Results 101 to 110 of about 348 (165)
Grape Version 1: First prototype of the low-cost personal space weather station receiver. [PDF]
Gibbons J +3 more
europepmc +1 more source
This study explores the meteorological source and vertical propagation of gravity waves (GWs) that drive daytime traveling ionospheric disturbances (TIDs), using the specified dynamics version of the SD-WACCM-X (Whole Atmosphere Community Climate Model ...
Kogure Masaru +8 more
doaj +1 more source
Internal report. Spectral methods for time delay estimation of MSTIDs signal
Internal ReportThe primary goal of this work is to summarize spectral meth- ods to estimate the time delay variations of the detrended Medium Scale Traveling Ionospheric Disturbances (MSTIDs) signals and pre- liminarily discuss the potential infuence of ...
Monte Moreno, Enrique +2 more
core
General resource for ionospheric transient investigations (GRITI): An open-source code developed in support of the Dinsmore et al. (2021) results. [PDF]
Dinsmore R, Mathews JD, Urbina J.
europepmc +1 more source
In order to characterize the phenomenon known as Medium-Scale Traveling Ionospheric Disturbances (MSTIDs), we present in this paper the resultsobtained from the statistical analysis of 10.5 years all-sky images of OI 630 nm airglow emission over the ...
Alexandre Alvares Pimenta +2 more
core +1 more source
To investigate solar activity dependence of the coupling between medium-scale traveling ionosphere disturbance (MSTID) and sporadic E (Es) layer, we analyzed the total electron content (TEC) obtained from a Japanese global positioning system (GPS ...
Veera Kumar Maheswaran +8 more
doaj +1 more source
Origin and Distribution of Daytime Electron Density Irregularities in the Low-Latitude F Region. [PDF]
Kil H, Lee WK, Paxton LJ.
europepmc +1 more source
Tropospheric jet-front systems and intense convection are known to be potential sources of atmospheric gravity waves (AGWs), which can propagate upward.
Barta Veronika +19 more
doaj +1 more source
The term “Medium-Scale Traveling Ionospheric Disturbances” is used to describe a number of different propagating phenomena in ionospheric plasma density with a scale size of hundreds of km.
Jeff Klenzing +20 more
doaj +1 more source
Observations of MSTIDs/GWs at the F2 layer heights in the near equatorial region.
Ionospheric vertical sounding observations, using a digital ionosonde (Canadian Advanced Digital Ionosonde(CADI)) , arebeing carried out on a routine basis at Manaus (2,9 0 S; 60,0 0 W; dip latitude 6,4 N, hereafter referred to as MAN), Brazil, locatedbetween the geographic and geomagnetic dip equators, since August 2002, (Fig. 1).
Silva de Lima, Newton +2 more
openaire +1 more source

