The climatology of zonal wave numbers 1 and 2 planetary wave structure in the MLT using a chain of Northern Hemisphere SuperDARN radars

Author:

Kleinknecht Nora H.1,Espy Patrick J.12,Hibbins Robert E.12

Affiliation:

1. Department of Physics; NTNU; Trondheim Norway

2. Birkeland Centre for Space Science; Bergen Norway

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference64 articles.

1. Planetary wave activity in the polar lower stratosphere;Alexander;Atmos. Chem. Phys.,2010

2. Angell , J. K. L. T. Flynn M. E. Gelman D. Hofmann C. S. Long A. J. Miller S. Zhou 2005 Northern Hemisphere Winter Summary Oltmans , S. http://www.cpc.ncep.noaa.gov/products/stratosphere/winter_bulletins/nh_04-05/

3. Angell , J. K. L. T. Flynn M. E. Gelman D. Hofmann C. S. Long A. J. Miller S. Oltmans S. Zhou 2006 Northern Hemisphere Winter Summary http://www.cpc.ncep.noaa.gov/products/stratosphere/winter_bulletins/nh_05-06/

4. Comparison of D-region Doppler drift winds measured by the SuperDARN Finland HF radar over an annual cycle using the Kiruna VHF meteor radar;Arnold;Ann. Geophys.,2003

5. The preconditioning of major sudden stratospheric warmings;Bancalá;J. Geophys. Res.,2012

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