Analysis of the 2024 Southern Hemisphere Ozone Hole

Abstract

The 2024 Southern Hemisphere ozone hole lasted about five months, reached  a minimum temperature of 180 K on 8 August, with an area of 22 x 10⁶ km² on 28 September, with a minimum O₃ concentration of 107 Dobson units on 7 October.

The season's ozone hole, on the average, was 26^th out of 45 ranked by area, 24^th out of 45 ranked by depth, 24^th out of 45 ranked by mass deficit, 27^th out of 45 ranked by mean ozone concentration, and 24^th out of 45 ranked by mean temperature.

By these measures, the past year was an average one over the satellite era.

The world is on track to return the Antarctic stratosphere to pre-1980 levels by approximately 2076, were the general trend of decline to continue.

Data Sources

Normally, I would not start out with this section, but NOAA and NASA are both under attack by the right wing in the current [mis]administration.   NOAA monitors ozone-depleting substances worldwide. And NASA satellites monitor ozone. The future existence of the repositories of these data is in doubt. Thus is is not unlikely that, at some point in the not-too-distant future, a click here or there will result in a "404 error".

Introduction

This is a re-analysis of NASA Ozone Watch data for the Southern Hemisphere Ozone Hole. The 2024 antarctic ozone hole closed at the end of December, as is usual. The area (in 10⁶ km²)  of the ozone hole is shown in figure 1. As is readily observed, the hole emerged in the late Antarctic winter, mid-July and closed five months later by mid-December. The basic science of stratospheric ozone depletion is well understood. 

...the primary cause of ozone depletion is the presence of chlorine-containing source gases (primarily CFCs and related halocarbons). In the presence of UV light, these gases dissociate, releasing chlorine atoms, which then go on to catalyze ozone destruction.

Figure 1. SH Ozone hole area

 

The ozone hole is usually characterized by its area, depth, and temperature. These properties are illustrated in the following set of figures.

Figure 2 shows the evolution of the ozone hole area over the years of the satellite era. NASA states "The minimum ozone is found from total ozone satellite measurements south of 40°S. No interpolation of missing values is performed. This means that the actual minimum value on a day may be estimated too high, especially in the polar night region."

Figure 2. Ozone hole area near September maximum

 

Figure three shows the mean amount of Antarctic stratospheric ozone in Dobson Units (DU). 

The Dobson unit is defined as the thickness (in units of 10 μm) of that layer of pure gas which would be formed by the total column amount at standard conditions for temperature and pressure (STP). This is sometimes referred to as a 'milli-atmo-centimeter'. A typical column amount of 300 DU of atmospheric ozone therefore would form a 3 mm layer of pure gas at the surface of the Earth if its temperature and pressure conformed to STP.  

The annual record is shown and compared with that over the satellite era. Note that the 2024 ozone hole was quite close to the satellite era mean, aside from a short-lived decrease in November 2024.

Figure 3. The mean ozone, found from
total ozone satellite measurements south of 40°S. 

Figure three shows the mean amount of Antarctic stratospheric ozone in DU. Note the pronounced minimum at the Antarctic spring remains quite pronounced,  reaching a low of 109 DU.  In this author's opinion, this behavior is not that of an atmosphere healed from the damage of ozone depleting substances.

Figure 4. The minimum ozone
 

Figure 5 shows the temperature of the stratosphere at a pressure of 10 hPa, an altitude of approximately 30 kilometers,  averaged around the polar cap for latitudes south of 60°S. NOAA states "This is a good measure of the overall temperature in the polar vortex." Note the temperatures for the formation of type I and type IIU polar stratospheric clouds (PSC), "composed of mostly supercooled droplets of water and nitric acid and is implicated in the formation of ozone holes." Once again, these data are quite close to the mean over the satellite era.

Figure 5. The 10 mPa temperature in Kelvin (K)
averaged for 55°S to 75°S.

Figure 6 shows the mass deficit of antarctic stratospheric ozone. From NASA's ozone watch site: 

The ozone mass deficit is determined from total ozone satellite measurements. It combines the effects of changes in area and depth. It is the total amount of mass that is deficit relative to the amount of mass present for a value of 220 Dobson Units (DU). 

This mass deficit reached a peak of 28.20 Megaton ozone in mid-September, slightly higher than the mean over the satellite era.  

