PPT-ALL ABOUT OZONE TROPOSPHERE
Author : faustina-dinatale | Published Date : 2018-03-14
A layer of the atmosphere that is closest to the Earths surface Almost all weather occurs here Temperature decreases as altitude increases STRATOSPHERE Layer above
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ALL ABOUT OZONE TROPOSPHERE: Transcript
A layer of the atmosphere that is closest to the Earths surface Almost all weather occurs here Temperature decreases as altitude increases STRATOSPHERE Layer above the troposphere Extends from 1850 km. Lesson Objectives. Describe how the temperature of the atmosphere changes with altitude.. Outline the properties of the troposphere.. Explain the role of the ozone layer in the stratosphere.. Describe conditions in the mesosphere.. The . troposphere. is the lowest layer of Earth's atmosphere. The troposphere starts at Earth's surface and goes up to a height of 7 to 20 km (4 to 12 miles, or 23,000 to 65,000 feet) above sea level. Most of the mass (about 75-80%) of the atmosphere is in the troposphere. Almost all weather occurs within this layer. Air is warmest at the bottom of the troposphere near ground level. Higher up it gets colder. Air pressure and the density of the air are also less at high altitudes. Nearly all of the water vapor and dust particles in the atmosphere are in the troposphere. That is why most clouds are found in this lowest layer, too. The troposphere is heated from below. The warm air, heated by the sun, tends to rise. That keeps the air in the troposphere "stirred up". The top of the troposphere is quite cold. Air also gets 'thinner' as you go higher up. . the Upper Troposphere - Lower Stratosphere. K. . Wargan, . S. . Pawson. , . M. . Olsen, . J. . Witte, . A. . Douglass. Global Modeling and Assimilation Office (GMAO). Chemistry and Dynamics Branch. NASA GSFC. The most important among these gases are therefore water vapourand carbon dioxide. The basic principles of the water cycle are well known: Evaporation of liquid water at the surface, condensation, clo Acknowledgement. G. . . Ancellet. , O. R. . Cooper, J. . Cuesta, G. . Dufour. , F. . Ebojie. , G. Huang, S. S. . Kulawik. , B. Latter, T. Leblanc, J. Liu, X. Liu, J. . Neu. , H. . Petetin. , I. . Petropavlovskikh. By. : Rolando . and Jeffrey. The troposphere is the closest and smallest layer of the earth`s atmosphere.. It`s the layer that contains all the weather and living beings.. Temperture: 15 degrees celcius to -57 degrees celcius.. 9. Next topic: Photochemistry (. Ch. 3 notes). Can these energies break chemical bonds?. weak O. 2. -O bond in ozone (~ 100 kJ/. mol. ). moderately strong C-H bond in formaldehyde (~368 kJ/. mol. ). Chemistry 380.01 . Fall 2014. Chris . Sturken. Crystal Chen. Ellen Lu. The . Damages . of T. ropospheric . O. zone on Plants . and . its R. oles . in the . Climate Change Loop. Roles:. GW. increases . What is a greenhouse?. Wikipedia | GNU . Greenhouse Effect. Process by which thermal radiation from a planetary surface is absorbed by atmospheric greenhouse gases, and is re-radiated in all directions. 1. AOSC . 637. Tropospheric . Ozone. Ozone is a major pollutant. It does billions of dollars worth of damage to agricultural crops each year and is the principal culprit in photochemical smog. Ozone, however, exists throughout the troposphere and, as a major OH source and a greenhouse gas, plays a central role in many biogeochemical cycles. That photochemical processes produce and destroy . GLY 4241 - Lecture 6 . Fall, . 2016. 2. Earth. Even in a high resolution image from space, the atmosphere is not visible. 3. Radiation. NASA graphic. 4. Chinese Smog. Haze over China. Increased desertification has added dust to China’s atmosphere. 2. observations and the role of the upper troposphere. Rachel Silvern. Atmospheric Chemistry Modeling Group, Harvard University. TEMPO Science Team Meeting. June 7, 2018. Previous work showed 60% reduction of . ). Presented By. Dr. . Banashree. . Saikia. Assistant Professor. Department of Geography. JN College,. . Boko. Structure of the Atmosphere . On the basis of the characteristics of temperature and air pressure there are four distinctive layers from the earth surface upward . . of . Atmosphere . Composition of the Atmosphere Permanent . constituents. Gases . that remain essentially constant by . percent: . Nitrogen. , Oxygen, Argon, Neon, Helium, Krypton, Hydrogen Variable constituents .
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