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9780816047901

A Change in the Weather

by ;
  • ISBN13:

    9780816047901

  • ISBN10:

    0816047901

  • Format: Hardcover
  • Copyright: 2004-04-01
  • Publisher: Facts on File
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List Price: $40.00

Summary

Examines the history of climate change and its impact on the earth.

Table of Contents

Preface xv
Introduction xvii
HOW THE ATMOSPHERE PRODUCES OUR WEATHER 1(9)
Composition and structure of the atmosphere
1(1)
Mars was not always a cold desert
1(1)
Atmospheres of Earth, Venus, and Mars
2(1)
How Earth acquired Its three atmospheres
2(1)
How oxygen accumulated
3(1)
Layers of the atmosphere
4(3)
Troposphere and tropopause
7(1)
Stratosphere and stratopause
7(1)
Mesosphere and mesopause
8(1)
Thermosphere, exosphere, and ionosphere
8(2)
GENERAL CIRCULATION OF THE ATMOSPHERE 10(8)
Seasons and Tropics
11(1)
Why Earth is not like the Moon
12(1)
Trade winds and Hadley cells
13(2)
George Hadley and Hadley cells
14(1)
Polar and Ferrel cells
15(3)
The Coriolis effect
16(2)
TRANSPORT OF HEAT BY THE OCEANS 18(10)
Ocean currents
18(2)
El Niño
19(1)
Thermohaline circulation and North Atlantic Deep Water
20(3)
The Great Conveyor
23(1)
Ocean gyres and boundary currents
24(4)
Why the Arctic is warmer than the Antarctic
25(3)
EVAPORATION AND CONDENSATION AND HOW THEY PRODUCE OUR WEATHER 28(9)
The water molecule and the hydrogen bond
29(1)
Breaking the bond: evaporation
30(1)
Specific heat capacity
30(2)
Latent heat and adiabatic cooling and warming
32(3)
Latent heat and dew point
32(2)
Adiabatic cooling and warming
34(1)
Potential temperature
35(2)
Potential temperature
35(2)
CLIMATES OF THE PAST 37(7)
Revealing the past
37(1)
Tree rings
37(1)
Radiocarbon dating
38(1)
Pollen and beetles
39(1)
Seabed sediment
40(1)
Ice cores
40(2)
Vostok, GISP, and GRIP
41(1)
Oxygen isotopes and "heavy" water
42(1)
Carbonate from the seabed
43(1)
CLIMATE CHANGES THAT HAVE CHANGED HISTORY 44(8)
Radiometric dating
44(1)
Reading stalagmites
45(1)
The Anasazi
45(1)
The domestication of animals and plants
46(2)
Indus Valley civilization.
48(1)
Out of the steppes of Central Asia
49(1)
The Mongol Empire
50(1)
Khmer Empire
51(1)
MILUTIN MILANKOVITCH AND HIS ASTRONOMICAL CYCLES 52(9)
Eccentricity
52(2)
Obliquity
54(1)
The axial wobble
55(1)
Hipparchus and the precession of the equinoxes
55(2)
The significance of precession
57(1)
When the cycles coincide
57(2)
The Milankovitch cycles
59(1)
Adhemar and Croll
59(1)
Milankovitch on Mars
60(1)
ICE AGES OF THE PAST-AND FUTURE? 61(9)
Louis Agassiz and the Great Ice Age
61(2)
Louis Agassiz and the Great Ice Age
62(1)
Glacials, interglacials, and geologic time
63(4)
How glaciers begin and move
67(1)
Snowball Earth
67(2)
Will there be more ice ages?
69(1)
EDWARD WALTER MAUNDER AND THE UNRELIABLE SUN 70(9)
The 11-year sunspot cycle
70(2)
Sunspots
71(1)
The Spörer Minimum, Dalton Minimum, and Maunder Minimum
72(1)
Tree rings and isotopes
73(2)
The inconstant Sun
75(1)
Sunspots and cloud formation
76(1)
The link persists
77(2)
THE MEDIEVAL OPTIMUM 79(8)
Cold weather during the Dark Ages
80(1)
Norse colonies and explorations
80(2)
Erik the Red and settlements in Greenland
82(1)
Warm weather everywhere
82(2)
Sea levels and higher rainfall
84(1)
Start of the deterioration
84(3)
THE LITTLE ICE AGE 87(7)
Increasingly severe storms
87(1)
Wet summers, poor harvests, and famines
88(1)
Diseases favored by wet weather
88(1)
Agriculture retreating from marginal land
89(1)
Glaciers begin advancing
90(1)
Cold winters in the lowlands
91(1)
Frost fairs
91(1)
Distribution of pressure
92(1)
Slow recovery and the origin of the "traditional" Christmas scene
93(1)
GREENHOUSE GASES AND THE GREENHOUSE EFFECT 94(11)
Effective temperature
94(2)
Radiation emission and absorption
96(2)
Jean-Baptiste Fourier, John Tyndall, and the greenhouse effect
98(1)
Svante Arrhenius
99(1)
The faint Sun paradox and the Gaia hypothesis
99(4)
Svante Arrhenius
100(1)
Snowball Earth and Greenhouse Earth
101(1)
The Gaia hypothesis
102(1)
The enhanced greenhouse effect and global warming potentials
103(2)
THE CARBON CYCLE 105(8)
Respiration
105(3)
Photosynthesis
106(2)
The carbon reservoirs
108(1)
The cycle-sources and sinks
109(1)
Carbonate lysocline and carbonate compensation depth
110(1)
Perturbing the natural cycle
111(1)
Carbon dioxide fertilization and the missing carbon sink
112(1)
