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sasip-climate · Jan 10, 2024 · 18381a7 · 18381a7
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 <!doctype html><html lang=en><head><meta charset=utf-8><meta http-equiv=x-ua-compatible content="ie=edge"><title>Video of the month - SASIP</title><meta name=viewport content="width=device-width,initial-scale=1"><link rel=icon href=https://sasip-climate.github.io/favicon.png><link rel=stylesheet href=/css/style.min.0c767542d2a010b5a842f934f628a7a33c7b23927fdbe53b352adbe80371ad13.css></head><body class='page page-services-single'><div id=main-menu-mobile class=main-menu-mobile><ul><li class=menu-item-news><a href=/news><span>News</span></a></li><li class=menu-item-about><a href=/pages/about><span>About</span></a></li><li class=menu-item-team><a href=/team/><span>Team</span></a></li><li class=menu-item-research><a href=/research><span>Research</span></a></li><li class="menu-item-code & data"><a href=/code><span>Code & Data</span></a></li><li class=menu-item-publications><a href=/pages/publications><span>Publications</span></a></li><li class=menu-item-jobs><a href=/jobs><span>Jobs</span></a></li></ul></div><div id=wrapper class=wrapper><div class='header header-absolute'><div class=container><div class=logo><a href=https://sasip-climate.github.io/><img alt="Figurit Homepage" src=https://sasip-climate.github.io/images/logo-sasip.png></a></div><div class=logo-mobile><a href=https://sasip-climate.github.io/><img alt="Figurit Homepage" src=https://sasip-climate.github.io/images/logo-sasip.png></a></div><div id=main-menu class=main-menu><ul><li class=menu-item-news><a href=/news><span>News</span></a></li><li class=menu-item-about><a href=/pages/about><span>About</span></a></li><li class=menu-item-team><a href=/team/><span>Team</span></a></li><li class=menu-item-research><a href=/research><span>Research</span></a></li><li class="menu-item-code & data"><a href=/code><span>Code & Data</span></a></li><li class=menu-item-publications><a href=/pages/publications><span>Publications</span></a></li><li class=menu-item-jobs><a href=/jobs><span>Jobs</span></a></li></ul></div><button id=toggle-main-menu-mobile class="hamburger hamburger--slider" type=button>
-<span class=hamburger-box><span class=hamburger-inner></span></span></button></div></div><div id=hero class="hero-image hero-image-setheight" style=background-image:url(/images/ice-bandeau.png)><div class=container><div class=hero-text><span class=hero-section>news</span><h1></h1><p></p></div></div></div><div class="container pt-4 pt-md-10 pb-4 pb-md-10"><div class="row justify-content-start"><div class="col-12 col-md-8"><div class="service service-single"><div class=content><p>This month we publish a video provided by S. Brenner @ Brown University, USA.</p><p>In a new paper in Geophysical Research Letters, S. Brenner and members of the SASIP team investigate floe-scale effects on ice-ocean boundary layer turbulence. These numerical simulations of the marginal ice zone, produced with the &ldquo;FloeDyn&rdquo; sea ice discrete element model, show sea ice motion together with the underying ocean current field (white/blue colourmap and vector arrows shows), followed by the associated turbulence generation under the ice (cyan/red colourmap). Three different floe size distributions are investigated. Despite maintaing the same bulk sea ice concentration (50%) and ocean forcing for each of the cases shown, distinct turbulence patterns emerge for the three floe size distributions. Read the paper: <a href=https://doi.org/10.1029/2023GL105703><strong><em>Scale-Dependent Air-Sea Exchange in the Polar Oceans: Floe-Floe and Floe-Flow Coupling in the Generation of Ice-Ocean Boundary Layer Turbulence</em></strong></a>.</p><p><img src=/images/news/2024-01-10_Simulation_Brenner.gif alt=meeting_pic></p><p><em>Fig.: Movie produced by S. Brenner @ Brown University, USA.
+<span class=hamburger-box><span class=hamburger-inner></span></span></button></div></div><div id=hero class="hero-image hero-image-setheight" style=background-image:url(/images/ice-bandeau.png)><div class=container><div class=hero-text><span class=hero-section>news</span><h1></h1><p></p></div></div></div><div class="container pt-4 pt-md-10 pb-4 pb-md-10"><div class="row justify-content-start"><div class="col-12 col-md-8"><div class="service service-single"><div class=content><p>This month we publish a video provided by S. Brenner @ Brown University, USA.</p><p>In a new paper in Geophysical Research Letters, S. Brenner and members of the SASIP team investigate floe-scale effects on ice-ocean boundary layer turbulence. These numerical simulations of the marginal ice zone, produced with the &ldquo;FloeDyn&rdquo; sea ice discrete element model, show sea ice motion together with the underying ocean current field (white/blue colourmap and vector arrows shows), followed by the associated turbulence generation under the ice (cyan/red colourmap). Three different floe size distributions are investigated. Despite maintaing the same bulk sea ice concentration (50%) and ocean forcing for each of the cases shown, distinct turbulence patterns emerge for the three floe size distributions. Read the paper: <a href=https://doi.org/10.1029/2023GL105703><strong><em>Scale-Dependent Air-Sea Exchange in the Polar Oceans: Floe-Floe and Floe-Flow Coupling in the Generation of Ice-Ocean Boundary Layer Turbulence</em></strong></a>.</p><p><div style=position:relative;padding-bottom:56.25%;height:0;overflow:hidden><iframe src=https://www.youtube.com/embed/oiFVlW3Ob28 style=position:absolute;top:0;left:0;width:100%;height:100%;border:0 allowfullscreen title="YouTube Video"></iframe></div><em>Fig.: Movie produced by S. Brenner @ Brown University, USA.
 Ocean current field and sea ice motion, 50%SIC, large floes.
 Sea ice floes are modelled using &ldquo;FloeDyn&rdquo; (Rabatel et. al., 2015; <a href=https://doi.org/10.1002/2015JC010909)>https://doi.org/10.1002/2015JC010909)</a>.</em></p><hr><hr><p><div style=position:relative;padding-bottom:56.25%;height:0;overflow:hidden><iframe src=https://www.youtube.com/embed/kX032chFaS4 style=position:absolute;top:0;left:0;width:100%;height:100%;border:0 allowfullscreen title="YouTube Video"></iframe></div><em>Fig.: Movie produced by S. Brenner @ Brown University, USA.
 Ocean current field and sea ice motion, 50%SIC, medium floes.