How do we know that recent CO<sub>2</sub> increases are due to human activities? (2023)

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by eric

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Note:This is an update to an earlier post, which many found to be too technical. The original, and a series of comments on it, can be found here. See also a more recent post here for an even less technical discussion.

Over the last 150 years, carbon dioxide (CO2) concentrations have risen from 280 to nearly 380 parts per million (ppm). The fact that this is due virtually entirely to human activities is so well established that one rarely sees it questioned. Yet it is quite reasonable to ask how we know this.

One way that we know that human activities are responsible for the increased CO2 is simply by looking at historical records of human activities. Since the industrial revolution, we have been burning fossil fuels and clearing and burning forested land at an unprecedented rate, and these processes convert organic carbon into CO2. Careful accounting of the amount of fossil fuel that has been extracted and combusted, and how much land clearing has occurred, shows that we have produced far more CO2 than now remains in the atmosphere. The roughly 500 billion metric tons of carbon we have produced is enough to have raised the atmospheric concentration of CO2 to nearly 500 ppm. The concentrations have not reached that level because the ocean and the terrestrial biosphere have the capacity to absorb some of the CO2 we produce.* However, it is the fact that we produce CO2 faster than the ocean and biosphere can absorb it that explains the observed increase.

Another, quite independent way that we know that fossil fuel burning and land clearing specifically are responsible for the increase in CO2 in the last 150 years is through the measurement of carbon isotopes. Isotopes are simply different atoms with the same chemical behavior (isotope means “same type”) but with different masses. Carbon is composed of three different isotopes, 14C, 13C and 12C. 12C is the most common. 13C is about 1% of the total. 14C accounts for only about 1 in 1 trillion carbon atoms.

CO2 produced from burning fossil fuels or burning forests has quite a different isotopic composition from CO2 in the atmosphere. This is because plants have a preference for the lighter isotopes (12C vs. 13C); thus they have lower 13C/12C ratios. Since fossil fuels are ultimately derived from ancient plants, plants and fossil fuels all have roughly the same 13C/12C ratio – about 2% lower than that of the atmosphere. As CO2 from these materials is released into, and mixes with, the atmosphere, the average 13C/12C ratio of the atmosphere decreases.

Isotope geochemists have developed time series of variations in the 14C and 13C concentrations of atmospheric CO2. One of the methods used is to measure the 13C/12C in tree rings, and use this to infer those same ratios in atmospheric CO2. This works because during photosynthesis, trees take up carbon from the atmosphere and lay this carbon down as plant organic material in the form of rings, providing a snapshot of the atmospheric composition of that time. If the ratio of 13C/12C in atmospheric CO2 goes up or down, so does the 13C/12C of the tree rings. This isn’t to say that the tree rings have the same isotopic composition as the atmosphere – as noted above, plants have a preference for the lighter isotopes, but as long as that preference doesn’t change much, the tree-ring changes wiil track the atmospheric changes.

Sequences of annual tree rings going back thousands of years have now been analyzed for their 13C/12C ratios. Because the age of each ring is precisely known** we can make a graph of the atmospheric 13C/12C ratio vs. time. What is found is at no time in the last 10,000 years are the 13C/12C ratios in the atmosphere as low as they are today. Furthermore, the 13C/12C ratios begin to decline dramatically just as the CO2 starts to increase — around 1850 AD. This is exactly what we expect if the increased CO2 is in fact due to fossil fuel burning. Furthermore, we can trace the absorption of CO2 into the ocean by measuring the 13C/12C ratio of surface ocean waters. While the data are not as complete as the tree ring data (we have only been making these measurements for a few decades) we observe what is expected: the surface ocean 13C/12C is decreasing. Measurements of 13C/12C on corals and sponges — whose carbonate shells reflect the ocean chemistry just as tree rings record the atmospheric chemistry — show that this decline began about the same time as in the atmosphere; that is, when human CO2 production began to accelerate in earnest.***

In addition to the data from tree rings, there are also of measurements of the 13C/12C ratio in the CO2 trapped in ice cores. The tree ring and ice core data both show that the total change in the 13C/12C ratio of the atmosphere since 1850 is about 0.15%. This sounds very small but is actually very large relative to natural variability. The results show that the full glacial-to-interglacial change in 13C/12C of the atmosphere — which took many thousand years — was about 0.03%, or about 5 times less than that observed in the last 150 years.

