Results 101 to 110 of about 22,029 (223)

Ion–Molecule Reaction Products as Probes and Precursors for Preparative Mass Spectrometry

open access: yesChemistry – A European Journal, Volume 32, Issue 14, 15 April 2026.
Ion–molecule reactions in the gas phase of mass spectrometers are important for preparative mass spectrometry because they (1) provide knowledge about the intrinsic reactivity of ions, helping to predict and control their reactivity at interfaces, and (2) generate new complex ions that can be mass selected and deposited on surfaces.
Markus Rohdenburg   +4 more
wiley   +1 more source

Minor ion composition in the polar ionosphere

open access: yesGeophysical Research Letters, 1991
Ion composition measurements from the EXOSD Suprathermal Ion Mass Spectrometer (SMS) are presented. Ions other than H+, notably O+, He+, O++ N+ and N++, are found to constitute a significant (>0.1) and at times dominant (>0.5) component of the thermal ion population in the high‐altitude polar ionosphere.
Andrew W. Yau   +2 more
openaire   +1 more source

Plasma Wave Experiments in the Polar Ionosphere

open access: yesAntarctic Record, 1975
Some important points on the plasma wave experiments in the polar ionosphere are indicated. Concrete proposals of the antarctic rocket experiments on the plasma waves are given.
Hiroshi MATSUMOTO, Iwane KIMURA
doaj   +1 more source

Turbulent boundary layer in the polar ionosphere.

open access: yesJournal of geomagnetism and geoelectricity, 1990
The interaction between ionosphere and neutral atmosphere at heights of the dynamo-region leads to the development of Alfven mode instability when the convection velocity exceeds the threshold value VΠ≈0.1km/s. The ionospheric Alfven resonator (IAR) plays an important role as an accumulator of turbulent energy.
V. Yu. TRAKHTENGERTS, A. Ya FELDSTEIN
openaire   +2 more sources

GPS scintillation effects associated with polar cap patches and substorm auroral activity: direct comparison

open access: yesJournal of Space Weather and Space Climate, 2014
We directly compare the relative GPS scintillation levels associated with regions of enhanced plasma irregularities called auroral arcs, polar cap patches, and auroral blobs that frequently occur in the polar ionosphere.
Jin Yaqi   +2 more
doaj   +1 more source

Rocket Observations of the Lower Ionosphere in the 12th-14th Japanese Antarctic Research Expeditions (1971-1973)

open access: yesAntarctic Record, 1975
The 12th, 13th and 14th Japanese Antarctic Research Expedition parties (1971-73), carried out firings of twenty-one rockets to observe the polar ionosphere and auroral phenomena at Syowa Station(69°00'S, 39°35'E; geomagnetic lat. 69.6°S, long.
Shigeru MIYAZAKI
doaj   +1 more source

Cold ions of ionospheric origin observed at the dayside magnetopause and their effects on magnetic reconnection [PDF]

open access: yes, 2015
Thesis (Ph.D.) University of Alaska Fairbanks, 2015Magnetic reconnection at the dayside magnetopause is one of the most important mechanisms that efficiently transfers solar wind particles, momentum, and energy into the magnetosphere.
Lee, Sun-Hee, 이, 선희
core  

Ionospheric Imaging for Canadian Polar Regions

open access: yes, 2013
Global Navigation Satellite Systems (GNSS) can be exploited as a cost-effective tool to remotely sense the Earth’s ionosphere and investigate its characteristics. This is due to the global coverage and dual frequency data availability offered through worldwide networks of GNSS stations.
openaire   +2 more sources

Field-aligned currents observed by the OGO 5 and Triad satellites [PDF]

open access: yes
The existence of field-aligned currents in the polar cap boundary layer as a permanent feature of the magnetosphere is investigated. Magnetic field observations from Triad at 800 km altitude and from OGO 5 in the high-altitude magnetosphere are examined.
Sugiura, M.
core   +1 more source

Ionosphere-thermosphere (IT) response to solar wind forcing during magnetic storms

open access: yesJournal of Space Weather and Space Climate, 2016
During magnetic storms, there is a strong response in the ionosphere and thermosphere which occurs at polar latitudes. Energy input in the form of Poynting flux and energetic particle precipitation, and energy output in the form of heated ions and ...
Huang Cheryl Yu-Ying   +5 more
doaj   +1 more source

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