Donald Rapp

Ice Ages and Interglacials (eBook, PDF)

Measurements, Interpretation, and Models

• Format: PDF

Produktbeschreibung

It is not so long ago (a mere 17,000 years - a blink in geologic time) that vast areas of the Northern Hemisphere were covered with ice sheets up to two miles thick, lowering the oceans by more than 120 m. By 11,000 years ago, most of the ice was gone.

Evidence from polar ice cores and ocean sediments show that Ice Ages were persistent and recurrent over the past 800,000 years. The data suggests that Ice Ages were the normal state, and were temporarily interrupted by interglacial warm periods about nine times during this period.

Quasi-periodic variations in the Earth cause the solar input to high northern latitudes to vary with time over thousands of years. The widely accepted Milankovitch theory implies that the interglacial warm periods are associated with high solar input to high northern latitudes. However, many periods of high solar input to high northern latitudes occur during Ice Ages while the ice sheets remain.

The data also indicates that Ice Ages will persist regardless of solar input to high northern latitudes, until several conditions are met that are necessary to generate a termination of an Ice Age. An Ice Age will not terminate until it has been maturing for many tens of thousands of years leading to a reduction of the atmospheric CO2 concentration to less than 200 ppm. At that point, CO2 starvation coupled with lower temperatures will cause desertification of marginal regions, leading to the generation of large quantities of dust. High winds transfer this dust to the ice sheets greatly increasing their solar absorptivity, and at the next up-lobe in the solar input to high northern latitudes, solar power melts the ice sheets over about a 6,000-year interval.

A warm interglacial period follows, during which dust levels drop remarkably. Slowly but surely, ice begins accumulating again at high northern latitudes and an incipient new Ice Age begins.

This third edition presents data and models to support this theory.

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Produktdetails

• Verlag: Springer Nature Switzerland
• Seitenzahl: 346
• Erscheinungstermin: 13. April 2019
• Englisch
• ISBN-13: 9783030104665
• Artikelnr.: 56821531

Autorenporträt

Donald Rapp has had a long and varied science and engineering career with since receiving his Ph.D. from the University of California in January 1960. He was a professor for 14 years, and achieved the rank of full professor at the age of 40. Over the years, he has developed a unique talent to move into a field, research it thoroughly, and write an incisive, perceptive summary of that field. His capabilities are widely sought for writing summary technical reports and technical proposals.

He has published numerous scientific papers and eight textbooks: Quantum Mechanics, Statistical Mechanics, Solar Energy, Financial Bubbles, Human Missions to Mars, Use of Extraterrestrial Materials in Human Missions to Mars and the Moon, The Climate Debate, and Assessing Climate Change.

His eight books are summarized at:

http://home.earthlink.net/~drdrapp

Inhaltsangabe

Preface.- 1. Life and climate in an ice age.- 2. Variability of the Earth's climate.- 3. Ice core methodology.- 4. Ice core data.- 5. Ocean sediment data.- 6. Other data sources.- 7. Summary of climate variations.- 8. Overview of the various models for ice ages.- 9. Variability of the Earth's orbit: astronomical theory.- 10. Comparison of astronomical theory with data.- 11. Future prospects.- 12. Abbreviations.- 13. References.

Rezensionen

From the reviews: "In an extensive, detailed review of research, Rapp evaluates theories, models, data and their sources, methodologies, and assumptions relative to the prevailing astronomical theory. ... His concerns ... remind readers that the scientific method and neutral, objective analyses must not be abandoned in the search for understanding how the Earth's climate is changing. Summing Up: Recommended. Upper-division undergraduate through professional collections." (L. S. Zipp, Choice, Vol. 47 (4), December, 2009)