Climate Change For Dummies. Elizabeth MayЧитать онлайн книгу.
the Case for Carbon
Scientists have collected evidence that confirms the buildup of carbon dioxide in the Earth’s atmosphere as by far the most likely cause of the current climate crisis. And they’ve built computer models to forecast future effects.
Geologic and prehistoric evidence
They can measure exactly how much carbon dioxide has been in the Earth’s atmosphere historically. Climatologists (scientists specializing in climate science) have drilled deep — as deep as 2 miles (3 kilometers) — into ancient ice in places such as Antarctica and Greenland. They’ve pulled up ice cores — long, thin samples of many layers of ice that has been packed down over thousands of years, which look like really (really) long pool noodles. (Figure 3-2 shows two scientists drilling for an ice core sample.) When the layers are clearly visible, the ice core looks like a pool noodle with horizontal stripes.
National Oceanic and Atmospheric Administration
FIGURE 3-2: Drilling for an ice core sample.
Scientists can date an ice core by counting the layers of ice — just like you can tell the age of a tree by counting its rings. The layers of ice tell them exactly when the ice was formed. Each layer of ice includes little pockets of trapped air. These frozen air bubbles are like time capsules of the ancient atmosphere. They’re full of gas, including carbon dioxide, that has been trapped for hundreds of thousands of years. Each layer of ice in the ice core also contains deuterium, a hydrogen isotope that enables scientists to determine what the temperature was when that ice layer was formed.
Scientists still don’t know the exact cause and effect relationship between GHGs and temperature throughout the planet’s history. The cause of the last ice age, for instance, probably wasn’t a drop in atmospheric carbon dioxide, but a result of the Earth tilting away from the sun in a phase in the planet’s Milankovitch cycle (which we discuss in the section “Considering Causes of Global Warming Other Than GHGs,” earlier in this chapter). This cooling then spurred the atmosphere’s carbon dioxide to drop, and the two events in tandem brought about the ice age. Ultimately, scientists still aren’t sure whether temperature affects carbon dioxide, or whether carbon dioxide affects temperature — it’s a question of which came first, the chicken or the egg.
What scientists do know for certain is that a distinct pattern and relationship between carbon dioxide and temperature exists; when one is high, so is the other, and when one is low, the other plunges, too. Scientists also know that the Milankovitch cycle has little to do with climate change over the past 200 or 300 years. In that time, human-produced carbon dioxide levels have skyrocketed, and temperature is starting to follow. As a result, scientists are certain that human-produced GHGs are currently warming the Earth. This close relationship between GHG concentrations and temperature suggests these higher levels of carbon dioxide will cause temperatures to continue rising.
Figure 3-3 shows the historic connection between carbon dioxide concentrations and fluctuations in temperature, as captured in ice-core deuterium levels.
Modeling and forecasting
To look forward, scientists make climate models (a model in this case is a computer program) to simulate the functioning of the Earth’s atmosphere and climate. These models cover the atmosphere, oceans, land, and ice of the planet. Researchers input data about the climate and how it works, and then start modifying that data to create various alternative scenarios.
Source: National Oceanic and Atmospheric (NOAA). Vostok Ice Core data and Mauna Loa carbon dioxide observations. Graph: John Streicker.
FIGURE 3-3: GHG levels and temperature fluctuations over the past 420,000 years.
These models have been proven; they work. Even conservative financial newspapers not known for positive views on climate change admit that the models have been “largely correct” in indicating the future path. The models keep getting more comprehensive and detailed — now people can see with real clarity the effects of continuing to emit carbon into the atmosphere.
The modelers are able to look at what would happen if, say, temperatures went up by, say, 3.6 or even 10.8 degrees F (2 or 6 degrees C) above 1850 levels. (These temperature increases refer to the global average, which we discuss in the following section.) (See the “How climate models work” sidebar, in this chapter, for more information.)
In particular, the models show how sensitive the climate is to what may seem like very small changes in temperature.
HOW CLIMATE COMPUTER MODELS WORK
The climate is affected by both the atmosphere (the part that everyone talks about the most) and the oceans. Changes in the air happen quickly, and changes in the oceans happen very slowly. So, scientists have been able to study air changes relatively easily, but they have quite literally had to wait and see what happens to the oceans. And because the ocean actually affects the bulk of the climate, they’re also having to wait and see what happens to the entire climate. So, scientists need climate models, projected scenarios created by super computers, to help predict major climate changes.
The most complex climate models, such as those used at NASA, look at the Earth in three dimensions. The scientists divide the atmosphere and oceans into square columns for input to the computer models. Each of these columns has its own set of weather information based on the history and current status of the area. This information gives the computer a base to work from. Then, the researcher running the model changes the numbers to see what would happen if one condition changed, such as air temperature. For short-term projections (looking forward a day to a month), an advanced computer can make the calculation in 20 minutes. But making longer-term projections (such as 50 years from now) can take a month or two. A global circulation climate model can take as long as a year to produce results after researchers input all the variables.
A few degrees is a lot
Three or four degrees F seems like a small number to make a big deal about. You may even be thinking that an extra 3.6 degrees F (2 degrees C) seems like a perfect amount of global warming. Your garden would grow better, you’d be hitting the beach more often, and the golf season might be longer, right? But 3.6 degrees F (2 degrees C) is actually a lot. The IPCC reports that the global average temperature in the middle of the last ice age was only 10 degrees F (5.5 degrees C) colder than it is today.