HOW BRIGHT IS THE EARTH? 113(8)
Albedo
113(4)
Albedo and temperature
117(1)
Positive feedback
118(1)
Ice-albedo feedback and climate warming
119(1)
Changing land use alters the albedo
120(1)
CLOUDS AND PARTICLES 121(7)
Some clouds are more reflective than others
121(2)
Reflection and absorption
123(1)
Cloud condensation nuclei
124(1)
John Aitken and cloud condensation nuclei
125(1)
Atmospheric aerosols
125(1)
Effect on radiation
126(1)
Aerosols and clouds
126(2)
RADIATION FROM THE SUN AND FROM THE EARTH 128(7)
Electromagnetic radiation
128(2)
Blackbody radiation
129(1)
The spectrum and the rainbow
130(2)
The complete electromagnetic spectrum
132(1)
Solar wind, cosmic rays, and radioactive decay
132(3)
The solar spectrum
133(2)
THE RADIATION BALANCE 135(8)
Latent heat and the Bowen ratio
136(1)
Diurnal and seasonal changes
137(1)
Incoming radiation and the ozone layer
138(2)
Why the sky is blue
140(1)
Outgoing radiation
140(3)
MEASURING CLIMATE CHANGE 143(8)
Siting the thermometer
143(1)
Need to standardize instruments
and the way they are used
144(2)
The Central England temperature record
146(1)
Measuring very small changes
147(2)
Central England temperature record
147(2)
Surface stations
149(1)
Weather balloons and satellites
149(1)
Is the world growing warmer?
150(1)
URBAN HEAT ISLANDS 151(7)
City air Is drier, but rainfall Is higher
151(1)
Humidity
152(1)
Cities are less sunny
152(2)
Cities are less windy, except along urban canyons
154(1)
Heat islands and urban domes
155(1)
Heat islands and global warming
156(2)
IS THE SEA RISING? 158(6)
The expansion and contraction of ice sheets
158(1)
Isostasy and glacial rebound
159(1)
Thermal expansion and storage
160(1)
Records of sea level
160(1)
Will the sea rise in years to come?
161(3)
Isle of the Dead
161(3)
GLOBAL WARMING 164(5)
The Intergovernmental Panel on Climate Change
164(1)
The Third Assessment Report
165(1)
Criticisms
166(2)
Doubts about economic growth
168(1)
MODELING THE ATMOSPHERE 169(6)
Constructing models
169(2)
The gas laws
170(1)
The development of climate models
171(2)
Lapse rates and stability
171(2)
Models have limitations
173(1)
Other approaches to modeling
174(1)
IS CLIMATE CHANGE ALL BAD? 175(6)
Evaporation and effective precipitation
175(1)
Effects on agriculture
176(1)
Effects on wildlife
176(1)
Most warming in high latitudes
177(1)
Exotic diseases
178(1)
Sea levels and storms
179(2)
CAN WE PREVENT CLIMATE CHANGE OR MUST WE ACCEPT AND ADAPT TO IT? 181(4)
The precautionary principle
181(1)
Reducing emissions
182(2)
The UN Framework Convention on Climate Change and the Kyoto Protocol
183(1)
Is Kyoto achievable?
184(1)
Appendixes
SI units and conversions
185(1)
Prefixes used with SI units
186(1)
Bibliography and further reading 187(4)
Index 191

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Excerpts

At present, climate change is a controversial topic. A Change in the Weather, a new volume in the Dangerous Weather set, looks at climate change and its consequences with a fair, critical eye. It examines the major controversies and locates them in the broader context of the climatic changes that have taken place in the past. Beginning with a definition of climate change, this volume provides a general account of the way the atmosphere and oceans work to produce climates, along with an outline of the astronomical and other influences that affect climatic changes. It then describes different types of climates that have prevailed in the past and explains the way past climates are studied. An important topic covered is the greenhouse effect and the history of this idea, which leads into an overview of the present concern over global warming induced by an enhanced greenhouse effect.
For middle school and high school students, teachers, and general readers, A Change in the Weather is filled with interesting facts on climate and climate change, providing a current and comprehensive survey of the issues surrounding this important topic.
Special features provide a comparison between the atmospheres of Earth, Venus, and Mars; information on George Hadley and Hadley cells; discussion of why the Arctic is warmer than the Antarctic; a look at adiabatic cooling and warming and latent heat; coverage of the Vostok, GRIP, and GISP projects; and an overview of the United Nations Framework Convention on Climate Change and the Kyoto Protocol.

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