![]() ![]() The poleward wave penetration limit (boundary) is defined as the location where significant wave height attenuation equals the estimated error in significant wave height. ![]() To address this, new techniques have been developed to measure the spatial extent of significant wave height attenuation in sea ice from variations in Ice, Cloud and land Elevation Satellite-2 (ICESat-2) surface heights. Legacy methods for defining the MIZ are typically based on sea ice concentration thresholds and do not directly relate to the fundamental physical processes driving MIZ variability. Improved large-scale (satellite-based) estimates of MIZ extent and variability are crucial for understanding atmosphere–ice–ocean interactions and biological processes and detection of change therein. The Antarctic marginal ice zone (MIZ) is a highly dynamic region where sea ice interacts with ocean surface waves generated in ice-free areas of the Southern Ocean. Fraser Received: – Discussion started: – Revised: – Accepted: – Published: ![]() Fraser Hide author detailsĬorrespondence: Alexander D. a now at: Department of Physics, The University of Auckland, Tāmaki Makaurau / Auckland, New ZealandĬorrespondence: Alexander D.8 Spire Global, Inc., Glasgow, United Kingdom.7 Australian Centre for Excellence in Antarctic Science, University of Tasmania, Hobart, Australia.6 Department of Earth Environmental and Planetary Sciences, Brown University, Providence, Rhode Island, USA.5 National Institute of Water and Atmospheric Research, Ōtautahi / Christchurch, New Zealand.4 School of Mathematics, University of East Anglia, Norwich, United Kingdom.3 Australian Antarctic Division, Kingston, Australia.2 Australian Antarctic Program Partnership, Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia.1 Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia. ![]()
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