
The Evolution of Earth's Climate
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Climate change is one of the most controversial and argued issues in the world today, and it has been for years. It has been politicized by politicians on all sides, some scientists have used the study of it for their own material gain above true scientific discovery, and some scientific theories surrounding it have been believed even though proven false. But there is not, by any means, complete agreement among all scientists throughout the world on this issue.
Written by two of the world's most well-respected environmental and petroleum engineers, this book is meant to be one voice in the scientific literature on this important subject. Other books, also available from Wiley-Scrivener, take the opposite stance, but it is important, in our scientific journey, to listen to all voices and rely on facts, rather than opinions. We trust the reader to make his or her decisions based on all of the facts, and not just some of them.
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John O. Robertson, PhD, is the owner of Earth Engineering, Inc. and an adjunct professor at ITT Tech in National City, CA. He has over 50 years of experience in petroleum and environmental engineering and geology and is the author of over 12 textbooks and 75 articles.
George V. Chilingar, PhD, is an Emeritus Professor of Engineering at the University of Southern California in Los Angeles, CA. He is one of the most well-known petroleum geologists in the world and the founder of several prestigious journals in the oil and gas industry. He has published over 70 books and 500 articles and has received over 100 awards over his career.
Oleg G. Sorokhtin is recognized for his work in geophysics, geology and ecology at the institute of Oceanology of the Russian Academy of Sciences. He passed away in 2010.
Nikolai Sorokhtin is a geologist and academician of the Russian Academy of Natural Sciences and has participated in over 20 major geological expeditions and author of more than 100 scientific publications, including six monographs.
Wennan Long is a reservoir engineer specialist in Synergy Oil and Gas, LLC in Long Beach, California and an active member of the Russian Academy of Nature Sciences He has published many engineering articles in the areas of climate change and environmental science.
Content
Introduction xv
Acknowledgments xix
Part I: Climatic Paradox 1
1 Climatic Paradox 3
Historic Temperatures of Early Earth 3
Concepts by Some of Global Warming 5
Earth's Historic Temperature Charts 6
Misuse of Temperature Charts 7
Use of Paleoclimatology to Estimate Prehistoric Temperatures 8
Use of the Oxygen Isotope Ratio to Estimate Historic Temperatures 9
Historic Temperature Charts for the Past 4.6 BY 10
Glacial Periods and Interglacial Periods (4.5 to 0.540 BY AGO) 10
Historic Temperature Record of the Past 540 MY 11
Today's Temperature Charts 16
The Sun-a Primary Source of Energy 17
Physical Aspects of the Sun 18
Sunspots 18
Solar Irradiation Reaching the Earth 20
The Sun's Energy 23
Energy Received by the Earth from the Sun 26
The Paradox Reviewed 27
2 Adiabatic Theory 29
Troposphere 29
How is Heat Transferred in the Troposphere? 31
Modeling the Earth's Troposphere 33
Features of the Earth's Atmosphere 33
Development of an Adiabatic Equation 35
Development of the Adiabatic Equation 37
Earth's Troposphere Model 41
Effect of Precession Angle 42
Application of Adiabatic Equation to the Planet Venus 47
3 The Earth's Synoptic Activities 51
Greenhouse Effect Adiabatic Theory 51
Model of Heat Transfer in the Troposphere 52
Part II: Development of the Hydrosphere 59
4 Development of Earth's Hydrosphere 61
Hydrosphere of the Primordial Earth 61
Formation of the Hydrosphere 66
Part III: Development of the Earth's Atmosphere 79
5 Earth's Historic Atmospheres 81
Earth's Primordial Atmosphere 81
Earth's First Atmosphere (Hadean time-4.56 to 4.0 BY ago) 83
Earth's Second Atmosphere (Archean time, 4.0 to 2.5 BY ago) 85
Earth's Third Atmosphere (Proterozoic to mid-Phanerozoic time - 2.5 to 0.54 BY ago) 86
Today's Atmosphere (Phanerozoic time, 0.542 BY ago to today) 89
The Earth's Future Atmosphere 89
6 Nitrogen in Earth's Atmosphere 91
Origin of Earth's Atmospheric Nitrogen 91
Estimate of the Earth's Volume of Organic-Nitrogen Sediments 95
7 Development of Free Oxygen in Earth's Atmosphere 99
Oxygen 99
History of Free Oxygen in Earth's Atmosphere 100
8 Development of Methane in Earth's Atmosphere 111
Methane the Gas 111
Historic Levels of Methane in the Earth's Atmosphere 114
Monitoring of Methane Gas Emissions 126
9 The Effect of the Greenhouse Gases 129
The Greenhouse Gases 129
The Classic Greenhouse Effect 130
The Greenhouse Gases 131
Understanding the Greenhouse Effect 134
The Greenhouse Effect 135
