Rodrigo Caballero Augi Professor of Dynamic meteorology

Contact

Name and title: Rodrigo Caballero AugiProfessor of Dynamic meteorology

Phone: +468164349

Workplace: Department of Meteorology Länk till annan webbplats.

Visiting address Room C666Svante Arrhenius väg 16 C

Postal address Meteorologiska institutionen (MISU)106 91 Stockholm

Research groups

Polar Meteorology and Oceanography

The global warming is not uniformly distributed over the Earth. The polar regions are especially sensitive for climate change and the warming in the Arctic is more than twice as fast as for the Earth on average. The effects of this warming are large, with a dramatic loss of sea ice as an example.

Circulation and connection land-sea-atmosphere

Over long timescales, the circulation systems co-evolve with ice sheets, mountain ranges, and redistributions of carbon between the atmosphere, ocean and land. The circulation and associated feedbacks influence exchanges of energy and materials between compartments of the climate system, and create teleconnections and natural climate variability.

About me

I am a professor at the Department of Meteorology, Stockholm University (MISU). My research group explores the multifarious ways in which atmospheric dynamics—from planetary-scale waves to the motion of individual cloud droplets—helps shape past, present and future climates. We do this using a combination of simple models, full-complexity general circulation models, observational data analysis and statistical modelling.

For more information and a list of publications, see my personal webpage.




Contact

Name and title: Rodrigo Caballero AugiProfessor of Dynamic meteorology

Phone: +468164349

Workplace: Department of Meteorology Länk till annan webbplats.

Visiting address Room C666Svante Arrhenius väg 16 C

Postal address Meteorologiska institutionen (MISU)106 91 Stockholm

Research groups

Polar Meteorology and Oceanography

The global warming is not uniformly distributed over the Earth. The polar regions are especially sensitive for climate change and the warming in the Arctic is more than twice as fast as for the Earth on average. The effects of this warming are large, with a dramatic loss of sea ice as an example.

Circulation and connection land-sea-atmosphere

Over long timescales, the circulation systems co-evolve with ice sheets, mountain ranges, and redistributions of carbon between the atmosphere, ocean and land. The circulation and associated feedbacks influence exchanges of energy and materials between compartments of the climate system, and create teleconnections and natural climate variability.