Atmospheric, Earth and Energy Division
University of Copenhagen, Denmark
Eberhard-Karls University of Tuebingen, Germany
University of Novi Sad, Serbia
Impacts of Arctic sea ice changes on atmospheric circulation patterns and weather extremes; remote drivers of precipitation changes (e.g., high latitude induced tropical precipitation shifts); Hadley cell dynamics and Intertropical Convergence Zone shifts; the role of atmospheric heat transport changes in polar amplification.
Dansgaard-Oeschger events, bipolar seesaw (phase relationship between Greenland and Antarctic temperature records), coupling between tropical and high latitude precipitation and temperature proxies.
Pedersen, R.A, Cvijanovic, I., Langen, P.L. and B. M. Vinther (2016): The Impact of Regional Arctic Sea Ice Loss on Atmospheric Circulation and the NAO.
Cvijanovic, I., Caldeira, K. and D.G. Macmartin (2015): Impacts of ocean albedo alteration on Arctic sea ice restoration and Northern Hemisphere climate.
Cvijanovic, I. and K. Caldeira (2015): Climate impacts of sea ice response in CO2 induced global warming.
Caldeira, K. and I. Cvijanovic (2014): Sea ice radiative forcing, sea ice area, and climate sensitivity.
Rasmussen et al. (2014): A framework for robust naming and correlation of past abrupt climatic changes during the recent glacial period based on three synchronized Greenland ice cores.
NEEM community members (2013): Eemian interglacial reconstructed from Greenland folded NEEM ice core strata,
Cvijanovic, I., Langen, P.L., Kaas, E. and P.D. Ditlevsen (2013): Southward Intertropical Convergence Zone shifts and implications for an atmospheric bipolar seesaw,
Cvijanovic, I. and J.C.H. Chiang (2013): Global energy budget changes to high latitude North Atlantic cooling and the tropical ITCZ response,
Cvijanovic, I., Langen, P.L. and E. Kaas (2011): Weakened atmospheric energy transport feedback in cold glacial climates,
Kollet, S.J., Cvijanovic, I., Schüttemeyer, D., Maxwell, R.M., Moene, A.F., and P. Bayer (2009): The influence of rain sensible heat and subsurface energy transport on the energy balance at the land surface,