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- Herausgeber: John Wiley & Sons
- Kategorie: Wissenschaft und neue Technologien
- Sprache: Englisch
- Veröffentlichungsjahr: 2022
Get clear about why climate change is so complicated and discover how you can help reverse it More and more frequent extreme weather events occur each year, and planet Earth is in danger of developing more climates where life -- whether animal, vegetable, or human -- is unsustainable. Climate Change For Dummies explains how rising temperatures, shrinking lakes, rising oceans, and shifting weather patterns affect your life on a daily basis. And of course the book goes a step further and offers suggestions about how you can take steps to limit your impact on the environment and help to reverse climate change. This straightforward guide demystifies the impact of climate's No. 1 enemy -- carbon dioxide -- and breaks down the many sources of this damaging but inescapable gas. From there, the book reveals how rising CO2 levels affect the weather, water levels, plant and animal species around the world, the food you eat, and your health. But the situation isn't hopeless! Climate Change For Dummies outlines actions governments, industries, and you can take to fight global warming and turn the tide to live in a cooler world. Discover details about * Short- and long-term effects of climate change * How some actions contribute to climate change and others reduce it * The many options for renewable energy and the pros and cons of nuclear energy * Actions nongovernmental organizations (NGOs) are taking to draw attention to the climate crisis * The debate around whether climate change even needs to be addressed Climate change won't be easy to overcome, but when you're armed with the facts, you can do your best to make a difference. Let Climate Change For Dummies point you in the right direction.
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Climate Change For Dummies®
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Published simultaneously in Canada
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Library of Congress Control Number: 2022933663
ISBN: 978-1-119-70310-5
ISBN 978-1-119-70317-4 (ebk); ISBN 978-1-119-70312-9 (ebk)
Climate Change For Dummies®
To view this book's Cheat Sheet, simply go to www.dummies.com and search for “Climate Change For Dummies Cheat Sheet” in the Search box.
Table of Contents
Cover
Title Page
Copyright
Introduction
About This Book
Foolish Assumptions
Icons Used in This Book
Beyond This Book
Where to Go from Here
Part 1: Understanding Climate Change
Chapter 1: Covering the Basics of Climate Change
Getting a Basic Overview — Global Warming 101
Tapping into The Roots of Global Warming
Examining the Effects of Global Warming around the World
Positive Politics: Governments and Global Warming
Solving the Problem
Chapter 2: Looking Closely at Greenhouse Earth
Examining Greenhouse Effect 101
Focusing On Carbon Dioxide: Leader of the Pack
Checking Out the Other GHGs
Chapter 3: Recognizing the Big Deal about Carbon
Considering Other Causes of Global Warming
Making the Case for Carbon
Eyeballing the Consequences of Continued Carbon Dioxide Increases
Part 2: Tracking Down the Causes
Chapter 4: Living in the Dark Ages of Fossil Fuels
From Fossils to Fuel — How Fossil Fuels Came to Be
Examining the Different Types of Fossil Fuels
Fueling Civilization’s Growth: Adding to the Greenhouse Effect
Chapter 5: Getting Right to the Source: The Big Emitters
Power to the People: Energy Use
The Road to Ruin: Transportation and GHGs
Draining the Carbon Sinks: Land Use
Chapter 6: Taking It Personally: Individual Sources of Emissions
Driving Up Emissions: Transportation and GHGs
Using Energy around the House
You Are What You Eat: Food and Carbon
Wasting Away
Part 3: Examining the Effects of Climate Change
Chapter 7: Focusing on Not-So-Natural Disasters
H
2
Oh No: Watery Disasters
Stormy Weather: More Intense Storms and Hurricanes
Forest Fires and Wildfires: Trees and Grasses as Fuel
Turning Up the Heat
Examining the Negative Side Effects of Positive Feedback Loops
Chapter 8: Risking Flora and Fauna: Impacts on Plants and Animals
Understanding the Stresses on Ecosystems
Warming the World’s Waters: Threats to the Underwater World
Risking Earth’s Forests
Preparing for Mass Extinctions
Chapter 9: Hitting Home: Global Warming’s Direct Effect on People
Focusing on the Health Scare — Outbreaks and Diseases
Putting Pressure on the Fields
Paying the Price for Global Warming
Feeling the Heat First: Unequal Effects
Part 4: Political Progress: Fighting Global Warming Nationally and Internationally
Chapter 10: Voting for Your Future: What Governments Can Do
If They Had a Million Dollars … Wait — They Do! — Funding Measures
Putting Programs into Place
Cleaning Up Transportation
Redefining Long-Term Investments
Laying Down the Law
Identifying Some Success Stories
Chapter 11: Beyond Borders: Progress on a Global Level
Understanding Why Global Agreements Are Important
Examining the U.N. Framework Convention on Climate Change
Looking At the Paris Agreement
Introducing the World’s Authority on Global Warming: The IPCC
Chapter 12: Developing in the Face of Climate Change
Identifying Challenges Faced by Developed and Developing Nations
Promising Developments: Looking at Progress in China, Brazil, and India
Choosing Sustainable Development
Part 5: Solving the Problem
Chapter 13: Powering the World — Renewable Green Energy
Addressing Energy Demand
Changing How to Handle Fossil Fuel’s Emissions
Reducing Energy Demand
Investigating Renewable Energy Options
Exploring Another Nonrenewable Energy Source: Nuclear Power
Chapter 14: Show Me the Money: Business and Industrial Solutions
Processing and Manufacturing Efficiently
