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WACSWAIN SIGNED

WArm Climate Stability of the West Antarctic ice sheet in the last INterglacial (WACSWAIN)

Total Cost €

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EC-Contrib. €

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Partnership

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 WACSWAIN project word cloud

Explore the words cloud of the WACSWAIN project. It provides you a very rough idea of what is the project "WACSWAIN" about.

temporal    emissions    recent    isostatic    glacio    gi    spatial    interglacial    data    site    shelves    signature    content    atmospheric    concentrations    sea    ross    centuries    mainly    circulation    estimate    retrieval    time    worrying    lack    2500    leave    130    direct    profile    recognisable    global    salt    antarctic    shelf    authors    co2    uplift    ronne    cores    of    last    few    remedy    sheets    came    outputs    warmth    question    aerosol    placed    rising    retreat    climate    ice    strategically    inferred    lost    obtain    obtaining    sensitive    critical    marine    pattern    sheet    periphery    course    assume    drilled    isotope    peripheral    contributed    timing    wais    west    metres    predict    isotopes    air    questions    models    water    ourselves    papers    core    115    surprising    ago    lig    caps    smaller    committing    predictions    realistic    clear    symptoms    proxies    reached    significantly    model    temperatures    bedrock    examine    regrowth   

Project "WACSWAIN" data sheet

The following table provides information about the project.

Coordinator
THE CHANCELLOR MASTERS AND SCHOLARSOF THE UNIVERSITY OF CAMBRIDGE 

Organization address
address: TRINITY LANE THE OLD SCHOOLS
city: CAMBRIDGE
postcode: CB2 1TN
website: www.cam.ac.uk

contact info
title: n.a.
name: n.a.
surname: n.a.
function: n.a.
email: n.a.
telephone: n.a.
fax: n.a.

 Coordinator Country United Kingdom [UK]
 Total cost 2˙817˙554 €
 EC max contribution 2˙817˙554 € (100%)
 Programme 1. H2020-EU.1.1. (EXCELLENT SCIENCE - European Research Council (ERC))
 Code Call ERC-2016-ADG
 Funding Scheme ERC-ADG
 Starting year 2017
 Duration (year-month-day) from 2017-08-01   to  2022-07-31

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    THE CHANCELLOR MASTERS AND SCHOLARSOF THE UNIVERSITY OF CAMBRIDGE UK (CAMBRIDGE) coordinator 1˙302˙035.00
2    UNITED KINGDOM RESEARCH AND INNOVATION UK (SWINDON) participant 1˙515˙518.00
3    NATURAL ENVIRONMENT RESEARCH COUNCIL UK (SWINDON WILTSHIRE) participant 0.00

Map

Leaflet | Map data © OpenStreetMap contributors, CC-BY-SA, Imagery © Mapbox

 Project objective

Recent papers predict the loss of most of the West Antarctic Ice Sheet (WAIS) by 2500 if CO2 emissions and rising global temperatures are not controlled. It is critical to test whether the models making such worrying predictions are realistic. I will do this by obtaining new data from the last interglacial (LIG, 130,000-115,000 years ago) to assess the response of the WAIS to comparable warmth.

During the LIG, sea level reached 6-9 m higher than today. It is inferred that Antarctic ice sheets contributed several metres of sea level rise, under a climate similar to the one we could be committing ourselves to in the next few centuries. Most authors assume that the lost ice came mainly from the WAIS. Models that predict large ice loss in the future also produce a very significant retreat of the WAIS and loss of the Ross and Ronne ice shelves under LIG conditions.

Were the WAIS and Ronne Ice Shelf significantly smaller in the LIG? If so, what was the time course of their retreat and regrowth? This project will remedy the surprising lack of direct evidence about these questions. I will examine data from ice cores that reach the LIG, drilled on the periphery of the WAIS. I will include retrieval of one new strategically-placed bedrock core, and obtain an isotope profile that will test the potential of another site. The loss of much of the WAIS would have several effects on peripheral ice caps: glacio-isostatic (GI) uplift and a change in atmospheric circulation would cause a recognisable spatial and temporal pattern of symptoms. The retreat of the Ronne Ice Shelf would leave a clear signature in marine aerosol concentrations in the ice. By examining changes in water isotopes, sea salt, air content and other proxies in all the cores, in comparison with different model outputs, I will estimate the timing and extent of WAIS retreat and regrowth during the LIG. This will support or question the use of sensitive models to predict future change in the WAIS.

 Publications

year authors and title journal last update
List of publications.
2019 Laurie Menviel, Emilie Capron, Aline Govin, Andrea Dutton, Lev Tarasov, Ayako Abe-Ouchi, Russell N. Drysdale, Philip L. Gibbard, Lauren Gregoire, Feng He, Ruza F. Ivanovic, Masa Kageyama, Kenji Kawamura, Amaelle Landais, Bette L. Otto-Bliesner, Ikumi Oyabu, Polychronis C. Tzedakis, Eric Wolff, Xu Zhang
The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0
published pages: 3649-3685, ISSN: 1991-9603, DOI: 10.5194/gmd-12-3649-2019
Geoscientific Model Development 12/8 2020-03-23
2020 Eric Wolff, Robert Mulvaney, Sentia Goursaud, Mackenzie Grieman, Helene Hoffmann, Jack Humby, Amy King, Emily Ludlow, Shaun Miller, Christoph Nehrbass‐Ahles, Scott Polfrey, Julius Rix, Isobel Rowell, Rebecca Tuckwell
What happened to WAIS during the last interglacial? ‐ how the new Skytrain Ice Rise core will help to answer that (abstract)
published pages: 73, ISSN: , DOI:
QUATERNARY RESEARCH ASSOCIATION ANNUAL DISCUSSION MEETING ABSTRACTS Annual 2020-03-23

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