Upload
gaston
View
38
Download
0
Embed Size (px)
DESCRIPTION
Section 3 Remote sensing of global change. 3. Greenhouse gasses Global Change Instructor: Dr. Cheng-Chien Liu Department of Earth Sciences National Cheng Kung University Office: Building of Earth Sciences, room 30206 Voice: +886-6-2757575 ext. 65422 E-mail: [email protected] - PowerPoint PPT Presentation
Citation preview
Section 3 Section 3 Remote sensing of global changeRemote sensing of global change
3. Greenhouse gasses3. Greenhouse gasses
Global ChangeInstructor: Dr. Cheng-Chien LiuDepartment of Earth SciencesNational Cheng Kung UniversityOffice: Building of Earth Sciences, room 30206Voice: +886-6-2757575 ext. 65422E-mail: [email protected] Office hours: Monday 14:00 – 17:00, Wednesday 9:00 – 12:00URL: http://mail.ncku.edu.tw./~ccliu88/
Last updated: 27 April 2004
4.1 Introduction4.1 Introduction
Definition of greenhouse gassesDefinition of greenhouse gasses• The gasses that prevent heat energy given off
by the sun from leaving our atmosphere back into space
Greenhouse effectGreenhouse effect• See §4.2
4.1 Introduction (cont.)4.1 Introduction (cont.)
A list of greenhouse gassesA list of greenhouse gasses• Carbon dioxide CO2
• Methane CH4
• Chlorofluorocarbon CFC• Ozone O3
• Water vapor H2O• Nitrous oxide N2O• Soot • …
4.2 Mechanism of Greenhouse effect 4.2 Mechanism of Greenhouse effect
Black body radiationBlack body radiation Selective absorption of energy by Selective absorption of energy by
greenhouse gassesgreenhouse gasses• Long wavelength radiation preferred• Daytime absorption (long : short = 89:50)• Nighttime release long radiation
ConsequencesConsequences• Make the Earth warmer• Reduce the diurnal variation of temperature
Fig. 4.2.1 The electromagnetic spectrum after and before penetrating the atmosphere. Source: http://www.ccrs.nrcan.gc.ca/ccrs/learn/tutorials/fundam/chapter1/chapter1_4_e.html
Fig. 4.2.1Fig. 4.2.1
4.3 Emission of Greenhouse Gases4.3 Emission of Greenhouse Gases
Slowdown Slowdown • International cooperation
CFC use (Phase-out) (Montreal Protocol )Slower growth of CH4
A steady rate of CO2 emissions
Significance of CHSignificance of CH44
• The warming effect CH4:CO2 = 1:2 • CH4 tropospheric O3
Tropospheric O3 is a principal ingredient in "smog," which is harmful to human health and reduces agricultural productivity
4.3 Emission of Greenhouse Gases 4.3 Emission of Greenhouse Gases (cont.)(cont.)
A cheaper and faster way A cheaper and faster way reduce CH reduce CH44Reduction of CH4 emissions and soot could yield a major near term
success story in the battle against global warming, thus providing time to work on technologies to reduce future CO2 emissions.
• A short video about CH4 and climate change http://svs.gsfc.nasa.gov/stories/greenhouse_20020103/MethPackage_QTbigprogress.mov
Long-term goal Long-term goal reduce CO2reduce CO2• Limiting CO2 will still be needed to slow global
warming over the next 50 years. If the same fossil fuel consumption rate with CH4 and pollution halted
for the next 50 years 0.70C If “business-as-usual” 1.40C the specter of imminent disaster
Fig. 4.3.1Fig. 4.3.1
Fig. 4.3.1 changes in 12 climate "forcings" or factors that have contributed to climate change since 1850Source: http://svs.gsfc.nasa.gov/stories/greenhouse_20020103/figure1m.gif
Fig. 4.3.2Fig. 4.3.2
Fig. 4.2.2 Growth rate of climate forcings by greenhouse gasesSource: http://svs.gsfc.nasa.gov/stories/greenhouse_20020103/figure2m.gif
4.4 Questions4.4 Questions
Ozone is one of the greenhouse gases. Ozone is one of the greenhouse gases. Does the depletion of ozone cause the Does the depletion of ozone cause the global warming directly? global warming directly?