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The Thermosphere
The warmest layer of the atmosphere is the Thermosphere
Outside the atmosphere the telescope has no interference, precisely by the atmosphere. The telescope can get a clearer picture, and see certain wavelengengths that don't reach Earth.Outside the atmosphere the telescope has no interference, precisely by the atmosphere. The telescope can get a clearer picture, and see certain wavelengengths that don't reach Earth.Outside the atmosphere the telescope has no interference, precisely by the atmosphere. The telescope can get a clearer picture, and see certain wavelengengths that don't reach Earth.Outside the atmosphere the telescope has no interference, precisely by the atmosphere. The telescope can get a clearer picture, and see certain wavelengengths that don't reach Earth.
The density of the gases in space is so low that we would not term them "air". As you increase in altitude from Sea Level the density of air gradually decreases right up until you reach space. There is no point where there is a sudden change so that someone can say that air has stopped and space has begun. Quite simply, the upper reaches of the atmosphere have been defined by picking an altitude. Below that altitude is "air"; above it is "space".
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the third layer of the atmosphere would be the mesosphere. this is the layer that burns up the meteorites before they reach earth.
The Thermosphere, which can reach temperatures up to 2,500�° C (4,500�° F).
The Himalayas, which reach 8,000 metres.
The Thermosphere
The SR-71 can reach an altitude of 80,000 feet. This is in the stratosphere portion of the Earth s atmosphere.
comets are found in the meosphere. this layer is quite cold. it can reach temperatures of -125
The lowest area of the atmosphere is the lower troposphere.
You reach the second to the last and that is the (Statosphere)
You don't have to be standing on the ground to reach the maximum altitude of Earth so the answer is "everywhere". The Earth's atmosphere is about 300 miles (480 km) thick, but most of the atmosphere (about 80%) is within 10 miles (16 km) of the surface of the Earth.
The thermosphere is the outer layer of the atmosphere and is literally known as the heat sphere. The temperature can constantly rise in this layer and reach up to 1000 degrees Celsius.
Temperatures decrease with altitude in the troposphere, the lowest layer of the atmosphere, from an average of about 20° C to below -50° C. In the next layer, the stratosphere, temperatures warm only slightly up to the ozone layer at the top of the stratosphere, where they increase rapidly with altitude until becoming about the same as on the earth's surface. Temperatures in the next layer, the mesosphere, cool rapidly with altitude to below -80° C. Temperatures rise rapidly with increases in altitude in the next layer, the thermosphere, but temperatures there can vary widely. Depending on the activity of ionized particles within this region, they reach a high of over 1,200° C in the daytime and become extremely cold at night. The next layer is the exosphere, which cools with altitude to where it ends about 1,000 km above the earth's surface.
The warmest layer of the atmosphere is the Thermosphere