Flats
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Spring tulips in bloom in Madison Square Park in Manhattan, with New York City's famous Flat Iron Building in the distance. Shot with the Olympus E-M1.
With Columbia Lake as a background, an empty Canadian Pacific coal train cruises into Canal Flats, British Columbia, on a beautiful June 27, 2006.
During sunset, a cloud flew in in an amazing shape (a bird, a dragon, and maybe an angel ...)
A little understanding of the physics of cloud formation underscores the complexity of the atmosphere and sheds light on why predicting weather for more than a few days is such a challenge.
Six types of clouds you can see and how they can help you understand the weather.
1) Cumulus clouds - On a sunny day, rays warm the earth, which heats the air located directly above it. The heated air rises upward due to convection and forms cumulus clouds. These “good weather” clouds are like cotton wool. If you look at the sky filled with cumulus clouds, you can see that they have a flat bottom, located at the same level for all clouds. At this altitude, air rising from ground level cools down to the dew point. It usually doesn't rain from cumulus clouds, which means the weather will be good.
2) Cumulonimbus clouds.
Small cumulus clouds do not rain, but if they grow and grow in height, it is a sign that heavy rain is coming soon. This often happens in summer when morning cumulus clouds turn into cumulonimbus during the day. Cumulonimbus clouds often have a flat top. Air convection occurs inside such a cloud, and it gradually cools until it reaches the temperature of the surrounding atmosphere. At this moment, it loses its buoyancy and can no longer rise higher. Instead, it spreads out to the sides, forming the characteristic anvil shape.
3) Cirrus clouds form in very high layers of the atmosphere. They are smoky because they are composed entirely of ice crystals falling in the atmosphere. When cirrus clouds are carried by winds moving at different speeds, they take on a characteristic curved shape. And only at very high altitudes or at high latitudes, cirrus clouds give out rain that reaches the ground.
4) Stratus Clouds - A low-lying, continuous cloud sheet that covers the sky. Stratus clouds are formed by slowly rising air or gentle winds that cover the cold land or sea surface with moist air. Stratus clouds are thin, therefore, despite the gloomy picture, it is unlikely to rain from them, a little drizzle at most. Stratus clouds are identical to fog, so if you've ever walked in a mountainous area on a foggy day, you've been inside a cloud.
5) Lenticular clouds. Smooth and lenticular lenticular clouds form when air is blown up and over a mountain range, and as it travels over a mountain, the air descends to its previous level. At this time, it heats up and the cloud evaporates. But it can slip further, as a result of which the air rises again and forms another lenticular cloud. This can result in a chain of clouds extending far beyond the mountain range. The interaction of wind with mountains and other surface features is one of the many details that must be taken into account in computer simulations to obtain accurate weather predictions.
6) Kelvin - Helmholtz like a breaking ocean wave. When air masses at different heights move horizontally at different speeds, their state becomes unstable. The boundary between the air masses begins to ripple and form large waves, such clouds are quite rare.
The photo was taken in the city of Konakovo. Russia. On the banks of the Volga River.
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I spotted this mountain like cloud with a flat top, known as a cumulonimbus in the Beagle Channel.This type of cloud usually means a storm may be on its way.
Salar de Talar is a large salt flat located in the high puna of northern Chilean Andes, at an altitude of 3,950 m. It is part of a series of salt lakes and salt flats located at the foothills of a chain of volcanoes stretching along the eastern side of the much greater Salar de Atacama. The salty flat is bordered on the west by Caichinque and on the east by Cerro Medano, is a mountain with striking shades of grey and brown, which contrast nicely with the sparkling white of the salt flat's surface. On top of that, colourful ponds fringe its shores. Salar de Talar is a part of the Central Andean dry puna ecoregion, which in this zone is characterized by tussock grass vegetation.
Up until Autumn 2006, Alkborough Flats was agricultural land. The flood-bank of the Humber Estuary was breached and 450 hectares of farmland were flooded. the confluence of the River Trent and River Ouse as they flow into the Humber. It was all part of a huge scheme that will restore some of the Humber Estuary's natural flood control basins, while simultaneously creating a haven for wildlife.
The Isle of Wight Red Funnel ferry 'Red Osprey' in IKEA colours - not bad for a flat-pack!!
Southampton, UK.
Banyule Swamp at Banyule Flats Reserve, Viewbank (Melbourne, Australia).
Sony FE 24-105mm F4 G OSS
59mm; 1/40 sec; f/8; ISO 100
Taken last winter on a visit to York. The medieval city of York has this wonderful old wall encircling it which is fully open to the public. It dates back to Roman times although most of the Roman bits were replaced by another wall built by the Viking invaders around 1400 years ago. The current wall, while retaining elements of the Roman and Viking structures, dates back to construction that took place from the 12th to 14th century, so basically it's a pretty old wall. What a treat it was for me to capture this elderly gentleman in his traditional flat cap strolling along this part of the wall. But look closely because this is something I just can't figure out. He doesn't appear to have any hands! I have no idea why that is. I haven't touched this image other than to process it in the normal way. Very weird indeed.
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A flat cap (sometimes "scally cap") is a rounded cap with a small stiff brim in front, originating in Great Britain and Ireland. The hat is known in Ireland as a paddy cap, in Scotland as a bunnet, in Wales as a Dai cap, in New Zealand as a cheese-cutter, and in the United States as a driving cap. Cloths used to make the cap include wool, tweed (most common), and cotton.
Choi Hung Estate (Chinese: 彩虹邨; literally: 'Rainbow Estate') is one of the oldest public housing estates in Hong Kong. Built in 1962-1964, Choi Kung Estate acommodates nearly 42,000 people.