Figure 6. Mass deficit of antarctic stratospheric ozone (Megatons) 

 

The causes of stratospheric ozone depletion were deduced by Paul J. Crutzen, Mario J. Molina and F. Sherwood Rowland, who were jointly awarded The Nobel Prize in Chemistry in 1995 "for their work in atmospheric chemistry, particularly concerning the formation and decomposition of ozone."

From the EPA:

When chlorine and bromine atoms come into contact with ozone in the stratosphere, they destroy ozone molecules. One chlorine atom can destroy over 100,000 ozone molecules before it is removed from the stratosphere. Ozone can be destroyed more quickly than it is naturally created.

Some compounds release chlorine or bromine when they are exposed to intense UV light in the stratosphere. These compounds contribute to ozone depletion, and are called ozone-depleting substances (ODS). ODS that release chlorine include chlorofluorocarbons (CFCs), hydrochlorofluorocarbons (HCFCs), carbon tetrachloride, and methyl chloroform. ODS that release bromine include halons and methyl bromide. Although ODS are emitted at the Earth’s surface, they are eventually carried into the stratosphere in a process that can take as long as two to five years.

These and similar substances are tracked by NOAA, which has developed and maintained an annual "Ozone Depleting Substance Index":

The ODGI is estimated directly from observations at Earth’s surface of the most abundant long-lived, chlorine and bromine containing chemicals whose production and consumption is controlled by the Montreal Protocol (15 individual chemicals). These ongoing, surface-based observations provide a direct measure of nearly all of the chlorine and bromine atoms in the lower atmosphere, or troposphere, contained in chemicals with lifetimes longer than approximately 0.5 yr. Because the lower atmosphere is quite well-mixed, these observations also provide an accurate estimate of the amount of chlorine and bromine entering the stratosphere from these chemicals.

The ODGI is shown in figure eight, "calculated for the Antarctic and mid-latitude stratosphere. As before, the ODGI derived directly from the Equivalent Effective Stratospheric Chlorine (EESC) determined from our atmospheric observations at remote surface sites". The mid-latitude index is seen to have peaked in 1997 and decreased to half its maximum in 2021, clear evidence of the success of the Montreal Protocols.

Figure 8. The Ozone Depleting Gas Index (ODGI) vs. time 

 

Figure nine, also from NOAA, shows past and projected future changes in reactive halogen concentrations in the atmosphere.  

Past concentrations are derived from NOAA measurements of both chlorine- and bromine-containing chemicals; “WMO scenarios” are from the WMO/UNEP 2018 Ozone Assessment, which are tied to NOAA observations in the past and, for the future, assume full adherence to controls on production and consumption of ODSs in the fully revised and amended Montreal Protocol (Carpenter and Daniel et al., 2022). Measured tropospheric changes are indicated with dashed curves and points, while inferred stratospheric changes are indicated as solid curves. Estimates are provided for different regions: the mid-latitude stratosphere and the Antarctic stratosphere. The down-pointing arrows represent the estimated dates that concentrations of stratospheric halogen will return to the benchmark levels present in 1980.

Figure 9. Past and projected future changes in reactive
halogen concentrations in the atmosphere.

Of course, the ultimate measure of the success of these policies and treaties is the improvement in human health. Here are some data from the Ozone Secretariat of the United Nations Environment Programme:

The Montreal Protocol has prevented large increases in surface UV-B radiation, with greatest benefits at high latitudes. Modelling studies indicate that without the Montreal Protocol, at northern and southern latitudes of less than 50° the ultraviolet index (UVI), which indicates the intensity of UV radiation with respect to sunburn, would have increased by 10-20% between 1996 and 2020. This would have increased by 25% at the southern tip of South America and by more than 100% at the South Pole in springtime.

In the United States, full implementation of the Montreal Protocol is expected to prevent approximately 443 million cases of skin cancer, 2.3 million skin cancer deaths, and 63 million cases of cataracts for people born in the years 1890–2100, according to the US Environmental Protection Agency.

Would-be dictator names three climate deniers to Energy Department

 I will not link to the news sources for this story, but I do have an image of the three new hires, who do seem to have a reputation for snake oil peddling.

The Antarctic stratospheric ozone hole in 2024

by OnymousGuy

Abstract

The data says 2024 was pretty average, and "far from being fully healed", but NASA's press office says "relatively small". So which is it? "Relatively small", or "far from being fully healed"?

