Understanding atmospheric circulation from a surface perspective

Informacje na temat projektu

UACSURF

Identyfikator umowy o grant: 654492

DOI

10.3030/654492

Realizacja projektu zakończyła się 13 Września 2016

Data podpisania przez KE 2 Marca 2015

Data rozpoczęcia 1 Kwietnia 2015

Data zakończenia 8 Sierpnia 2017

Finansowanie w ramach

• EXCELLENT SCIENCE - Marie Skłodowska-Curie Actions

Koszt całkowity

€ 195 454,80

Wkład UE

€ 195 454,80

Koordynowany przez

THE UNIVERSITY OF READING
United Kingdom

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

Okres sprawozdawczy: 2015-04-01 do 2017-03-31

Podsumowanie kontekstu i ogólnych celów projektu

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.

Prace wykonane od początku projektu do końca okresu sprawozdawczego oraz najważniejsze dotychczasowe rezultaty

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.

Innowacyjność oraz oczekiwany potencjalny wpływ (w tym dotychczasowe znaczenie społeczno-gospodarcze i szersze implikacje społeczne projektu)

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