Near orbital twilight, with low angled lighting, thunderheads rising high above the cloud layer produce steep shadows. These shadows can be hundreds of miles long, adding a striking contrast between the white cloud tops and the shadowy valleys.
Near orbital twilight, with low angled lighting, thunderheads rising high above the cloud layer produce steep shadows. These shadows can be hundreds of miles long, adding a striking contrast between the white cloud tops and the shadowy valleys.
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