Greenhouse Gas Effect on the Economy and You

How Rising CO2 Levels Are Making Your World a Hothouse

greenhouse gases trapping heat
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The greenhouse effect is when carbon dioxide and other gases in the Earth's atmosphere capture the Sun's heat radiation. Greenhouse gases include carbon dioxide, water vapor, methane, nitrous oxide, and ozone. They also include small but lethal amounts of hydrofluorocarbons and perfluorocarbons.

The greenhouse effect functions like the glass roof on a greenhouse that traps the sun's heat. We need some greenhouse gases. Without any, the atmosphere would be 91 degrees Fahrenheit cooler. The Earth would be a frozen snowball and most life on Earth would cease to exist. 

But since the 1850s, humans have been adding too many of these gases. They've been burning massive amounts of plant-based fuels such as coal, oil, and trees. These fuels emit the carbon dioxide the plants had absorbed and stored during their lifetimes. Temperatures have risen since then.

Carbon Dioxide

 into the atmosphere each year. But it also absorbs that same amount through plants and the oceans. It remained balanced until 10,000 years ago when humans began burning wood. It slowly rose to 278 parts per million until 1850, when humans began burning oil, kerosene, and gasoline. The term 278 ppm means there are 278 molecules of carbon dioxide per million molecules of total air.

Oil and other fossil fuels are the remains of prehistoric plants. When they were alive, the plants absorbed carbon from the atmosphere during photosynthesis. In that process, they harness the sun’s energy to make sugar. They combine hydrogen from water with carbon from carbon dioxide. They emit oxygen as a byproduct. When they die, their remains contain all the carbon they absorbed. When we burn them as fuel, the carbon combines with oxygen and enters the atmosphere.

As proof of the impact of photosynthesis, every spring the Northern Hemisphere becomes green and the concentration of carbon dioxide in the atmosphere dips. In the fall and winter, the foliage dies, and CO2 rises. Some scientists say it's like .

Heat and power generation release 25 percent of the carbon man has put into the atmosphere.

Often overlooked is land use. Food production has released 135 gigatons of carbon into the atmosphere. The most damaging methods are clear-cutting, plowing, and heavy grazing. These methods obliterate carbon dioxide-absorbing plant life.

As of February 2019, NASA-recorded C02 levels were  In 2002, they were . In 1880, C02 levels were only 280 ppm.   that we need to remove these of "legacy CO2" to stop further climate change.

The was in the Pliocene era. Sea levels were 66 feet higher, there were trees growing at the South Pole, and temperatures were 3-4 C higher then they are today. It will take time for the CO2 levels to warm the planet to this level, but it will happen.

There is so much excess CO2 that it would take  for it all to dissipate at natural absorption rates. For that to work, humanity would have to stop emitting all CO2 immediately.

Will people stop emitting CO2 anytime soon? There are goals to reduce carbon emissions, but significant emitters have no plans to stop using carbon-based fuels. Daniel Cziczo, Ph.D., associate professor of atmospheric chemistry at the Massachusetts Institute of Technology, estimates it could reach 600 ppm before humanity changes its ways. That could drive the temperature increase to 2, 3, or 4 degrees Celsius.

If CO2 emissions continue at current rates, parts per million in 100 years. At that level, stratocumulus clouds break up. The disappearance of this cooling mechanism would add 8 C. At that point, palm trees would grow in the Arctic and seawater would be 104 F in the tropics. Conditions would be of 50 million years ago.

In 2018, carbon dioxide emissions . That's worse than the 1.6 percent rise in 2017. The increase brings emissions to a record high of 37.1 billion tons. China, the largest emitter, increased by 4.7 percent. Trump's trade war is slowing its economy. As a result, leaders are allowing coal plants to run more to boost production.

The United States, the second-largest emitter, increased by 2.5 percent. People continue to buy larger vehicles, increasing oil use. The European Union, the third-largest emitter, reduced by 0.7 percent. India increased emissions by 6.3 percent. 

Methane 

Methane or CH4 traps heat 25 times greater than an equal amount of carbon dioxide. But . CO2 lasts for hundreds of years, if not thousands. 

