Articles | Volume 33, issue 10
https://doi.org/10.5194/angeo-33-1321-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/angeo-33-1321-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Regular paper
| 
30 Oct 2015
Regular paper |
| 30 Oct 2015
Observational evidence of quasi-27-day oscillation propagating from the lower atmosphere to the mesosphere over 20° N
K. M. Huang
School of Electronic Information, Wuhan University, Wuhan, China
State Observatory for Atmospheric Remote Sensing, Wuhan, China
A. Z. Liu
Department of Physical Science, Embry-Riddle Aeronautical University, Daytona Beach, Florida, USA
S. D. Zhang
CORRESPONDING AUTHOR
School of Electronic Information, Wuhan University, Wuhan, China
State Observatory for Atmospheric Remote Sensing, Wuhan, China
School of Electronic Information, Wuhan University, Wuhan, China
State Observatory for Atmospheric Remote Sensing, Wuhan, China
C. M. Huang
School of Electronic Information, Wuhan University, Wuhan, China
State Observatory for Atmospheric Remote Sensing, Wuhan, China
Q. Gan
School of Electronic Information, Wuhan University, Wuhan, China
State Observatory for Atmospheric Remote Sensing, Wuhan, China
Y. Gong
School of Electronic Information, Wuhan University, Wuhan, China
State Observatory for Atmospheric Remote Sensing, Wuhan, China
Y. H. Zhang
College of Hydrometeorology, Nanjing University of Information Science and Technology, Nanjing, China
R. Wang
SOA Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai, China
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Short summary
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Short summary
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Short summary
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Short summary
Short summary
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Short summary
Short summary
We present the first statistical results of vertical wind fluctuation spectra, which revealed a very shallow spectral structure, with mean slopes of −0.58 and −0.23 in the troposphere and lower stratosphere, respectively. No existing spectral theories can comprehensively explain the observed three-dimensional wind spectra, indicating that the spectral features of atmospheric fluctuations are far from fully understood.
Yue Jia, Shao Dong Zhang, Fan Yi, Chun Ming Huang, Kai Ming Huang, Yun Gong, and Quan Gan
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Q. Gan, J. Yue, L. C. Chang, W. B. Wang, S. D. Zhang, and J. Du
Ann. Geophys., 33, 913–922, https://doi.org/10.5194/angeo-33-913-2015, https://doi.org/10.5194/angeo-33-913-2015, 2015
Short summary
Short summary
The 6.5-day traveling planetary wave is able to impact the ionosphere/thermosphere via a dissipation mechanism. Ionospheric TEC and thermosphere O/N2 exhibit an apparent decrease as the result of extra meridional circulation induced by 6.5-day wave dissipation. Our work suggests that the modulation of E-dynamo is not the unique pathway through which planetary waves substantially influence the IT system.
C. Huang, S. Zhang, Q. Zhou, F. Yi, K. Huang, Y. Gong, Y. Zhang, and Q. Gan
Ann. Geophys., 33, 865–874, https://doi.org/10.5194/angeo-33-865-2015, https://doi.org/10.5194/angeo-33-865-2015, 2015
Short summary
Short summary
The diurnal tide and its variability in the lower atmosphere over Chongyang (114.14ºE，29.53ºN) were studied based on the newly established Wuhan University VHF radar observations in the whole year of 2012. We find that the diurnal tide was the dominant tidal component and showed remarkable height and season variations, as well as dramatic short-term variability.
S. D. Zhang, C. M. Huang, K. M. Huang, F. Yi, Y. H. Zhang, Y. Gong, and Q. Gan
Ann. Geophys., 32, 1129–1143, https://doi.org/10.5194/angeo-32-1129-2014, https://doi.org/10.5194/angeo-32-1129-2014, 2014
J.-S. Wang, Z. Chen, and C.-M. Huang
Ann. Geophys., 32, 563–569, https://doi.org/10.5194/angeo-32-563-2014, https://doi.org/10.5194/angeo-32-563-2014, 2014
K. M. Huang, S. D. Zhang, F. Yi, C. M. Huang, Q. Gan, Y. Gong, and Y. H. Zhang
Ann. Geophys., 32, 263–275, https://doi.org/10.5194/angeo-32-263-2014, https://doi.org/10.5194/angeo-32-263-2014, 2014
K. M. Huang, A. Z. Liu, S. D. Zhang, F. Yi, C. M. Huang, Q. Gan, Y. Gong, and Y. H. Zhang
Ann. Geophys., 31, 2039–2048, https://doi.org/10.5194/angeo-31-2039-2013, https://doi.org/10.5194/angeo-31-2039-2013, 2013
C. M. Huang, S. D. Zhang, F. Yi, K. M. Huang, Y. H. Zhang, Q. Gan, and Y. Gong
Ann. Geophys., 31, 1731–1743, https://doi.org/10.5194/angeo-31-1731-2013, https://doi.org/10.5194/angeo-31-1731-2013, 2013
Y. Y. Huang, S. D. Zhang, F. Yi, C. M. Huang, K. M. Huang, Q. Gan, and Y. Gong
Ann. Geophys., 31, 1061–1075, https://doi.org/10.5194/angeo-31-1061-2013, https://doi.org/10.5194/angeo-31-1061-2013, 2013
