20090815-0048 Rotheca serrata (L.) Steane & Mabb.
20090815-0060 Rotheca serrata (L.) Steane & Mabb.
20090815-0077 Brassica juncea (L.) Czern.
20090815-0083 Brassica juncea (L.) Czern.
20090815-0084 Brassica juncea (L.) Czern.
20090815-0096 Curcuma pseudomontana J.Graham
20090815-0150 Tectona grandis L.f.
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20090815-0357 Myriophyllum sp.
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20090816-0646 Lindernia sp.
20090816-0654 Spermacoce articularis L.f.
20090816-0665 Impatiens acaulis Arn.
20090816-0666 Impatiens acaulis Arn.
20090816-0669 Sonerila scapigera Dalzell
20090816-0681 Sonerila scapigera Dalzell
20090816-0762 Sonerila scapigera Dalzell
20090816-0696 Utricularia striatula Sm.
20090816-0707 Utricularia striatula Sm.
20090810-0149
20090810-0128
20090810-0098 Eriocaulon sp.
20090810-0093 Eragrostis unioloides (Retz.) Nees e…
20090810-0067
20090810-0060
20090810-0057 Spermacoce articularis L.f.
20090810-0051 Spermacoce articularis L.f.
20090810-0036
20090810-0021 Curcuma pseudomontana J.Graham
20090810-0013 Gloriosa superba L.
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20090809-0800 Pityrogramma calomelanos (L.) Link
20090809-0799 Pityrogramma calomelanos (L.) Link
20090809-0782 Ariopsis peltata Nimmo
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20090811-0201 22° Solar Halo
![20090811-0201 22° Solar Halo 20090811-0201 22° Solar Halo](https://cdn.ipernity.com/141/40/55/31264055.69ca28f1.640.jpg?r2)
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22° Solar Halo
Photographed in Mahad on August 11, 2009.
A 22° halo is an optical phenomenon forming a circle 22° around the sun, or occasionally the moon. It forms as sunlight is refracted in hexagonal ice crystals suspended in the atmosphere. As the light beam passes through two sides of the prism forming a 60° angle, the angle of minimum deviation is almost 22° (e.g. 21,84° in average; 21,54° for red and 22.37 for blue.) This wavelength-dependent variation in refraction causes the inner edge of the circle to be reddish while the outer edge is bluish.
Light passing through the hexagonal ice prisms is deflected twice which produces deviation angles ranging from 22° to 50°. Lesser deviation results in a brighter halo along the inner edge of the circle, while greater deviation contribute to the weaker outer part of the halo. As no light is refracted at smaller angles than 22° the sky is darker inside the halo.
22° halos form when the sky contains millions of poorly oriented ice crystals. Some of these happen to be aligned perpendicular to the sun light as viewed by one observer which produces the illuminated 22° circle, while other crystals produces the same phenomenon for other observers. An Alexander's band can be seen inside the halo.
Like other ice halos, 22° halos appear when the sky is covered by thin cirrus clouds containing the ice crystals which causes the phenomenon. Small colourful coronas much nearer the sun produced by water droplets can occasionally be confused with 22° halos.
Ref. en.wikipedia.org/wiki/22%c2%b0_halo
Photographed in Mahad on August 11, 2009.
A 22° halo is an optical phenomenon forming a circle 22° around the sun, or occasionally the moon. It forms as sunlight is refracted in hexagonal ice crystals suspended in the atmosphere. As the light beam passes through two sides of the prism forming a 60° angle, the angle of minimum deviation is almost 22° (e.g. 21,84° in average; 21,54° for red and 22.37 for blue.) This wavelength-dependent variation in refraction causes the inner edge of the circle to be reddish while the outer edge is bluish.
Light passing through the hexagonal ice prisms is deflected twice which produces deviation angles ranging from 22° to 50°. Lesser deviation results in a brighter halo along the inner edge of the circle, while greater deviation contribute to the weaker outer part of the halo. As no light is refracted at smaller angles than 22° the sky is darker inside the halo.
22° halos form when the sky contains millions of poorly oriented ice crystals. Some of these happen to be aligned perpendicular to the sun light as viewed by one observer which produces the illuminated 22° circle, while other crystals produces the same phenomenon for other observers. An Alexander's band can be seen inside the halo.
Like other ice halos, 22° halos appear when the sky is covered by thin cirrus clouds containing the ice crystals which causes the phenomenon. Small colourful coronas much nearer the sun produced by water droplets can occasionally be confused with 22° halos.
Ref. en.wikipedia.org/wiki/22%c2%b0_halo
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