EU-ISOTREC

Climatic and environmental changes in the Eurasian Subarctic inferred from tree-ring and stable isotope chronologies for the past and recent periods

 Coordinatore PAUL SCHERRER INSTITUT 

 Organization address address: Villigen
city: VILLIGEN PSI
postcode: 5232

contact info
Titolo: Ms.
Nome: Irene
Cognome: Walthert
Email: send email
Telefono: +41 56 310 2664
Fax: +41 56 310 2717

 Nazionalità Coordinatore Switzerland [CH]
 Totale costo 179˙667 €
 EC contributo 179˙667 €
 Programma FP7-PEOPLE
Specific programme "People" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call FP7-PEOPLE-IIF-2008
 Funding Scheme MC-IIF
 Anno di inizio 2010
 Periodo (anno-mese-giorno) 2010-03-01   -   2013-04-30

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    PAUL SCHERRER INSTITUT

 Organization address address: Villigen
city: VILLIGEN PSI
postcode: 5232

contact info
Titolo: Ms.
Nome: Irene
Cognome: Walthert
Email: send email
Telefono: +41 56 310 2664
Fax: +41 56 310 2717

CH (VILLIGEN PSI) coordinator 179˙667.42

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 Word cloud

Esplora la "nuvola delle parole (Word Cloud) per avere un'idea di massima del progetto.

ring    oxygen    carbon    model    periods    isotope    al    et    chronologies    ad    physiological    temperature    period    environmental    trees    past    climatic    tree    warm    data    holocene   

 Obiettivo del progetto (Objective)

'The goal of this project is: • to develop a comprehensive description of the climatic and environmental changes in the Eastern Taimyr [72N-102E] for the warmest periods during the Holocene using tree ring width, latewood density, cell size, carbon and oxygen isotope data in wood and cellulose; • to improve our understanding of the physiological response of larch trees to environmental changes in the Eurasian north. We propose to investigate three periods, which are characterized by high temperatures during the Holocene: • the natural warm period BC 3700-3800, with an average temperature, which was three degrees higher than at present; • the Medieval Warm period AD 950-1150, with a similar rise in temperature compared to today; • the current period AD 1945-2006, which is characterized by the highest level of atmospheric carbon dioxide due to anthropogenic activities besides a temperature increase. The work will be conducted in three major fields: 1. Climatology – analyses of statistical relationships between climatic parameters (temperature, precipitation, relative humidity, and vapor pressure deficit) and carbon, oxygen isotope data during the current period. Comparison of isotope chronologies along the Subarctic latitudes from Yakutia to Sweden with Greenland ice core and pollen data. 2. Physiology - investigation of the physiological response of trees to environmental changes during the current and past periods based on a combined carbon and oxygen isotope fractionation model developed by Scheidegger et al. (2000). 3. Modeling – the new isotope and tree ring chronologies will be used to verify the ecophysiological model [Hemming et al. 2001; Vaganov et al. 2006] for the current period and to extend the model for the past to infer new environmental information (e.g. on water use efficiency).'

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