Results 61 to 70 of about 118,766 (238)
Equatorial airglow and the ionospheric geomagnetic anomaly [PDF]
OGO D observations of OI (6300A) emissions reveal a global pattern in the equatorial airglow undetected from the ground-based observations. The post sunset emission rate of OI is generally asymmetrical with respect to the geomagnetic equator and shows no apparent correlation with the ultraviolet airglow (OI 1304 and 1356A) and F region electron density
S. Chandra +3 more
openaire +1 more source
He+ dominance in the plasmasphere during geomagnetically disturbed periods: 1. Observational results [PDF]
Observations made by the DMSP 1710 satellite during the recovery phase from geomagnetic disturbances in June 1991 show regions of He+ dominance around 830 km altitude at 09:00 MLT.
Wilford, C. R. +13 more
core +2 more sources
Tidal Variability in the Lower Thermosphere: Relative Importance of ENSO, QBO, PJO, MJO, and Lyα
Abstract Atmospheric tides in the lower thermosphere play an important role in regulating upper‐atmospheric conditions relevant to space weather. However, their spatial and temporal variability remains poorly understood, apart from seasonal variations. Previous studies have shown that tides can be influenced by meteorological and solar conditions. This
Yosuke Yamazaki +4 more
wiley +1 more source
Equatorial electrojet as part of the global circuit: a case-study from the IEEY [PDF]
Geomagnetic storm-time variations often occur coherently at high latitude and the day-side dip equator where they affect the normal eastward Sq field. This paper presents an analysis of ground magnetic field and ionospheric electrodynamic data related
A. T. Kobea +7 more
doaj +1 more source
Longitudinal correlation of equatorial ionospheric scintillation [PDF]
Studies at the Air Force Research Laboratory are investigating methods for the incorporation of expected data sets from the Communication/Navigation Outage Forecast System (C/NOFS) satellite into existing scintillation specification models for an improved knowledge of the regional scintillation environment.
Ron Caton, Keith Groves
openaire +1 more source
Thermal Structure of the Equatorial Topside Ionosphere [PDF]
151-153The thermal structure of the equatorial topside ionosphere is theoretically investigated to explain the experimentally observed features, viz. (i) isothermal region in the 400-500 km range, (ii) close coupling of electron and ion temperatures, and
Singh, Risal, Rao, B. C. Narasinga
core
Abstract Lightning activity is strongly concentrated in tropical continental “chimneys”, among which the African lightning chimney stands out as the most intense globally. However, until recently, the incomplete and spatially uneven detection efficiency of ground‐based lightning networks, together with the limited spatio‐temporal coverage of satellite ...
K. Németh +8 more
wiley +1 more source
Generation of large-scale equatorial F-region plasma depletions during lowrange spread-F season [PDF]
All-sky imaging observations of the F-region OI 630nm nightglow emission allow us to visualize large-scale equatorial plasma depletions, generally known as trans-equatorial plasma bubbles. Strong range type spread-F is the radio signature of these
Y. Sahai +6 more
doaj +1 more source
Saturn's Ionosphere: Some Evidence of Equatorial Anomaly [PDF]
143-146Electron density profiles obtained from radio science experiments on Pioneer-11, Voyager-1 and Voyager-2 have been analyzed to look for equatorial anomaly in the ionosphere of Saturn. Although there is no measurement right at the magnetic equator,
Srilakshmi, M V, Mahajan, K K, Kar, J
core
Abstract The Mw 7.7 Myanmar earthquake on 28 March 2025 ruptured ∼480 km of the Sagaing Fault. Its fault slip distribution remains poorly constrained by three‐dimensional surface displacement data due to sparse GNSS‐coverage near the fault. Satellite‐based synthetic aperture radars capture meters of right‐lateral displacements but isolating vertical ...
Mala S. Bagiya +5 more
wiley +1 more source

