Hopp til hovedinnhold

Kalender

Monday seminar: Using teleconnections to link weather to climate

Tidspunkt

16. desember 2024, 13:15-14:00

Sted

Bjerknes lecture room (4th floor, room 4020)

Dear all, 

Monday (16th December) at 14:15, there will be the last BCCR seminar of 2024, by Clemens Spensberger on “Using teleconnections to link weather to climate”.

The seminar will take place in Bjerknes lecture room (4th floor, room 4020). For those not able to attend in person, it will be possible to join on zoom.

Abstract

Conventionally, teleconnections in the atmosphere are described by correlations between monthly mean fields. These correlations are supposedly caused by stationary Rossby waves. I will in this talk explore the hypothesis that teleconnections are instead established by chains of events on synoptic timescales, that is by weather.

This talk will be my farewell to GFI and the Bjerknes Centre, and I will use the occasion to synthesise a number of published and recent results to underpin what was the main hypothesis for my attempt at an ERC Starting Grant, now instead published as a WCD Idea paper.

About the speaker

I am a researcher in dynamic meteorology and have been at GFI and the Bjerknes Centre since early 2011, moving to Bergen to take a PhD with Thomas Spengler. I have been abroad a few years for a postdoc mobility stipend, but otherwise spent all my academic life here in Bergen. I started out trying to better understand the behaviour of individual mid-latitude weather systems, first and foremost jet streams, but increasingly tried to use this lens to build bridges to longer time scales.

Flere kalenderoppføringer

Se alle
Illustrasjonsbilde
02.09.26

Stormtracks group meeting

Our first meeting will be on 02/09, same time (14:00 to 15:00 every Wednesday) and same room (U105 for most of the time).
Illustrasjonsbilde
17.08.26

BCCR Monday seminar: Atmospheric River Cyclone Events Disrupting an Antarctic Peninsula Field Campaign: Dynamics, Predictability, and Climatological Context”.

The next BCCR Monday Seminar will be given by Deniz Bozkurt from the Universidad de Valparaíso, Chile. Abstract The Antarctic Peninsula is one of the most dynamic regions of Antarctica, where interactions between large scale atmospheric circulation, atmospheric rivers, extratropical cyclones, and complex terrain can produce high impact weather events. This study examines a sequence of three storms that disrupted a glaciological field campaign in the northern Antarctic Peninsula during January 2025. Using observations, ERA5 reanalysis, Polar WRF simulations, and operational forecast products, the study investigates the atmospheric processes responsible for the storm sequence and the factors that amplified its local impacts. The results show that repeated interactions between atmospheric rivers and extratropical cyclones, together with a persistent blocking pattern and favorable tropical extratropical teleconnections, sustained strong moisture transport toward the Antarctic Peninsula. High resolution simulations reveal that local topography substantially enhanced near surface winds over distances of only a few kilometers, explaining why the field camp experienced much more severe conditions than nearby coastal locations. The study also evaluates forecast predictability across spatial scales and places these events in a longer term climatological context, highlighting the increasing occurrence of atmospheric river affected days and the implications for future Antarctic field operations and climate extremes. Speaker information Dr. Deniz Bozkurt is a Professor in the Department of Meteorology at the University of Valparaíso, Chile, and a researcher at COPAS Coastal and the Center for Climate and Resilience Research (CR2). His research focuses on regional climate modeling, climate variability, atmospheric circulation, and hydrometeorological extremes in Antarctica and South America. He combines observations, reanalysis, and regional and global climate models to investigate the atmospheric processes driving extreme events, hydroclimate variability, atmosphere-cryosphere interactions, and climate change impacts over complex terrain.