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PALEOCORE

Financiado

Core dynamics on millennial timescales

PALEOCORE will provide the first comprehensive observational constraints on the dynamics of Earth’s core on multi-centennial to millennial timescales. Such constraints are essential to understand the core processes responsible for... ver más

28/02/2029

LUNDS UNIVERSITET

2M€

Presupuesto del proyecto: 2M€

Líder del proyecto

LUNDS UNIVERSITET No se ha especificado una descripción o un objeto social para esta compañía.

TRL 4-5

Financiación concedida El organismo HORIZON EUROPE notifico la concesión del proyecto el día 2023-12-06

Línea de financiación objetivo El proyecto se financió a través de la siguiente ayuda:

ERC-2023-COG: ERC CONSOLIDATOR GRANTS

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LUNDS UNIVERSITET

2.00M€ | Lider

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Últimas noticias

29-11-2024: IDAE En las últimas 48 horas el Organismo IDAE ha otorgado 4 concesiones

29-11-2024: ECE En las últimas 48 horas el Organismo ECE ha otorgado 2 concesiones

29-11-2024: CMVAMADRID En las últimas 48 horas el Organismo CMVAMADRID ha otorgado 37 concesiones

Duración del proyecto: 62 meses Fecha Inicio: 2023-12-06
Fecha Fin: 2029-02-28

Líder del proyecto

LUNDS UNIVERSITET

TRL 4-5

Presupuesto del proyecto 2M€

Descripción del proyecto PALEOCORE will provide the first comprehensive observational constraints on the dynamics of Earth’s core on multi-centennial to millennial timescales. Such constraints are essential to understand the core processes responsible for the rapid decay of Earth’s dipole field strength over the past century and to forecast future field changes. Generated through convective motions in the liquid iron core, Earth’s magnetic field acts as a shield against harmful cosmic radiation and plays a crucial role for the habitability of our planet. The past two decades of satellite monitoring of the magnetic field, in combination with major advancements in numerical simulations of the geodynamo, have generated a wealth of knowledge on relatively rapid processes in the core. However, due to the lack of reference data with adequate resolution, the dynamics of the core on timescales longer than the convective overturn time (~130 years) are still poorly understood. Observational constraints of core dynamics on these timescales are crucial to evaluate proposed driving mechanisms of the geodynamo. Through recent technical innovations, models based on indirect paleomagnetic observations of Earth’s magnetic field are providing information on past field changes with unprecedented resolution. These models suggest that the recent dipole decay is part of a millennial-scale recurrent pattern associated with weak field anomalies, like the present-day South Atlantic Anomaly. The aim of PALEOCORE is to construct the first ever integrated core-field core-flow model over millennial timescales to study such ancient analogues and reveal the underlying core dynamics responsible for driving these changes. This will be achieved through a combination of (i) strategic paleomagnetic data acquisition and key modelling innovations (solving bottlenecks in the current approach), (ii) incorporation of independent radionuclide data and (iii) adaptation of data assimilation algorithms for paleomagnetic data.

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