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[PDF] Top 20 A study of atmospheric gravity waves and travelling ionospheric disturbances at equatorial latitudes

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A study of atmospheric gravity waves and travelling ionospheric disturbances at equatorial latitudes

A study of atmospheric gravity waves and travelling ionospheric disturbances at equatorial latitudes

... Abstract. A global coupled thermosphere-ionosphere- plasmasphere model is used to simulate a family of large-scale imperfectly ducted atmospheric gravity waves (AGWs) and ... Voir le document complet

10

A study of the Joule and Lorentz inputs in the production of atmospheric gravity waves in the upper thermosphere

A study of the Joule and Lorentz inputs in the production of atmospheric gravity waves in the upper thermosphere

... CIRES/University of Colorado, NOAA Space Environment Laboratory, 325 Broadway, Boulder, CO 80303, USA Received: 15 March 1996 / Revised: 12 February 1997 / Accepted: 24 February 1997 ...results of a ... Voir le document complet

8

Mathematical study of the betaplane model: Equatorial waves and convergence results

Mathematical study of the betaplane model: Equatorial waves and convergence results

... feature of the response of a rotating fluid to gravity is that it does not adjust to a state of rest, but rather to an equilibrium which contains more potential energy than does ... Voir le document complet

106

A modeling study of ionospheric F2-region storm effects at low geomagnetic latitudes during 17-22 March 1990

A modeling study of ionospheric F2-region storm effects at low geomagnetic latitudes during 17-22 March 1990

... to a change in the global thermo- spheric wind circulation system. As a consequence of this high-latitude heating and expansion, equatorward directed neutral winds are generated which lift up ... Voir le document complet

27

Travelling ionospheric disturbance over California mid 2000

Travelling ionospheric disturbance over California mid 2000

... launch of a Minuteman-II missile on 8 July 2000 (UTC) is processed to reveal traveling ionospheric disturbance (TID) all over the network on average 15 min after the ...occurring at one single ... Voir le document complet

8

Gravity travelling waves for two superposed fluid layers, one being of infinite depth: a new type of bifurcation

Gravity travelling waves for two superposed fluid layers, one being of infinite depth: a new type of bifurcation

... 5.5 at section 5.(e)). The divergence of the resolvent operator when k → 0 is worse for ε = 0, than for ε 6= 0, as can be seen on formula (40) of (Iooss 1999), and in subsequent expressions ... Voir le document complet

92

A study of transient variations in the Earth's electromagnetic field at equatorial electrojet latitudes in western Africa (Mali and the Ivory Coast)

A study of transient variations in the Earth's electromagnetic field at equatorial electrojet latitudes in western Africa (Mali and the Ivory Coast)

... framework of the French-Ivorian participation to the IEEY, a network of 10 electromag- netic stations were installed at African ...aim of this experiment was twofold: ®rstly, to ... Voir le document complet

22

Modelling ionospheric effects for L band GNSS receivers at high latitudes.

Modelling ionospheric effects for L band GNSS receivers at high latitudes.

... solar and geomagnetic ...kinds of effects: mean effects and dynamic ...delay and the signal phase advance when going through the ionosphere. At the first order this delay depends on the ... Voir le document complet

5

Excitation of the ionospheric resonance cavity by neutral winds at middle latitudes

Excitation of the ionospheric resonance cavity by neutral winds at middle latitudes

... prises of two ...mode and its eigenfrequency and damping rate strongly depend on ...orders of magnitude smaller than that for the shear Alfv´en ...enhancement of the damping rate ... Voir le document complet

14

Irregular structures of the F layer at high latitudes during ionospheric heating

Irregular structures of the F layer at high latitudes during ionospheric heating

... periods. At 22:18±22:30 UT, when the drift is approximately per- pendicular to the tomographic image plane, the tilt ofthe ionosphere lies well within the heating ...hand, at 17:46±18:01 UT the tilt extends ... Voir le document complet

14

A statistical study of gravity waves from radiosonde observations at Wuhan (30° N, 114° E) China

A statistical study of gravity waves from radiosonde observations at Wuhan (30° N, 114° E) China

... ellipse, and the asterisk and plus symbols demonstrate that the disturbance wind vector rotates anti- ...inertial gravity waves, the anti-clockwise rotating hodograph indi- cates that in the ... Voir le document complet

10

Traveling ionospheric disturbances propagating ahead of the Tohoku-Oki tsunami: a case study,

Traveling ionospheric disturbances propagating ahead of the Tohoku-Oki tsunami: a case study,

... More specifically, we note the following features: G the CTIDs and ATIDs are slower/similar and faster propagating wave fronts, respectively, H for the tsunami arrival at epicentre dista[r] ... Voir le document complet

12

DMT alters cortical travelling waves

DMT alters cortical travelling waves

... FW travelling waves increase during visual stimulation, whereas BW waves decrease, in-line with their putative functional role in information transmission ( Pang et ...sake of comparison, we ... Voir le document complet

17

Midday reversal of equatorial ionospheric electric field

Midday reversal of equatorial ionospheric electric field

... storm at 1218 h 75  E on 24 October ...variations of the various parameters for the period 22 to 25 October ...depressions of storm time H ®eld at ABG with a magnitude of ÿ100 ... Voir le document complet

8

Travelling Waves in a Chain of Coupled Nonlinear Oscillators

Travelling Waves in a Chain of Coupled Nonlinear Oscillators

... reducibility of quasilinear elliptic systems in infinite cylindrical ...to a suitable neighborhood of 0, is equivalent to a flow on a finite dimensional ...validity of a ... Voir le document complet

30

Non-trough <i>fo</i>F2 enhancements at near-equatorial dip latitudes

Non-trough <i>fo</i>F2 enhancements at near-equatorial dip latitudes

... three equatorial ionosondes of the IEEY network in West Africa have revealed small-scale daytime peak F2 structures, super- posed on the slowly varying minimum or ``trough'' distribution in the ‹5° magnetic ... Voir le document complet

11

Morning quiet-time ionospheric current reversal at mid to high latitudes

Morning quiet-time ionospheric current reversal at mid to high latitudes

... look at a series of ten days for the X component in December 1989, as shown in ...Three of the observatories CTA, NEW and TOO, are on the east- ern side of Australia while the ... Voir le document complet

8

Analytical Solution for Waves in Planets with Atmospheric Superrotation. I. Acoustic and Inertia-Gravity Waves

Analytical Solution for Waves in Planets with Atmospheric Superrotation. I. Acoustic and Inertia-Gravity Waves

... first of a two-part study devoted to developing tools for a systematic classification of the wide variety of atmospheric waves expected on slowly rotating planets ... Voir le document complet

19

The relationship between small-scale and large-scale ionospheric electron density irregularities generated by powerful HF electromagnetic waves at high latitudes

The relationship between small-scale and large-scale ionospheric electron density irregularities generated by powerful HF electromagnetic waves at high latitudes

... occur at latitudes both above and below that corresponding to field-aligned which is ...three of the passes the peak occurs south of field-aligned (the minimum of the 2 curve), ... Voir le document complet

10

IonoSeis: A Package to Model Coseismic Ionospheric Disturbances

IonoSeis: A Package to Model Coseismic Ionospheric Disturbances

... to a point source on Earth’s surface. The code has now been used in a few studies ...]), and we continue to make improvements, including reducing the approximations made in the ...]), and ... Voir le document complet

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