn" includes the simulation with start at 5 days, all the forcing switched on, the drag coefficients are recalibrated In each file: - rho_a the air density (1.3 kg/m3) - rho_w the water density (1028 kg/m3) - rho_i the ice density (910kg/m3) - C_w the water drag coefficient (calibrated) - C_a the air drag coefficient (calibrated) - turn the turning angle (25 degrees) - Nansen the Nansen number evaluated using C_a and C_w - aalpha a model parameter (proportional to air and ice parameters) - abeta a model parameter (proportional to water and ice parameters) - ag amplitude of the geostrophic current ...