H2020Individual fellowship2022–2024

ITHACA · medITerranean HydroclimAte variability over the Common erA

Horizon 2020 — Marie Skłodowska-Curie Actions

Duration
2022-09-01 → 2024-08-31
EU contribution
€160,932
Participants
1
Scheme
MSCA-IF

Lines connect the coordinator with its partners.

Results in brief

medITerranean HydroclimAte variability over the Common erA

The ITHACA project investigates hydroclimate extremes in the Mediterranean over the last two thousand years. It develops a cutting-edge paleo data assimilation product, combining proxy-data with climate model simulations, to provide historical context for future climate projections. This research informs policy-making, assesses climate change risks, and attributes anthropogenic activities to hydroclimatic changes. Ultimately, this knowledge can assist in developing effective strategies for adapting to and mitigating the impacts of climate change in the Mediterranean region and beyond.

Data: CORDIS, © European Union

Project objective

The Mediterranean region is known for its high seasonal contrast in temperature and rainfall, subject to extreme hydroclimatic events (e.g., droughts and pluvials). In most Mediterranean regions, water resources are scarce and observational data and climate models suggest a transition to an even more arid climate is underway. Uncertainties in future climate change projections over the Mediterranean region still remain, however, thus demanding an understanding of the natural range of climate variability prior to the era of significant anthropogenic interference in the climate system. The ITHACA's goal is to advance the understanding of paleoclimate over the Mediterranean basin to the point where it can inform policy and decision-making about the risks of climate change from a paleo perspective and place future projections within a broad historical context. This project will investigate the characteristics (frequency, intensity, extent, seasonality) and causes of hydroclimate extremes (droughts and pluvials) during the Common Era (CE, the last two thousand years) over the Mediterranean region by developing a state-of-the-art paleo data assimilation product, which will effectively combine high-resolution paleo proxy-data time series with the physical constraints of an atmosphere-ocean climate model simulation. Finally, by using this new product the project will address the attribution of anthropogenic activities to current changes in hydroclimatic extremes and will provide guidance for process-based risk assessment tools.

Original text from CORDIS.

Participants

  • AGENCIA ESTATAL CONSEJO SUPERIOR DE INVESTIGACIONES CIENTIFICAS · MadridCoordinatorSpain

Links

Data: CORDIS, © European Union