Trading Carbon between Manufacturers — The Carbon Market
Constructing Greener Buildings
Identifying Corporate Success Stories
Recognizing Corporate Nonsuccess Stories
Focusing on Support from the Professional Service Sector
Looking At Farming and Forestry
Chapter 15: Activists without Borders: Nongovernmental Organizations
Understanding What NGOs Do
Meeting This Generation
Getting Involved
Chapter 16: Lights, Camera, Action: The Media and Climate Change
Growing News Coverage
Focusing on Science on the Red Carpet
Worldwide Warming: Climate Change Blogs
Bestselling Books: Reading between the Lines
Chapter 17: Figuring Out How to Change before Global Warming Is Unstoppable
Asking Tough Questions
Making the Changes in Limited Time
Addressing What Needs to be Done
Understanding Disruption
Ending the Dominance of Fossil Fuels as Humanity’s Main Source of Energy
Understanding How Disruption Can Be Accelerated
Getting There from Here: A Conversation among Citizens
Part 6: The Part of Tens
Chapter 18: Ten (Plus One) Things You Can Do to Fight Climate Change
Greening Your Car
Upgrading Major Appliances
Buttoning Up Your House
Making Your Daily Living More Energy Efficient
Going Vegetarian or Vegan (Sort of)
Reducing Food Waste
Supporting Clean, Renewable Energy
Being a Smart Investor and Encouraging Smart Disinvestment
Getting (or Making) a Green Collar Job
Helping To Make Change Where You Live
Spreading the Word
Chapter 19: Ten (Plus Three) Inspiring Leaders in the Fight
Arnold Schwarzenegger
Angela Merkel
Mia Amor Mottley
Bill McKibben
George Monbiot
Sheila Watt-Cloutier
Elizabeth Wathuti
Greta Thunberg
Michael Mann
Katharine Hayhoe
James Hansen
Bill Gates
Nandita Bakhshi
Chapter 20: Top Ten Myths about Climate Change Debunked
Knowing That a Debate Doesn’t Exist among Scientists
Recognizing That Human Activity Has Caused Current Global Warming
Looking into the Danger of Increased Carbon Dioxide Concentrations
Discovering the Truth about Sunspots
Understanding That Scientists Don’t Exaggerate to Get More Funding
Grasping the Misconceptions about the Science of Global Warming
Thinking It’s All Your Fault
Considering You Can’t Do Anything about It
Pinning the Blame on Developing Countries Isn’t Realistic
Living with Climate Change — and Doing Something about It
Chapter 21: Ten (Plus One) Online Climate Change Resources
National Geographic
Three Other Kid-Friendly Sites
Intergovernmental Panel on Climate Change
Climate Analysis Indicators Tool
Canada’s Environment and Climate Change
The U.K.’s Climate Challenge
Environmental Protection Agency
The International Energy Agency
Gateway to the UN System’s Work on Climate Change
Index
About the Authors
Connect with Dummies
End User License Agreement
List of Tables
Chapter 2
TABLE 2-1 Global Warming Potential of GHGs
Chapter 10
TABLE 10-1 Low-Carbon Cities
Chapter 14
TABLE 14-1 Businesses Reducing GHG Emissions
List of Illustrations
Chapter 2
FIGURE 2-1: The greenhouse effect in action.
FIGURE 2-2: The carbon cycle.
FIGURE 2-3: The relationship between carbon dioxide and the oceans.
FIGURE 2-4: The process of photosynthesis.
FIGURE 2-5: How trees and soil work side-by-side with carbon dioxide.
FIGURE 2-6: Water evaporates and lingers in the atmosphere.
Chapter 3
FIGURE 3-1: Clouds reflect light during the day and hold in surface heat overni...
FIGURE 3-2: Drilling for an ice core sample.
FIGURE 3-3: GHG levels and temperature fluctuations over the past 420,000 years...
FIGURE 3-4: Effects from climate change will intensify as temperatures rise.
Chapter 4
FIGURE 4-1: How fossil fuel is created.
Chapter 5
FIGURE 5-1: Burning carbon, in the form of coal, to create electricity.
FIGURE 5-2: Where an inadequately insulated building loses heating and cooling....
Chapter 6
FIGURE 6-1: Passenger cars lead the way in terms of GHG emissions.
FIGURE 6-2: Where you use energy in your home.
Chapter 7
FIGURE 7-1: Projected sea level rise.
FIGURE 7-2: Mountain glaciers provide freshwater.
FIGURE 7-3: World ocean currents.
FIGURE 7-4: Simplified flow patterns of the Gulf Stream.
FIGURE 7-5: White ice reflects heat, but dark water absorbs it.
FIGURE 7-6: Positive feedback loops that global warming might cause.
Chapter 8
FIGURE 8-1: Phytoplankton are the critical food source in the entire ocean food...
FIGURE 8-2: How climate change could continue to affect ecosystems.
Chapter 11
FIGURE 11-1: Comparing NDCs versus performance 1990–2019.
Chapter 12
FIGURE 12-1: The 46 least developed nations in the world, according to the UN.
Chapter 13
FIGURE 13-1: A co-generation system takes wasted heat from a normal system and ...
FIGURE 13-2: How carbon capture and storage happens in theory.
FIGURE 13-3: Solar thermal energy in action.
Chapter 17
FIGURE 17-1: Carbon budget science — politics and business.
Guide
Cover
Title Page
Copyright
Table of Contents
Begin Reading
Index
About the Authors
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Introduction
On Monday, news reports tell you the ice caps are melting, and people everywhere are about to be swept off in a giant flood. On Tuesday, you hear a radio interview with a scientist who says global warming is galloping faster than expected. Wednesday finds you standing in the grocery line, listening to people upset to see deaths in the unprecedented heatwave. By Thursday, you just don’t know whether it’s time to actively dig in to be engaged in the issue.
Think of today as Friday — the day all these stray pieces come together right here in your hands, thanks to Climate Change For Dummies.
Climate change is here. It’s no longer a future threat — catastrophic events due to global warming occur somewhere around the world daily. Wildfires, extreme droughts, heatwaves, more intense hurricanes, and deadlier tornados are causing massive economic losses and tragic loss of lives.
