Abstract
Noctilucent clouds are immediately recognizable, even when being seen for the first time. The name suggests it all: they are night-shining clouds. From mid-latitudes(ø > 50°), they can be seen during the summer in the twilight arch which moves around the north (or south, in the southern hemisphere) horizon as the night progresses. In form much like cirrostratus clouds, they are usually silvery-white or pale blue in colour and they stand out clearly behind the darker twilight sky. Ordinary (i.e. tropospheric) clouds are dark silhouettes under these conditions; noctilucent clouds shine. The reason for this is that noctilucent clouds are very high in the atmosphere and remain in sunlight long after the Sun has set at ground level.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1989 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Gadsden, M., Schröder, W. (1989). Noctilucent Clouds. In: Noctilucent Clouds. Physics and Chemistry in Space Planetology, vol 18. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-48626-5_1
Download citation
DOI: https://doi.org/10.1007/978-3-642-48626-5_1
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-48628-9
Online ISBN: 978-3-642-48626-5
eBook Packages: Springer Book Archive