How high in the atmosphere, are the weather satellites located???
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There are two types of satellites: polar and geostationary. Polar satellites circle the earth, covering the north pole and the south pole on every circle, at an altitude of about 850 km. A geostationary satellite "moves with the earth" and is always situated over the same place over the equator, at an altitude of about 36000 km.
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About 87% of Jupiter's atmosphere is molecular hydrogen, about 13% helium.  It is believed that towards the core of the planet temperature and pressure become so extreme the hydrogen first liquefies, then assumes a metallic, earthlike material...or so we 'calculate'.  \n\nRegardless though, with cyclonic storms blowing over 400mph and temperatures of -193F, it would be a flight I'd not be willing to take!
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They have specialist called meteorologist who use special technology that connects to satellites that are orbiting the air and picking up waves from the atmosphere. There are several parts to the atmosphere so the also use special kinds of barometers. To make a long story short it's all in technology.
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Troposphere                ground to 6 miles\nStratosphere                6 miles-50 miles\nIonosphere                50-300 miles\nExosphere                300-600 miles\nSpace Shuttle                150 miles\nOther manned spacecraft        90-300 miles\nEarth-observing satellites500 miles\nNavigational satellites        6,200-13,000 miles\nGeostationary satellites 22,000 miles\nMoon                        238,857 miles
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The Atmosphere is hot(~~)
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Their distance from the Sun
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Check that first letter. I think it is "atmosphere."\n\nCheck this link:\n\nhttp://liftoff.msfc.nasa.gov/academy/space/atmosphere.html
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In the stratosphere, or simply put the sky.
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When you say sky you must mean atmosphere. It divides into:\n\ntroposphere: The troposphere is the lowest layer of the atmosphere starting at the surface going up to between 7 km at the poles and 17 km at the equator with some variation due to weather factors.\n\nstratosphere: from that 7–17 km range to about 50 km, temperature increasing with height. \n\nmesosphere: from about 50 km to the range of 80 km to 85 km, temperature decreasing with height. \n\nthermosphere: from 80–85 km to 640+ km\n\nexosphere: from 640 to 900 km - space.\n\nSo you can say the sky is am least 640 and at most 900 high.
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Are you for real? Do you really think the clouds can be on the other side of the sun? The sun is 93 million miles away. Our atmosphere ends, for all practical purposes 150 or so miles up. After that is outer space. Clouds do not exist outside of the atmosphere. \nNow just maybe this is a trick question and you are meaning nebular clouds or clouds around other planets. If so then yes there are always clouds on the other side of the sun.
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check out this site\n\nhttp://www.space.com/spacewatch/061103_night_sky.html
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Approximately 600 kilometers (372 miles)above the surface of the Earth
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NO!\n\nIN THE HEAVENS: ABOVE OUR HEADS....\nIN SPACE......\n\nOUTSIDE OF THE EARTH'S ATMOSPHERE\n\nAMONGST THE PLANETS\n\n THERE IS ABSOLUTE ORDER\n\nHERE ON EARTH.....\nJUST PICK UP THE LOCAL PAPER....WATCH THE LOCAL NEWS CHANNELS.....
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climate or atmosphere
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The Atmosphere\n\nHow is the atmosphere structured?\nThe atmosphere consists of four distinct layers, which are seperated by a boundaries that end in the suffix "pause". There is a lot of information in the Earth Science Reference Tables page 14. \nTroposphere-This layer of the atmosphere is closest to the earth and 99% of all weather takes place here because most of the water vapor is located here. \nStratosphere-This layer is above the troposphere and contains ozone, which is an important gas, because it absorbs cancer-causing ultra violet rays from the Sun. \nMesosphere-This layer is above the stratosphere. \nThermosphere-This is the uppermost layer of the atmosphere. \nEarth Science Reference Table page 14: \nHow do we describe the present condition of the atmosphere?\nThe present condition of the atmosphere is called WEATHER and it is described using observations of temperature, air pressure, humidity, wind, cloudiness and precipitation. \nWhat is temperature?\nTemperature is a measure of the average kinetic energy of the particles of a substance. In other words, the more molecules vibrate within a substance, the higher the temperature. \nMeasurement - There are three scales that measure temperature: CELSIUS, FAHRENHEIT AND KELVIN scales. There is a conversion scale on page 13 of your ESRT. \nMaps - Meteorologists find it useful to map temperatures and they use lines to connect equal temperatures called Isotherms. \nWhat is air pressure and how is it used to predict the weather?\nAir Pressure - Air pressure is also called barometric or atmospheric pressure. By definition, it is the weight of the atmosphere pushing down on the earth. \nBarometer - A barometer is the instrument that measures air pressure and it uses units of millibars (mb) or inches of mercury (inches). \nFactors that affect air pressure:\nTemperature - As the temperature of the air increases, the air pressure decreases, which is an indirect relationship. \nHumidity - As the humidity of the air increases, the air pressure decreases, which is an indirect relationship.\nYou might ask "WHY?": Humid air is lighter than dry air. When water vapor enters dry air, it does not squeeze in between the molecules of air. Instead, the water vapor pushes out many of the air's heaviest molecules like Nitrogen and Oxygen. In other words, lighter molecules of water vapor replace heavier molecules and the result is the air weighs less and therefore has less air pressure. \n\nHigh air pressure - means that the atmosphere is heavy at that location and from our notes above, you can conclude that the air is probably cool and dry (if you are not sure, see notes above). So, if the barometer indicates high pressure or rising air pressure, you can conclude that the weather will be cool and dry. \nLow air pressure - means that the atmosphere is not heavy at that location and from our notes above, you can conclude that the air is probably warm and humid (if you are not sure, see notes above). So, if the barometer indicates low pressure or falling air pressure, you can conclude that the weather will be warmer and humid. \nMaps - Meteorologists find it useful to map air pressure and they use lines to connect equal equal air pressures called Isobars
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Look at the website   http://www.heavens-above.com/  \n\nPlug in your location info (bookmark it) and you'll get all the local astronomical information you need.
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Towards the equator, where it doesn't rain too much!  Just kidding.  What exactly do you want to know?