We don’t know how bad things can get; we only know that humanity has time to avoid the worst. The more climate changes around the world, the more you have to understand what global warming is. But you know what? It’s really quite exciting. Although global warming is connected to scary scenarios featuring soaring temperatures and worsening hurricanes and monsoons, it’s also a link to a better future. Global warming is opening doors for the development of new types of energy, leading the shift to reliable energy sources, and creating a vision of a greener tomorrow. And the best part? You’re right in the middle of it all, helping to make those changes.
About This Book
Climate Change For Dummies is your guide to climate change. We use the terms climate change, climate emergency, climate crisis, and global warming interchangeably in this book, though they’re slightly different things, as we discuss in Chapter 1. This book gives you the basics so that you can understand the problem, relate it to your daily life, and be inspired to start working on solutions to this complex and important issue.
In this book, we explain the concepts behind global warming clearly and simply by using the latest, most credible science, mainly from the Sixth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC). The IPCC is a team of more than 2,000 scientists who assess peer-reviewed climate change science and compile the assessments into a number of reports. These reports are mainly to inform the politicians and bureaucrats at the United Nations’ decision-making table, but anyone looking for detailed scientific information on climate change can read them. The IPCC is the most credible source of climate change information in the world today. (We discuss the IPCC in greater detail in Chapter 11.)
Although this book covers what climate change is and its impact on the world, Climate Change For Dummies isn’t just about the science. The handy guide also looks at a wide range of solutions to tackle climate change. We explore everything from the big-picture solutions that governments and businesses can implement to a slew of practical, can-do-it-today solutions for you at work, at home, and on the road.
In this book we include the following updates:
The increased urgency of acting to hold to 1.5 degrees C
The Paris Agreement
The significant and growing threat of ocean acidification
The good news of rapid acceleration of renewable energy
Foolish Assumptions
We wrote this book assuming that you know zero, nil, zilch about global warming. You don’t have to look up the definitions of big, ridiculous words or drag out your high school science textbook to read this book.
We also assume, however, that you know climate change exists, that you recognize humans contribute to this problem, and that you want to understand why global warming is happening.
Icons Used in This Book
Throughout this book, you see little icons sprinkled in the left margin. These handy symbols flag content that’s of particular interest.
This icon marks feel-good stories and major advances in the fight against climate change.
This icon marks a piece of information that’s important to know in order to understand global warming and the issues that surround it.
Don’t worry about reading paragraphs with this icon. This icon flags material that we think is interesting, but might be a little too detailed for your tastes.
Ready to make a difference? This icon points you to simple solutions that can help you reduce your greenhouse gas emissions or become a part of a bigger solution.
This icon marks paragraphs in which we talk about serious issues that humanity needs to deal with as soon as possible.
Beyond This Book
This book is full of information in plain English about climate change. If you want some additional pieces that you can refer to on a regular basis, check out the book’s Cheat Sheet at www.dummies.com. Just search for “Climate Change For Dummies Cheat Sheet.”
Where to Go from Here
This book like all other Dummies books is linear, meaning you can read any chapter or section that interest you. If you already know something about the subject or want to find out more about a specific topic, you can open any chapter and start reading. You also can scan the Table of Contents or the index, find a topic that piques your interest, and turn to that chapter to begin reading.
If you’re entirely new to the subject of climate change, you’ll likely want to read this book the old-fashioned way, starting at the beginning and working through to the end. Or, if you’re interested in reading about potential solutions, head to Part 5. No matter where you start, you can find out about causes, effects, progress, and probable solutions.
Part 1
Understanding Climate Change
IN THIS PART …
Explore the science behind the climate emergency: what are the causes, what are the effects, what can humans do about it?
Understand what greenhouse gases are, why they’re vital for life on Earth, and how they’re heating up the atmosphere.
Investigate why scientists are certain that greenhouse gases are the cause of the global warming that the Earth is experiencing today.
Look at some of the other factors contributing to climate change.
Chapter 1
Covering the Basics of Climate Change
IN THIS CHAPTER
Getting to know what global warming is all about
Figuring out what started climate change in the first place
Investigating the changes global warming might bring
Examining the role governments can play in fighting global warming
Finding solutions to the problem
The phrase “global warming” has been in the news since the late 1980s, but climate change, as global warming is also known, has been around much longer. In fact, it has been a constant throughout history. Earth’s climate today is very different from what it was 2 million years ago, let alone 10,000 years ago. Since the beginnings of the most primitive life forms, this planet has seen many different climates, from the hot, dry Jurassic period of the dinosaurs to the bleak, frozen landscapes of the ice ages.
Today, however, the planet is experiencing something new: Its climate is experiencing rapid and dangerous changes. Scientists are certain that these changes have been caused by emissions produced by human activities. By examining previous changes in the Earth’s climate, using computer models, and measuring current changes in atmospheric chemistry, they can estimate what global warming might mean for the planet, and their projections are scary.
Fortunately, Earth isn’t locked into the worst-case-scenario fate yet. By banding together, people can put the brakes on global warming. In 2009, when this book was first released, we had more time to apply the brakes than now. This chapter explains the essentials of global warming and what everyone can do to achieve a greener future.
Getting a Basic Overview — Global Warming 101
When “global warming” became a household phrase, greenhouse gases (GHGs), which trap heat in the Earth’s atmosphere, got a bad reputation. After all, those gases are to blame for heating up the planet. But, as we discuss in Chapter 2, GHGs in reasonable quantities aren’t villains, they’re heroes. They capture the sun’s warmth and keep it around so that life as it’s known is possible on Earth. The problem starts when the atmosphere contains too great an amount of GHGs. (In Chapter 3, we look at how scientists have determined the correlation between carbon dioxide in the atmosphere and temperature.)
