Javascript must be enabled to continue!
Eastward‐Propagating Planetary Waves Prior to the January 2009 Sudden Stratospheric Warming
View through CrossRef
AbstractEastward‐propagating planetary waves (EPWs) were investigated prior to the boreal January 2009 major sudden stratospheric warming (SSW) event simulated by the National Center for Atmospheric Research's Whole Atmosphere Community Climate Model with specified dynamics. About 22 days before SSW onset, a background flow with jet maxima around the upper polar stratosphere and subtropical mesosphere developed due to the net forcing by gravity and planetary waves. The mesospheric wind structure was largely unstable and supported a wave geometry conducive to overreflection. With a zonal phase speed of ∼10 m s−1, EPWs appeared near their turning and critical layers as wavenumber‐2 perturbations in the stratosphere and mesosphere. Accompanied by upward EPW activity from the lower stratosphere, EPW growth exhibited characteristics of wave instability and overreflection.
American Geophysical Union (AGU)
Title: Eastward‐Propagating Planetary Waves Prior to the January 2009 Sudden Stratospheric Warming
Description:
AbstractEastward‐propagating planetary waves (EPWs) were investigated prior to the boreal January 2009 major sudden stratospheric warming (SSW) event simulated by the National Center for Atmospheric Research's Whole Atmosphere Community Climate Model with specified dynamics.
About 22 days before SSW onset, a background flow with jet maxima around the upper polar stratosphere and subtropical mesosphere developed due to the net forcing by gravity and planetary waves.
The mesospheric wind structure was largely unstable and supported a wave geometry conducive to overreflection.
With a zonal phase speed of ∼10 m s−1, EPWs appeared near their turning and critical layers as wavenumber‐2 perturbations in the stratosphere and mesosphere.
Accompanied by upward EPW activity from the lower stratosphere, EPW growth exhibited characteristics of wave instability and overreflection.
Related Results
Spatial and Open Research Data Infrastructure for Planetary Science - Lessons learned from European developments
Spatial and Open Research Data Infrastructure for Planetary Science - Lessons learned from European developments
The planetary community has access to a wealth of raw research data by using central data distribution platforms such as the Planetary Data System (PDS) [1], the Planetary Science ...
Planetary wave‐gravity wave interactions during mesospheric inversion layer events
Planetary wave‐gravity wave interactions during mesospheric inversion layer events
AbstractRayleigh lidar temperature observations over Gadanki (13.5°N, 79.2°E) show a few mesospheric inversion layer (MIL) events during 20–25 January 2007. The zonal mean removed ...
Planetary Cartography: Challenges for Mapping and Research Data Management
Planetary Cartography: Challenges for Mapping and Research Data Management
<p>The aim of this contribution is to summarize recent activities in the field of Planetary Cartography by highlighting current issues the community is facing, and by...
Oscillatory frequencies in spatiotemporal system with local inhomogeneity
Oscillatory frequencies in spatiotemporal system with local inhomogeneity
Target waves usually emit concentric circular waves, whereas spiral waves rotate around a central core (topological defect) region, the two forms of waves are closely related due t...
Stratosphere-Troposphere Coupling and Global Warming
Stratosphere-Troposphere Coupling and Global Warming
<p>The atmospheric circulation response to the anthropogenic increase of CO<sub>2</sub> is known to generally involve a number of pathways...
Impacts of Stratospheric Ozone on Antarctic Spring Sea Ice: Based on WACCM6
Impacts of Stratospheric Ozone on Antarctic Spring Sea Ice: Based on WACCM6
Austral spring (September–November) represents the season with the most pronounced chemical depletion of stratospheric ozone over Antarctica, during which the associated radiative ...
Final Sudden Stratospheric Warmings and the memory of the stratosphere
Final Sudden Stratospheric Warmings and the memory of the stratosphere
<p>Sudden Stratospheric Warming (SSW) is the most spectacular dynamic event occurring in the middle atmosphere. It can lead to a warming of the winter polar stratosph...
Origin of De Broglie Waves
Origin of De Broglie Waves
The famous 1927 Solvay Conference was considered a turning point in the world of Physics. The scientific realists like Albert Einstein had lost and the instrumentalists like Niels ...

