دانلود کتاب Can Physics Save Miami (and Shanghai and Venice, by Lowering the Sea)?

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PRELIMS.pdf
Preface
Author biography
Edward Wolf
CH001.pdf
Chapter 1 The sea-level threat exemplified by Miami and Venice
1.1 Introduction to the Anthropocene
1.2 The recent rise of sea level
The deployable 6 billion dollar sea gates of Venice
1.3 The River Thames flood barrier
1.4 The ‘Big U’ water fence for New York
1.5 Why Miami is more difficult
1.6 Amplification of sea-level threat by tides, storm-surges and the high vapor pressure of warm water
1.7 Quantifying damages and liabilities: fractional attributable risk
References
CH002.pdf
Chapter 2 Carbon burning has ‘engineered’ a new era of high temperature and high sea level
2.1 Radiation balance sets Earth temperature
2.1.1 Stefan–Boltzmann law of radiation from hot matter
2.1.2 Earth temperature
2.2 The greenhouse gas discoveries of Tyndall and Arrhenius
2.2.1 Properties of Earth’s atmosphere
2.2.2 Direct observation of the greenhouse effect
2.3 Carbon dioxide rose during the fossil fuel era from 280 ppm to 410 ppm
2.4 Temperature and sea level rises are accelerating, will there be a tipping point?
References
CH003.pdf
Chapter 3 Instability of Earth climate and sea level
3.1 The ice core record of 420 000 years
3.2 Sea level rise since the last glaciation
3.3 The ‘Hothouse Earth’: an earlier era of high sea level
3.3.1 The euxinic ocean
3.3.2 The role of volcanism
References
CH004.pdf
Chapter 4 What was learned from Mt Pinatubo eruption in 1991
4.1 Sulfur dioxide emission and stratospheric aerosol
4.2 Cooling of the Earth by the Mt Pinatubo eruption
4.3 Lowering sea level from Mt Pinatubo in the altimeter record
4.4 Particulate matter in the contemporary atmosphere
References
CH005.pdf
Chapter 5 Solar engineering to cool the Earth
5.1 Size and type of artificial aerosol: a back-of-the-envelope estimate
5.2 Expected lifetime, cooling, and other aspects
5.3 A more general look at light scattering particles
5.4 Model predictions of climate alterations
5.5 Methods of aerosol insertion
5.6 Cost estimates are low
References
CH006.pdf
Chapter 6 Can sea level be lowered by cooling to save Miami?
6.1 Thermal expansion of sea water
6.2 Sea level predictions based on the volcanic eruptions
6.3 Sea level predictions using geoengineering and climate models
6.4 Saving Miami and Shanghai and Venice by lowering the sea
References
CH007.pdf
7 Some useful constants