Effect of the Precession Angle 138
Convective Heat Transsphere in Troposphere 140
Effect of Water Vapor on Heat Transfer 140
Effect of Carbon Dioxide on Temperature Distribution 141
The Effect of Carbon Dioxide Anthropogenic Emissions 143
10 Development of Carbon Dioxide in Earth's Atmosphere 147
Carbon Dioxide 147
Sources of Carbon Dioxide 148
The Carbon Cycle 148
Mass of Carbon in the Earth's Crust 151
Mass of Carbon in the Earth's Mantle 151
Historic Content of Carbon Dioxide in the Earth's Atmosphere 155
Earth's Hadean Atmosphere (4.56 to 4.0 BY ago) 155
Earth's Archaean Atmosphere (4.0 to 2.4 BY ago) 156
Earth's Proterozoic and Phanerozoic Atmosphere (2.4 BY ago to today) 159
Anthropogenic Carbon Dioxide in the Atmosphere 163
Historic Effect of Anthropogenic Carbon Dioxide 168
11 Ozone in the Earth's Atmosphere 173
Properties of Ozone 173
Ozone Layer as the "Earth's Shield" 174
Atmospheric Gases Ability to Absorb Energy 175
The Ozone Hole 184
Ozone - Methane Reaction 188
Concluding Remarks 189
12 Evolution of Atmospheric Composition and Pressure 191
Partial Pressure of Atmospheric Gases 191
Part IV: Various Factors Affecting the Evolution of the Earth's Climate 197
13 Earth's Orbital Distance from the Sun 199
Effect of Gravity on Earth's Orbital Paths 199
Earth's Orbital Path About the Sun 200
Kepler's Laws Pertaining to Planetary Orbits 202
Eccentricity of an Object's Orbit 205
Effect of Other Planets on Earth's orbit 206
The Effect of the Planet Jupiter on Earth's Orbital Path 212
14 Climatalogical Effect of Continental Drift 223
Continental Drift's Effect on the Earth's Precession Angle 223
Latitudinal Temperature Contrast on Earth's Surface 228
15 Earth's Future Climate 235
Conclusions 239
References and Bibliography 241
Author Index 271
Subject Index 275
Chapter 1
Climatic Paradox
Historic Temperatures of Early Earth
Today, the Earth is the one planet out of all the planets in the solar system that has an atmosphere providing a favorable climate for the evolution of life (both flora and fauna) on its surface. To better understand the historic development of the Earth and its atmosphere, geologists have divided the age of the Earth into eons, eras and periods. Figure 1.1 displays the geologic system of time division used in this book, showing the development of life and how it relates to the changing environmental geologic development of the Earth. When discussing the climate of the Earth, a critical component is that of temperature. A temperature chart covering the entire history of Earth is presented in Figure 1.2. The arrow on the right side of this figure points to today's average surface temperature of the Earth. The Earth has experienced both cooler and warmer periods of temperature with cyclic occurrence. In general, Figure 1.2 reveals that the Earth has been much warmer in the past than it is today, and that over the past 65 million years (MY) has progressively cooled.
Figure 1.1 Development of life on Earth for the past 4.5 BY. (After pbhslifescience, https://pbhslifescience.wordpress.com/2016/11/04/evolution-slides-1.)
Figure 1.2 Schematic 4.5 BY Earth chart. (Original data from Frakes (1979); in: Watts, https://Wattsvpwiththat.com/2014/09/08/Monday.)
Sorokhtin et al. (2011) defined life on the Earth as a concourse of several circumstances. These circumstances include: (1) a quiet star, e.g., Sun; (2) the optimum distance of the Earth to the Sun throughout the Earth's orbit about the Sun; (3) the presence of a massive satellite, e.g., the moon; (4) chemical composition of the primordial Earth and its atmosphere; and (5) several other causes reviewed in detail in the monograph by Sorokhtin and Ushakov (2002). Climatic conditions for life habitation on the Earth was a result of changing atmospheric composition (see Figure 1.3) and pressure and to a feedback between the evolution of the Earth biota and atmosphere.
Figure 1.3 A climatic paradox: The sun luminosity increases over time, whereas Earth's temperature gets cooler. Curve 1 - average isotopic water temperature that is sea-flint forming in, also describes the average temperature for the global, near-bottom of sea floor ocean water. The dots are d18O values for the sea-flint (after Schopf, 1982). Curve 2 - temperature of an absolutely black body at the distance of Earth-from-sun, which describes the sun's luminosity.
Concepts by Some of Global Warming
Today by some, a major environmental concern is the release of human generated carbon to the atmosphere (anthropogenic). It is thought by these individuals, without either historic or scientific evidence, that humans are putting too much carbon in the form of carbon dioxide (CO2) or methane (CH4) into the atmosphere and that this anthropogenic carbon is somehow responsible for what they feel is global warming.
