PPT-Shortwave and longwave contributions to global warming unde
Author : pamella-moone | Published Date : 2016-08-05
2 Aaron Donohoe University of Washington CLIVAR CONCEPT HEAT Meeting Exeter September 30 2015 Energy imbalance and temperature change ASR OLR Unperturbed Atmospheric
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Shortwave and longwave contributions to global warming unde: Transcript
2 Aaron Donohoe University of Washington CLIVAR CONCEPT HEAT Meeting Exeter September 30 2015 Energy imbalance and temperature change ASR OLR Unperturbed Atmospheric Emission Level. Many people consider that Global Warming is the greatest environmental threat of the 21. st. Century. . However, during the 80s and early 90s scientists argued about the causes and effects of global warming. . Radiative. Transfer of West Atlantic Cumulus. Chang Sun. 1. , . Jiaxi. Wang. 2. , . Shuwan. . Huang. 2. 1. Scripps . Institution . of Oceanography. 2. Department of . Chemistry . and Biochemistry. M. W. Frierson. Department of Atmospheric Sciences. Day 3: 04/06/2010. ATM S 111, Global Warming: Understanding the Forecast. Climate . Forcings. . vs. Climate Feedbacks. Climate . forcings. : . Things that change global temperatures directly. By Matthew and saeb . What is global warming. Carbon dioxide and other air pollution that is collecting in the atmosphere like a thickening blanket, trapping the sun's heat and causing the planet to warm up. Coal-burning power plants are the largest U.S. source of carbon dioxide pollution -- they produce 2.5 billion tons every year. Automobiles, the second largest source, create nearly 1.5 billion tons of CO2 annually. By Amanda Vang and Sydney Billington. What is Global. Warming?. Global warming is a when the earth’s temperature increases and it can change the earth’s climate permanently. Released greenhouse gases, increased amount of carbon dioxide, burning fossil fuels and human activities such as driving and cutting down trees and plants can cause global . Robin Hogan. ECMWF and University of Reading. Contributions from: . Sophia . Schäfer. , Christine . Chiu (University of Reading). Carolin. . Klinger, Bernhard . Mayer (LMU Munich). Susanne . Crewell. Define the Problem. Gather the Evidence. Identify the Causes. Evaluate an Existing Policy. Develop Solutions. Select the Best Solution (Feasibility . vs. Effectiveness. ). PPA Steps. What do you think Global Warming is?. transmitted. absorbed. reflected. 1. transmission. Radiation passes through atmosphere unimpeded.. Shortwave and longwave “windows” . 2. absorption. Energy is transferred to absorber; absorber emits energy. Coover ii 2008 Leslie Charles Coover ALL RIGHTS RESERVED Coover iii EXECUTIVE SUMMARY The greenhouse effect results when certain gasses trap the energy of the sun as it radiates upward from the eart Global warming is a key threat to biodiversity but few researchers have assessed the magnitude2climates calculated changes in habitatnumerous uncertainties in this approach we undertook a sensitivity Global warming is when the earth heats up and the temperature increases. More recently, the temperatures have been rising, causing more dangers for people, animals, plants and our environment.. The Greenhouse Effect. longwave is calculated by combining the output of two longwave sensors. Net shortwave is calculated separately by combining the output of two shortwave sensors. This model includes two shortwave and Qnet. = (. Downwelling. Shortwave + Upwelling Shortwave (albedo)) + (. Downwelling. . Longwave – Upwelling Longwave). Substituting the GEOS-5 expressions for each of these fields gives:. Sfc. . Robert G. Strom, Professor Emeritus. Department of Planetary Sciences and Lunar and Planetary Laboratory. University of . Arizona. Tucson, Arizona. List of Presentations. Part 1 --- Summary of Global Warming.
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