https://martinwearing.com/publications/2024-08-01T12:17:44+00:00weekly0.6https://martinwearing.com/contact/2024-05-16T07:45:46+00:00weekly0.6https://martinwearing.com/research/https://martinwearing.com/wp-content/uploads/2021/11/figure_1_secondary_flow.pngFigure_1_secondary_flowhttps://martinwearing.com/wp-content/uploads/2018/05/gaus_velocity_5int_mm_walls.pnggaus_velocity_5int_mm_wallsFigure (7): Flow field for a Golden Syrup (Newtonian) Ice Shelf. From left to right: Low-pass Gaussian filter velocity field; TIme-averaged velocity field; Along-flow strain rate field; Centreline velocity. Red dashed lines represent position of grounding line. Yellow dashed line marks end of channel.https://martinwearing.com/wp-content/uploads/2018/05/thickness_profile_example_image_annotated.pngthickness_profile_example_image_annotatedFigure 6: Side view of experiment. Red dashed line denoted ocean surface, orange dashed line denotes viscous fluid surface.https://martinwearing.com/wp-content/uploads/2018/05/ice_shelf_in_parallel_channel_diagram_plan_view.pngIce_shelf_in_parallel_channel_diagram_plan_viewFigure (5b): Experiment set-up plan viewhttps://martinwearing.com/wp-content/uploads/2018/05/ice_shelf_in_parallel_channel_diagram.pngIce_shelf_in_parallel_channel_diagramFigure (5a): Experiment set-up side viewhttps://martinwearing.com/wp-content/uploads/2018/05/fimbul_strain_shear_p1_p2_modis.pngFimbul_strain_shear_P1_P2_modisFigure (1): Fimbul Ice Shelf: (a) MODIS visual imagery, (b) speed, (c) along-flow strain rate, (d) shear rate, (e) 1st Principal Strain Axis, (f) 2nd Principal Strain Axis. Reference: Wearing, M. G. (2016). The Flow Dynamics and Buttressing of Ice Shelves. University of Cambridge.https://martinwearing.com/wp-content/uploads/2018/05/15j116_figure_9.png15J116_figure_9Figure (3b): Relationship from linear regression relationship in log-log plotted in linear space.https://martinwearing.com/wp-content/uploads/2018/05/15j116_figure_8.png15J116_figure_8Figure (3a): Linear regression in log-log space. Purple crosses represent ice shelves that are not laterally confined at calving front or that have damaged margins.https://martinwearing.com/wp-content/uploads/2018/05/n3_shear-and-ext_hss.pngn3_shear-and-ext_HssFigure (2): Steady state; thickness profile, speed, along-flow strain rate and centreline strain rate for an ice shelf with shear and extensional dynamics.https://martinwearing.com/wp-content/uploads/2018/05/steady_state_n3_parallel_3figs.pngSteady_state_n3_parallel_3figsFigure (1): Steady state; thickness profile, speed and along-flow strain rate for a shear-dominated ice shelf with Glen's Flow Law rheology (power law) n=3.2021-11-25T11:08:08+00:00weekly0.6https://martinwearing.com/outreach/2021-11-25T11:01:46+00:00weekly0.6https://martinwearing.com/blog/2020-07-09T12:02:48+00:00weekly0.6https://martinwearing.com/fieldwork/https://martinwearing.com/wp-content/uploads/2018/03/p1010395.jpgP1010395Icebergs calving off McMurdo Ice Shelf into sea icehttps://martinwearing.com/wp-content/uploads/2018/03/p1030073.jpgP1030073Sea icehttps://martinwearing.com/wp-content/uploads/2018/03/p1030225.jpgP1030225Sea icehttps://martinwearing.com/wp-content/uploads/2018/03/p1010307.jpgP1010307https://martinwearing.com/wp-content/uploads/2018/03/p1010355.jpgP1010355Scott Base and pressure ridgeshttps://martinwearing.com/wp-content/uploads/2018/03/p1010887.jpgP1010887https://martinwearing.com/wp-content/uploads/2018/03/p1030047.jpgP1030047Fracture rift filled with ice and snow (approximately 0.5 - 1 km wide)https://martinwearing.com/wp-content/uploads/2018/03/p1030220.jpgP1030220Fracture in Ross Ice Shelf Calving Fronthttps://martinwearing.com/wp-content/uploads/2018/03/p1030263.jpgP1030263Ross Ice Shelf calving fronthttps://martinwearing.com/wp-content/uploads/2018/03/img_20171130_103923.jpgIMG_20171130_103923Gravimeters inside the LC-1302018-03-21T18:32:33+00:00weekly0.6https://martinwearing.com/2018/03/21/the-journey-begins/2018-03-21T14:33:14+00:00monthlyhttps://martinwearing.comdaily1.02024-08-01T12:17:44+00:00