(above the “F1 region”, ‘atomic oxygen’ becomes the dominant constituent because lighter particles tend to occupy higher altitudes above the ‘turbopause’ (at ~100 km))
(this ‘atomic oxygen’ provides the ‘O+ atomic ions’ that make up the “F2 layer”)
(the outer boundary of the “F2 layer” is the “ionopause”)
(nearer to the surface, “solar-wind dynamic pressure” reaches a balance with the pressure from the “ionosphere”, in a region called the “ionopause”)
(this interaction typically prevents “solar-wind stripping” from being the dominant loss process of the ‘atmosphere’)
.
.
*👨🔬🕵️♀️🙇♀️*SKETCHES*🙇♂️👩🔬🕵️♂️*
.
.
.
.
👈👈👈☜*THE ‘F’ LAYER* ☞ 👉👉👉
*EARTH’S IONO-SPHERE*
.
.
💕💝💖💓🖤💙🖤💙🖤💙🖤❤️💚💛🧡❣️💞💔💘❣️🧡💛💚❤️🖤💜🖤💙🖤💙🖤💗💖💝💘
.
.
*🌈✨ *TABLE OF CONTENTS* ✨🌷*
.
.
🔥🔥🔥🔥🔥🔥*we won the war* 🔥🔥🔥🔥🔥🔥