Historical Perspectives on Climate ChangeOxford University Press, 10 sept 1998 - 208 páginas This intriguing volume provides a thorough examination of the historical roots of global climate change as a field of inquiry, from the Enlightenment to the late twentieth century. Based on primary and archival sources, the book is filled with interesting perspectives on what people have understood, experienced, and feared about the climate and its changes in the past. Chapters explore climate and culture in Enlightenment thought; climate debates in early America; the development of international networks of observation; the scientific transformation of climate discourse; and early contributions to understanding terrestrial temperature changes, infrared radiation, and the carbon dioxide theory of climate. But perhaps most important, this book shows what a study of the past has to offer the interdisciplinary investigation of current environmental problems. |
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Página 6
... meteorological observers , and the development of statistical analysis , a picture ( albeit abstract and imperfect ) ... observations , extended into the in- definite past by paleoclimatic techniques , and , finally , globalized in the era ...
... meteorological observers , and the development of statistical analysis , a picture ( albeit abstract and imperfect ) ... observations , extended into the in- definite past by paleoclimatic techniques , and , finally , globalized in the era ...
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... observations over large expanses of the country . Chapter 3 deals with the growth of observing systems and the de ... meteorological observing systems contributed to a radical transformation of climate discourse and the emergence of a ...
... observations over large expanses of the country . Chapter 3 deals with the growth of observing systems and the de ... meteorological observing systems contributed to a radical transformation of climate discourse and the emergence of a ...
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Índice
3 | |
1 Climate and Culture in Enlightenment Thought | 11 |
2 The Great Climate Debate in Colonial and Early America | 21 |
The Expansion of Observing Systems | 33 |
4 Climate Discourse Transformed | 45 |
5 Joseph Fouriers Theory of Terrestrial Temperatures | 55 |
6 John Tyndall Svante Arrhenius and Early Research on Carbon Dioxide and Climate | 65 |
7 T C Chamberlin and the Geological Agency of the Atmosphere | 83 |
8 The Climatic Determinism of Ellsworth Huntington | 95 |
9 Global Warming? The Early Twentieth Century | 107 |
Historical Dimensions | 129 |
Notes | 139 |
Bibliography | 167 |
Index | 190 |
Otras ediciones - Ver todo
Términos y frases comunes
Abbé Du Bos absorb absorption Amer American Philosophical Society Archives Arrhenius's atmo carbon cycle carbon dioxide carbonic acid caused century chapter Charles cited civilization climate change climatology CO₂ cold cultivation culture early Earth Ellsworth Huntington environmental essay Europe experiments forests Forry France G. S. Callendar gases geological geologist Geophysical glaciation global change global cooling global warming globe greenhouse effect Herschel History Högbom human Hume Huntington Papers Ibid ice ages increase infrared Institution John Tyndall Joseph Fourier latitudes London Meteorol meteorological observations Meteorological Society Montesquieu National Observatory ocean Panofsky Paris physics published radiant heat radiation radiative rise Roger Revelle Royal Society Science scientific scientists solar Suess surface Svante Arrhenius T. C. Chamberlin terrestrial temperatures theory of climate Thomas Jefferson thought tion Trans Tyndall Collection Tyndall's United University Press variations water vapor weather William winter York
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Página 3 - I have of late— but wherefore I know not— lost all my mirth, forgone all custom of exercises; and indeed it goes so heavily with my disposition that this goodly frame, the earth, seems to me a sterile promontory; this most excellent canopy, the air, look you, this brave o'erhanging firmament, this majestical roof fretted with golden fire, why, it appears no other thing to me than a foul and pestilent congregation of vapours.
Página 46 - evidence of things not seen," in the fulness of Divine grace ; and was profound on this, the greatest concern of human life, while unable even to comprehend how the " inclination of the earth's axis to the plane of its orbit" could be the cause of the change of the seasons.
Página 73 - The aqueous vapour constitutes a local dam, by which the temperature at the earth's surface is deepened : the dam, however, finally overflows, and we give to space all that we receive from the sun. The sun raises the vapours of the equatorial ocean ; they rise, but for a time a vapour screen spreads above and around them.
Página 86 - Branscomb is a member of the National Academy of Sciences, the American Academy of Arts and Sciences, and the American Philosophical Society...
Página 71 - No doubt, therefore, can exist of the extraordinary opacity of this substance to the rays of obscure heat ; and particularly such rays as are emitted by the earth after it has been warmed by the sun. It is perfectly certain that more than ten per cent of the terrestrial radiation from the soil of England is stopped within ten feet of the surface of the soil.
Página 143 - In 1811, he published, in one volume, 8vo., his Observations on the Climate in different Parts of America, compared with the Climate in corresponding Parts of the other Continent...
Página 39 - Jefferson and the Reverend James Madison, president of the College of William and Mary, are credited with making the first simultaneous meteorological measurements in 1778.
Página 51 - There is nothing in these curves to countenance the idea of any permanent change in the climate having taken place or being about to take place ; in the last 90 years of thermometric records, the mean temperatures showing no indication whatever of a sustained rise or fall.
Página 178 - Tables and Results of the Precipitation in Rain and Snow in the United States...
Página 71 - The warmth of our fields and gardens would pour itself unrequited into space, and the sun would rise upon an island held fast in the iron grip of frost. The aqueous vapour constitutes a local dam, by which the temperature at the earth's surface is deepened : the dam, however, finally overflows, and we give to space all that we receive from the sun.