Background

We are approaching the end of season for this year's Antarctic stratospheric ozone hole, as the increasing springtime sunlight stimulates the Chapman cycle to produce more ozone. 

NASA's ozone watch documents the status of the Antarctic stratospheric ozone hole, with updates about every week or so, but less frequently at the end of the season. Certain parameters are tracked:

The data for the ozone hole area, the minimum ozone, and the minimum stratospheric temperature are available. Also available is a table of values showing the maximum ozone hole area and the minimum ozone values for each year...

The graphs ... show the progress of the ozone hole for 2024. The gray shading indicates the highest and lowest values measured since 1979. The red numbers are the maximum or minimum values. The stratospheric temperature and the amount of sunlight reaching the south polar region control the depth and size of the Antarctic ozone hole. The dashed line in the minimum temperature plot indicates the temperature below which Type I (NAT) PSCs can form. 

Ozone concentrations are reported in Dobson units.

The Dobson Unit (DU) is the unit of measure for total ozone. If you were to take all the ozone in a column of air stretching from the surface of the earth to space, and bring all that ozone to standard temperature (0 °Celsius) and pressure (1013.25 millibars, or one atmosphere, or “atm”), the column would be about 0.3 centimeters thick. Thus, the total ozone would be 0.3 atm-cm. To make the units easier to work with, the “Dobson Unit” is defined to be 0.001 atm-cm. Our 0.3 atm-cm would be 300 DU. 

Here are some recent images.

• ozone hole area, minimum ozone, minimum stratospheric temperature,

• annual maximum ozone hole area, annual minimum ozone.

Here is a recent false color image of the ozone hole. 

Discussion

From these figures, I would say that the 2024 ozone hole has been pretty close to its average over the satellite era. So I was a bit surprised to read this puffery from NASA:

Healing continues in the atmosphere over the Antarctic: a hole that opens annually in the ozone layer over Earth's southern pole was relatively small in 2024 compared to other years. 

During the peak of the ozone depletion season from Sept. 7 through Oct. 13, the 2024 area of the ozone hole ranked the seventh smallest since recovery began in 1992, when the Montreal Protocol, a landmark international agreement to phase out ozone-depleting chemicals, began to take effect...

The improvement is due to a combination of continuing declines in harmful chlorofluorocarbon (CFC) chemicals, along with an unexpected infusion of ozone carried by air currents from north of the Antarctic, scientists said. 

A little bit of realism creeps into the blurb from NASA, lower down in the press release.

In previous years, NASA and NOAA have reported the ozone hole ranking using a time frame dating back to 1979, when scientists began tracking Antarctic ozone levels with satellite data. Using that longer record, this year's hole ranked 20th smallest in area across the 45 years of observations.

IMO, 20th out of 45 sounds pretty average. One of the GML scientists spills the beans:

"For 2024, we can see that the ozone hole's severity is below average compared to other years in the past three decades, but the ozone layer is still far from being fully healed," said Stephen Montzka, senior scientist of the NOAA Global Monitoring Laboratory.

So which is it? "Relatively small", or "far from being fully healed"?

Ozone Depleting Substances

The ozone hole, of course, depends on the concentration of stratospheric chlorine and bromine; sources of atomic Cl and Br in the stratosphere are called ozone depleting substances. The Trump administration excised EPA information about ozone depletion and the like, so one must look to the European Union for such things.

A compound that contributes to stratospheric ozone depletion. Ozone-depleting substances (ODS) include CFCs, HCFCs, halons, methyl bromide, carbon tetrachloride, and methyl chloroform. ODS are generally very stable in the troposphere and only degrade under intense ultraviolet light in the stratosphere. When they break down, they release chlorine or bromine atoms, which then deplete ozone.

These species have one thing in common: they contain halogens, specifically chlorine or bromine. Each halogenated compound is associated with an ozone-depleting potential (ODP), a direct measure of its ability to destroy ozone. More from the EU:

The ozone-depleting potential (ODP) of a substance refers to the relative amount of ozone depletion caused by it. It is the ratio of the impact on ozone of the emission of a chemical substance to the impact of a similar emission by mass of CFC-11. The quantity in metric tonnes of a particular controlled substance is multiplied by its ODP to give its overall potential to deplete the ozone layer. For instance, 1 metric tonne of CFC-11 corresponds to 1 ODP tonnes (as its ODP is equal to 1), whilst for bromotrifluoromethane or halon 1301 (with an ODP = 10), 1 metric tonne corresponds to 10 ODP tonnes. The ODPs of controlled and new substances are listed in Annexes I and II of the Ozone Regulation (Regulation (EC) No 1005/2009). Some new substances have a range, rather than a single ODP value. In this online data viewer, the highest value of the ODP value range is used.