For those who are interested in the details, some relevant references are:
Stuiver, M., Burk, R. L. and Quay, P. D. 1984. 13C/12C ratios and the transfer of biospheric carbon to the atmosphere. J. Geophys. Res. 89, 11,731-11,748.
Francey, R.J., Allison, C.E., Etheridge, D.M., Trudinger, C.M., Enting, I.G., Leuenberger, M., Langenfelds, R.L., Michel, E., Steele, L.P., 1999. A 1000-year high precision record of d13Cin atmospheric CO2. Tellus 51B, 170–193.
Quay, P.D., B. Tilbrook, C.S. Wong. Oceanic uptake of fossil fuel CO2: carbon-13 evidence. Science 256 (1992), 74-79
*How much they can be expected to absorb in the long run is an interesting and important scientific question, discussed in some detail in Chapter 3 of the IPCC report. Clearly, though, it is our ability to produce CO2 faster than the ocean and biosphere can absorb that it is the fundamental cause of the observed increase since pre-industrial times.
**The development of continuous series of tree rings going back thousands of years by using trees of overlapping age, is known as dendrochronology (see the Arizona Tree Ring lab web pages for more information on this).
***There is a graph illustrating such sponge data here. Thanks to F. Boehm for providing.

Reader Interactions

11 Responses to "How do we know that recent CO2 increases are due to human activities?"

  1. How do we know that recent CO<sub>2</sub> increases are due to human activities? (7)Jerram L. Brown says

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    You probably saw the review of Crichton’s book in the New Yorker recent issue. It was critical and alarming.

    I was very pleased to see your web site. It is needed.

    Thanks I had just read this today. It is a well-written review, and is available on line at the moment even if you don’t subscribe. –Eric

  2. How do we know that recent CO<sub>2</sub> increases are due to human activities? (8)bill says

    is it? pollutant?

    Response: It depends. Like the definition of ‘weed’ as a plant growing where you don’t want it to grow, CO2 in the atmopshere is clearly reaching undesirable levels. The same plant maybe a fine addition to a garden somewhere (as CO2 is a necessary ingredient for photosynthesis), but for that time and place and concentration, it is unwanted. Therefore it is clearly a pollutant in that respect. However, in the US, the word ‘pollutant’ has a legal meaning due to its inclusion in the laws governing the EPA. In essence, the EPA can only regulate ‘pollutants’, and so whether they have juristriction of CO2 emissions depends on the definition of CO2 as a pollutant. Hence the agressiveness with which certain people in the US pursue seemingly inconsequential semantic arguments with no real point. – gavin

  3. How do we know that recent CO<sub>2</sub> increases are due to human activities? (9)Nina Dessau says

    Thanks for your initiative.
    I would suggest that you give a link to Weart’s “The Discovery of Global Warming”, on the site of the American Institute of Physics.
    (A Hyperlinked History of Climate Change Science)

    Weart’s history is quite a remarquable work. It is also well-written and easily accessible for many. I believe that for many people the historical description of how one has come to a particular insight, (for example the question “How do we know Co2-increases are due to human activities”)might be enlightening. Especially in view of the current “debate” where many viewpoints and conclusions are presented by the press as if they came out of a hat.

  4. How do we know that recent CO<sub>2</sub> increases are due to human activities? (10)Andrew Lonigro says

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    Is there any evidence that carbon dioxide concentrations in the atmosphere, prior to the industrial revolution, ever approached the concentrations that we are seeing now?

    [Response CO2 levels are currently higher than for any time when we have direct measurements (directly, from 1950; before that, from air trapped in ice cores), which amounts to the last 780,000 years (see, e.g., a picture here for the last 400 kyr). Various considerations suggest that in the far past CO2 levels were considerably higher. From memory, the last time CO2 levels exceeded present was about 40 million years ago – William]

  5. How do we know that recent CO<sub>2</sub> increases are due to human activities? (11)m de gosson says

    This is Science, of course! Bravo!

  6. How do we know that recent CO<sub>2</sub> increases are due to human activities? (12)Dan Hughes says

    Can you point me to the details of the calculation mentioned in this statement:

    ” The roughly 500 billion metric tons of carbon we have produced is enough to have raised the atmospheric concentration of CO2 to nearly 500 ppm.”

    I’m especially interested in finding out (1) the extent (volume and mass) of the atmosphere into which the carbon mass was added and (2) the ranges of uncertainty associated with both the extent of the atmosphere and the mass of carbon produced.