Other factors, which we discuss briefly in the following sections, affect the Earth’s climate. Some are short-term — mostly those are seen as variations in weather, like El Niño or El Niña. The ones that matter most, though, are those that have long-term effects on climate. When the overall temperature of the Earth and the oceans rise, that’s not just a change in the weather. And it’s not just a normal variation that might have been observed in the past. That’s a change in the Earth’s climate.
Heating things up with GHGs
Human activities — primarily, the burning of fossil fuels (which we look at in the section “Tapping the Roots of Global Warming,” later in this chapter) — have resulted in growing concentrations of carbon dioxide and other GHGs in the atmosphere. As we explain in Chapter 2, these increasing quantities of GHGs are retaining more and more of the sun’s heat. The heat trapped by the carbon dioxide blanket is raising temperatures all over the world — hence, global warming.
Since the beginning of the Industrial Revolution, Earth has seen a 1.4-degree Fahrenheit (1.1 degree Celsius) increase in global average temperature because of increased GHGs in the atmosphere. Temperatures in polar regions, such as the Arctic, are experiencing temperature rises that are three times the global average.
Investigating other causes of global warming
Global warming is a very complex issue that you can’t totally understand without looking at the ifs, ands, or buts. Scientists have been certain for decades that the rapid changes to climate systems are due to the buildup of GHGs. With every new scientific report, they’re more certain and more concerned that changes must be made to avoid the worst-case scenarios. Other elements play a role in shaping the planet’s climate, however, including the following:
Cloud cover:
Clouds are connected to humidity, temperature, and rainfall. When temperatures change, so does the cloud cover — and vice versa.
Long-term climate trends:
The Earth has a history of going in and out of ice ages and warm periods. Scientific records of carbon dioxide levels in the atmosphere go back 800,000 years, but people can only give educated guesses about the climate earlier than that.
Solar cycles:
The sun goes through a cycle that brings it closer to or farther away from the Earth. This cycle ultimately affects the temperature of this planet and thus the climate. However, scientists have eliminated solar cycles as a factor in current warming.
We go over these other issues in greater detail in Chapter 3.
CLIMATE CHANGE — THE STORY IN A NUTSHELL
Earth has been around for about 5 billion years, starting as a ball of swirling gas and dust left over from the formation of the sun. In the first part of this very long time, the iron and silica that make up most of the planet separated — the hot heavy iron went down to the core and the lighter silicates came to the surface and cooled. Volcanoes belched material and gases up to the surface. Continents formed and move around on the surface of the planet. The Earth froze from pole to pole, heated, thawed, froze again. The mix of gases in the atmosphere changed as volcanoes and sun had their effects.
An overview of life on Earth
Life began and then ebbs and flows ensued:
3½ billion years ago: Single-celled organisms and viruses appeared.2½ billion years ago: Photosynthesis began in bacteria; sunlight provided the energy to convert carbon to cellular growth and emit oxygen as waste.900 million years ago: The first multi-celled organisms appeared.450 to 600 million years ago: Life exploded, and plants and animals from the oceans began to colonize the land.250 million years ago: The first mass extinction happens — the survivors are the early dinosaurs and mammals.200 million years ago: Another mass extinction occurs — now the dinosaurs become dominant. At the same time, some little mammals become warm-blooded, with new abilities to live in varying climates.150 to 100 million years ago: The first birds and flowering plants appear; large dinosaurs coexist with four distinct groups of mammals.66 million years ago: An asteroid hits eastern Mexico, the cloud of dust and steam blocks the sun for years, plants die, and the dinosaurs (and all other animals weighing more than 55 pounds [25 kg]) go extinct.55 million years ago: Another mass extinction happens, this one perhaps caused by a rise in greenhouse gases, that make the atmosphere a more effective insulator and causes Earth to heat past the survival limits of many species. It’s a tough place to live, Earth. Nothing is certain.6 million years ago: The first humans appear.Human beings have been around in the same basic form for 6 million of the 5 billion years of Earth, one-eighth of one percent of all that time. During that (short) time, humans survived ice ages and developed tools, agriculture, writing, states and governments, music, and art. The human population grew constantly but slowly, held within the limits of what Earth and natural processes could provide, at about 0.04 percent per year, from 10,000 BC to 1700 AD. By 1700 about 600 million people lived on Earth, rising to about 1 billion by 1800.
But then things changed. Between 1800 and 1928, the human population doubled to 2 billion. From then on, the rate of increase rose rapidly until about 1968 — and population went up to 2.5 billion, to 5 billion by 1987, and 7.7 billion by 2019. The rate of increase peaked in 1968 and has been decreasing ever since, but still the population is expected to rise to a maximum of about 11 billion by 2100.
So humans have come to dominate Earth as no other life form ever has. And it’s not just people — the animals that humans keep are now by far the largest part of the world’s total animal biomass (biomass is the total mass of living matter in a given area).
In addition to the rising population, humans learned in the early part of the 1800s how to use the energy stored in the Earth millions of years ago. It all came from those old plants that millions of years ago used energy from the sun to grow and make their carbon tissue. When the plants died, their tissues rotted and decomposed, and over millions of years were compressed into coal and oil.
Beginning to use fossil fuels
Black or brown coal, the compressed remains of ancient plants, is a wonderful source of high-density energy. It’s sometimes easy to find on the surface of the Earth, so it has been used for thousands of years for fuel (and humans had learned to make a sort of coal equivalent, charcoal, by heating wood without enough oxygen to actually burn). But most of the coal in the world is underground, not so easy to pick up and take home to the fire. People dug shallow mines to get the coal out, but often water would flood in and prevent further digging.
And then came the revolution, the start of what this book is about.
In the late 1700s and early 1800s, a Scottish engineer named James Watt made the first steam engines with high enough efficiency to be used to reliably pump water out of coal mines. So the coal provided the fuel to heat the water to make the steam to drive the engine to work the pump to get rid of the water to get at the coal, and the Industrial Revolution was launched.