What are the current levels of atmospheric chlorine? NOAA's Global Monitoring Laboratory reports this trend.

It seems that the most that one could say, based on the data, is that mid-latitude amounts of ozone-depleting substances have dropped below half of their pre-Montreal Protocol maximum. Yes, the world is still on track to see Antarctic  mounts of ozone-depleting substances have dropped below half of their pre-protocol maxima by 2076 or so, provided that we remain vigilant in observing the protocols and their amendments. HCFCs are the issue.

And then NOAA scientists weigh in on the minimum.

NOAA scientists also release instrumented weather balloons from the South Pole Baseline Atmospheric Observatory to observe ozone concentrations directly overhead in a measurement called Dobson Units. The 2024 concentration reached its lowest value of 109 Dobson Units on October 5. The lowest value ever recorded over the South Pole was 92 Dobson Units in October 2006.

NASA and NOAA satellite observations of ozone concentrations cover the entire ozone hole, which can produce a slightly smaller value for the lowest Dobson Unit measurement.

"That is well below the 225 Dobson Units that was typical of the ozone cover above the Antarctic in 1979," said NOAA research chemist Bryan Johnson. "So, there's still a long way to go before atmospheric ozone is back to the levels before the advent of widespread CFC pollution." 

There you have, at the very end of the puff piece: "There's still a long way to go before atmospheric ozone is back to the levels before the advent of widespread CFC pollution."

Putting current radiative forcing in context

Guest post by Jim

Abstract

Current radiative forcing from all greenhouse gases, omitting aerosols from nonmetal oxides and the like, is now just under 3.5 W/m², with an Annual Greenhouse Gas Index of about 1.52. This represents approximately 1.5% of average surface insolation.  Unlike solar energy, which rises and falls with the sun, this infrared energy captured from the earth itself accumulates second by second, day and night.

How significant is this? Consider this analogy. A typical adult on a 2000 kcal/day diet ingesting daily 1.5% calories in excess will gain 31 pounds per decade, with profound consequences. Now we have been burning fossil fuels at the same high rate as our over-eater for more than two decades. How can we possibly imagine that the consequences for the planet will be less severe?

Background

My most recent re-analysis of NOAA's greenhouse gas data stated that the current Annual Greenhouse Gas Index (AGGI) stood at 1.5177, on the scale where the 1990 AGGI is set to one.

NOAA's data from 1990 reported that total forcing was 2.301 W/m², so an AGGI of 1.5177 corresponds to radiative forcing of 3.492 W/m². This is the amount of energy emitted by the earth (which glows in the infrared) and captured by greenhouse gases in the atmosphere over each square meter of the earth's surface, each second. How does this compare to the energy from the sun?

The accompanying figure is from Total Solar Irradiance CDR, at the National Centers for Environmental Information, part of NOAA. It shows Total Solar Irradiance (TSI) at the top of the atmosphere, scaled to a uniform distance from the sun.

"The Total Solar Irradiance (TSI) Climate Data Record (CDR) measures the spectrally integrated energy input to the top of the Earth's atmosphere at a base mean distance from the Sun (i.e., one Astronomical Unit)."

There are a couple of things worth noting. First, TSI over the satellite era (1979-present) is almost constant, roughly 1362 W/m², clearly negating the denialisti claims that "It's the sun!". Second, historic reconstructions of TSI over the last four centuries show that variations in TSI average about 0.5 W/m², so an increase in radiative forcing of just 1W/m² is larger than most variations in the TSI signal. An increase of 3.5 W/m² is far larger than the usual variation.

Since the earth is nearly a sphere of radius R, its surface area, approximately 4πR² , is about four times its circular cross-section, about πR². So insolation - sunlight energy falling on each unit of area - over the entire globe is about one fourth that directly under the sun, (1362/4) W/m² . This implies that the average global insolation at the top of the atmosphere is about 340.5 W/m². At the surface, this is further reduced by the albedo (reflectivity) of the earth.

The American Meteorological Society sums up the current estimates of planetary albedo:

On the average, the earth reflects 31 units of solar radiation back to the space for every 100 units received (thus, the total earth albedo is 0.31). The cloud albedo accounts for 23 units of the 31. For individual clouds, local albedo may be in excess of 0.7.

