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SYNC

Synchronizing Palaeoclimate data for better understanding of the Solar effect on European Climate

Total Cost €

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EC-Contrib. €

0

Partnership

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 SYNC project word cloud

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

novelty    plateaux    reliably    periodic    abruptness    holocene    records    solar    modulated    tackle    decreasing    mere    royal    counting    grand    few    innovate    shifts    velocity    holloway    time    dating    varve    london    supports    accurate    sediments    existence    varved    gaps    core    resolved    tephrochronology    store    1996    methodological    correlated    tephra    lakes    seasonal    minimize    eruptions    diss    2020    phasing    explosive    14c    magnitude    describing    annually    palaeoclimate    facilities    uncertain    sun    cosmogenic    isotopes    trigger    layers    natural    ages    abrupt    proxy    ed    reconstructions    minimum    maar    germany    error    meerfelder    estimating    ash    perspective    lies    absolute    centennial    forcing    synchronization    timing    resolution    2070    quasic    volcanic    england    decadal    hampered    community    precise    atmospheric    markers    archives    chronologies    interdisciplinary    deposited    multidisciplinary    climatic    university    designed    synchronous    signals    climate    eruption    individual    variability    synchronously    data    minima   

Project "SYNC" data sheet

The following table provides information about the project.

Coordinator
ROYAL HOLLOWAY AND BEDFORD NEW COLLEGE 

Organization address
address: EGHAM HILL UNIVERSITY OF LONDON
city: EGHAM
postcode: TW20 0EX
website: http://www.rhul.ac.uk

contact info
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name: n.a.
surname: n.a.
function: n.a.
email: n.a.
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 Coordinator Country United Kingdom [UK]
 Project website https://pure.royalholloway.ac.uk/portal/en/projects/synchronizing-palaeoclimate-data-for-better-understanding-of-hte-solar-effect-on-european-climate
 Total cost 195˙454 €
 EC max contribution 195˙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-2015
 Funding Scheme MSCA-IF-EF-ST
 Starting year 2016
 Duration (year-month-day) from 2016-09-01   to  2018-08-31

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    ROYAL HOLLOWAY AND BEDFORD NEW COLLEGE UK (EGHAM) coordinator 195˙454.00

Map

 Project objective

The sun activity is decreasing since 1996 and a grand solar minimum is expected to occur from 2020 to 2070. The magnitude of solar forcing on the current climate is still uncertain. This project aims to test the existence of quasic-periodic decadal to centennial natural climate variability modulated by grand solar minima during the Late Holocene, which resulted in abrupt climate changes in Europe on time-scale of a few years and has the potential to trigger comparable changes in the future. Describing the timing and the abruptness of the climate response to shifts in the solar activity requires very accurate climate reconstructions and dating, in particular where absolute ages are hampered by the presence of 14C plateaux. This research project will focus on the precise comparison of Late Holocene palaeoclimate records from annually resolved (varved) archives across Europe, with the core goal of estimating the velocity of the climate response to grand solar minima and possible seasonal effects. The project’s novelty lies in the synchronization of very accurate varve chronologies from two European lakes, Diss Mere (England) and Meerfelder Maar (Germany), using tephra layers as synchronous markers. Tephrochronology and varve counting will thus be integrated as a multidisciplinary dating method to minimize the uncertainty derived from individual chronologies (varve counting error). Tephra (volcanic ash) from explosive eruption and atmospheric cosmogenic isotopes s are deposited over large areas synchronously and are reliably correlated to known eruptions. Varved sediments provide accurate chronologies and also store climatic signals at seasonal resolution. The interdisciplinary perspective adopted by this study is designed to tackle gaps in our knowledge of the solar-climate phasing and to provide the most precise proxy data to the climate modelling community. The facilities of Royal Holloway, University of London supports the innovate methodological approach.

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