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Showing posts with label Greenhouse Gas. Show all posts
Showing posts with label Greenhouse Gas. Show all posts

Tuesday, April 26, 2022

Charts of Atmospheric CO2, Carbon Isotopes, Oxygen and Methane

 I started making charts of atmospheric CO2 in 2009, when the global average CO2 concentration was 386 ppm.  I updated my charts in 2012, at 392 ppm, and in 2017, at 405 ppm, and at the end of 2021, at 418 ppm. 

The monitoring stations are located from the far north, at 82° N in Canada to the South Pole.  Scripps Institute has managed most of these stations since the 1950s, first under the direction of Charles Keeling, and later under his son, Ralph Keeling.  I also included records from a few obsolete legacy stations that were operated by foreign governments.  I standardized my chart displays using cool colors to represent the Northern Hemisphere, and warm colors for the Southern Hemisphere.

The amplitude of the CO2 seasonal cycle varies with latitude, from high amplitude in far northern latitudes to very little amplitude at the South Pole.  The seasonal cycle is driven by seasonal plant growth and decay on lands with temperate climate, which are concentrated in the Northern Hemisphere.  Agriculture, which is also concentrated in the Northern Hemisphere, also contributes to the seasonal cycle.  I took advantage of this for my standard display, overlaying low amplitude over higher amplitude traces, so that all traces can be seen.

In general, CO2 concentration in the atmosphere is growing exponentially, a fact noted by Isaac Asimov in 1959.  In 2009, I made an exponential function, beginning at the pre-industrial CO2 concentration of 280 ppm in 1800, with an eyeball-fit to the data from 1957 to 2009.  Here’s the function, and the chart beginning in 1800, updated with CO2 data through 2021.  This chart has the “hockey stick” impression that characterizes many climate-change charts.

CO2 concentration, ppm = e(n*0.001854) + 280, where n = the number of months since Jan. 1800

This function would predict that global CO2 would pass 450 ppm in January, 2032 (ten years from now), and pass 500 ppm in August, 2043.

The exponential function seems to be slightly overstating the rate of CO2 growth since 2009, so I tried an alternate formula for the forecast in coming decades, a second-degree polynomial with a least-squares fit to the global average CO2 from 1974 to 2009.  That formula is CO2 in ppm = 0.000104*x2+0.0897*x+331.66, where x is the number of months from July, 1974.  This formula predicts global CO2 will pass 450 ppm in June, 2034, and pass 500 ppm in July, 2050. 

Certainly, these forecasts are simple extrapolations, and include none of the analysis of policies and economics which should be the basis of forecasting.  But it’s worth noting that my exponential forecast from 13 years ago is pretty much right on the money, overshooting by only one or two parts per million.  The last thirteen years has seen unprecedented growth in renewable energy technologies, but so far without significant impact on the rate of CO2 growth.  Here are the two forecasts on the same chart.


The seasonal cycle can easily be filtered from the data, leaving the long-term trend at each station.  From this, it’s easy to see that the Northern Hemisphere leads the Southern Hemisphere in rising CO2.  About 90% of fossil fuel burning happens in the Northern Hemisphere, and CO2 accumulates in the far north, while dispersing to the south. 

The difference in concentration from the far north to the South Pole has been increasing as larger volumes of fossil fuels are burned each year, from about 3 ppm in the 1980s to over 5 ppm now.  The chart below shows the difference in the one-year time-averaged CO2 concentration measured in Alert, Canada, at latitude 82° North, and the South Pole. 

The amplitude of the seasonal cycle has also been increasing in the far north.  The amplitude of the cycle increased from 15 ppm to 20 ppm since the mid-1970s.  This probably reflects increased agriculture and farm productivity in the Northern Hemisphere as world population has doubled.  Previous work showed that seasonal fossil-fuel use is volumetrically inadequate to produce the change in the atmospheric CO2 seasonal cycle.  https://dougrobbins.blogspot.com/2012/04/modeling-global-co2-cycles.html

Carbon comes in two common naturally occurring isotopes, C12 and C13.  Various processes, including life processes, sort the isotopes, favoring the accumulation of one or the other isotope.  Photosynthesis favors C12, so everything with carbon derived from plants, including lumber, your mashed potatoes, you, me, and fossil fuels is enriched in C12.  Scientists use a measure of the C13/C12 ratio written as d13C , and called delC13.  As fossil fuels are burned the C12-enriched carbon in CO2 changes the ratio of these isotopes in the atmosphere, lowering the value of delC13.  DelC13 continued to fall from 2009 to 2021, reflecting a growing fraction of carbon from fossil fuels in the atmosphere. 

Carbon isotopes in the atmosphere are also affected by the seasonal cycle of plant growth on the temperate land mass of the Northern Hemisphere.  As plants grow during the northern summer, the lighter isotope C12 is preferentially removed from the atmosphere, and returned during the winter months as plants decay.

