We are pleased to announce that on January 21, 2010 ‘Kind of blurry’ became official member 20331 of The Cloud Appreciation Society.
The Cloud Appreciation Society is an organization based in the UK promoting an interest in clouds, and has over 20,000 members all over the world. Read more about it in this previous article.
If you feel curious to know how high (or low) a cloud is, you can learn now how to calculate it.
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Height = 125 x (outside temperature ºC – dew point ºC)
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The Cloud Appreciation Society is an organization promoting an interest in clouds, with news, forums, photograph gallery and members area. It has published as well an amount of books in different languages, such as ‘The Cloudspotter’s Guide’ and ‘The Cloud Collector’s Handbook’. Read the rest of this article
霞 【かすみ】 kasumi, (spring) mist [frequently translated as 'haze']
朝霞 【あさがすみ】 asagasumi, morning mist
夕霞 【ゆうがすみ】 yūgasumi, evening mist
遠霞 【とおがすみ】 tōgasumi, distant mist
Current satellite image of the Grand Banks
© Environment Canada / NOAA Polar Orbiting Sat imagery
The foggiest place in the world is the Grand Banks off the island of Newfoundland, Canada, with over 200 foggy days each year.
Fog is frequent here as the Grand Banks is the meeting place of the cold Labrador Current from the north and the much warmer Gulf Stream from the south. The cold Labrador Current runs over the Grand Banks, and when warm air passes over this water, a dense fog forms.
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Clouds found on the earth’s surface which obscure visibility to less than 1000 metres are called fog. Ground fog or low lying fog refers to fog located below eye level. Fog is formed when vapour-laden air cools down or when cool air and warm air mix together. The names given to sorts of fog in meteorology reveal the conditions under which a given sort is formed.
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When you know about them, you will notice them: cloud streets. They occur in coastal regions if the wind blows from sea. They consist of individual cumulus clouds, which are organized in parallel lines or streets. The distance between two streets is typical 1.5 km. On the Frisian island Terschelling, where I spend a few weeks any year, I usually spot such streets a few times during each stay. They occur there during south-western wind, that is when the wind direction is parallel with the island. Over Terschelling, about 4 km wide, there are usually three of these streets; between them the sky is clear. If you are unlucky enough, such a street keeps you many hours out of the sun. Over the sea there are no clouds at all.
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Dutch landscape painting of the 17 century has gained a unique place in art history; for the first time landscape played a role of its own due to its realist naturalistic reproduction. But the ‘realism’ in the paintings of the Dutch ‘Golden Age’ must not be wrongly interpreted that they represent a linear copy of nature (de Vries 1991), as an early form of landscape photography. The paintings have to be understood as compositions, composed of realistically reproduced elements where the whole is much more than a summary of the single parts. Hedinger (2001) has called this an ‘invented reality’ of landscape.
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