    [Response: the CO2 produced is spread throughout essentially the entire atmosphere (by mass at least). Atmospheric pressure is approx 100,000 Pa/m2 and from that you can work out the mass (about 5×10^18 kg). 500 billion tons CO2 = 5×10^14 kg ~ 1.5×10^15 kg CO2, so by mass that much CO2 increases the atmos by a/b, ie 3×10^-4, which is about right. These done off the top of my head, so please check (JBS?). The extent of the atmos (and of the bit which CO2 is spread through) is very well known, as are fossil fuel emissions – William]

    To me the opening sentences of the second paragraph:

    “One way that we know that human activities are responsible for the increased CO2 is simply by looking at historical records of human activities. Since the industrial revolution, we have been burning fossil fuels and clearing and burning forested land at an unprecedented rate, and these processes convert organic carbon into CO2.”

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    are not very clear as follows. The addition of carbon into the atmosphere by human activities does not automatically imply that the atmospheric concentration must necessarily increase. Might the natural sinks of carbon at some times be able to absorb the human additions and result in no net increase?

    [Response: If we see CO2 increasing in the atmosphere, and humans emitting enough CO2 to account for that rise, then you have to go through some odd contortions to avoid a connection. You would have to postulate a suddenly increased natural sink (to remove the human CO2) and then a suddenly increased natural source (to increase the atmospheric CO2) – William]

    Thanks for your assistance.

  7. How do we know that recent CO<sub>2</sub> increases are due to human activities? (13)Tony Weddle says

    I don’t think there is any question that 6 billion living people, and rising, will have some effect on CO2 levels (not to mention CH4 levels). What seems clear, however, is that we don’t know exactly what that effect is. From the article above, the expected rise to 500 ppm hasn’t occurred. Nowhere near. But the precise reasons for the apparent shortfall are not known. So we really can’t say how much of an effect humans are having and whether they might be responsible for all or part of the current rise. The concensus that humans are responsible for all of the rise seems to be intuitive rather than scientific. I’d agree with the intuitive conclusion that humans are responsible for most of it, but that isn’t the story going out.

    Response. How can I word my response strongly enough? NO, NO, NO. Intuition has nothing to do with this. This is one of the best understood aspects in the entire science of climate change, and it really is not that complicated! We understand very very well why the level hasn’t (yet) reached 500 ppm. If you add CO2 to the atmosphere some of it will have to go into the ocean. This is very basic chemistry. Imagine taking a bottle filled half with water and half with pure air that has no CO2 in it. Add CO2 to the air in the bottle. Some of the CO2 will dissolve in the water, resulting in less CO2 in the air that you have originally put in. We expect this to happen, and the isotope measurements demonstrate it IS happening, and at what rate.

    In response to the question whether the natural sinks of carbon might compensate for the CO2 we are putting into the atmosphere, the answer is yes, but not very quickly. In the short term, the ocean cannot simply, magically, absorb all the excess CO2. If you try to pack all this excess CO2 in the surface ocean, it will come right back out. Again, that is what chemical equilibrium demands — there is no way around this. In the long term, the deep ocean will (probably) absorb much more of the CO2 we have put into the atmosphere, but this is the long term. If humans stopped producing CO2 today, it would take around 700 years to come back down to the original value. This is essentially because the timescale of ocean circulation is of order 1000 years.

    If you really want to understand the details here, the college-level textbook by Kump and others “The Earth System” would be a good place to start.


  8. How do we know that recent CO<sub>2</sub> increases are due to human activities? (14)Tony Weddle says

    Thanks for the response, eric. I hadn’t realised that the rate of absorption of all possible carbon sinks was extremely well known. Most reporting indicates that it isn’t. It seems that accurate reporting will be crucial in getting the right message across.

    Response You are missing the point. If it is 4:00 p.m. in Los Angeles, we don’t conclude that rush hour is just about to end just because we don’t know precisely how many cars are getting off the road. All we need to know — to accurately predict that rush hour is just beginning and that we’ll be stuck in traffic for a while — is that the number of cars getting off the road is much smaller than the number getting on. See my comment below.

