Abstract
Over recent decades, the stratospheric polar vortex has shifted toward more frequent weak States, which can explain Eurasian cooling trends in boreal winter in the era of Arctic amplification.
| Original language | English |
|---|---|
| Pages (from-to) | 49-60 |
| Number of pages | 12 |
| Journal | Bulletin of the American Meteorological Society |
| Volume | 99 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 1 Jan 2018 |
Funding
ACKNOWLEDGMENTS. We thank Peter Hitchcock and two anonymous reviewers for their useful comments and suggestions to improve the manuscript, and we thank ECMWF and GMAO for making the ERA-Interim and the MERRA-2 data available. The work was supported by the German Federal Ministry of Education and Research, Grant 01LN1304A (M.K., D.C.); National Science Foundation (NSF) Grants AGS-1303647 and PLR-1504361 (J.C.); NOAA Grant NA15OAR4310077 (J.C.); and NSF Grant AGS-1303604 (E.T.). The research project resulted from M.K. visiting J.C., and M.K. would like to thank AER and Harvard for hosting. E.T. would like to thank the Weizmann Institute for its hospitality during parts of this work.
| Funders | Funder number |
|---|---|
| National Science Foundation | 1504361, PLR-1504361, AGS-1303647 |
| National Oceanic and Atmospheric Administration | NA15OAR4310077, AGS-1303604 |
| Bundesministerium für Bildung und Forschung | 01LN1304A |
| Norsk Sykepleierforbund |