With abundant coal, industrial applications became possible all over England. Engines made by Watts and others drove all sorts of processes, factories of all sorts, wool and cotton spinning, steam looms, steel mills, railroads and steamships: Coal powered England to become the first great industrial empire. The technology was then exported around the world, to Europe and the new states in America, and industrial output exploded.
With this new kind of industry, people began to be employed in large numbers in centralized locations. The move from the country to the cities accelerated. In the cities, coal was burned for heat, for hot water, and “coal gas” lit indoor and outdoor spaces. People worked longer hours of work and enjoyed evening entertainments in theaters and music halls.
But wait. There's still more.
The second Industrial Revolution begins
In 1859, oil was produced from a well in Pennsylvania, and the second Industrial Revolution began. Coal remained dominant for a long time, but the use of oil and its companion product methane gas (called natural gas to help with marketing) grew rapidly until the use of oil equaled coal by the 1950s and then displaced coal from most uses (except to make electricity and steel) by the 1970s. Oil is easier to handle than coal, produces more usable energy with less smoke and soot, and is just a better fuel source for railroads and ships, for industry, and for electrical generation. So King Coal lost its crown.
But humans were making more and more stuff and were still burning a lot of coal and now a lot of oil and gas as well. When that coal and oil was burned, humans got to use that ancient solar energy again to make things and move things and keep things warm. And all that carbon was released again, off into atmosphere as carbon dioxide and other gases called greenhouse gases because they act like the glass in a greenhouse to keep heat in. So, like any good greenhouse, the Earth became warmer. And it’s still getting warmer today. And that’s the problem to solve.
Tapping into The Roots of Global Warming
Just what are humans doing to release all those GHGs into the atmosphere? You can pin the blame on two main offenses, which we discuss in the following sections: burning fossil fuels and deforestation.
Fueling global warming
When you burn fossil fuels, such as coal and oil (named fossil fuels because they’re composed of ancient plant and animal material), they release vast amounts of GHGs (largely, but not exclusively, carbon dioxide), which trap heat in the atmosphere. Fossil fuels are also a limited resource — meaning that humanity can’t count on them over the long term because eventually they’ll just run out.
The fossil fuel that produces the most GHG emissions is coal, and burning coal to produce electricity is the major source of coal-related GHGs. The second-worst offender is using gasoline and diesel for transportation, followed by burning oil to generate heat and electricity. In fact, if people could replace the coal-fired power plants around the world and switch away from the internal combustion engine, humanity would have most of the problem licked. This switch is happening now, more and more quickly, but industries that have been built on the fossil fuel bonanza, and their supportive governments and bankers, continue to delay the inevitable progress. (Check out Chapter 4 for more fossil fuel info, Chapter 13 for the scoop on energy alternatives, and Chapter 17 for an introduction to the disruption expected and feared by those industries.)
Heating up over deforestation
Forests, conserved land, and natural habitats aren’t important just for the sake of saving trees and animals. Forests and all greenery are important players in keeping the climate in check. Plants take in the carbon that’s in the atmosphere and give back oxygen, and older trees hold on to that carbon, storing it for the duration of their lives. By taking in carbon dioxide, they’re significantly reducing the greenhouse effect. (See Chapter 2 for more about how plants help the Earth keep atmospheric carbon at a reasonable level.)
Unfortunately, much of the world’s forests have been cut down to make way for farmland, highways, and cities. Deforestation is responsible for about a quarter of GHG emissions. Rainforests and mangrove forests (very productive forests that grow in wetlands) are especially good at soaking up carbon dioxide because they breathe all year round. Temperate forests, on the other hand, don’t absorb much carbon dioxide over the winter, practically going into hibernation. (Chapter 5 has more about deforestation.)
Examining the Effects of Global Warming around the World
This book could easily be called Climate Emergency For Dummies. Although “global warming” is the common term for the climate changes that the planet’s experiencing (and scientists agree that average global temperature is increasing with the buildup of GHGs), the term doesn’t tell the whole story. The Earth’s average surface temperature is certainly going up. But while the average keeps rising, the variations around the average are also getting larger and larger. So some areas of the planet may actually get colder or experience more extreme bouts of rain, snow, or ice build-up. Consequently, most scientists prefer the term “climate change.” In the following sections, we look at how different places around the world will experience climate change.
Much of this section is pretty depressing. But nothing is exaggerated — the information here is all based on peer-reviewed scientific reports. Just how serious could the global impact of climate change be? The first global comprehensive scientific conference, which was held in Toronto, Canada, in 1988, described the potential effects of climate change this way: “Humanity is conducting an unintended, uncontrolled, globally pervasive experiment whose ultimate consequences could be second only to a global nuclear war.”
Of course, different parts of Earth have very different climates now, and climate change won’t affect every part of the planet in the same way. The following sections explain in general terms how some parts of the world are being affected by climate change.
The United States and Canada
In the United States and Canada, average temperatures have been rising because of climate change. As a result, the growing season has lengthened; trees have been sucking in more carbon, and for a while, farms were more productive. The recent years have had far more severe wet years followed by extreme drought. The 2021 drought had negative and long-term impact on wheat, corn, and other crops, according to Forbes.
Many plants and animals are spreading farther north to adapt to climate changes, affecting the existing species in the areas to which they’re moving. Increased temperatures have already been a factor in more forest fires and wildfires and damage by forest insects, such as the pine beetle epidemic in the interior of British Columbia, Canada. (See Chapter 8 for more information about how global warming will affect animals and forests.)
Scientists project that the United States and Canada will feel the effects of climate change more adversely in the coming years. Here are some of the problems, anticipated to only get worse if civilization doesn’t dramatically reduce GHG emissions:
Droughts and heat domes:
Rising temperatures are increasing droughts in areas that are already arid, putting even larger pressure on scarce water sources in areas such as the U.S. Southwest. In Canada, 600 people died from extreme heat in 2021 as a
heat dome
(happens when the atmosphere traps hot ocean air) formed over the west and drove temperatures to record levels. Some areas of British Columbia experienced temperatures of 122 degrees Fahrenheit (50 degrees Celsius).