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  9. How do we know that recent CO<sub>2</sub> increases are due to human activities? (15)eric says


    Just to clarify further, the point is that all of the possible important carbon sinks are well known enough that we are certain we are not going to see the carbon we put into the atmosphere disappear any time soon. The numbers we’re talking about are very large, and there are uncertainties in those numbers that are themselves large enough to be interesting scientifically. Furthermore the uncertainties are important politically, because the accounting used in Kyoto tries to give credit to countries with larger sinks (e.g. the US, which argued that the regrowth of New England forests is an important sink, which is probably true — but not enough to outweigh the US sources!).

    Let me give you some numbers:
    Three numbers we know well are the following (data are from Takahashi, Science, Vol 305, Issue 5682, 352-353, 16 July 2004).
    a) Emissions from fossil fuel combustion plus cement production is estimated to be 244 +/- 20 GT C (GT = 1 billion metric tons).
    b) The amount of carbon in the atmosphere that is greater than the 1850 level in the atmosphere of 165 +/- 4 GT as of 1994.
    c) The amount of C emitted to the atmosphere from land use changes (burning forest land, etc.) is about 140 +/- 40 GT
    d) The ocean has taken up 118 +/- 19 GT of this carbon.
    If you add these numbers up, you’ll find that 100 GT +/- 60 of C has gone into new growth in the terrestrial biosphere. Calculated this way, the size of that number is quite uncertain (we know it no better than +/-60%), but it is still clearly much smaller than the amount of C that has gone into the atmosphere and ocean combined . Independent calculations of how much C has gone into the terrestrial biosphere concur with this calculation.

  10. How do we know that recent CO<sub>2</sub> increases are due to human activities? (16)Tony Weddle says

    Thanks for that eric. I didn’t like your analogy of the LA rush hour, but I take your point.

    I may not be as good at math as I used to be but the figure I got, from what you wrote was 101 GT +/-83 of new terrestial growth of C. Excuse my ignorance, but how does this figure being much smaller that the amount that has gone into the atmosphere and ocean (283 GT C +/-23) give certainty that all atmosphere increases are anthropogenic? And are there any offsetting additional amounts of terrestial carbon (such as new forests or plant growth, or is this accounted for in the 3rd figure?).
    (Unfortunately, I can’t check the Science source until next week)

    Response The point is that more is being produced by humans than is winding up in the atmosphere and this is what we expect to happen. Sure, it is possible that not “all atmospheric increases are anthropogenic.” I never claimed otherwise. But to suggest that the natural environment has arbitrarily decided to start increasing the flux of CO2 into the atmosphere, right around the same time we are doing it is bizarre. Let me turn this around: what is the evidence that would suggest this is happening, and why?

    This is a dynamic system and CO2 would not be constant even without human influences. There is CO2 continually leaving the ocean and entering the atmosphere in places where ocean upwelling brings carbon-rich waters to the surface. There is CO2 entering the atmosphere from plant and animal respiration. Indeed, on an annual basis, CO2 increases during N. Hemisphere winter because plant respiration exceeds photosynthesis. The points though are that a) CO2 began to rise when we starting producing it in earnest, b) its isotopic signature demonstrates it comes predominantly from fossil fuels, and c) such an increase has not happened in at least 800,000 years as far as we can tell.

    As I said before, please read the scientific literature on this.


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What is the reason for the rise in CO2 levels? ›

Carbon dioxide concentrations are rising mostly because of the fossil fuels that people are burning for energy.

How do we know that the recent rise in atmospheric carbon dioxide concentration is primarily due to burning of fossil fuels? ›

How do we know that the recent rise in atmospheric carbon-dioxide concentration is primarily due to burning of fossil fuels? -Atmospheric carbon dioxide contains a decreasing amount of 13C relative to 12C, indicating a plant-based (not volcanic) source (either modern or fossil organic carbon).

What are 2 ways humans have increased CO2 levels in Earth's atmosphere? ›

Burning fossil fuels, releasing chemicals into the atmosphere, reducing the amount of forest cover, and the rapid expansion of farming, development, and industrial activities are releasing carbon dioxide into the atmosphere and changing the balance of the climate system.

What kind of human activity adds the most CO2 to the atmosphere? ›

The largest source of greenhouse gas emissions from human activities in the United States is from burning fossil fuels for electricity, heat, and transportation. EPA tracks total U.S. emissions by publishing the Inventory of U.S. Greenhouse Gas Emissions and Sinks.

