© Yakov
Leningrad Oblast, Russian Federation
Latitude: 59° 53' 23'' N
Longitude: 31° 2' 16'' E
08 August 2015 0320 (Local Time)
Camera direction: towards NE
Image P/S code: S.10U.3
Image I.D.: 5579
Noctilucent clouds (NLC) are high-altitude, “night-shining” clouds that are only visible to observers in mid to high latitudes (approximately 50°N to 65°N or 50°S to 65°S). They only form during the summer when the temperatures in the mesosphere are the coldest.
NLC are visible against the background of a dark twilight sky when the Sun is well below the horizon, but the clouds themselves are still illuminated by the Sun. Generally, NLC will be seen close to the horizon (as shown in this picture), typically extending up to around 15° to 20° above the horizon along the twilight arch. However, they can extend to higher elevations.
Noctilucent cloud is distinguished by its typical bluish-white colour. The clouds are brighter than the twilight sky. In this picture, billows (type III) are clearly visible at 2 and 3. A patch of tropospheric cloud appears in silhouette on the left of the picture.
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Noctilucent clouds (NLC) are usually only visible to observers in mid to high latitudes (roughly 50°N to 65°N or 50°S to 65°S) and in the twilight or night sky for a few months in summertime, when temperatures in the mesosphere are the coldest. This photograph was taken in late June, during summer in the northern hemisphere, from a location 55.78°N.
Noctilucent clouds are generally observed during the twilight periods when the Sun is between 6° and 16° below the observer's horizon. It is during this period that the background sky is dark enough for the cloud to be seen, yet the high-altitude clouds are still illuminated by sunlight.
Typically what sets noctilucent clouds visually apart from tropospheric clouds is their visibility in the night and their obvious, and sometimes bright, blue-white colour. The low-level tropospheric clouds at 2 and 3 are within the Earth's shadow and they stand out as dark silhouettes against the relatively brighter background sky. In contrast, noctilucent clouds are always brighter than the twilight sky. Near the horizon, they may have a reddish tint. Two main types of NLC are shown here: bands (type II) – these are long streaks – and billows (type III), seen at 7 and 8 – these are closely spaced, roughly parallel streaks.
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Type III – billows: these are arrangements of closely spaced, roughly parallel short streaks. There are two types:
– Type IIIa: comprised of short, straight and narrow streaks
– Type IIIb: exhibiting a wave-like structure with undulations
The billow type shown in this picture is type IIIb – a wave-like structure with undulations.
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