Evaporating lakes:
The cities in the great heartland of the Great Lakes Basin will face retreating shorelines when the water levels of the Great Lakes drop because of increased evaporation. Lower water levels will also affect ship and barge traffic along the Mississippi, St. Lawrence, and other major rivers.
Floods:
Warmer air contains more moisture, and North Americans are already experiencing more sudden deluge events, causing washed out roads and bridges, and flooded basements and even Manhattan’s subways. In British Columbia in 2021, a form of rainstorm so extreme it’s called an
atmospheric river
caused massive flooding. The estimated damage to farms and transportation infrastructure was about $5.9 billion US, $7.5 billion Canadian. Bridges and other sections of roads and highways were washed away, isolating coastal areas from the rest of Canada for weeks.
Major storms: Warming oceans increase the risk of extreme weather that will plague coastal cities. Think of Hurricane Katrina, arguably the most devastating weather event ever to hit a North American city, as a precursor of storms like Superstorm Sandy. Katrina was whipped into a hurricane with a massive punch from the super-heated waters of the Gulf of Mexico in 2005. In 2021 a devastating series of tornadoes, way outside the “normal” tornado season, clobbered the southern and central United States, killing almost 100 people and causing millions in damage.
Not all extreme weather events are hurricanes. Global warming is expected to increase ice storms in some areas and thunderstorms in others.
Melting glaciers:
Glaciers from the Rockies to Greenland, are in rapid retreat, according to the National Snow and Ice Data Center. Glacier National Park could someday be a park where the only glacier is in the name. When glaciers go, so does the spring recharge that flows down into the valleys, increasing the pressure on the remaining water supplies. People who depend on drinking water from rivers or lakes that are fed by mountain glaciers will also be vulnerable.
Rising sea levels:
Water expands when it gets warmer, so as global average temperatures rise, warmer air warms the ocean. Oceans are expanding, and sea levels are rising around the world, threatening coastal cities — many of which are in the United States and Canada. This sea level rise will be far more devastating if ice sheets in Greenland and Antarctica collapse.
Changes across northern Canada and Alaska are more profound than in the south. We discuss these impacts in the section “Polar regions,” later in this chapter.
On average, North Americans have many resources, in comparison to developing regions of the world, to help them adapt to climate change. The Intergovernmental Panel on Climate Change (IPCC) says Canada and the United States can take steps to avoid many of the costs of climate change, to better absorb the effects, and to avoid the loss of human lives. For example, North America could establish better storm warning systems and community support to make sure that poor people in inner cities have some hope of relief during more frequent killer heat waves. (See Chapter 10 for more information about what governments can do to help their countries adapt to the effects of climate change.)
Latin America
South America has seen some strange weather in the past few years. Drought hit the Amazon in 2005, Bolivia had hail storms in 2002, and the torrential rainfalls lashed Venezuela in 1999 and 2005. In 2003, for the first time ever, a hurricane hit Brazil. More recently, the World Meteorological Association says:
“Latin America and the Caribbean (LAC) is among the regions most challenged by extreme hydro-meteorological events. This was highlighted in 2020 by the death and devastation from Hurricane Eta and Iota in Guatemala, Honduras, Nicaragua, and Costa Rica, and the intense drought and unusual fire season in the Pantanal region of Brazil, Bolivia, Paraguay, and Argentina. Notable impacts included water and energy-related shortages, agricultural losses, displacement and compromised health and safety, all compounding challenges from the COVID-19 pandemic.”
Other changes in Latin America may be attributable to global warming. Rain patterns have been changing significantly. More rain is falling in some places, such as Brazil, and less in others, such as southern Peru. Glaciers in the Andes Mountains and across the continent are melting. This glacier loss is a particular problem in Bolivia, Ecuador, and Peru, where many people depend on glacier-fed streams and rivers for drinking water and electricity from small-scale hydroelectric plants. (See Chapter 9 for more about how global warming will affect humans.)
Scientists project that the worst is yet to come. The IPCC models anticipate that about half of the farmland in South America could become more desert-like or suffer saltwater intrusions. If sea levels continue to rise at a rate of 0.08 to 0.12 inches (2 to 3 millimeters) per year, it could affect drinking water on the west coast of Costa Rica, shoreline tourism in Mexico, and mangroves in Brazil.
The threat to the Amazonian rainforest from logging and burning has attracted the concern of celebrities such as Sting and Leonardo DiCaprio. But human-caused global warming could potentially do more damage than loggers. By mid-century, the IPCC predicts that parts of the Amazon could change from wet forest to dry grassland, and that reduction in rainfall during dry months will reduce agricultural yields. Recent scientific reports confirm even a 2 degree C temperature increase could wipe out the Amazon. (We cover how ecosystems will be affected by climate change in Chapter 8.)
Europe
Recent findings have shown that climate change is already well under way in Europe. Years ago, the IPCC projected the changes that the continent is experiencing today: rising temperatures, devastating floods, increased intensity and frequency of heat waves, and increased glacier melt.
As for what’s in store for Europe, the IPCC reports a 99-percent chance that Europe will experience other unfavorable climate changes. Changes experienced so far include the following:
More flash floods and loss of life in inland areas:
In 2021, floods in Germany and Belgium killed more than 200 people and caused billions in damage — experts agree that such previously called “once in 400-year” floods are much more likely because of climate change.
More heat waves, forest fires and droughts in central, eastern, and southern Europe:
These events significantly impacted health and tourism in southern Europe in particular. The worst year on record for forest fires was 2019, until 2021 burned 1.2 million acres (half a million hectares). Much of the forest burned was in southern Europe, but fires are having increasing effects in the north as well.