After filtering the seasonal cycle, we see that the Northern Hemisphere leads the Southern Hemisphere in falling DelC13.  As an aside, the residual fluctuations in the trend have a strong correlation to the Oceanic Nino Index (ONI), reflecting sea surface temperatures in the Pacific.  https://dougrobbins.blogspot.com/2013/11/carbon-isotopes-in-atmosphere-part-ii.html

Interestingly, if all of the carbon released by fossil fuels stayed in the air, the DelC13 value would be much lower, about -13, instead of -8.5.  The measured dilution of carbon with the isotope signature of fossil fuels provides a way of estimating the volume of all carbon reservoirs exchanging carbon with the atmosphere.  Currently, the reservoirs freely exchanging carbon with the atmosphere have a carbon mass of about 5200 gigatonnes, before accounting for additional carbon in the system from new burning of fossil fuels.  That’s about 6 times the mass of carbon currently in the atmosphere.  https://dougrobbins.blogspot.com/2013/11/how-big-is-carbonsphere.html

Atmospheric oxygen is also influenced by burning of fossil fuels.  Oxygen is consumed, causing atmospheric O2 to fall.  The atmosphere is about 21% oxygen, and the decline is only about 0.08%, so there is no threat to breathing.  Still, the decline can be measured precisely.  The decline in oxygen is reported in units per meg, which is equivalent to ppm in this range of values.

After filtering the seasonal cycle, we see that the Northern Hemisphere leads the Southern Hemisphere in oxygen decline, because most fossil fuels are burned in the Northern Hemisphere.  The total volume of oxygen decline is very close to the expected consumption of oxygen considering the reported volumes of fossil fuels burned and deforestation, as reported in this previous post.  https://dougrobbins.blogspot.com/2019/12/understanding-source-of-rising.html

Atmospheric methane (C4) is also increasing as a result of human emissions.  Methane is a much more powerful greenhouse gas than CO2, but has a shorter lifespan.  CO2 has a half-life of 120 years, while methane has a half-life of about 10 years.  This is why the climate scientists use the parameter GWP (global warming potential) to represent the different strength of various greenhouse gases over an effective time frame.  The GWP of CO2 equals 1, by definition, for all time intervals.  For methane, the warming potential over 20 years (GWP-20) is 84 – 87, and over 100 years is 28 – 36.  Over shorter intervals, methane is an even stronger greenhouse gas.  Currently, methane concentration in the atmosphere is about 1.9 ppm (i.e. 1900 ppb).  In absolute terms, methane warmed the earth by about 0.52 W/m2, compared to 2.11 W/m2 for CO2, for the latest year reported by NOAA, 2020.  All other greenhouse gases combined contributed another 0.55 W/m2.  Methane also has a seasonal cycle in both hemispheres with high values in the summer and low values in the winter, but I don’t know the explanation for the seasonal cycle. 

As the concentrations of CO2 and methane in the air rise, the atmosphere will absorb heat at a faster rate, leading to destructive climate change.  Temperatures and climate change will not stabilize until carbon emissions reach zero.  I will update my charts on carbon emissions when summary data for 2021 is released in the BP Statistical Summary of World Energy in July.  Apart from a small pandemic-related decline in emissions in 2020, the world continues to add CO2 to the atmosphere at an ever-increasing rate.  If the world had acted to reduce emissions three decades ago, simply reducing emissions might have been a reasonable policy.  However, in our current situation, outright elimination of carbon emissions is required to avoid some level of catastrophic consequences. 

Globally, we need to reduce emissions to 50% by 2035, and to zero some time between 2050 and 2070.  I am very pessimistic that we have the public understanding or political will to reach these goals.  As Bill Gates wrote in 2021, "To avoid a climate disaster, we have to get to zero greenhouse gas emissions….The case for zero was, and is, rock solid.  Setting a goal to only reduce our emissions—but not eliminate them—won’t do it.  The only sensible goal is zero.”

References:

CO2, CO2 carbon isotopes, oxygen and methane data, including obsolete CO2 stations

https://scrippsco2.ucsd.edu/data/atmospheric_co2/sampling_stations.html

https://scrippso2.ucsd.edu/data.html

https://gml.noaa.gov/dv/data/

https://data.ess-dive.lbl.gov/view/doi:10.3334/CDIAC/ATG.015

https://www.osti.gov/dataexplorer/biblio/dataset/1409297

https://carbonmapper.org/data/

Isaac Asimov, "No More Ice Ages?" prediction and commentary on global warming,
in Fantasy and Science Fiction, Jan. 1959, republished in Fact & Fancy, 1962 and Asimov on Chemistry, 1974. 

