Jonas Nycander Professor of Physical oceanography

Contact

Name and title: Jonas NycanderProfessor of Physical oceanography

Phone: +468164336

Workplace: Department of Meteorology Länk till annan webbplats.

Visiting address Room C 652Svante Arrhenius väg 16 C

Postal address Meteorologiska institutionen (MISU)106 91 Stockholm

Research groups

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.

The North Atlantic and Arctic Oceans

In the North Atlantic, a mighty current system conveys, via the Gulf Stream and North Atlantic Current, warm surface waters to northerly subpolar areas where deep water is formed. This current system, which is an important link in the global ocean circulation connecting the Atlantic and Pacific Oceans, also carries warm Atlantic water into the Arctic Ocean.

Middle and Upper Atmosphere

Middle atmosphere research at MISU focuses on altitudes between about 10 and 130 km. We use satellites, sounding rockets and ground-based instruments to explore this fascinating part of our planet. As a current highlight, we launched Sweden’s new research satellite in November 2022: MATS.

Baltic Sea Oceanography

The Baltic Sea is one of the best-surveyed and studied seas on Earth. Yet the Baltic Sea circulation and its role in the complex climate system is neither fully quantified nor understood, in spite of important implications for coastal societies of the Baltic Sea region.

About me

My PhD degree was in plasma physics, but I later switched to physical oceanography. Since 2000 I have been working at the Dept. of Meteorology (MISU). Here are some research themes I have been persuing since then.

  • Internal waves generated by tides.
  • Analysis of overturning circulation. By projecting the circulation on various coordinates it is possible to tell whether it is mechanically or thermally forced, and to diagnose the water mass transformation.
  • Effects on the nonlinear equation of state on the ocean circulation.
  • The ocean carbon cycle and its role for the low atmospheric CO2 concentration during the ice ages.
  • .Vegetation dynamics, in particular the direct effect of CO2.
  • Climate economics.




Contact

Name and title: Jonas NycanderProfessor of Physical oceanography

Phone: +468164336

Workplace: Department of Meteorology Länk till annan webbplats.

Visiting address Room C 652Svante Arrhenius väg 16 C

Postal address Meteorologiska institutionen (MISU)106 91 Stockholm

Research groups

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.

The North Atlantic and Arctic Oceans

In the North Atlantic, a mighty current system conveys, via the Gulf Stream and North Atlantic Current, warm surface waters to northerly subpolar areas where deep water is formed. This current system, which is an important link in the global ocean circulation connecting the Atlantic and Pacific Oceans, also carries warm Atlantic water into the Arctic Ocean.

Middle and Upper Atmosphere

Middle atmosphere research at MISU focuses on altitudes between about 10 and 130 km. We use satellites, sounding rockets and ground-based instruments to explore this fascinating part of our planet. As a current highlight, we launched Sweden’s new research satellite in November 2022: MATS.

Baltic Sea Oceanography

The Baltic Sea is one of the best-surveyed and studied seas on Earth. Yet the Baltic Sea circulation and its role in the complex climate system is neither fully quantified nor understood, in spite of important implications for coastal societies of the Baltic Sea region.