BEGIN:VCALENDAR VERSION:2.0 PRODID:-//jEvents 2.0 for Joomla//EN CALSCALE:GREGORIAN METHOD:PUBLISH BEGIN:VEVENT UID:5af5779b2fbd18e9b8d823771f02f4ff CATEGORIES:Polar Conferences, Meetings and Events CREATED:20171123T150627 SUMMARY:Antarctic Surface Hydrology and Future Ice-shelf Stability LOCATION:Lamont-Doherty Earth Observatory\, Palisades\, New York DESCRIPTION:Workshop on Antarctic Surface Hydrology and Future Ice-shelf Stability\nat Lamont-Doherty Earth Observatory, Palisades, New York, on February 21st to 23rd, 2018.\nA number of research groups are currently examining processes related to coupling between surface meltwater production and future Antarct ic ice loss. Recent studies have suggested that surface hydrological system s in Antarctica may expand and proliferate this century. Meanwhile, numeric al models of the Antarctic Ice Sheet that incorporate meltwater's impact on ice shelves, predict Antarctic contributions of up to a meter of global se a-level rise this century in response to atmospheric warming.\nGiven the em erging interest in surface hydrology, ice-shelf stability and future sea-le vel rise, it is vital for the scientific community to come together to iden tify and address critical knowledge gaps in this field.\nThis workshop will bring together scientists with expertise in ice-sheet dynamics, glacial hy drology, climatology and other disciplines in order to move the community t owards answering several fundamental questions raised by observations of An tarctic surface hydrological processes. \n\nThese could include: \nWhat cli mate dynamics are responsible for surface meltwater generation in Antarctic a? \nWhat controls the spatiotemporal distribution of meltwater ponds on An tarctic ice shelves? \nWhere is meltwater generated, where does it pond tod ay and how will this change this century? \nWhat controls the movement of w ater across the ice surface and into the sub-surface of Antarctic ice shelv es?\nHow will meltwater impact the stability of ice shelves this century?\n Specifically we aim to: \n(1) Establish the state-of-the-science of Antarct ic surface hydrology,\n(2) Identify key research questions and future prior ities in this field, and\n(3) Facilitate collaborations\nThe workshop will consist of short science talks, poster sessions and group discussions on va rious topics within this broad field. Oral and poster presentations could r eport modelling studies, remote sensing, fieldwork, laboratory experiments related to any aspect of the dynamics of Antarctic surface meltwater and ic e shelves.\nIf you would like to attend please email abstracts (300 word li mit), including affiliation information to Frances Simpson (This email addr ess is being protected from spambots. You need JavaScript enabled to view i t. document.getElementById('cloak8aae0c643bfe19f895c17d6751491ef6').inn erHTML = ''; var prefix = 'ma' + 'il' + 'to'; var pa th = 'hr' + 'ef' + '='; var addy8aae0c643bfe19f895c17d6751491ef6 = 'fs& #105;mpson' + '@'; addy8aae0c643bfe19f895c17d6751491ef6 = addy 8aae0c643bfe19f895c17d6751491ef6 + 'ldeo' + '.' + 'col&# 117;mbia' + '.' + 'edu'; var addy_text8aae0c643b fe19f895c17d6751491ef6 = 'fsimpson' + '@' + 'ldeo' + '.' + 'columbia' + '.' + 'edu';docum ent.getElementById('cloak8aae0c643bfe19f895c17d6751491ef6').innerHTML += '< a ' + path + '\'' + prefix + ':' + addy8aae0c643bfe19f895c17d6751491ef6 + ' \'>'+addy_text8aae0c643bfe19f895c17d6751491ef6+''; ) by January 8th, 2018 . Attendance is limited to around 30 people, so if necessary, abstracts wil l be chosen by the organizing committee based on scientific relevance and d iversity, and maximizing gender, geographic and career-stage diversity..\nW e are very keen to encourage the participation of early-career scientists a nd under-represented groups of scientists! We have NSF funding to support t ravel for a limited number of US-based attendees. This funding will be dist ributed on the basis of need, the potential benefit to early-career scienti sts and the scientific and diversity considerations listed above. Sorry, on ly US-based applicants are eligible for travel support.\nIf you would like to apply for travel support, please include in your application (in additio n to your abstract) a separate statement including the length of time since obtaining your last degree, a description of your need for funding and the potential benefit to you that attending this workshop could bring (300 wor d limit).\nPlease feel free to contact any of the organizing committee for more details before submitting.\n X-ALT-DESC;FMTTYPE=text/html:

Workshop on Antarctic Surface Hydrology and Future Ice-shelf Sta bility

at Lamont-Doherty Earth Observatory, Palisade s, New York, on February 21st to 23rd, 2018.

A number of res earch groups are currently examining processes related to coupling between surface meltwater production and future Antarctic ice loss. Recent studies have suggested that surface hydrological systems in Antarctica may expand a nd proliferate this century. Meanwhile, numerical models of the Antarctic I ce Sheet that incorporate meltwater's impact on ice shelves, predict Antarc tic contributions of up to a meter of global sea-level rise this century in response to atmospheric warming.

