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UID:d0b2f6862d4d80ed7febe6405f4328f0
CATEGORIES:Polar Conferences, Meetings and Events
CREATED:20170809T114724
SUMMARY:Future Developments in Climate Sea Ice Modelling
LOCATION:University of Cambridge\, UK
DESCRIPTION:Future Developments in Climate Sea Ice Modeling\n25 September 2017\nCambrid
 ge, United Kingdom\nTo register for the workshop, go to the workshop regist
 ration webpage. (https://www.arcus.org/sites/all/modules/civicrm/extern/url
 .php?u=3775&amp;qid=221659)\nMore information is available on the workshop 
 homepage. (https://www.arcus.org/sites/all/modules/civicrm/extern/url.php?u
 =3776&amp;qid=221659)\nOrganizers invite registration for a workshop entitl
 ed, "Future Developments in Climate Sea Ice Modeling." This workshop will c
 onvene 25 September 2017 at the University of Cambridge in Cambridge, Unite
 d Kingdom.\nThis one-day event will address climate model representation of
  sea ice and the fundamental and applied issues in mathematical modeling of
  sea ice. In particular, it will seek to identify future priorities for cli
 mate sea ice model development. The workshop will include the presentation 
 and discussion of different views and modeling approaches, issues relevant 
 to adequate simulation of sea ice from the perspective of the mathematical 
 modeler, and will be relevant to those working on climate models, specifica
 lly for sea ice.\n \nBackground\nObservations, theory and numerical modelli
 ng strongly indicate a substantial alteration of the Earth’s climate with g
 lobal average warming in the coming decades. Our understanding of current a
 nd future climate is substantially derived from climate models. Climate mod
 els solve systems of equations that simulate the circulation and physical e
 volution of the Earth’s atmosphere, ocean, land surface, and cryosphere. Se
 a ice, an important component of the cryosphere, provides a partial barrier
  to exchanges of momentum, heat, and freshwater between the atmosphere and 
 ocean and is a complex composite of ice and brine that exhibits varying str
 uctural, thermodynamic and mechanical properties across a range of length a
 nd timescales. The last decade’s rapid and substantial reduction of the Arc
 tic sea ice cover has been widely reported and further changes are expected
  in the coming years. While loss of sea ice will not alter sea level, it do
 es alter the exchanges and feedbacks between the atmosphere and ocean and h
 as a significant impact on the polar regions and global climate through its
  impact on atmospheric and oceanic circulations. \n \nThis one-day event sp
 ecifically addresses climate model representation of sea ice and will addre
 ss fundamental and applied issues in mathematical modelling of sea ice. In 
 particular, it will seek to identify future priorities for climate sea ice 
 model development.\n \nAims and Objectives\nTo identify priorities for futu
 re climate sea ice model development, we will discuss the following questio
 ns:\nWhat do climate models need sea ice for?\nA top-down, system level vie
 w of what sea ice models should produce from the perspective of a climate m
 odeller.\nWhat sea ice physics is missing from models?\nA bottom-up view of
  what is missing from current sea ice models from the perspective of a sea 
 ice scientist.\nWhat modelling approaches can be used to address the comple
 xity of sea ice and the needs of climate models?\nThis workshop will enable
  the presentation and discussion of different views and modelling approache
 s, as well as issues relevant to adequate simulation of sea ice from the pe
 rspective of the mathematical modeller. It will be of interest and relevanc
 e to those working on climate models, specifically for sea ice.\nTo book an
  appointment, please email This email address is being protected from spamb
 ots. You need JavaScript enabled to view it.
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X-ALT-DESC;FMTTYPE=text/html:<p><strong>Future Developments in Climate Sea Ice Modeling</strong></p><p><
 strong>25 September 2017</strong><br /><strong>Cambridge, United Kingdom</s
 trong></p><p>To register for the workshop, go to the <a href="https://www.a
 rcus.org/sites/all/modules/civicrm/extern/url.php?u=3775&amp;qid=221659" ta
 rget="_blank" rel="noopener noreferrer">workshop registration webpage.</a><
 /p><p>More information is available on the <a href="https://www.arcus.org/s
 ites/all/modules/civicrm/extern/url.php?u=3776&amp;qid=221659" target="_bla
 nk" rel="noopener noreferrer">workshop homepage.</a></p><p>Organizers invit
 e registration for a workshop entitled, "Future Developments in Climate Sea
  Ice Modeling." This workshop will convene 25 September 2017 at the Univers
 ity of Cambridge in Cambridge, United Kingdom.</p><p>This one-day event wil
 l address climate model representation of sea ice and the fundamental and a
 pplied issues in mathematical modeling of sea ice. In particular, it will s
 eek to identify future priorities for climate sea ice model development. Th
 e workshop will include the presentation and discussion of different views 
 and modeling approaches, issues relevant to adequate simulation of sea ice 
 from the perspective of the mathematical modeler, and will be relevant to t
 hose working on climate models, specifically for sea ice.</p><p>&nbsp;</p><
 p><strong>Background</strong></p><p>Observations, theory and numerical mode
 lling strongly indicate a substantial alteration of the Earth’s climate wit
 h global average warming in the coming decades. Our understanding of curren
 t and future climate is substantially derived from climate models. Climate 
 models solve systems of equations that simulate the circulation and physica
 l evolution of the Earth’s atmosphere, ocean, land surface, and cryosphere.
  Sea ice, an important component of the cryosphere, provides a partial barr
 ier to exchanges of momentum, heat, and freshwater between the atmosphere a
 nd ocean and is a complex composite of ice and brine that exhibits varying 
 structural, thermodynamic and mechanical properties across a range of lengt
 h and timescales. The last decade’s rapid and substantial reduction of the 
 Arctic sea ice cover has been widely reported and further changes are expec
 ted in the coming years. While loss of sea ice will not alter sea level, it
  does alter the exchanges and feedbacks between the atmosphere and ocean an
 d has a significant impact on the polar regions and global climate through 
 its impact on atmospheric and oceanic circulations. <br /> <br />This one-d
 ay event specifically addresses climate model representation of sea ice and
  will address fundamental and applied issues in mathematical modelling of s
 ea ice. In particular, it will seek to identify future priorities for clima
 te sea ice model development.<br /> <br /><strong>Aims and Objectives</stro
 ng></p><p>To identify priorities for future climate sea ice model developme
 nt, we will discuss the following questions:</p><p>What do climate models n
 eed sea ice for?<br />A top-down, system level view of what sea ice models 
 should produce from the perspective of a climate modeller.</p><p>What sea i
 ce physics is missing from models?<br />A bottom-up view of what is missing
  from current sea ice models from the perspective of a sea ice scientist.</
 p><p>What modelling approaches can be used to address the complexity of sea
  ice and the needs of climate models?</p><p>This workshop will enable the p
 resentation and discussion of different views and modelling approaches, as 
 well as issues relevant to adequate simulation of sea ice from the perspect
 ive of the mathematical modeller. It will be of interest and relevance to t
 hose working on climate models, specifically for sea ice.</p><p>To book an 
 appointment, please email <span id="cloak90320cb42cce853415313055184a3ca7">
 This email address is being protected from spambots. You need JavaScript en
 abled to view it.</span><script type='text/javascript'>
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CONTACT:Daniel Feltham
DTSTAMP:20261013T123437
DTSTART;TZID=UTC;VALUE=DATE:20170925
DTEND;TZID=UTC;VALUE=DATE:20170926
SEQUENCE:0
TRANSP:OPAQUE
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