Rising sea levels, which will increase erosion: These rising sea levels, coupled with storm surges, will also cause coastal flooding. The Netherlands and Venice are experiencing greater impacts than other areas in Europe dealing with the rising sea level. Venice, a 1,600-year-old Italian city that is one of the world’s greatest heritage sites, is built on log piles (which are gradually sinking) among canals, and so is particularly vulnerable to climate change. Rising sea levels are increasing the frequency of high tides that inundate the city.
A report published by the U.S. National Academy of Science says that loss of up to 50 percent of Europe’s native species of plants and animals may be likely if climate change isn’t arrested. Fisheries will also be stressed.
These impacts are all serious, but none of them represents the worst-case scenario — the Gulf Stream stalling. The results of this (stopping of a major ocean current) would be disastrous for Europe. (We look at the Gulf Stream Ocean current issue in Chapter 7.)
Africa
On a per-person basis, Africans have contributed the very least to global warming because of overall low levels of industrial development. Just look at a composite photo of the planet at night: The United States, southern Canada, and Europe are lit up like Christmas trees, burning energy that results in GHG emissions. Africa, on the other hand, shows very few lights: some offshore oil rigs twinkle, and a few cities shine, but the continent is mostly dark.
Despite contributing very little to the source of the problem, many countries in Africa are already experiencing effects of global warming. East Africa Hazards Watch says
“Major cities in East Africa have witnessed an increase in temperatures that almost doubles the 1.1 degrees C warming that the globe has experienced since pre-industrial times. Since 1860 Addis Ababa (Ethiopia) has warmed by 2.2 degrees C, Khartoum (Sudan) by 2.09 degrees C, Dar es Salaam (Tanzania) by 1.9 degrees C, Mogadishu (Somalia) by 1.9 degrees C, and Nairobi (Kenya) by 1.9 degrees C.”
Global warming is expected to melt most of Africa’s glaciers within the next few decades, which will reduce the already critically low amount of water available for farming. Long periods of drought followed by deluge rainfall have had devastating impacts in places such as Mozambique. Coastal areas in East Africa have suffered damage from storm surges and rising sea levels. The World Bank projects that by 2050 86 million people could be displaced by climate-related changes.
Unfortunately, because of pervasive poverty and the historic scourge of HIV/AIDS and now of COVID, many areas of Africa lack the necessary resources to help people living there cope with climate change. And the effects of global warming may act as a barrier to development and aggravate existing problems. At present, as many as 400 million (or 33 percent of the continent’s population) lack drinkable water, according to the World Resources Institute. The IPCC projects that some countries could see a 50-percent drop in crop yields over the same period and a 90-percent drop in revenue from farming by the year 2100. (We look at how developing nations are affected by and are addressing global warming in Chapter 12.)
Asia
More people call Asia home than any other continent — 4.7 billion in all. This high population, combined with the fact that most of Asia’s countries are developing, means that a lot of people won’t be able to sufficiently adapt to climate change impacts. As in Africa, climate change will bring pressures to the continent that will slow down development.
Here are some impending concerns for many parts of the continent:
Future availability of drinkable water:
This has been and continues to be a major problem because of population growth, pollution, and low or no sanitation. The IPCC projects that anywhere from 120 million to 1.2 billion people may find themselves without enough drinkable water within the next 42 years, depending on the severity of climate change. Already, rising temperatures are causing glaciers in the Himalayas to melt. These disappearing glaciers, which are the water supply to 2 billion people, are also contributing to increased avalanches and flooding.
Rising sea levels for coastal Asia:
The IPCC reports that mangroves, coral reefs, and wetlands will be harmed by higher sea levels and warming water temperatures. Unfortunately, this slightly salty water won’t be good for freshwater organisms, as a whole. (See
Chapter 8
for more about the impact global warming will have on the oceans.)
Illnesses:
They’re also expected to rise because of global warming. Warmer seawater temperatures could also mean more, and more intense, cases of cholera. Scientists project that people in South and Southeast Asia will experience more cases of diarrheal disease, which can be fatal. (
Chapter 9
offers more information about how global warming might increase the environmental conditions that promote the spread of diseases.)
Australia and New Zealand
If you ask an Australian or a Kiwi about global warming, you probably won’t get any argument about its negative effects. According to the World Wildlife Fund (WWF), Australia has experienced increased extreme and deadly bush fires, heat waves, less snow, and changes in rainfall. Extreme drought conditions persisted from 2003 to 2012 and from 2017 to today. This heat and lack of precipitation will likely worsen while global warming’s effects intensify.
The ozone layer in the Earth’s atmosphere is sort of like sunscreen for the planet — ozone intercepts some of the ultraviolet radiation that causes sunburn and skin cancer. The use of chlorofluorocarbons for refrigerants and other purposes caused the ozone layer to get thinner, resulting in an ozone hole over Australia and New Zealand. Partly as a result, Australians have the highest incidence of skin cancer on Earth. In 1987, the nations of the world came together to regulate the use of these chemicals, and their concentration in the atmosphere continues to decrease and the ozone layer is making a comeback. But now, increasing average temperatures in Australia and New Zealand are compounding these effects — one problem reduced by international cooperation is still affected by the lack of international cooperation on another.
Climate change has also strongly affected the ocean. Sea levels have already risen 2.8 inches (70 millimeters) in Australia since the 1950s, and increasing ocean temperatures threaten the Great Barrier Reef. The reef is at risk of bleaching, half its coral has disappeared since 1995 and the possibility that it may be lost altogether is becoming more real. (See Chapter 8 for details.)