So only 69% of that 340.5 W/m², about 235 W/m², hits the earth's surface. The radiative forcing from all greenhouse gases, except the short-lived species such as ozone, SOx, or NOx, is 3.492 W/m², about 1.486% of average surface insolation. Unlike solar energy, this  infrared energy captured from the earth itself accumulates second by second, day and night.

Comparison with diet

To see what impacts this energy has on the planet, let's look at the effects of over-eating on a typical adult who maintains a healthy weight with a 2000 kcal/day diet. That same percent, 1.486%, of their daily calorie intake is 29.7 kcal/day, almost the same as the energy content of 4 g of butter, a scant teaspoon. As we all come to know sooner or later, excess calories are stored in the body as fat, roughly 3500 kcal per pound of fat. This overeating will lead to weight gain, roughly one pound every 118 days, about 3.1 pounds each year, year after year. 

A decade of this overeating leads to a gain in weight of about 31 pounds. This will make that adult at least overweight, if not obese.  The CDC states

Obesity in children and adults increases the risk for the following health conditions:

• High blood pressure and high cholesterol which are risk factors for heart disease.
• Type 2 diabetes.
• Breathing problems, such as asthma and sleep apnea.
• Joint problems such as osteoarthritis and musculoskeletal discomfort.
• Gallstones and gallbladder disease.

Two decades will make them class III obese (formerly known as morbidly obese), if not worse. The Cleveland Clinic advises

"If left untreated, class III obesity may shorten life expectancy up to 14 years. In addition to contributing to potentially serious health problems, class III obesity is associated with reduced economic and social opportunities and reduced quality of life."

As stated in the abstract, we have been burning fossil fuels at the same high rate as our over-eater for more than two decades. How can we possibly imagine that the consequences for the planet will be less severe?

Current Composition of the Atmosphere, November, 2024

Guest post by Jim

NOAA has once again released its monthly updates to CO₂, CH₄, and N₂O. See the data section for each gas. 

https://gml.noaa.gov/ccgg/

Here are the updated results. Little has changed. By 2030 the atmosphere will have such a high concentration of greenhouse gases that the effective radiative forcing will be  twice that of the pre-industrial era. 

The 2x crossing is now estimated to occur 1 April, 2030 (no joke!), give or take a month; changes in this estimate over the last year are more likely due to month-to-month fluctuations, not long term changes in trends.

Here is the combination of historic data, satellite era data, and the most recent updates from NOAA:

 

What could possibly go wrong?

 Source:https://www.dailykos.com/stories/2024/11/11/2284411/-Cartoon-Over-the-cliff

Recent trends in atmospheric methane.

A guest post from Jim

Over the last year, the global increases in methane emissions have begun to raise alarms.

Here's a brief sample:

• Sarah Kaplan's report in the Washington Post, reporting 10 Sept 2024, "Emissions of methane — a powerful greenhouse gas — are rising at the fastest rate in recorded history, scientists said Tuesday, defying global pledges to limit the gas and putting the Earth on a path toward perilous temperature rise."
• The European Space Agency's post, also on 10 Sept 2024, "The Global Methane Budget 2024 paints a troubling picture of the current state of global methane emissions. The new report reveals that human activities are now responsible for at least two-thirds of global methane emissions. This marks a significant increase in human-produced methane sources over the past two decades, with emissions rising by 20%, with the fastest rise occurring over the last five years."
• NOAA's summary of 5 Apr 2024, No sign of greenhouse gases increases slowing in 2023, reports that "Atmospheric methane, less abundant than CO2 but more potent at trapping heat in the atmosphere, rose to an average of 1922.6 parts per billion (ppb). The 2023 methane increase over 2022 was 10.9 ppb, lower than the record growth rates seen in 2020 (15.2 ppb), 2021(18 ppb)  and 2022 (13.2 ppb), but still the 5th highest since renewed methane growth started in 2007. Methane levels in the atmosphere are now more than 160% higher than their pre-industrial level,"

Climate bloggers have begun to notice. For example, here's David Appell at Quark Soup: 

"I haven't followed methane much because I couldn't find a good data source, but now I have, from NASA. And even better source is the Global Carbon Project, which is updated every 7.6 days. 

After that weird lull in the mid-aughts, methane is on the rise again and is the highest it's been in 800,000 years.   