Methane comes from three primary sources. The production and transport of coal, natural gas, and oil make up 40 percent. Cow digestion contributes another 26 percent, while manure management adds 10 percent. The decay of organic waste in municipal solid waste landfills kicks in 16 percent.

Researchers have found  to the emission of methane from cows. Farmers should add seaweed to the animals' diet. Researchers found that replacing 2 percent of the feed with Australian red algae would reduce methane emissions by 99 percent. The researchers are testing milk and beef to make sure the seaweed doesn't affect the product. 

In 2016, California said it would . It has 1.8 million dairy cows and 5 million beef cattle. The seaweed diet, if proven successful, would be an inexpensive solution.

The Environmental Protection Agency has launched the  to help reduce methane from landfills. The program helps municipalities use the biogas as a renewable fuel.

In 2018, Shell, BP, and Exxon their methane emissions from natural gas operations. In 2017, a group of investors with roughly $30 trillion under management launched a five-year initiative to push the biggest corporate emitters to reduce emissions.

Nitrous Oxide

Nitrous oxide, also called N2O,  of greenhouse gas emissions. It remains in the atmosphere for 114 years. It absorbs 300 times the heat of a similar amount of carbon dioxide. It is produced by agricultural and industrial activities. It's also a byproduct of fossil fuel and solid waste combustion.

More than two-thirds results from its use in fertilizer. Farmers can reduce nitrous oxide emissions by reducing nitrogen-based fertilizer use.

Fluorinated Gases

Fluorinated gases are the longest lasting. They are thousands of times more dangerous than an equal amount of carbon dioxide. Because they are so potent, they are called High  Gases.

There are four types. Hydrofluorocarbons are used as refrigerants. They replaced chlorofluorocarbons that were  in the atmosphere. Hydrofluorocarbons, though, is also being replaced by hydrofluoroolefins. These have a shorter lifespan.

Perfluorocarbons are emitted during aluminum production and the manufacturing of semiconductors. They remain in the atmosphere between 2,600 and 50,000 years. They are 7,390 to 12,200 times more potent than CO2. The EPA is working with the  and  industries to reduce the use of these gases.

Sulfur hexafluoride is used in magnesium processing, semiconductor manufacturing, and as a tracer gas for leak detection. It's also used in electricity transmission. It’s the most dangerous greenhouse gas. It remains in the atmosphere for 3,200 years and is 22,800 times as potent as CO2. The  to detect leaks and recycle the gas.

Nitrogen trifluoride remains in the atmosphere for 740 years. It is 17,200 times more potent than CO2.

Greenhouse Effect Is Well Established by Science

Scientists have known for more than 100 years that carbon dioxide and temperature are related. In the 1850s, John Tyndall and Svante Arrhenius studied how gases responded to sunlight. They found that most of the atmosphere has no effect because it is inert. But 1 percent is very volatile. These components are CO2, ozone, nitrogen, nitrous oxide, CH4, and water vapor. When the sun's energy hits the earth's surface, it bounces off. But these gases act like a blanket. They absorb the heat and reradiate it back to the earth.

Since they are so potent, a 40 percent increase is huge. The volume is having huge impacts on temperatures.

In 1896, Svante Arrhenius found that if you doubled CO2, which was then at 280 ppm, it would increase temperatures by 4 degrees Celsius.

In 1880, CO2 was 280 ppm. In 2012, it was 400 ppm. That’s a 43 percent increase in CO2. The average temperature is 1 degree Celsius warmer. Over large land areas, it’s 1.5 degrees Celsius warmer. It’s the warmest it’s been in thousands of years. Why hasn’t the temperature increased by Arrhenius’ predictions?

Clouds, fog, particles, and ice sheets reflect the sun’s radiation back into space before it ever reaches the earth’s surface. Scientists call it the Direct Effect. The Indirect Effect of particles creates more clouds. They cool the temperature at the same time greenhouse gases warm the temperature. Without the clouds created by pollution, it would be as warm as Arrhenius predicted. According to Cziczo, that’s what makes it so difficult to predict temperatures.