The Earth's climate (temperature) is primarily determined by: (1) the Sun's radiation intensity, (2) the composition and density of the Earth's atmosphere and (3) the Earth's atmospheric capability to absorb and retain the Sun's energy. It is often, incorrectly assumed, that the heating of the Earth's atmosphere and surface is, to a substantial extent, only due to the capacity of various atmospheric gases that absorb the IR (heat) radiation from the Sun, ignoring the atmospheric pressure.
The concept that the Earth's atmosphere is heated by the greenhouse gases was first proposed by the Swedish scientist Svante Arrhenius at the end of the nineteenth century. This idea is now postulated as obvious and accepted without verification [Maslin (2004) in: Enzler (2015); Budyko (1974 & 2002); Greenhouse effect (1989); and Petrosyants (1994)]. Svante proposed a relationship between atmospheric carbon dioxide concentrations in the atmosphere and global temperature, i.e., if only one increased the concentration of carbon dioxide, the atmosphere would absorb more energy.
Since then, this concept today is found within the conclusions of the Intergovernmental Panel on Climate Change (IPCC), Greenpeace, United Nations Environmental Program (UNEP), and World Meteorological Organization (WMO). This same viewpoint was totally supported in the resolutions of the International Ecological Congresses in Rio de Janeiro, Brazil (1992) and Kyoto, Japan (1997).
It is assumed that the main danger to the Earth's climate arises from the fundamental energy sources of the modern economy through the release of greenhouse gases, especially carbon dioxide, into the atmosphere. Under some forecasts of the proponents of the manmade (anthropogenic) global warming concept, a warming of the Earth's surface temperature could increase 2.5 to 5 °C by the year 2100. The rise in the ocean level caused by this warming would reach 0.6 to 1.0 m, resulting in problems for the densely populated areas of the Earth along the continental shores. Other consequences of global warming have also been forecast, e.g., the spread of deserts, permafrost melting, soil erosion, etc.
The conventual theory of global warming states that the heating of the atmosphere's troposphere occurs as a direct result of the anthropogenic addition of carbon dioxide (CO2) and the methane (CH4) that is added to the Earth's atmosphere by man. As a result, the petroleum industry has often been singled out for blame, for the release of additional carbon (methane and carbon dioxide) into the atmosphere as it produces, handles and burns hydrocarbons. Some of these environmentalists also believe that today's increase in atmospheric carbon dioxide can be primarily attributed to any human activities that are related to the release of CO2 or CH4 to the atmosphere.
Earth's Historic Temperature Charts
Today's literature is filled with a wide variety of options about global warming and climate change. Unfortunately, these opinions are not always grounded in the Earth's temperature history or scientific facts, but rather in emotional feelings. This range of opinions include those by: (1) The National Oceanic and Atmosphere Administration (NOAA) which has claimed that there has been no recent slowdown in global warming; (2) the Space and Science Research Corporation stating that the Earth is presently in a sustained phase of global cooling; and (3) some experts who state that we have been in a transition phase without significant warming or cooling for the past 20 years. These opinions are made without looking at the historic temperature charts of the Earth, leaving open the question of "Are we cooling, transitioning, or warming?"
Misuse of Temperature Charts
To correctly answer the question of the Earth's cooling or warming controversy, one must first look at temperature charts over the whole time of the Earth's geologic history to understand where we have been and where are we going. Understanding where we have been requires obtaining temperature charts (records) of temperatures before recorded history. Unfortunately, before recorded history, there was no recording of temperatures; however, there are several methods we can use to infer temperatures during these earlier periods of time. Temperature charts can be prepared by inferring temperatures obtained from ice cores, tree rings, etc. It should be noted that these values of temperatures obtained are approximations and not necessarily the exact values of the Earth's average surface temperatures (see Figure 1.2). Therefore, temperature charts, with values obtained by one method, may not always exactly match those temperatures obtained by a different method for the same period. Whenever possible, in preparing a temperature chart, it is preferable to use only temperatures that have been obtained by one technique. It has been said, Oranges are easily comparable to other oranges, but not necessarily when you directly compare apples to oranges. Also, many times it is not the inferred values of temperature that are important, but rather, the trends that a temperature chart data displays for a given period of time. This is particularly true when you have inferred temperatures from more than one method indicating slightly different numbers, but showing a similar trend.
Today, some portions of our planet experience extreme heat, whereas other areas experience the opposite. Temperature inferred at the poles should be expected to be cooler than the average surface temperatures inferred in other areas of the Earth and, therefore, not necessarily be expected to represent an average surface temperature for the Earth at that time. It has also been noted that climatic conditions of the two poles are not always similar. In examining a temperature chart, it is crucial to: (1) know what method was utilized to determine the temperatures and (2) whether in preparation of the chart, only one method was used to determine the temperatures.
Use of Paleoclimatology to Estimate Prehistoric Temperatures
Paleoclimatology is the study of historic climatic conditions, examining their causes and effects in the geologic past, using current data found in glacial...
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