The earth is surrounded by a large envelope of gases called atmosphere. The condition of the atmosphere and the changes it undergoes influence all physical, chemical and biological activities over the earth. The study pertaining to lower...
moreThe earth is surrounded by a large envelope of gases called atmosphere. The condition of the atmosphere and the changes it undergoes influence all physical, chemical and biological activities over the earth. The study pertaining to lower atmosphere and its changes is called atmosphere physics or meteorology. In modern usage, meteorology denotes the science of weather and includes the study of atmospheric phenomena. Definition Meteorology can be defined as the science that deals with the study of the atmosphere. The temperature at the tropopause is of the order of-80˚C over the equator and around-56˚C over the poles. The height as well as temperature of the tropopause varies with the seasons and weather situation, the lowest values occurring during the winter. The tropopause is not a continuous surface. There are breaks separating polar, extra-tropical (middle) and tropical tropopauses, sometimes one overlapping the other. These breaks facilitate the exchange of air between the tropopause and the region above. Inversions and isothermal layers can be seen in the troposphere. Nearly 75 percent of the mass of the atmosphere is in the troposphere. 1.3.2. Stratosphere Above the troposphere is an isothermal layer followed by a region of inversion extending upto nearly 50km. This is termed as the stratosphere. Temperatures increase from around 20km becoming roughly 0˚C by about 50km, which is stratopause. This rise in temperature is due to the absorption of ultraviolet radiation in the ozone layer between, say, 20 and 50km. This region sometimes gets rapidly warmed, mainly in the higher latitudes, at times by as much as 30 to 40˚C in a matter of a few days. This phenomenon is termed explosive warming of the stratosphere. 1.3.3. Mesosphere Above the stratosphere is the mesosphere extending from roughly 50 to 80km. The temperature in this region once again decreases with altitude, lowering to about-95˚C at the mesopause around 80km. 1.3.4. Thermosphere Temperatures rise rapidly above the mesopause, reaching nearly 1000˚C by about 300km. This region is known as the thermosphere. 1.3.5. Exosphere The lighter gases, hydrogen and helium, slowly become free of the earth's gravitational field and escape to space by about 600km. This region has been named as the exosphere, which gradually merges into the interplanetary space. 1.4.Composition of atmosphere 1.4.1.Gases The atmosphere we live in is a mixture of gases composed mainly of nitrogen and oxygen. The proportion of the various gases in the atmosphere by volume is 78 percent nitrogen, 21 percent oxygen and the rest 1 percent made up of small amounts of argon, carbon dioxide, neon, helium, krypton, xenon, hydrogen and traces of ozone, methane, sulphur dioxide, nitrogen oxides etc. The atmospheric gases are held on to the earth by the pull of gravitation. Each constituent has its own role to play in sustaining life on earth. Oxygen is essential for us to live and for combustion to take place. The role of nitrogen is also important. We cannot breathe pure oxygen. Nitrogen slows down the burning process. Carbon dioxide constitutes 0.03 percent and provides food for plants through photosynthesis, which replenishes oxygen. Ozone is found mostly between 20 and 50km with the maximum concentration around 25km amsl. It absorbs the ultraviolet radiation from the sun and thus filters the injurious radiation from harming us. Carbon dioxide and water vapour absorb the infrared radiation emanating from the earth and prevent excessive radiational cooling. The atmosphere acts as a protective cover to the earth by regulating the heat flow. 1.4.2. Water vapour Water vapour is present in varying proportions. This composition remains more or less constant upto a height of 80km. The moisture content in the atmosphere varies depending on the latitude, temperature, wind and atmospheric systems. Water can be present in the vapour, liquid or solid phase, sometimes as much as 4 percent. Water and its change of phase are important in the occurrence of weather phenomena. Water vapour decreases as altitude increases. 1.4.3. Aerosols Atmospheric aerosols are a suspension of fine solid and liquid particles in the atmosphere. These clouds of suspended matter range from dust and smoke to mists, smogs and haze. They are not always the result of pollution from human activities; some enters the atmosphere from volcanic eruptions or dust storms. Some aerosols particles are invisible to the human eyes because they are smaller than the wavelength of light.