Clouds that can be found throught the year in St.Paul, Minnesota. For example: Stratus, Cirrus...
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All types of clouds can be found throught the year in St. Paul, Minnesota. I can't name them all, but go to the weather channel. They have all kinds of information.
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Hey buddy, try out Google Desktop Search! That includes a Weather update software also.. It's really very good..
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Clouds are formed by water vapor. And high pressure can hold more water vapor. So when vapor moves into a low pressure system it condenses and and forms clouds and those clouds precipitate when the system cant hold no more water vapor
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Definitely Fall.\n\nHere in Minnesota we have great seasons (as do other states).\n\nSince we moved here, I have always raked the leaves in Fall into a huge pile... and plopped into them! :)
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They end up becoming the 'seeds' of clouds.  That is, water in the air condenses around them, & once the process starts, those condensation  trails sometimes form into clouds up to 500 miles long.\n\nI read about it in, I believe, Popular Science a couple years ago.  There was also a fascinating article about a study that took place during the 3 days in 9/01 when all planes in the U.S. were grounded:  due apparently to the reduced cloud cover, temps everywhere were a couple degrees higher those days!
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It measures the density of cumulative clouds. Good Luck !  :)
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A cloud is a visible mass of condensed droplets or frozen crystals suspended in the atmosphere above the surface of the Earth or another planetary body. The branch of meteorology in which clouds are studied is nephology.\n\nOn Earth, the condensing substance is water vapor, which forms small droplets of water or ice crystals, typically 0.01 mm in diameter. When surrounded with billions of other droplets or crystals, they are visible as clouds. Dense deep clouds exhibit a high reflectance (70% to 95%) throughout the visible range of wavelengths: they thus appear white, at least from the top. Cloud droplets tend to scatter light very efficiently, so that the intensity of the solar radiation decreases with depth into the cloud, hence the grey or even sometimes dark appearance of the clouds at their base. Thin clouds may appear to have acquired the color of their environment or background, and clouds illuminated by non-white light, such as during sunrise or sunset, may be colored accordingly. In the near-infrared range, however, clouds would appear very dark because the water that constitutes the cloud droplets strongly absorbs solar radiation at these wavelengths.\n\nCloud formation and properties\nClouds form when the invisible water vapor in the air condenses into visible water droplets or ice crystals. This can happen in three ways:\n\n1. The air is cooled below its saturation point. This happens when the air comes in contact with a cold surface or a surface that is cooling by radiation, or the air is cooled by adiabatic expansion (rising). This can happen:\n* along warm and cold fronts (frontal lift)\n* where air flows up the side of a mountain and cools as it rises higher into the atmosphere (orographic lift)\n* by the convection caused by the warming of a surface by insolation (diurnal heating)\n* when warm air blows over a colder surface such as a cool body of water.\n\n2. Clouds can be formed when two air masses below saturation point mix. Examples are breath on a cold day, aircraft contrails and Arctic sea smoke.\n\n3. The air stays the same temperature but absorbs more water vapor into it until it reaches saturation point.\n\nThe water in a typical cloud can have a mass of up to several million tonnes. However, the volume of a cloud is correspondingly high, and the net density of the relatively warm air holding the droplets is low enough that air currents below and within the cloud are capable of keeping it suspended. As well, conditions inside a cloud are not static: water droplets are constantly forming and re-evaporating. A typical cloud droplet has a radius on the order of 1 x 10-5 m and a terminal velocity of about 1-2 cm/s. This gives these droplets plenty of time to re-evaporate as they fall into the warmer air beneath the cloud.\nCumulonimbus cloud\nEnlarge\nCumulonimbus cloud\n\nMost water droplets are formed when water vapor condenses around a condensation nucleus, a tiny particle of smoke, dust, ash, or salt. In supersaturated conditions, water droplets may act as condensation nuclei.\n\nWater droplets large enough to fall to the ground are produced in two ways. The most important means is through the Bergeron Process, theorized by Tor Bergeron, in which supercooled water droplets and ice crystals in a cloud interact to produce the rapid growth of ice crystals; these crystals precipitate from the cloud and melt as they fall. This process typically takes place in clouds with tops cooler than -15°C. The second most important process is the collision and wake capture process, occurring in clouds with warmer tops, in which the collision of rising and falling water droplets produces larger and larger droplets, which are eventually heavy enough to overcome air currents in the cloud and the updraft beneath it and fall as rain. As a droplet falls through the smaller droplets which surround it, it produces a "wake" which draws some of the smaller droplets into collisions, perpetuating the process. This meth
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The shape is completely random, based on how air currents (wind and updrafts) are moving around and inside the cloud. You get so many cloud shapes over time that a few random patterns are bound to resemble something else we're familiar with, such as a heart or a dog.
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the sun was behind the clouds, therefore there was a shadow.
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CIRRUS CLOUDS \n– high-level, wispy clouds. The name originates from the Latin word meaning "curl of hair". These feathery clouds form very high up in the sky (at altitudes between 5 km and 14 km) where it is very cold.They are thin clouds.   And look like horse tails They are therefore made up of tiny ice crystals rather than water droplets. Cirrus clouds occur in warm air which is being slowly lifted over a large area by an approaching cold front, and they are therefore often the signal of bad weather. ............................................................................................ \n \n\n                                              STRATUS CLOUDS\n– low-level blankets of cloud. The name "stratus" means "layers" in Latin, although you in fact rarely see the layers in stratus clouds. Instead they appear as a grey, shapeless sheet of cloud extending in all directions across the sky. They are usually only about 1 km thick, but can be as much as 1000 km wide. Stratus clouds build up when a layer of warm, moist air rises slowly over a mass of colder air. These clouds are often dark and gloomy, and are associated with rain and drizzle. Stratus clouds can sometimes rest on the ground or sea instead of up in the air, and they are then called ‘fog’.
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November (in the Northern hemisphere)
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you're talking about the aurora borealis (sp) otherwise known as Northern Lights. The farther north you are, the more likely you'll see them. Canada and even northern US can sometimes. You can probably look it up at http://en.wikipedia.org
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BECAUSE THOSE AREAS MIGHT HAVE HIGH HILLS WHERE THE CLOUDS HIT HARD AND RAIN .MIGHT BE THE LOW AREAS AND FINALLY DUE TO CLOSE TO SEAS
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Losing yourself in the skies and clouds are natures gift to us. I've seen objects, faces and "calming" designs. Cloud formations are majestic, serene, power and forces you to daydream and go to places only in your heart and mind. Clouds bring out the best in ones mind and with its changing of texture and color warn us of danger. A great "present" given to all by Mother nature.Give thanks, enjoy it and protect it.
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For the U.S try\nhttp://www.weather.gov/\n\nFor Canada try\nhttp://www.weatheroffice.ec.gc.ca/
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Oregon Scientific makes a good one:\nhttp://www.ambientweather.com/wmorscwiprwe.html\n\nYou can look at some alternates there too.
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http://www.brainyweather.com/states/state_northdakota.html\n\nClick on any area and any year, and it will tell you. Hope I helped!\n\nps it took like five minutes to find this on google. So you might be able to find more. I did weather history in North Dakota.