@misc{feser_storminess_over_2015, 
author={Feser, F., Barcikowska, M., Krueger, O., Schenk, F., Weisse, R., Xia, L.},
title={Storminess over the North Atlantic and northwestern Europe - A review},
year={2015},
howpublished = {journal article},
doi = {https://doi.org/10.1002/qj.2364},
abstract = {Storm trends derived from reanalyses data and climate model data for the past are mostly limited to the last four to six decades. The majority of these studies find increasing storm activity north of about 55–60° N over the North Atlantic with a negative tendency southward. This increase from about the 1970s until the mid-1990s is also mirrored by long-term proxies and the North Atlantic Oscillation and constitutes a part of their decadal variability. Studies based on proxy and measurement data or model studies over the North Atlantic for the past which cover more than 100 years show large decadal variations and either no trend or a decrease in storm numbers. Future scenarios until about the year 2100 indicate mostly an increase in winter storm intensity over the North Atlantic and western Europe. However, future trends in total storm numbers are quite heterogeneous and depend on the model generation used.},
note = {Online available at: \url{https://doi.org/10.1002/qj.2364} (DOI). Feser, F.; Barcikowska, M.; Krueger, O.; Schenk, F.; Weisse, R.; Xia, L.: Storminess over the North Atlantic and northwestern Europe - A review. Quarterly Journal of the Royal Meteorological Society. 2015. vol. B 141, no. 687, 350-382. DOI: 10.1002/qj.2364}}