Abstract
Abstract A major stratospheric sudden warming occurred in the Northern Hemisphere during late December 1984, one of the earliest times such an event has been observed during winter. The seasonal evolution of the stratospheric circumpolar vortex during this winter is strongly affected by this disruption, particularly in the lower stratosphere, and normal midwinter conditions are not reestablished until mid-February. The anomalous postwarming state has a pronounced effect on the vertical propagation of planetary waves from the troposphere.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
