@misc{sokolova_planetary_and_2007, 
author={Sokolova, E., Dethloff, K., Rinke, A., Benkel, A.},
title={Planetary and synoptic scale adjustment of the Arctic atmosphere to sea ice cover changes},
year={2007},
howpublished = {journal article},
doi = {https://doi.org/10.1029/2007GL030218},
abstract = {flow, the quasi-stationary planetary and the baroclinic waves. The wave energy fluxes on time scales 2 to 6 days increase in the middle troposphere between 30 and 60° N during the high sea ice phase and enhance the zonal wind. Their increase is compensated by a strong reduction in the Eliassen-21 Palm fluxes on time scales from 10 to 90 days between 60 and 70° N during high sea ice phases, accompanied by reduced zonal winds. High sea ice cover phases are related to the zonal wind changes during the positive phases of the AO especially over the northern part of the Atlantic Ocean.},
note = {Online available at: \url{https://doi.org/10.1029/2007GL030218} (DOI). Sokolova, E.; Dethloff, K.; Rinke, A.; Benkel, A.: Planetary and synoptic scale adjustment of the Arctic atmosphere to sea ice cover changes. Geophysical Research Letters. 2007. vol. 34, no. 17, L17816. DOI: 10.1029/2007GL030218}}