What causes CO2 increase and decrease? ›

During the day or in spring and summer, plants take up more carbon dioxide through photosynthesis than they release through respiration [1], and so concentrations of carbon dioxide in the air decrease.

What level of CO2 is harmful to humans? ›

This could occur when exposed to levels above 5,000 ppm for many hours. At even higher levels of CO2 can cause asphyxiation as it replaces oxygen in the blood-exposure to concentrations around 40,000 ppm is immediately dangerous to life and health.

How do we know carbon is increasing in the atmosphere? ›

Careful accounting of the amount of fossil fuel that has been extracted and combusted, and how much land clearing has occurred, shows that we have produced far more CO2 than now remains in the atmosphere.

When were CO2 concentrations as high as they are today? ›

Welcome to the Pliocene. That was the Earth about three to five million years ago, very different to the Earth we inhabit now. But in at least one respect it was rather similar. This is the last time that carbon dioxide (CO2) levels were as high as they are today.

What is the latest estimate of the CO2 concentration in the atmosphere? ›

Carbon dioxide now makes up about 428 parts per million (ppm) of that air. The CO2 level is the world's thermostat. The higher it goes, the warmer things will get. At this rate the planet could warm by a dangerous 3°C above pre-industrial levels by 2100.

How does an increase in CO2 levels in the atmosphere due to human activities affect the rate of acidification of our oceans? ›

Because of human-driven increased levels of carbon dioxide in the atmosphere, there is more CO2 dissolving into the ocean. The ocean's average pH is now around 8.1 , which is basic (or alkaline), but as the ocean continues to absorb more CO2, the pH decreases and the ocean becomes more acidic.

How much CO2 is emitted by human activity in a year? ›

Human activities add a worldwide average of almost 1.4 metric tons of carbon per person per year to the atmosphere. Before industrialization, the concentration of carbon dioxide in the atmosphere was about 280 parts per million.

How much CO2 do humans exhale per breath? ›

= 0.0005 kilograms of air per breath. 3.8 carbon dioxide molecules per 10000 air molecules.

What human activities affect the carbon cycle? ›

Human activities have a tremendous impact on the carbon cycle. Burning fossil fuels, changing land use, and using limestone to make concrete all transfer significant quantities of carbon into the atmosphere.

How do human activities contribute to greenhouse gases? ›

Burning fossil fuels, cutting down forests and farming livestock are increasingly influencing the climate and the earth's temperature. This adds enormous amounts of greenhouse gases to those naturally occurring in the atmosphere, increasing the greenhouse effect and global warming.

Can CO2 blood levels fluctuate? ›

CO2 plays various roles in the human body including regulation of blood pH, respiratory drive, and affinity of hemoglobin for oxygen (O2). Fluctuations in CO2 levels are highly regulated and can cause disturbances in the human body if normal levels are not maintained.

Does CO2 rise or fall in a room? ›

Typically, carbon dioxide levels rise during the night when people are sleeping, especially if the door and windows are closed. The concentrations then fall during the day if the room is unoccupied.

What is normal CO2 level in home? ›

400–1,000 ppm: typical level found in occupied spaces with good air exchange. 1,000–2,000 ppm: level associated with complaints of drowsiness and poor air. 2,000–5,000 ppm: level associated with headaches, sleepiness, and stagnant, stale, stuffy air.

What happens if CO2 levels are too high? ›

Respiratory failure can happen when your respiratory system is unable to remove enough carbon dioxide from the blood, causing it to build up in your body. The condition can also develop when your respiratory system can't take in enough oxygen, leading to dangerously low levels of oxygen in your blood.

Is CO2 increasing in the atmosphere? ›

The concentration of carbon dioxide in Earth's atmosphere is currently at nearly 412 parts per million (ppm) and rising. This represents a 47 percent increase since the beginning of the Industrial Age, when the concentration was near 280 ppm, and an 11 percent increase since 2000, when it was near 370 ppm.

How much CO2 is in the atmosphere in 2022? ›

The atmospheric CO2 concentration increased 2.5 parts per million (ppm) in 2021 and is projected to increase by around 2.5ppm in 2022, resulting in global atmospheric concentrations of 417.2ppm on average for the year.

How do human activities contribute to climate change Brainly? ›

Human activities contribute to climate change by causing changes in Earth's atmosphere in the amounts of greenhouse gas- es, aerosols (small particles), and cloudiness. The largest known contribution comes from the burning of fossil fuels, which releases carbon dioxide gas to the atmosphere.

