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Policy Implications of Greenhouse Warming: Mitigation, Adaptation, and the Science Base (1992)
Committee on Science, Engineering, and Public Policy (COSEPUP)

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National Research Council. "A Questions and Answers About Greenhouse Warming." Policy Implications of Greenhouse Warming: Mitigation, Adaptation, and the Science Base. Washington, DC: The National Academies Press, 1992. 1. Print.

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Highly uncertain:

Local details of climate change

 

Regional distribution of precipitation

 

Regional vegetation changes

 

Increase in tropical storm intensity or frequency

20. What about storms and other extreme weather events?

The factors governing tropical storms are different from those governing mid-latitude storms and need to be considered separately.

One of the conditions for formation of typhoons or hurricanes today is a sea surface temperature of 26°C (79°F) or greater. With higher global average surface temperature, the area of sea with this temperature should be larger. Thus the number of hurricanes could increase. However, air pressure, humidity, and a number of other conditions also govern the creation and propagation of tropical cyclones. The critical temperature for their creation may increase as climate changes these other factors. There is no consistent indication whether tropical storms will increase in number or intensity as climate changes. Nor is there any evidence of change over the past several decades.

Mid-latitude storms are driven by equator-to-pole temperature contrast. In a warmer world, this contrast will probably weaken since surface temperatures in high latitudes are projected to increase more than at the equator (at least in the northern hemisphere). Higher in the atmosphere, however, the temperature contrast strengthens. Increased atmospheric water vapor could also supply extra energy to storm development. We do not currently know which of these factors would be more important and how mid-latitude storms would change in frequency, intensity, or location.

21. Can projections be improved?

Better computers alone will not solve the problems associated with positive and negative feedbacks. Better understanding of atmospheric physics and chemistry and better mathematical descriptions of relevant mechanisms in the models are also needed, as are data to validate models and their subcomponents. Significant improvements may require decades.

22. Is it possible to avoid the projected warming?

It is possible only at great expense or by incurring risks not now understood, unless the earth is itself self-correcting. Continued increases in atmospheric concentrations of greenhouse gases would probably result in additional global warming. Avoiding all future warming either would be very costly (if we significantly reduce atmospheric concentrations of greenhouse gases) or potentially very risk (if we use climate engineering). However, a comprehensive action program could slow or reduce the onset of greenhouse warming.

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Front Matter (R1-R26)
Part One: Synthesis (1-2)
1 Introduction (3-4)
2 Background (5-11)
3 The Greenhouse Gases and Their Effects (12-28)
4 Policy Framework (29-35)
5 Adaptation (36-47)
6 Mitigation (48-64)
7 International Considerations (65-67)
8 Findings and Conclusions (68-72)
9 Recommendations (73-83)
Individual Statement by a Member Of The Synthesis Panel (84-86)
Part Two: The Science Base (87-88)
10 Introduction (89-90)
11 Emission Rates and Concentrations Of Greenhouse Gases (91-99)
12 Radiative Forcing and Feedback (100-110)
13 Model Performance (111-116)
14 The Climate Record (117-134)
15 Hydrology (135-139)
16 Sea Level (140-144)
17 A Greenhouse Forcing and Temperature Rise Estimation Procedure (145-152)
18 Conclusions (153-154)
Part Three: Mitigation (155-156)
19 Introduction (157-170)
20 Framework for Evaluating Mitigation Options (171-200)
21 Residential and Commercial Energy Management (201-247)
22 Industrial Energy Management (248-285)
23 Transportation Energy Management (286-329)
24 Energy Supply Systems (330-375)
25 Nonenergy Emission Reduction (376-413)
26 Population (414-423)
27 Deforestation (424-432)
28 Geoengineering (433-464)
29 Findings and Recommendations (465-498)
Part Four: Adaptation (499-500)
30 Findings (501-507)
31 Recommendations (508-514)
32 Issues, Assumptions, and Values (515-524)
33 Methods and Tools (525-540)
34 Sesitivities, Impacts, and Adaptations (541-652)
35 Indices (653-656)
36 Final Words (657-658)
Individual Statement by a Member of the Adaptation Panel (659-660)
Appendixes (661-662)
A Questions and Answers About Greenhouse Warming (663-691)
B Thinking About Time in the Context of Global Climate Change (692-707)
C Conservation Supply Curves for Buildings (708-716)
D Conservation Supply Curves for Industrial Energy Use (717-726)
E Conservation Supply Data for Three Transportation Sectors (727-758)
F Transportation System Management (759-766)
G Nuclear Energy (767-774)
H A Solar Hydrogen System (775-778)
I Biomass (779-785)
J Cost-Effectiveness of Electrical Generation Technologies (786-791)
K Cost-Effectiveness of Chlorofluorocarbon Phaseout—United States and Worldwide (792-797)
L Agriculture (798-807)
M Landfill Methane Reduction (808-808)
N Population Growth and Greenhouse Gas Emissions (809-811)
O Deforestation Prevention (812-813)
P Reforestation (814-816)
Q Geoengineering Options (817-835)
R Description of Economic Estimates of the Cost of Reducing Greenhouse Emissions (836-839)
S Glossary (840-846)
T Conversion Tables (847-848)
U Prefaces from the Individual Panel Reports (849-854)
V Acknowledgments from the Individual Panel Reports (855-857)
W Background Information on Panel Members and Professional Staff (858-868)
Index (869-918)
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