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VEILA SIGNED

Identifying the source of unknown volcanic eruptions in Late Antiquity

Total Cost €

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EC-Contrib. €

0

Partnership

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 VEILA project word cloud

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

potentially    period    cooling    equatorial    played    correlating    circa    sulphate    glaciology    notably    sulphur    implicated    sediment    unknown    eurasian    antarctic    outputs    fingerprints    7th    era    century    centennial    upheavals    eruptions    680    ashes    forcing    deposition    empires    regional    migrations    trapped    horizons    interdisciplinary    aerosols    particles    reorganisations    ash    human    veils    caused    occurred    left    inform    530    impacts    stratospheric    atmosphere    societal    geochemical    tephrochronologists    shorter    coincides    age    shaped    volcanic    arctic    political    characterising    climate    trajectory    temporal    interface    little    contributed    demise    ice    ce    methodological    lake    1300    micrometric    polar    sources    volcanism    dendrochronology    locate    global    source    6th    correlations    eurasia    lia    suspected    clustering    tephrochronology    history    samples    climatology    antique    cooler    archives    extract    dispersal    1850    cores    lalia    climatic    latter    series    episode    travelled   

Project "VEILA" 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 183˙454 €
 EC max contribution 183˙454 € (100%)
 Programme 1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
 Code Call H2020-MSCA-IF-2017
 Funding Scheme MSCA-IF-EF-ST
 Starting year 2019
 Duration (year-month-day) from 2019-02-01   to  2021-01-31

 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 183˙454.00

Map

 Project objective

Volcanism has shaped the human trajectory as a result of the regional impacts of ash deposition and through global climate change caused by stratospheric veils of volcanic sulphate aerosols. Volcanic forcing of climate is suspected to be implicated in centennial scale climatic cooling during the Common Era, notably in triggering the Little Ice Age (LIA, circa 1300-1850 CE), and the shorter but cooler Late Antique Little Ice Age (LALIA, circa 530-680 CE). The latter episode would have contributed to major societal reorganisations that occurred across Eurasia, including the rise and demise of empires, migrations and political upheavals. The LALIA coincides with a series of large volcanic eruptions of unknown source, only identified by sulphur-rich horizons in polar ice cores, left by aerosols trapped in the ice after dispersal through the high atmosphere. This project aims to locate the volcanic sources of these unknown 6th and 7th century eruptions, by characterising and correlating their geochemical fingerprints in global archives, including Antarctic and Arctic ice cores and equatorial lake sediment cores. An interdisciplinary approach at the interface of glaciology, tephrochronology, dendrochronology, and climatology will be used to extract and analyse micrometric particles of far-travelled ashes and to identify correlations between different the samples and potentially to identify the source. The results of the proposed research will provide methodological advances of wider interest to tephrochronologists, and will facilitate modelling of the climate impacts of these eruptions. The outputs will provide a better understanding of the role of volcanism in centennial scale climate cooling during the Common Era, and inform the extent to which volcanism and associated climate forcing played a role in Eurasian history in the Late Antique period. They will also be relevant to understanding the potential impacts of future temporal clustering of climate-forcing eruptions.

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The information about "VEILA" are provided by the European Opendata Portal: CORDIS opendata.

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