Understanding atmospheric circulation from a surface perspective

Informations projet

UACSURF

N° de convention de subvention: 654492

DOI

10.3030/654492

Projet clôturé le 13 Septembre 2016

Date de signature de la CE 2 Mars 2015

Date de début 1 Avril 2015

Date de fin 8 Août 2017

Financé au titre de

• EXCELLENT SCIENCE - Marie Skłodowska-Curie Actions

Coût total

€ 195 454,80

Contribution de l’UE

€ 195 454,80

Coordonné par

THE UNIVERSITY OF READING
United Kingdom

Periodic Reporting for period 1 - UACSURF (Understanding atmospheric circulation from a surface perspective)

Période du rapport: 2015-04-01 au 2017-03-31

Résumé du contexte et des objectifs généraux du projet

While the thermodynamic effects of rising concentrations of greenhouse gases in the atmosphere are largely well understood, theoretical and experimental work on the effect of a warming planet on atmospheric dynamics is relatively scarce. This limits our ability to detect, understand and predict the effect of climate change on atmospheric circulation and weather regimes, which cause extreme events ranging from storms over heavy precipitation to draughts or heat waves. The present project aims to make a contribution to advance that understanding by examining the effect of drag on atmospheric circulation and its representation in weather and climate models.

Travail effectué depuis le début du projet jusqu’à la fin de la période considérée dans le rapport et principaux résultats atteints jusqu’à présent

During the project, climate model sensitivity experiments were run and analysed alongside available model output from standard CMIP5 experiments. Theoretical analyses and work with simplified models served to better understand the link between changes in surface drag and changes in atmospheric circulation. The main results were published in an open acces GRL paper (Climate model biases in jet streams, blocking and storm tracks resulting from missing orographic drag, doi: 10.1002/2016GL069551). The researcher was also involved in preparing a workshop on the effects of drag on large-scale circulation held at the European Center for Medium-Range Weather Forecasts in September 2016.

Progrès au-delà de l’état des connaissances et impact potentiel prévu (y compris l’impact socio-économique et les conséquences sociétales plus larges du projet jusqu’à présent)

We were able to show that missing parameterised low-level drag can explain typical biases in CMIP5 models to a large extent. This shows a potential for impriving these models climatologies in a computationally cheap way (improving model formulations instead of increasing numerical resolution). In some cases, model biased are linked to spread in future projections, which makes such improvemens key for predicting future circulation changes with confidence.

Zonal wind changes caused by switching off orographic blocking and typical modal biases