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Seasonal and Daily Variations in the Ion Content of the Earth’s Middle Atmosphere and Ionosphere. / Grankin, Dmitriy; Mironova, Irina; Rozanov, Eugene.

In: Bulletin of the Russian Academy of Sciences: Physics, Vol. 89, No. 5, 01.05.2025, p. 762-767.

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@article{267bd24852c849b4b1ed412b54253e37,
title = "Seasonal and Daily Variations in the Ion Content of the Earth{\textquoteright}s Middle Atmosphere and Ionosphere",
abstract = "Abstract: The high latitude Earth{\textquoteright}s atmosphere is ionized via direct solar radiation. This results in the formation of positively charged ions through, e.g., photoionization and the ionization of NO. A one-dimensional chemical and climatic model with interactive neutral and ionic chemistry is used to track the ionic compositions of the D region of the ionosphere on daily and seasonal scales. It is found that ion clusters dominate the total ion content up to altitudes of 95 km in winter and 80 km in summer.",
keywords = "ionic content, middle atmosphere and ionosphere, seasonal and daily variations",
author = "Dmitriy Grankin and Irina Mironova and Eugene Rozanov",
year = "2025",
month = may,
day = "1",
doi = "10.1134/S1062873825711109",
language = "English",
volume = "89",
pages = "762--767",
journal = "Bulletin of the Russian Academy of Sciences: Physics",
issn = "1062-8738",
publisher = "Allerton Press, Inc.",
number = "5",

}

RIS

TY - JOUR

T1 - Seasonal and Daily Variations in the Ion Content of the Earth’s Middle Atmosphere and Ionosphere

AU - Grankin, Dmitriy

AU - Mironova, Irina

AU - Rozanov, Eugene

PY - 2025/5/1

Y1 - 2025/5/1

N2 - Abstract: The high latitude Earth’s atmosphere is ionized via direct solar radiation. This results in the formation of positively charged ions through, e.g., photoionization and the ionization of NO. A one-dimensional chemical and climatic model with interactive neutral and ionic chemistry is used to track the ionic compositions of the D region of the ionosphere on daily and seasonal scales. It is found that ion clusters dominate the total ion content up to altitudes of 95 km in winter and 80 km in summer.

AB - Abstract: The high latitude Earth’s atmosphere is ionized via direct solar radiation. This results in the formation of positively charged ions through, e.g., photoionization and the ionization of NO. A one-dimensional chemical and climatic model with interactive neutral and ionic chemistry is used to track the ionic compositions of the D region of the ionosphere on daily and seasonal scales. It is found that ion clusters dominate the total ion content up to altitudes of 95 km in winter and 80 km in summer.

KW - ionic content

KW - middle atmosphere and ionosphere

KW - seasonal and daily variations

UR - https://www.mendeley.com/catalogue/06b7c9b6-9f96-3e30-a02a-6787f1c9dc9e/

U2 - 10.1134/S1062873825711109

DO - 10.1134/S1062873825711109

M3 - Article

VL - 89

SP - 762

EP - 767

JO - Bulletin of the Russian Academy of Sciences: Physics

JF - Bulletin of the Russian Academy of Sciences: Physics

SN - 1062-8738

IS - 5

ER -

ID: 135960269