Given the emerging interest in surf ace hydrology, ice-shelf stability and future sea-level rise, it is vital f or the scientific community to come together to identify and address critic al knowledge gaps in this field.

This workshop will bring together sc ientists with expertise in ice-sheet dynamics, glacial hydrology, climatolo gy and other disciplines in order to move the community towards answering s everal fundamental questions raised by observations of Antarctic surface hy drological processes.

These could include:
What climate dynamics are responsible for surface meltwater generation i n Antarctica?
What controls the spatiotemporal distribution of meltwa ter ponds on Antarctic ice shelves?
Where is meltwater generated, whe re does it pond today and how will this change this century?
What con trols the movement of water across the ice surface and into the sub-surface of Antarctic ice shelves?
How will meltwater impact the stability of ice shelves this century?

Specifically we aim to: (1) Establish the state-of-the-science of Antarctic surface hydrology,< br />(2) Identify key research questions and future priorities in this fiel d, and
(3) Facilitate collaborations

The workshop will consist o f short science talks, poster sessions and group discussions on various top ics within this broad field. Oral and poster presentations could report mod elling studies, remote sensing, fieldwork, laboratory experiments related t o any aspect of the dynamics of Antarctic surface meltwater and ice shelves .

If you would like to attend please email abstracts (300 word limit) , including affiliation information to Frances Simpson (This email address is being protected from sp ambots. You need JavaScript enabled to view it. ) by January 8th, 2018. Attendance is limited to around 30 people, so if necessary, abstracts will be chosen by the organizing commit tee based on scientific relevance and diversity, and maximizing gender, geo graphic and career-stage diversity..

We are very keen to encourage th e participation of early-career scientists and under-represented groups of scientists! We have NSF funding to support travel for a limited number of U S-based attendees. This funding will be distributed on the basis of need, t he potential benefit to early-career scientists and the scientific and dive rsity considerations listed above. Sorry, only US-based applicants are elig ible for travel support.

If you would like to apply for travel suppor t, please include in your application (in addition to your abstract) a sepa rate statement including the length of time since obtaining your last degre e, a description of your need for funding and the potential benefit to you that attending this workshop could bring (300 word limit).

Please fee l free to contact any of the organizing committee for more details before s ubmitting.

CONTACT:This email address is being protected from spambots. You need JavaScript enabled to view it. document.getElementById('cloakd4693e9e2ea86c687218bdf8e00467fe').innerHTML = ''; var prefix = 'ma' + 'il' + 'to'; var path = 'hr' + 'ef' + '='; var addyd4693e9e2ea86c687218bdf8e00467fe = 'j.kingslake' + '@'; addyd4693e9e2ea86c687218bdf8e00467fe = addyd4693e9e2ea86c687218bdf8e00467fe + 'columbia' + '.' + 'edu'; var addy_textd4693e9e2ea86c687218bdf8e00467fe = 'j.kingslake' + '@' + 'columbia' + '.' + 'edu';document.getElementById('cloakd4693e9e2ea86c687218bdf8e00467fe').innerHTML += ''+addy_textd4693e9e2ea86c687218bdf8e00467fe+''; , This email address is being protected from spambots. You need JavaScript enabled to view it. document.getElementById('cloakd1cd537c664c40142619dbb2c50f04c5').innerHTML = ''; var prefix = 'ma' + 'il' + 'to'; var path = 'hr' + 'ef' + '='; var addyd1cd537c664c40142619dbb2c50f04c5 = 'trusel' + '@'; addyd1cd537c664c40142619dbb2c50f04c5 = addyd1cd537c664c40142619dbb2c50f04c5 + 'rowan' + '.' + 'edu'; var addy_textd1cd537c664c40142619dbb2c50f04c5 = 'trusel' + '@' + 'rowan' + '.' + 'edu';document.getElementById('cloakd1cd537c664c40142619dbb2c50f04c5').innerHTML += ''+addy_textd1cd537c664c40142619dbb2c50f04c5+''; , This email address is being protected from spambots. You need JavaScript enabled to view it. document.getElementById('cloakc99e0f5a7e8358d21eadb4ed8b269afb').innerHTML = ''; var prefix = 'ma' + 'il' + 'to'; var path = 'hr' + 'ef' + '='; var addyc99e0f5a7e8358d21eadb4ed8b269afb = 'mtedesco' + '@'; addyc99e0f5a7e8358d21eadb4ed8b269afb = addyc99e0f5a7e8358d21eadb4ed8b269afb + 'ldeo' + '.' + 'columbia' + '.' + 'edu'; var addy_textc99e0f5a7e8358d21eadb4ed8b269afb = 'mtedesco' + '@' + 'ldeo' + '.' + 'columbia' + '.' + 'edu';document.getElementById('cloakc99e0f5a7e8358d21eadb4ed8b269afb').innerHTML += ''+addy_textc99e0f5a7e8358d21eadb4ed8b269afb+''; DTSTAMP:20260422T003431Z DTSTART;TZID=UTC;VALUE=DATE:20180221 DTEND;TZID=UTC;VALUE=DATE:20180224 SEQUENCE:0 TRANSP:OPAQUE END:VEVENT END:VCALENDAR