Biblio
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A brief history of climate e the northern seas from the last Glacial Maximum to global warming. Quaternary Science Reviews 106, (2014).
Dynamical drivers of Greenland blocking in climate models. Weather and Climate Dynamics (WCD) 2, (2021).
ENSO teleconnections in terms of non-NAO and NAO atmospheric variability. Climate Dynamics (2023).doi:10.1007/s00382-023-06697-8
Observed Atmospheric Coupling between Barents Sea ice and the Warm-Arctic Cold-Siberia anomaly pattern. Journal of Climate (2015).doi:10.1175/JCLI-D-15-0046.1
Observed atmospheric coupling between Barents Sea ice and the warm-Arctic cold-Siberian anomaly pattern. Journal of Climate 29, (2016).
Reconciling conflicting evidence for the cause of the observed early 21st century Eurasian cooling. Weather and Climate Dynamics (WCD) 4, (2023). Abstract
The relationship between the eddy-driven jet stream and northern European sea level variability. Tellus A: Dynamic Meteorology and Oceanography 73, (2021).
THE ROLE OF THE BARENTS SEA IN THE ARCTIC CLIMATE SYSTEM. Reviews of geophysics 51, (2013). Download: The role of the Barents_ROG.pdf (3.32 MB)