Methane's radiative forcing has increased by about 0.4 W/m^2 since 1979, while CO2's has jumped about 1.6 W/m^2 in the same interval...

It's incredible that the world, despite all the rhetoric and (token) efforts, keeps allowing this to happen. Clearly, I think, these trends will only be taken seriously once some catastrophic effects happen, and by then it will be too late. So human and we can't even help ourselves."

The Global Carbon Project's methane budget links to recent publications:

• " The primary reference ...(pre-print) Global Methane Budget 2000–2020 Here's an excerpt from the abstract: "Understanding and quantifying the global methane (CH4) budget is important for assessing realistic pathways to mitigate climate change. Emissions and atmospheric concentrations of CH4 continue to increase, maintaining CH4 as the second most important human-influenced greenhouse gas in terms of climate forcing after carbon dioxide (CO2). The relative importance of CH4 compared to CO2 for temperature change is related to its shorter atmospheric lifetime, stronger radiative effect, and acceleration in atmospheric growth rate over the past decade, the causes of which are still debated. "
• Additional Analyses for Methane Budget 2024:Human activities now fuel two-thirds of global methane emissions. "Methane is rising faster in relative terms than any major greenhouse gas and is now 2.6-fold higher than in pre-industrial times. Global average methane concentrations reached 1931 parts per billion (ppb) in January of 2024 (Lan et al 2024). Annual increases in methane are also accelerating for reasons that are debated..." 

With these in mind, let's look at recent trends in methane from NOAA's Global Monitoring Laboratory

Here is a graph of global methane (as ppm CO₂ equivalent) since 2000.

We can remove the monthly variations to look at the underlying trend by doing a moving twelve-month average. Most of the variations have been averaged out. Here's the result:

 

A glimpse at the raw data reveals that the annual rate of change of global atmospheric methane has been monotonically positive since 2005. These data are well-approximated by a quadratic polynomial. The error in the quadratic fit to the twelve month moving average of the observed data for atmospheric methane (in ppm CO₂ eq) ranges from -0.140411 ppm to 0.113803 ppm with an rms error 0.0665136 ppm, a percent error less than 0.21%.

This graph shows the raw methane as ppm CO₂ equivalent (in black), its twelve-month moving average (in yellow), and the moving average's best fit quadratic (in blue). 

Removal of the seasonal variation in methane does not eliminate all of the short term departures from the best fit quadratic. The remaining fluctuations appear to have a period of about seven years. It is not clear what is the underlying physical processes responsible for this variation but it appears quite regular.

Seasonal variations, in methane, removed by the moving average, account for a difference of about 0.14 ppm CO₂ eq, less than 0.4% of the annual average. Long-term variations in the moving average methane, compared to the quadratic fit, account for another difference of about 0.067 ppm CO₂ eq, less than 0.2% of the annual average. Seasonal variations account for about 80% of the total variance between the quadratic model and the observed data.

In summary, the increase in methane is well approximated by a quadratic fit to the twelve-month moving average of emissions; we project that methane emissions will rise from 33.08 ppm CO₂ eq in 2005 to about 37.37 ppm CO₂ eq in 2025, an increase of 12.9% over only two decades. 

The International Energy Agency writes,"Methane has a much shorter atmospheric lifetime than CO2 (around 12 years compared with centuries for CO2), but it is a much more potent greenhouse gas, absorbing much more energy while it exists in the atmosphere...The Intergovernmental Panel on Climate Change (IPCC) has indicated a GWP for methane between 84-87 when considering its impact over a 20-year timeframe (GWP20) and between 28-36 when considering its impact over a 100-year timeframe (GWP100). This means that one tonne of methane can considered to be equivalent to 28 to 36 tonnes of CO2 if looking at its impact over 100 years."

Methane emissions are currently increasing annually by a relative rate of about 0.95%, clearly a serious situation.

Current Composition of the Atmosphere, September, 2024

Guest post by Jim

NOAA has once again released its monthly updates to CO₂, CH₄, and N₂O. See the data section for each gas. 

https://gml.noaa.gov/ccgg/

Here are the previous results.

Here are the updated results; changes are more likely due to month-to-month fluctuations, not long term changes in trends:

Here are recent month to month variations from the moving average and its best fit.The crossing is now estimated to occur early March, 2030, give or take a month.

Here is the combination of historic data, satellite era data, and the most recent updates from NOAA: