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Contributions to Molecular Physics in the Domain of Radiant Heat

Author: John Tyndall
Publisher:
ISBN:
Category : Heat
Languages : en
Pages : 480

Book Description

Contributions to Molecular Physics in the Domain of Radiant Heat

Author: John Tyndall
Publisher:
ISBN:
Category : Heat
Languages : en
Pages : 508

Book Description
First edition of an important collection of memoirs, from Febr. 1861 on, in the field of Tyndall's major work, the effects of solar and heat radiation on atmospheric gases (1860-1870). He then considered the scattering of light particles in the atmosphere (the Tyndall effect) and explained the blue color of the sky (Rayleigh scattering). The scattering of sunlight by dust particles led him to consider means of destroying airborne organic matter by heat . Tyndall is remembered chiefly for his efforts to verify the high absorptive and radiative power of aqueous vapor; to measure the absorption and transmission of heat by many different gasses and liquids . Practical applications of his work in meteorology, fog signaling, and bacteriology were seen within his lifetime. . (DSB).

Contributions to Molecular Physics in the Domain of Radiant Heat

Author: John Tyndall
Publisher:
ISBN:
Category :
Languages : en
Pages : 502

Book Description

Paleoclimatology

Author: Colin P. Summerhayes
Publisher: John Wiley & Sons
ISBN: 1119591473
Category : Science
Languages : en
Pages : 560

Book Description
Life on our planet depends upon having a climate that changes within narrow limits – not too hot for the oceans to boil away nor too cold for the planet to freeze over. Over the past billion years Earth’s average temperature has stayed close to 14-15°C, oscillating between warm greenhouse states and cold icehouse states. We live with variation, but a variation with limits. Paleoclimatology is the science of understanding and explaining those variations, those limits, and the forces that control them. Without that understanding we will not be able to foresee future change accurately as our population grows. Our impact on the planet is now equal to a geological force, such that many geologists now see us as living in a new geological era – the Anthropocene. Paleoclimatology describes Earth’s passage through the greenhouse and icehouse worlds of the past 800 million years, including the glaciations of Snowball Earth in a world that was then free of land plants. It describes the operation of the Earth’s thermostat, which keeps the planet fit for life, and its control by interactions between greenhouse gases, land plants, chemical weathering, continental motions, volcanic activity, orbital change and solar variability. It explains how we arrived at our current understanding of the climate system, by reviewing the contributions of scientists since the mid-1700s, showing how their ideas were modified as science progressed. And it includes reflections based on the author’s involvement in palaeoclimatic research. The book will transform debate and set the agenda for the next generation of thought about future climate change. It will be an invaluable course reference for undergraduate and postgraduate students in geology, climatology, oceanography and the history of science.