Articles | Volume 36, issue 2
https://doi.org/10.5194/angeo-36-489-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/angeo-36-489-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Seasonal variations of thermospheric mass density at dawn/dusk from GOCE observations
Libin Weng
CAS Key Laboratory of Geospace Environment, School of Earth and Space
Sciences, University of Science and Technology of China, Hefei, China
College of Meteorology and Oceanography, National University of
Defense Technology, Nanjing, China
Jiuhou Lei
CORRESPONDING AUTHOR
CAS Key Laboratory of Geospace Environment, School of Earth and Space
Sciences, University of Science and Technology of China, Hefei, China
Eelco Doornbos
Delft Institute of Earth Observation and Space Systems, Delft
University of Technology, Delft, the Netherlands
Hanxian Fang
College of Meteorology and Oceanography, National University of
Defense Technology, Nanjing, China
Xiankang Dou
CAS Key Laboratory of Geospace Environment, School of Earth and Space
Sciences, University of Science and Technology of China, Hefei, China
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The influences of sudden stratospheric warming in the Northern Hemisphere on quasi-2-day waves are studied with both observations and simulations. We found the energy of W3 is transferred to W2 through the nonlinear interaction with SPW1 and the instability at winter mesopause could provide additional amplification for W3. The summer easterly is enhanced during SSW, which is more favorable for the propagation of quasi-2-day waves.
X. Luan and X. Dou
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Y. L. Zhou, S. Y. Ma, R. S. Liu, H. Luehr, and E. Doornbos
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Thermospheric mass density from the GOCE satellite for Sun-synchronous orbits between 83.5° S and 83.5° N normalized to 270 km during 2009–2013 has been used to develop our GOCE model at dawn/dusk local solar time sectors based on the empirical orthogonal function (EOF) method. We find that both amplitude and phase of the seasonal variations have strong latitudinal and solar activity dependences, and the annual asymmetry and effect of the Sun–Earth distance vary with latitude and solar activity.
Thermospheric mass density from the GOCE satellite for Sun-synchronous orbits between 83.5° S...