What is the trend on recent CO2 levels? ›

Coal accounted for over 40% of the overall growth in global CO2 emissions in 2021, reaching an all-time high of 15.3 billion tonnes. CO2 emissions from natural gas rebounded well above their 2019 levels to 7.5 billion tonnes.

Are CO2 levels higher now than ever before? ›

Carbon dioxide now more than 50% higher than pre-industrial levels | National Oceanic and Atmospheric Administration.

What are the most recent CO2 levels measured? ›

414.67 ppm

This table presents the most up-to-date, daily average reading for atmospheric CO2 on the planet. Units = parts per million (ppm). Measurement location = Mauna Loa Observatory, Hawaii.

How does increased CO2 affect the internal environment in our body? ›

Answer: CO2 levels are the main influence, oxygen levels only affect breathing with dangerously low. If CO2 levels increase, the respiratory center( medulla and pons) is stimulated to increase the rate and depth of breathing. This increases the rate of CO2, removal and returns concentrations to normal resting levels.

How many kg of CO2 do humans release per day? ›

In one day, the average person breathes out around 500 litres of the greenhouse gas CO2 – which amounts to around 1kg in mass.

How much CO2 does a person produce per minute? ›

A A healthy adult man who weighs about 154 pounds, or 70 kilograms, exhales 250 milliliters (thousandths of a liter) or a quarter of a liter of carbon dioxide every minute when he is at rest, according to Dr. John G.

How much CO2 is released daily? ›

We know that burning fuels releases carbon dioxide, and our own “fuel,” or the food we eat, is no different. We capture the energy from the food we eat and then release the carbon from that food into the environment. On average, we eat about 2,000 calories a day and release about 2 pounds of carbon dioxide a day.

How many ppm CO2 does a human breath? ›

All animals and humans inhale oxygen and exhale carbon dioxide. The carbon dioxide level in exhaled air about 3.8%, or 38,000ppm (parts per million). When carbon dioxide is exhaled it is quickly mixed with the surrounding air and, if the ventilation is good, the concentration is quickly reduced to harmless levels.

How much CO2 is removed by our lungs per hour? ›

The volume of air inspired or expired during normal respiration is defined as the tidal volume. The average tidal volume of a healthy human being is 500mL/min. Thus, the amount of carbon-di-oxide given out is 500mL/min.

Do we breathe out 100% CO2? ›

When we exhale, the composition of the air remains almost the same as the air we inhale, only the percentage of carbon dioxide and oxygen changes. The amount of inhaled air contains 21% of oxygen and 0.04% of carbon dioxide, while the air we breathe out contains 16.4% of oxygen and 4.4% of carbon dioxide.

What are three 3 examples of carbon emissions from human activity? ›

The main human activity that emits CO2 is the combustion of fossil fuels (coal, natural gas, and oil) for energy and transportation. Certain industrial processes and land-use changes also emit CO2.
Carbon Dioxide Emissions
  • Transportation. ...
  • Electricity. ...
  • Industry.
16 May 2022

What are the effects of carbon cycle on humans and in the environment? ›

The changes in the carbon cycle impact each reservoir. Excess carbon in the atmosphere warms the planet and helps plants on land grow more. Excess carbon in the ocean makes the water more acidic, putting marine life in danger.

How do human activities damage the environment and what are the consequences? ›

Humans impact the physical environment in many ways: overpopulation, pollution, burning fossil fuels, and deforestation. Changes like these have triggered climate change, soil erosion, poor air quality, and undrinkable water.

What three human activities produce the most greenhouse gases? ›

Globally, the primary sources of greenhouse gas emissions are electricity and heat (31%), agriculture (11%), transportation (15%), forestry (6%) and manufacturing (12%). Energy production of all types accounts for 72 percent of all emissions.

What human activity produces the most greenhouse gases? ›

The largest source of greenhouse gas emissions from human activities in the United States is from burning fossil fuels for electricity, heat, and transportation. EPA tracks total U.S. emissions by publishing the Inventory of U.S. Greenhouse Gas Emissions and Sinks.

How does burning fossil fuels affect the carbon in the atmosphere? ›

When fossil fuels are burned, they release large amounts of carbon dioxide, a greenhouse gas, into the air. Greenhouse gases trap heat in our atmosphere, causing global warming. Already the average global temperature has increased by 1C.