Impact

Between 2002 and 2011, 9.3 billion tons of carbon was emitted per year. Plants absorbed 26 percent of that. Almost half went into the atmosphere. The oceans absorbed 26 percent.

Oceans absorb 22 million tons of CO2 per day. That adds up to 525 billion tons since 1880. That's made the ocean 30 percent more acidic in the past 200 years. This destroys the shells of mussels, clams, and oysters. It also affects the spiny portions of urchins, starfish, and corals. In the Pacific Northwest, have already been affected.

As the oceans absorb CO2, they also warm. Higher temperatures are causing fish to migrate northward. As much as 50 percent of coral reefs have died off.

more than the lower layers. That keeps lower, colder layers from moving to the surface to absorb any more CO2. These lower ocean layers also have more plant nutrients such as nitrate and phosphate. Without it, phytoplankton starve. These microscopic plants absorb CO2 and sequester it when they die and sink to the bottom of the ocean. As a result, the oceans are reaching their capacity to absorb CO2. It's likely that the atmosphere will warm at a faster rate than in the past.

It also affects to smell. It dampens scent receptors fish need to locate food when visibility is poor. They would also be less likely to avoid predators.

In the atmosphere, rising CO2 levels help plant growth since plants absorb it during photosynthesis. But higher CO2 levels lower the  of crops.  most farms to move further north.

Scientists  that the . Higher temperatures, rising sea levels and an increase in droughts, hurricanes, and wildfires more than offset any gains in plant growth. 

Reversing the Greenhouse Effect

In 2014, the  countries must remove carbon from the atmosphere. Even if we stopped emitting gases, there are already enough greenhouse gases in the air to create a catastrophe. These include the collapse of polar glaciers and flooded coastal cities. 

In 2015, the  was signed by 195 countries. They pledged to cut greenhouse gas emissions by 26 to 28 percent below 2005 levels by 2025. Its goal is to keep global warming from worsening another 2 degrees Celsius above pre-industrial levels. Many experts consider that the tipping point. Beyond that, the consequences of climate change become unstoppable.

In 2017 alone, China installed as many solar panels as those that exist in France and Germany. But renewables only meet 19 percent of global energy demand. To meet the Paris Agreement climate goals, clean energy must grow five times as fast as it did in 2017.

China is the world’s biggest car market. of its vehicles to run on batteries by 2025. Japan’s government wants manufacturers to stop building conventional cars by 2050. 

To reverse the greenhouse effect, man must also pull carbon dioxide out of the atmosphere and render it inert.

Several strategies have been discussed. None of these approaches are yet proved or affordable at the scale needed to make a difference. The most obvious hurdle is the additional energy some of them require. Unless this increased energy comes from a free, renewable source, it would add more costs.

  • Scrubbing the air with great air conditioner-like machines.
  • Fertilizing the oceans with iron dust to prompt algal blooms that, when they die, carry captured carbon to the bottom of the sea.
  • Capturing and storing the carbon dioxide that results when energy is produced by burning trees and other plants that removed carbon from the atmosphere during their growth.
  • Crushing and spreading certain types of rock, like basalt, that naturally absorb atmospheric carbon.

Carbon farming does this more affordably by growing plants. For example, builders are putting plants into bio-roofs. Agroforestry grows trees and crops together to increases carbon retention. No-till agriculture reduces the erosion and carbon loss caused by plowing. Keeping farmland covered would store more carbon than bare dirt bleeds carbon.

 is an ecologist at the University of California, Berkeley. She found that the best approach was to use manure as compost on the fields. It kept it from emitting carbon gases while it festered in lagoons. It also nourished grasses that absorbed more carbon. If only 41 percent of the rangeland were treated, it would offset 80 percent of California's agricultural emissions.

You can become carbon neutral. The United Nations program allows you to offset all the carbon you've emitted by purchasing credits. It helps you calculate your specific carbon emission, or you can just use an average. These credits fund green initiatives throughout the world. You can select the specific project that interests you.