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He ion dominance in the high-latitude upper ionosphere as observed in “active” experiment
Ion density measurements using the Bennett-type mass spectrometer aboard the Intercosmos-24 satellite (I=82.6°, P=510 km, A=2500 km) were analyzed from about 130 full orbits from December 1989 to March 1991. He + dominance has been studied for regions of the polar hole, invariant latitudes larger th...
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Published in: | Advances in space research 1998, Vol.22 (9), p.1381-1384 |
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container_title | Advances in space research |
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creator | Ershova, V.A Kochnev, V.A Roste, O.Z Shultchishin, Yu.A Šmilauer, J Třísková, L |
description | Ion density measurements using the Bennett-type mass spectrometer aboard the Intercosmos-24 satellite (I=82.6°, P=510 km, A=2500 km) were analyzed from about 130 full orbits from December 1989 to March 1991. He
+ dominance has been studied for regions of the polar hole, invariant latitudes larger than 70°. He
+ dominance occurs in the winter dusk ionosphere (solar zenith angle
χ>100°), mainly for night sector at 1000 to 2400 km heights; it seems to be a feature of winter solstice, at least for periods of high solar activity. In regions of He
+ dominance, He
+ concentrations in the range of 2.10
7–2.10
9 m
−3 were observed. The role of solar zenith angle and convection processes as well as dependence on universal time is shown. |
doi_str_mv | 10.1016/S0273-1177(98)80040-9 |
format | article |
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+ dominance has been studied for regions of the polar hole, invariant latitudes larger than 70°. He
+ dominance occurs in the winter dusk ionosphere (solar zenith angle
χ>100°), mainly for night sector at 1000 to 2400 km heights; it seems to be a feature of winter solstice, at least for periods of high solar activity. In regions of He
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7–2.10
9 m
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+ dominance has been studied for regions of the polar hole, invariant latitudes larger than 70°. He
+ dominance occurs in the winter dusk ionosphere (solar zenith angle
χ>100°), mainly for night sector at 1000 to 2400 km heights; it seems to be a feature of winter solstice, at least for periods of high solar activity. In regions of He
+ dominance, He
+ concentrations in the range of 2.10
7–2.10
9 m
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+ dominance has been studied for regions of the polar hole, invariant latitudes larger than 70°. He
+ dominance occurs in the winter dusk ionosphere (solar zenith angle
χ>100°), mainly for night sector at 1000 to 2400 km heights; it seems to be a feature of winter solstice, at least for periods of high solar activity. In regions of He
+ dominance, He
+ concentrations in the range of 2.10
7–2.10
9 m
−3 were observed. The role of solar zenith angle and convection processes as well as dependence on universal time is shown.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/S0273-1177(98)80040-9</doi><tpages>4</tpages></addata></record> |
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title | He ion dominance in the high-latitude upper ionosphere as observed in “active” experiment |
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