Small islands
You probably aren’t surprised to hear that when it comes to climate change, rising sea levels and more extreme storms create an enormous risk for small islands everywhere, such as the South Pacific island of Tuvalu. Some islands will simply disappear due to rising sea levels if global efforts to limit global warming aren’t successful. Here are other climate-related concerns for small island nations:
Forests vulnerable to major storms:
Storms can easily topple island forests because a forest’s small area doesn’t provide much of a buffer and the root systems of trees are generally quite shallow on islands.
Limited resources:
Some islands can’t adapt physically and/or financially.
Proximity of population to the ocean:
At least 50 percent of island populations live within a mile (1.5 kilometers) of water, and these populations are threatened by rising sea levels. Tsunamis (they used to be called
tidal waves
) caused by earthquakes and volcanoes, and storm surges from hurricanes and typhoons do much more damage when the ordinary level of the sea surrounding an island is even a little higher than it used to be.
Risks to drinkable water:
The intrusion of ocean saltwater because of rising sea levels could contaminate islands’ drinkable water, which is already limited on most islands.
Reliance on tourism:
Beach erosion and coral reef damage, two possible effects of climate change, would undermine tourism, which many islands rely on for their source of income.
Vulnerable agriculture:
Island agriculture, often a key part of the local economy, is extremely susceptible to harmful saltwater intrusions, as well as floods and droughts.
Polar regions
The planet’s polar regions are feeling climate change’s effects more intensely than anywhere else in the world. Warming temperatures are melting the ice and thawing the permafrost (the permanently frozen layer of earth in northern regions of Alaska, Canada, and Siberia) that used to be solid ground.
The Arctic is home to many changes brought on by global warming, including the following:
Lost traditions:
Some indigenous people who make their homes in the Arctic are having to abandon their traditional ways of life. The Arctic ice and ecosystem are both core to many of these people’s cultures and livelihoods. For more on this issue, flip ahead to
Chapter 9
.
Melting ice:
The Greenland ice sheet is melting, adding to sea level rise. Arctic ice is also steadily losing ice volume. All of this melting is diluting ocean waters and affecting ocean currents.
New plant life:
Greenery and new plants have been appearing in the Arctic in recent years. The
tree line
(where tree growth use to end and tundra began) is shifting farther north, but the soil isn’t there to support a forest. Soils and ecosystems take thousands of years to develop — the changes happening now are rapid and unpredictable.
Some people look forward to the changes that the Arctic is experiencing. Now that so much sea ice has melted, ships can navigate the Arctic Ocean more efficiently, taking shorter routes. Without any sense of irony, oil companies now keenly anticipate being able to reach more fossil fuels below what used to be unreachable areas because of ice cover. Communities in the Arctic may be able to harness river flows that have been boosted or created by ice melt to run hydroelectric power. But these short-term economic developments can’t outweigh the negative planetary impacts.
In the Antarctic, some scientists project major change because of global warming, thinking there’s a chance that the western Antarctic ice sheet might collapse by the end of the 21st century. The western Antarctic ice sheet is simply enormous. It contains about 768,000 cubic miles (3.2 million cubic kilometers) of ice, about 10 percent of the world’s total ice. It appears to be weakening because warmer water is eroding its base. For the first time in the 2021 Sixth Assessment Report, IPCC scientists accepted as plausible, but not likely, that the entire sheet could melt. The Greenland ice sheet is also melting — quickly. Both the western Antarctic and Greenland ice sheets are adding to sea level rise.
The melting polar ice is also endangering many species, such as polar bears and penguins, which rely on the ice as a hunting ground. (Chapter 8 offers more information about the ways the polar animals are being affected by global warming.)
Positive Politics: Governments and Global Warming
Governments are often the first institutions that the public looks to for big solutions. Governments represent the people of a region, after all, and are expected to make decisions for the good of the public. So, governments need to be able to respond to global warming effectively. Climate change is a very big problem for which no one has all the answers. Despite this challenge, governments around the world are willing to play their part — and it’s an important one.
Governments need to take the lead. The next sections lay out some of the necessary actions at all levels from your local water authority to the international institutions.
Making a difference from city hall to the nation’s capital
All levels of government, from cities and towns, to states and provinces, to countries, have the ability to affect taxes and laws that can help in the fight against climate change:
Local governments:
Can implement and enforce city building codes, improve public transit systems, and implement full garbage, recycling, and composting programs.
Regional governments:
Can set fuel efficiency standards, establish taxes on carbon dioxide emissions, and set efficient building codes.
Federal governments:
Can lead on the largest of issues, such as subsidizing renewable energy sources, removing subsidies from fossil-fuel energy sources, taxing carbon, and developing national programs for individuals who want to build low-emission housing. Federal governments can also set standards and mandatory targets for GHG reductions for industry, provinces, and states to follow.
The most effective governments work with each other — partnerships between cities, states, and countries exist around the world, supporting one another while they work on the same projects. To read more about what governments can do and are already doing, check out Chapter 10.
Working with a global government
Countries must work together through global agreements to deal with, and conquer, a problem as urgent, complex, and wide-sweeping as climate change. Global agreements create a common level of understanding and allow countries to create collaborative goals, share resources, and work with each other towards global warming solutions. No one country can solve climate change on its own, just like no one country created global warming in the first place.
The core international law around climate change is the 1992 UN Framework Convention on Climate Change (UNFCCC) and a series of subsequent agreements, from the 1997 Kyoto Protocol to the current 2015 Paris Agreement. Countries have agreed that globally they will hold to as far below 2 degrees C as possible and preferably to no more than 1.5 degrees. But, collectively, despite marked progress in some nations, particularly within the European Union, the world’s countries aren’t on track to deliver on these goals.
The international discussions are ongoing; government representatives meet on an annual basis for the United Nations Climate Change Conference. These targets we re-affirmed at the last such meeting in Glasgow, Scotland in 2021. We discuss just what goes on at those meetings in Chapter 11.
Helping developing countries
The effects of climate change are taking a particularly heavy toll on the populations of developing countries
