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Climate ReOrganizations at Synoptic Scale as Recorded in the Offshore Archives o...

Climate ReOrganizations at Synoptic Scale as Recorded in the Offshore Archives of the Dead Sea Water availability in the Mediterranean basin is projected to decrease in the future in the 6th IPCC report. It is largely influenced by wintertime synoptic atmospheric circulations, as the westerlies play a crucial role in the di... ver más

31/08/2025

GFZ

265K€

Presupuesto del proyecto: 265K€

Líder del proyecto

HELMHOLTZ ZENTRUM POTSDAM DEUTSCHES GEOFORSCH... No se ha especificado una descripción o un objeto social para esta compañía.

TRL 4-5

Fecha límite participación Sin fecha límite de participación.

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Financiación concedida El organismo H2020 notifico la concesión del proyecto el día 2021-04-29

MSCA-IF-2020: Individual Fellowships Objective:The goal of the Individual Fellowships is to enhance the creative and innovative potential...

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3 Participantes

GFZ

264.67K€ | Lider

THE RESEARCH FOUNDATION OF S...

SUNY

177.27K€ | Participante

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Duración del proyecto: 52 meses Fecha Inicio: 2021-04-29
Fecha Fin: 2025-08-31

Líder del proyecto

HELMHOLTZ ZENTRUM POTSDAM DEUTSCHES GEOFORSCH... No se ha especificado una descripción o un objeto social para esta compañía.

TRL 4-5

Presupuesto del proyecto 265K€

Fecha límite de participación Sin fecha límite de participación.

Descripción del proyecto Water availability in the Mediterranean basin is projected to decrease in the future in the 6th IPCC report. It is largely influenced by wintertime synoptic atmospheric circulations, as the westerlies play a crucial role in the distribution of both rainfall and heat. However, to date, climate models have lacked the accuracy to predict the evolution of atmospheric circulations, making water availability projections uncertain and thus hampering adaptation strategies by policy makers. The Holocene epoch has been extensively studied to refine our understanding of climate and test the efficiency of climate models and proxies. And yet, mismatches among proxies and models leave the issue of the mechanisms and evolution of the westerlies still unresolved. In this fellowship, we will address this issue by studying the Holocene sediments recovered from the deep Dead Sea. The deep Dead Sea temperature is mainly influenced by winter air temperature and its level depends on the Jordan discharge that is fueled by winter rainfall, making this site ideal to reconstruct the winter variables affected by the westerlies. We will use novel methods based on spectroscopy and spectrometry on salt fluid inclusions (FIs) to reconstruct Holocene lake temperature and composition and we will develop a new method exploiting the lake composition, thickness of deposited salt, speed of sound in FIs, sediments microfacies and X-ray fluorescence elemental composition to reconstruct lake levels. As, in these arid latitudes, it has been impossible so far to obtain Holocene winter temperatures and hydrological reconstructions are scant, and because this site responds in an unusual way to changes in westerlies, I believe this action will prove key in understanding the evolution of the westerlies.

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