Evidence for the Influence of DE3 Tide on the Occurrence of Equatorial Counterelectrojet

2018 ◽  
Vol 45 (5) ◽  
pp. 2145-2150 ◽  
Author(s):  
Dupinder Singh ◽  
S. Gurubaran ◽  
Maosheng He
Keyword(s):  
De3 Tide

A Simulation of the Influence of DE3 Tide on Nitric Oxide Infrared Cooling

2020 ◽  
Vol 125 (3) ◽  
Author(s):  
Zhipeng Ren ◽  
Weixing Wan ◽  
Jiangang Xiong ◽  
Xing Li
Keyword(s):  
Nitric Oxide ◽  
De3 Tide

scholarly journals Influence of DE3 tide on the equinoctial asymmetry of the zonal mean ionospheric electron density

2014 ◽  
Vol 66 (1) ◽  
pp. 117 ◽  
Author(s):  
Zhipeng Ren ◽  
Weixing Wan ◽  
Jiangang Xiong ◽  
Libo Liu
Keyword(s):  
Electron Density ◽  
Ionospheric Electron Density ◽  
De3 Tide

scholarly journals Longitudinal Structure in the Altitude of the Sporadic E Observed by COSMIC in Low-Latitudes

2021 ◽  
Vol 13 (22) ◽  
pp. 4714
Author(s):  
Zhendi Liu ◽  
Qingfeng Li ◽  
Hanxian Fang ◽  
Ze Gao
Keyword(s):  
Dominant Role ◽  
Longitudinal Structure ◽  
Zonal Wavenumber ◽  
Low Latitudes ◽  
June Solstice ◽  
Sporadic E ◽  
First Time ◽  
De3 Tide ◽  
Northern And Southern Hemispheres

The longitudinal structure in the altitude of the Sporadic E (Es) was investigated for the first time based on the S4 index provided by the Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) in low latitudes. The longitudinal structure is identified as a symmetrically located wavenumber-4 (WN4) pattern within 30°S–30°N. The WN4 occurs primarily during the daytime at the June solstice and equinoxes, with the largest amplitude at the September equinox and the smallest one at the March equinox. It moves eastward with a speed of ~90°/day. The strongest WN4 appears within 10–20°N and 5–15°S in the Northern and Southern hemispheres, respectively. At the June solstice and the September equinox, the WN4 is stronger in the Northern hemisphere than in the Southern hemisphere, while the situation is reversed at the March equinox. The altitude distribution of the convergence null in the diurnal eastward non-migrating tide with zonal wavenumber-3 (DE3) for the zonal wind is similar to that of the WN4. This and other similar features, such as the seasonal variation, eastward speed, and the symmetrical locations, support the dominant role of the DE3 tide for the formation of the WN4 structure.

Hough Mode Decomposition of the DE3 tide extracted from TIMED observations

2019 ◽  
Vol 195 ◽  
pp. 105140
Author(s):  
Xing Li ◽  
Weixing Wan ◽  
Jinbin Cao ◽  
Xianghui Xue ◽  
Zhipeng Ren
Keyword(s):  
Mode Decomposition ◽  
De3 Tide

Annual Variation and Global Structures of The DE3 Tide

2008 ◽  
Vol 25 (6) ◽  
pp. 2323-2326 ◽  
Author(s):  
Chen Ze-Yu ◽  
Lu Da-Ren
Keyword(s):  
Annual Variation ◽  
De3 Tide

scholarly journals Correlation between the ionospheric WN4 signature and the upper atmospheric DE3 tide

2010 ◽  
Vol 115 (A11) ◽  
pp. n/a-n/a ◽  
Author(s):  
W. Wan ◽  
J. Xiong ◽  
Z. Ren ◽  
L. Liu ◽  
M.-L. Zhang ◽  
...  
Keyword(s):  
De3 Tide

A simulation of the influence of DE3 tide on nitric oxide infrared cooling

2021 ◽  
Author(s):  
Zhipeng Ren ◽  
Weixing Wan ◽  
Jiangang Xiong ◽  
Xing Li
Keyword(s):  
Nitric Oxide ◽  
Cooling Rate ◽  
High Latitude ◽  
Driving Mechanism ◽  
Low Latitude ◽  
A Value ◽  
Zonal Wavenumber ◽  
The Absolute ◽  
The Difference ◽  
De3 Tide

<p>Using GCITEM-IGGCAS model, we simulate the influence of the eastward propagating non-migrating diurnal tide with zonal wavenumber-3 (DE3) on nitric oxide (NO) infrared cooling rate. We find that the DE3 tide can drive a DE3 signal in lower thermospheric NO cooling rate, and the simulated altitudinal and seasonal variations are according with that of DE3 signal in equatorial lower thermospheric NO cooling rate observed by Oberheide et al. [2013], which is based on the TIMED/SABER observations during the solar minimum year 2008. This signal mainly shows an annual variation, which is stronger between June and September, and weaker near November. The maximum of the absolute signal, whose value is about 0.35*10<sup>-9</sup> W/m<sup>3</sup>, occurs near the height of 130 km, but the relative signal mainly shows its peak with a value of 40% near the height of 100 km. Due to the difference of the driving mechanism, the distribution of NO signals in different latitudinal regions shows obvious difference. The middle- and low-latitude NO signal show smooth variation, while the high-latitude signal is discontinuous. The DE3 signal in NO cooling rate is mainly controlled by DE3 temperature tide and DE3 NO tide, meanwhile, the influences of DE3 neutral density tide on the DE3 signal can be ignored. The relative contributions of the DE3 NO tide and of the DE3 temperature tide vary with geographic latitude. The DE3 cooling rates in middle- and low- latitude and in high-latitude are respectively mainly driven by the DE3 temperature tide DE3 NO tide. DE3 tide may not only drive the DE3 signal, but also affect the lower thermospheric zonal mean NO cooling rate. The maximum of the absolute influence, whose value is about 0.12*10<sup>-9</sup> W/m<sup>3</sup>, occurs above the height of 140 km, but the relative influence mainly shows its peak with a value of 10% near the height of 100 km.</p><p></p><p></p><p></p><p></p><p></p>

Global structures of the DE3 tide

2008 ◽  
Vol 54 (6) ◽  
pp. 1073-1079 ◽  
Author(s):  
ZeYu Chen ◽  
DaRen Lu
Keyword(s):  
De3 Tide
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