What information do scientists use to determine the relative proportion of atmospheric CO2 emitted from fossil fuels? ›

By examining the isotopic mixture in the atmosphere, and knowing the isotopic fingerprint of each reservoir, atmospheric scientists can determine how much carbon dioxide is coming and going from each reservoir, making isotopes an ideal tracer of sources and sinks of carbon dioxide.

How have scientists used isotopic analysis to determine that the rise of atmospheric CO2 is mostly from the burning of fossil fuels? ›

How have scientists used isotopic analysis to determine the rise of atmospheric CO2 is mostly from the burning of fossil fuels? The low proportions of 13C and 14C within atmospheric CO2 indicates the source is fossil carbon.

Why did the carbon dioxide levels rise and fall over the course of a year? ›

Levels of carbon dioxide in the atmosphere rise and fall each year as plants, through photosynthesis and respiration, take up the gas in spring and summer, and release it in fall and winter. Now the range of that cycle is expanding as more carbon dioxide is emitted from burning fossil fuels and other human activities.

What happens when carbon dioxide increases? ›

Carbon dioxide in the atmosphere warms the planet, causing climate change. Human activities have raised the atmosphere's carbon dioxide content by 50% in less than 200 years.

Which of the following environmental problems causes climate change? ›

Greenhouse Gases

These greenhouse gas emissions have increased the greenhouse effect and caused the earth's surface temperature to rise. Burning fossil fuels changes the climate more than any other human activity.

What happens if we stop using fossil fuels? ›

With the effects of anthropogenic climate change becoming increasingly impactful, it is clear that reversing them is largely preferable to stalling them. If we stopped using fossil fuels today, warming would certainly slow, but greenhouse gas removal from the atmosphere will need to happen eventually.

What methods are used to determine the amount of carbon dioxide in the atmosphere? ›

Carbon Dioxide (CO2) is measured with a gas sensor specifically made to measure the concentration of carbon dioxide (CO2) in the air. There are three main types of Carbon Dioxide (CO2) sensors: Electrochemical sensors, Non-Dispersive Infrared (NDIR) Sensors, and Metal Oxide Semiconductor (MOS) Sensors.

How do scientists measure past CO2 levels? ›

For this reason, scientists continuously measure the average level of CO2 in the atmosphere by sampling the air at several remote sites around the world, including one atop the Hawaiian volcano Mauna Loa. This site has tracked the level of carbon dioxide in the atmosphere since the 1950s.

How can scientists tell how much CO2 was in the ancient atmosphere? ›

In a new study, scientists have estimated carbon dioxide levels from the past 66 million years using two methods analyzing tiny organisms found in sediment cores from the deep seafloor, and found a consistent picture of the evolution of the ocean-atmosphere carbon dioxide levels.

Which technique is used for measurement of isotopic composition? ›

To tease out such isotope ratios, researchers typically use a technique called mass spectroscopy.

How do we know that carbon dioxide from fossil fuels has increased the total amount of atmospheric carbon dioxide? ›

Measurements of CO2 concentration in the atmosphere over time tell us that CO2 is increasing. Countries and industry use economic data to report how much fossil fuel they have burnt each year (such as can be seen above, in the graph on the left), and scientists calculate how much CO2 is produced from the fossil fuels.

What instrument is used to measure carbon dioxide in the atmosphere? ›

A carbon dioxide sensor or CO2 sensor is an instrument for the measurement of carbon dioxide gas. The most common principles for CO2 sensors are infrared gas sensors (NDIR) and chemical gas sensors.

Why does CO2 increase in fall and winter? ›

In spring, plants in the Northern Hemisphere begin to grow and absorb CO2 from the atmosphere, so atmospheric CO2 concentration decreases—the line dives down. In fall, plants begin to decay and release their CO2 back into the atmosphere, so atmospheric CO2 concentration increases—the line shoots up.


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Name: Fredrick Kertzmann

Birthday: 2000-04-29

Address: Apt. 203 613 Huels Gateway, Ralphtown, LA 40204

Phone: +2135150832870

Job: Regional Design Producer

Hobby: Nordic skating, Lacemaking, Mountain biking, Rowing, Gardening, Water sports, role-playing games

Introduction: My name is Fredrick Kertzmann, I am a gleaming, encouraging, inexpensive, thankful, tender, quaint, precious person who loves writing and wants to share my knowledge and understanding with you.