Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell

• Other Authors: AADC (originator), AU/AADC > Australian Antarctic Data Centre, Australia (resourceProvider)
• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: climatologyMeteorologyAtmosphere; oceans; GLACIERS/ICE SHEETS; EARTH SCIENCE; CRYOSPHERE; ICEBERGS; ICE EXTENT; SEA ICE; SWELLS; OCEAN WAVES; WAVE PERIOD; SIGNIFICANT WAVE HEIGHT; SEA ICE CONCENTRATION; ICE SHELF; ICE SHELF STRAIN; SMMR > Scanning Multichannel Microwave Radiometer; SSM/I > Special Sensor Microwave/Imager; SATELLITES; MODELS; DMSP > Defense Meteorological Satellite Program; Nimbus-7; ACE/CRC; AMD/AU; AMD; CEOS; GEOGRAPHIC REGION > POLAR; CONTINENT > ANTARCTICA; OCEAN > SOUTHERN OCEAN; ANTARCTICA > ANTARCTIC PENINSULA; Antarctic; Southern Ocean; The Antarctic; Antarctic Peninsula; Wilkins; Antarc*; Antarctica; British Antarctic Survey; Ice Sheet; Ice Shelf; Ice Shelves; Iceberg*; National Snow and Ice Data Center; Sea ice
• Online Access: https://researchdata.ands.org.au/antarctic-ice-shelf-ocean-swell/1333623; https://data.aad.gov.au/metadata/records/AAS_4116_IceShelfStudy; https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4116_IceShelfStudy; https://data.aad.gov.au/eds/4712/download; https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4116

The data are from our Nature Article from June 2018: "Antarctic ice shelf disintegration triggered by sea ice loss and ocean swell". The abstract is: "Understanding the causes of recent catastrophic ice shelf disintegrations is a crucial step towards improving coupled models of the Antarctic Ice Sheet and predicting its future state and contribution to sea-level rise. An overlooked climate-related causal factor is regional sea ice loss. Here we show that for the disintegration events observed (the collapse of the Larsen A and B and Wilkins ice shelves), the increased seasonal absence of a protective sea ice buffer enabled increased flexure of vulnerable outer ice shelf margins by ocean swells that probably weakened them to the point of calving. This outer-margin calving triggered wider-scale disintegration of ice shelves compromised by multiple factors in preceding years, with key prerequisites being extensive flooding and outer-margin fracturing. Wave-induced flexure is particularly effective in outermost ice shelf regions thinned by bottom crevassing. Our analysis of satellite and ocean-wave data and modelling of combined ice shelf, sea ice and wave properties highlights the need for ice sheet models to account for sea ice and ocean waves." Details of the analyses and data used, and the data generated by this study, are given in the paper: https://www.nature.com/articles/s41586-018-0212-1. Code availability: Analytical scripts used in this study are freely available from the authors via the corresponding author upon reasonable request. Data availability: The datasets and products generated during the current study are available from the corresponding author on reasonable request. The datasets forming the basis of the study are available as follows: (1) Sea ice: Daily estimates of satellite-derived sea ice concentration (gridded at a spatial resolution of 25 x 25 km) derived by the NASA Bootstrap algorithm for the period 1979-2010 were obtained from the US National Snow and Ice Data Center (NSIDC) dataset at: http://nsidc.org/data/NSIDC-0079. Accessed August 2015. (2) Waves: Ocean wave-field data were obtained from the CAWCR (Collaboration for Australian Weather and Climate Research) Wave Hindcast 1979–2010 dataset run on a 0.4 x 0.4° global grid: https://doi.org/10.4225/08/523168703DCC5. Accessed September 2017. (3) Satellite visible and thermal infrared imagery of ice shelves and disintegration events: The NOAA AVHRR image of the Larsen1995 disintegration used in Figure 2 was obtained from the British Antarctic Survey: http://www.nerc-bas.ac.uk/icd/bas_publ.html. Accessed June 2015. MODIS visible and 839 thermal infrared imagery from the US NSIDC archive at: http://nsidc.org/data/iceshelves_images/. Accessed June 2012. The study involved 2 model components, and model output is described below. The 2 models are: (i) a model of ocean swell attenuation by sea ice; and (ii) an ice shelf-ocean wave interaction model. Descriptions of both are given in the Nature paper (Methods section). DESCRIPTIONS OF THE 13 INDIVIDUAL DATA FILES PROVIDED (NB DESCRIPTIONS OF DATASETS GENERATED RELATIVE TO THE FIGURES) ARE GIVEN IN THE FILES: (1) Source data for Figures 4 (parts a-d), 5 and 6a are given in Excel spreadsheet files "Source-Data_2017-07-09041A_Figure.xlsx". (2) Source data for Extended Data Figures 1 (parts a-b), 3 (parts b,d and parts a,c), 4 (parts b,d and a,c) and 6 are given in Excel spreadsheet files "Source-Data_2017-07-09041A_EDFig.xlsx". The purpose of the dataset is to investigate the role of ocean swells in triggering ice shelf disintegration events on the Antarctic Peninsula since 1995 in the absence of a protective sea ice "buffer".