Please answer the question clearly.
Consider sunlight striking the atmosphere off-zenith (e.g., at high latitudes). What impact does this have on the height and peak density of a Chapman layer as compared to zenith illumination?
When sunlight striking the atmosphere off-zenith (e.g., at high latitudes), The height of a chapman layer as compared to zenith illumination is Greater or simply due to this, the chapman layer has Greater height.
The peak density of the chapman layer is lower as compared to Zenith illumination.
So, When sunlight striking the atmosphere off-zenith, it resulted Greater height and Lower density in Chapman Layer.
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Please answer the question clearly. Consider sunlight striking the atmosphere off-zenith (e.g., at high latitudes). What...
Consider sunlight striking the atmosphere off-zenith (e.g., at high latitudes). What impact does this have on the height and peak density of a Chapman layer as compared to zenith illumination?
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