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<p class="MsoNormal">Dear Colleagues [apologies if you receive this multiple times]<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">The centennial IUGG is this year in Montreal, Canada (July 8-18)
<o:p></o:p></p>
<p class="MsoNormal"><a href="http://iugg2019montreal.com/jg.html">http://iugg2019montreal.com/jg.html</a><o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">We welcome abstracts submitted to the following session via <a href="http://iugg2019montreal.com/abstract-submission.html">
http://iugg2019montreal.com/abstract-submission.html</a> (abstract deadline is <span style="font-size:10.5pt;font-family:"Arial",sans-serif;color:black;background:white">
February 18, 2019)</span><o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">JG01  - INTERACTIONS OF SOLID EARTH, ICE SHEETS AND OCEANS  (IAG, IACS, IASPEI)
<o:p></o:p></p>
<p class="MsoNormal">Description:<o:p></o:p></p>
<p class="MsoNormal">Measurements of solid Earth, sea-level and ice-sheet change are influenced by a complex interaction of processes occurring over a large range of spatial and temporal scales. Proxy observations that constrain past ice sheets are influenced
 by glacial isostatic adjustment and changing mantle dynamic topography. Present-day observations of solid Earth deformation in one location are affected by present and past changes in global surface loading. Recent work highlights the role that solid Earth
 deformation has to play in controlling ice-sheet change, while seismological investigations are revealing crucial spatial variations in Earth rheology. In this symposium, we showcase model- and data-driven efforts to understand feedbacks between surface load
 changes and the solid Earth over all timescales.<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">Topics of interest include (but are not limited to):<o:p></o:p></p>
<ul style="margin-top:0cm" type="disc">
<li class="MsoNormal" style="mso-list:l1 level1 lfo3">observations of mass changes in the cryosphere and oceans, and their interaction with solid Earth deformation<o:p></o:p></li><li class="MsoNormal" style="mso-list:l1 level1 lfo3">influence of mantle dynamic topography and glacial isostatic adjustment on paleo observations of sea level or ice sheet behaviour<o:p></o:p></li><li class="MsoNormal" style="mso-list:l1 level1 lfo3">seismic studies of the rheology of the solid Earth in the context of sea-level and ice-sheet studies<o:p></o:p></li></ul>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal">Co-Conveners: Matt King (Australia, IACS/IAG), Pippa Whitehouse (UK, IACS/IAG), Martin Horwath (Germany, IAG), Bert Wouters (Netherlands, IACS), Anya Reading (Australia, IASPEI)<o:p></o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><o:p> </o:p></p>
<p class="MsoNormal"><b><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;mso-fareast-language:EN-AU">Matt King<o:p></o:p></span></b></p>
<p class="MsoNormal"><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;mso-fareast-language:EN-AU">Professor of Polar Geodesy | Head of Discipline, Geography and Spatial Sciences
<o:p></o:p></span></p>
<p class="MsoNormal"><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;mso-fareast-language:EN-AU">Discipline of Geography and Spatial Sciences | School of Technology, Environments and Design | College of Sciences and Engineering<o:p></o:p></span></p>
<p class="MsoNormal"><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;mso-fareast-language:EN-AU">Private Bag 76, University of Tasmania, Hobart, Tasmania, 7001, Australia<o:p></o:p></span></p>
<p class="MsoNormal"><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;mso-fareast-language:EN-AU">Office: Room 161, Surveying and Spatial Sciences | w3w.co/stormed.hungry.rods
<o:p></o:p></span></p>
<p class="MsoNormal"><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;mso-fareast-language:EN-AU">+61 3 6226 1974 |
<a href="mailto:Matt.King@utas.edu.au"><span style="color:blue">Matt.King@utas.edu.au</span></a> | Skype mattking_ncl | Twitter @DeformedEarth<o:p></o:p></span></p>
<p class="MsoNormal"><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;color:#4472C4;mso-fareast-language:EN-AU"><a href="http://www.utas.edu.au/profiles/staff/cose-ted/matt-king"><span style="color:blue">www.utas.edu.au/profiles/staff/cose-ted/matt-king</span></a>
</span><span style="font-size:7.5pt;font-family:"Verdana",sans-serif;color:blue;mso-fareast-language:EN-AU"><a href="http://www.utas.edu.au/geophysics"><span style="color:blue;text-decoration:none">www.utas.edu.au/geophysics</span></a><u>
<o:p></o:p></u></span></p>
<p class="MsoNormal"><span style="font-size:10.0pt;font-family:"Courier New";mso-fareast-language:EN-AU"><o:p> </o:p></span></p>
<p class="MsoNormal"><span style="font-size:10.0pt;font-family:"Courier New";mso-fareast-language:EN-AU">CRICOS 00586B<o:p></o:p></span></p>
<p class="MsoNormal"><o:p> </o:p></p>
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<p style="font-size:10pt; line-height:10pt; font-family: Calibri,sans-serif;"><br>
<br>
University of Tasmania Electronic Communications Policy (December, 2014). <br>
This email is confidential, and is for the intended recipient only. Access, disclosure, copying, distribution, or reliance on any of it by anyone outside the intended recipient organisation is prohibited and may be a criminal offence. Please delete if obtained
 in error and email confirmation to the sender. The views expressed in this email are not necessarily the views of the University of Tasmania, unless clearly intended otherwise.
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