Impact of the Polar Vortex on Sub-Seasonal O/N 2 Variability in the Lower Thermosphere Using GOLD and WACCM-X
We provide observational evidence that the stability of the stratospheric Polar vortex (PV) is a significant driver of sub-seasonal variability in the thermosphere during geomagnetically quiet times when the PV is anomalously strong or weak. We find strong positive correlations between the Northern Annular Mode (NAM) index and subseasonal (10-90 days) Global Observations of the Limb and Disk (GOLD) O/N-2 perturbations at low to mid-northern latitudes, with a largest value of +0.55 at similar to 30.0 degrees N when anomalously strong or weak (NAM >2.5 or < -2.1) vortex times are considered. Strong agreement for O/N-2 variability and O/N-2-NAM correlations is found between GOLD observations and the Whole Atmosphere Community Climate Model with thermosphere-ionosphere eXtension (WACCM-X) simulations, which is then used to delineate the global distribution of O/N-2-NAM correlations. We find negative correlations between subseasonal variability in WACCM-X O/N-2 and NAM at high northern and southern latitudes (as large as -0.54 at similar to 60.0 degrees S during anomalous vortex times). These correlations suggest that PV driven upwelling at low latitudes is accompanied by corresponding downwelling at high latitudes in the lower thermosphere (similar to 80-120 km), which is confirmed using calculations of residual mean meridional circulation from WACCM-X.
document
https://n2t.org/ark:/85065/d7db8635
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2024-06-21T00:00:00Z
Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
None
OpenSky Support
UCAR/NCAR - Library
PO Box 3000
Boulder
80307-3000
name: homepage
pointOfContact
OpenSky Support
UCAR/NCAR - Library
PO Box 3000
Boulder
80307-3000
name: homepage
pointOfContact
2025-07-10T20:01:03.474025