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BEGIN:VEVENT
UID:420ff3edb57d168575686b1c37722c82
CATEGORIES:Polar Conferences, Meetings and Events
CREATED:20170609T143750
SUMMARY:Multi-scale Modeling of Sea Ice Characteristics and Behavior
LOCATION:Cambridge\, United Kingdom
DESCRIPTION:<p style="text-align: center;"><strong><span style="color: #000000; font-fa
 mily: Helvetica; font-size: 12px; font-style: normal; letter-spacing: norma
 l; text-align: start; text-indent: 0px; text-transform: none; white-space: 
 normal; word-spacing: 0px; float: none;">Call for Registration: Multi-scale
  Modeling of Sea Ice Characteristics and Behavior; Isaac Newton Institute f
 or Mathematical Sciences<br />11-15 September 2017, Cambridge, United Kingd
 om</span></strong></p><p>&nbsp;</p><p>This workshop will address sea ice pr
 ocesses across a wide range of lengths and time scales, with an emphasis on
  understanding emergent and scale-invariant phenomena. Mathematical methods
  that account for the smaller scale processes and enable computation and an
 alysis of these processes' effect on larger scales relevant for coarse-grai
 ned climate models will be a focus of the workshop and linkage of scales is
  a central theme of this workshop.</p><p><strong>Registration deadline: Sun
 day, 11 June 2017.</strong></p><p><em>Workshop Theme:</em></p><p>Realistic 
 models of Earth's climate system are essential to making projections about 
 what we may experience as our climate changes. Polar sea ice forms a critic
 al system component which must be accurately accounted for in global climat
 e models. It forms the thin boundary layer coupling the polar oceans and at
 mosphere and has seen rather dramatic changes over the past two or three de
 cades. An important feature of sea ice is that it displays rich structure a
 nd behavior on scales ranging over 10 orders of magnitude, length scales fr
 om microns to hundreds of kilometers, and time scales from milliseconds to 
 decades. This broad range of scales for sea ice structure and properties is
  relevant to biological, chemical, industrial, weather, and climate-related
  processes. It also leads to sea ice structure at certain scales being simi
 lar to other materials such as porous human bone and polycrystalline metals
 , which can be used to bring new techniques to studying sea ice.</p><p>The 
 complex behavior of sea ice over such a large range of scales presents a fu
 ndamental challenge to modeling these systems. For example, many key proces
 ses, whose relevant length scales may be centimeters or meters to kilometer
 s, impact climate and must be incorporated into largescale numerical climat
 e models with grid sizes often on the order of tens of kilometers. Moreover
 , some sea ice properties exhibit scale invariance or predictable scale dep
 endence while others appear to be wholly emergent, a consequence of interac
 ting processes within and applied to the ice cover.</p><p><em>Potential wor
 kshop topics include:</em></p><p>- Large-scale numerical models of the evol
 ution of polar sea ice;<br />- Sea ice simulations including variability, p
 redictability, and climate projections;<br />- Sea ice microphysics, fluid 
 transport, convection, and the porous brine microstructure;<br />- Melt pon
 ds on Arctic sea ice;<br />- Ice thickness distribution, melting, freezing,
  mechanical redistribution, ridging, and rafting;<br />- Waves in the margi
 nal ice zone;<br />- Scaling in sea ice fracture and dynamics, sea ice rheo
 logy;<br />- Momentum balance including form drag, interactions with curren
 ts, tides and winds;<br />- Sea ice thermodynamics and exchange processes;<
 br />- Low order models of polar climate;<br />- Tipping point phenomena; a
 nd<br />- Stochastic processes in sea ice modeling.</p><p>For more informat
 ion about the workshop and to apply for registration, go to: <a href="https
 ://www.newton.ac.uk/event/sipw01">https://www.newton.ac.uk/event/sipw01</a>
 .</p><p>For questions, contact:<br />Daniel Feltham<br />Email: <span id="c
 loak61a9c8dc5f17c925c4eeea6220f6e02b">This email address is being protected
  from spambots. You need JavaScript enabled to view it.</span><script type=
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CONTACT:This email address is being protected from spambots. You need JavaScript enabled to view it.
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DTSTAMP:20260418T053949Z
DTSTART;TZID=UTC;VALUE=DATE:20170911
DTEND;TZID=UTC;VALUE=DATE:20170916
SEQUENCE:0
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