H+ - O+ Coulomb Collision Frequency in the Polar Wind Plasma
The polar wind is an ambipolar plasma outflow from the terrestrial ionosphere at high latitudes. As the ions drift upward along geomagnetic flux tubes, they move from collision-dominated to collisionless regions. A Monte Carlo simulation was used to calculate the temperature and Coulomb collisio...
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| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
An-Najah National University
2003-12-01
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| Series: | مجلة جامعة النجاح للأبحاث العلوم الطبيعية |
| Online Access: | https://journals.najah.edu/media/journals/full_texts/h-o-coulomb-collision-frequency-polar-wind-plasma.pdf |
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