Layers of the Atmosphere

Without our atmosphere, at that place would be no life on earth. Two gases stumble up the pile of the earths atmosphere nitrogen (78%), and oxygen (21%). Argon, carbon dioxide and various trace gases make up the remainder. Scientists divided the atmosphere into four seams according to temperature troposphere, stratosphere, mesosphere, and thermosphere. The temperature drops as we go up through the troposphere, entirely it rises as we move through the next social class, the stratosphere. The farther away from earth, the thinner the atmosphere gets. 1. TROPOSPHEREThis is the work of the atmosphere close-hauled to the Earths surface, extending up to roughly 10-15 km above the Earths surface. It contains 75% of the atmospheres mass. The troposphere is wider at the equator than at the poles. Temperature and pressure drops as you go higher up the troposphere. The TropopauseAt the really all overhaul of the troposphere is the tropopause where the temperature reaches a (stable) minimum. Some scientists call the tropopause a thermal layer or frosty jam because this is a point where rising wet vapour can non go higher because it changes into ice and is trapped.If there is no cold trap, Earth would loose all its water Most of what we call brave out occurs in the troposphere. The uneven heating of the regions of the troposphere by the Sun causes convection currents and winds. Warm direct from Earths surface rises and cold air above it rushes in to replace it. When spry air reaches the tropopause, it cannot go higher as the air above it (in the stratosphere) is fastball and lighter preventing much air convection beyond the tropopause. The tropopause acts like an invisible bulwark and is the reason why nearly clouds form and bear phenomena occur at bottom the troposphere.The Greenhouse EffectHeat from the Sun warms the Earths surface but most of it is radiated and sent back into space. Water vapour and carbon dioxide in the troposphere trap some of t his heat, preventing it from escaping thus keep the Earth warm. This trapping of heat is called the greenhouse effect. However, if there is too much carbon dioxide in the troposphere therefore it will trap too much heat. Scientists are afraid that the change magnitude amounts of carbon dioxide would raise the Earths surface temperature, bringing significant changes to worldwide weather patterns hifting in climatic zones and the melting of the polar ice caps, which could raise the train of the worlds oceans. 2. STRATOSPHERE This layer lies directly above the troposphere and is about 35 km deep. It extends from about 15 to 50 km above the Earths surface. The stratosphere is warmer at the top than the bottom. The lower portion has a nearly constant temperature with height but in the upper portion the temperature increases with altitude because of absorption of sunlight by ozone. This temperature increase with altitude is the opposite of the situation in the troposphere.The Ozone L ayerThe stratosphere contains a thin layer of ozone molecules (with three oxygen atoms) which forms a protective layer shielding life on Earth from the Suns denigrating ultraviolet radiation. But this ozone layer is being depleted, and is getting thinner over Europe, Asia, North American and Antarctica. Holes are appearing in the ozone layer. 3. MESOSPHERE Directly above the stratosphere, extending from 50 to 80 km above the Earths surface, the mesosphere is a cold layer where the temperature generally decreases with increasing altitude.Here in the mesosphere, the atmosphere is very rarefied nonetheless thick enough to slow down meteors hurtling into the atmosphere, where they burn up, leaving wild trails in the night sky. 4. THERMOSPHERE The thermosphere extends from 80 km above the Earths surface to outside space. The temperature is hot and may be as high as thousands of degrees as the few molecules that are present in the thermosphere receive extraordinary heavy(a) amounts o f qualification from the Sun.However, the thermosphere would actually feel very cold to us because of the prospect that these few molecules will hit our skin and transfer enough energy to cause appreciable heat is extremely low. The thermosphere corresponds to the heterosphere , a zone where there is no uniform distribution of gases. In other words, the gases are not well-mixed instead they are stratified that is layered, in accordance to their molecular masses. In contrast, the gases in the homosphere (consisting of the troposphere, stratosphere and mesosphere) are uniformly distributed.