Global Warming Potential

https://www.epa.gov/ghgemissions/understanding-global-warming-potentials#:~:text=Methane%20(CH4)%20is%20estimated,uses%20a%20different%20value.).

GWP-20 for methane = 84 to 87; GWP-100 for methane = 28 to 36 (also reported as 25)

Radiative Forcing for various greenhouse gases

https://gml.noaa.gov/aggi/aggi.html

Saturday, July 20, 2019

Key References for Understanding Climate Change


Here are key references for understanding the cause and evidence for global warming and climate change. Also included are references for some of the consequences with a focus on Alaska.   Some of the references link to primary data (such as atmospheric data at Scripps); some assembly may be required.

CO2 Emissions
Boden, Marland & Andres, Global and National Fossil Fuel CO2, 2017
BP Statistical Review of World Energy (annual fossil fuel CO2 emissions, by nation & type)
U.S. Energy Information Agency, Data Tables, U.S. Energy Information Agency, Office of Energy Analysis, U.S. Department of Energy, Washington D.C. data tables, 2014
Houghton 2008 (CO2 emissions from land use changes)
Burton, 2013 (volcanic CO2 emissions)
Lee 2016 (volcanic CO2 emissions)
EIA World CO2 Emissions Forecast to 2050, International Energy Outlook 2017
Forecast CO2 Emissions by Region
ForecastCO2 Emissions by Fuel Type – select appropriate table.

Atmospheric CO2
Global CO2 and del C13 isotopes. http://scrippso2.ucsd.edu/cosub2sub-data
Global O2.   http://scrippso2.ucsd.edu/  
Formerly available at CDIAC. https://cdiac.ess-dive.lbl.gov/

Heat Retention by Greenhouse Gases
Tyndall, 1861, 1872, cited in Arrhenius, 1906.
Arrhenius, 1896, On the Influence of Carbonic Acid in the Air upon the Temperature on the Ground
Arrhenius, 1906, The Probable Cause of Climate Fluctuations http://www.friendsofscience.org/assets/documents/Arrhenius%201906,%20final.pdf
NOAA Greenhouse Gas Index.  Page includes formulas for predictive calculation of radiative forcing as function of concentration, and a table for historical annual radiative forcing for major greenhouse gases.
IPPC 5th Assessment Report, Anthropogenic Effective Radiative Forcing history, pp 1404 – 1409.
Table includes historical radiative forcing for greenhouse gases, and negative radiative forcing for cooling anthropogenic emissions. 
Trenberth, et al, 2009, Earth’s Global Energy Budget. 
Ramaswamy, et al 2001, Radiative Forcing of Climate Change.

Ocean Heat Content

Melting Ice
National Snow and Ice Data Center
NASA Global Ice Viewer
Global Cryosphere Watch
Antarctic and Greenland
Gravity measure of Antarctic and Greenland Ice Loss
IMBIE: Ice Sheet Mass Balance Inter-Comparison Exercise
Antarctic and Greenland Ice-loss data preceding NASA GRACE mission.
NASA Ice-Bridge Project
Arctic Sea Ice
Polar Science Center
Chart with relative volume loss (km3) 1980 – 2018.
Sequential maps of Arctic sea ice extent and thickness.
Sea Ice Data Portal
NOAA Arctic Report Card
Continental Glaciers
World Glacier Monitoring Service
WGMS Global Glacier Change Bulletin 2013
Zemp et al, 2019, Global glacier mass changes and their contributions to sea-level rise from 1961 to 2016.
Permafrost
Pacific Marine Environment Laboratory, NOAA
UAF Geophysical Institute
Jorgenson, 2006, Abrupt Increase in Permafrost Degradation in Arctic Alaska
USGS, Alaska’s Thawing Permafrost

Warming Surface Temperature

General Climate Change
Climate Dashboard, Climate.gov
IPCC Fifth Climate Assessment, 2013
IPCC Fifth Climate Assessment 2013, Executive Summary, 2013
Fourth National Climate Assessment, Vol. I and II, 2014
Key findings of the 4th National Climate assessment, organized by topic and by region. https://nca2014.globalchange.gov/highlights#section-5683
NASA Climate Change
JPL Satellite Data & Climate Models, Earth’s Energy Balance, Oceans & Ice, Carbon & Water
NOAA Climate Change
National Climate Data Center/NOAA
NOAA Sea Level Rise Viewer
USGS
European Space Agency Climate Work
World Meteorological Organization, Global Climate Observing System

Sea Level
Lambeck et al, 2014, Sea level and global ice volumes from the Last Glacial Maximum to the Holocene
R. Rohde, K. Fleming, Post-Glacial Sea Level
NASA Sea Level
Zemp et al, 2019, Global glacier mass changes and their contributions to sea-level rise from 1961 to 2016.
University of South Florida Satellite Oceanography Laboratory
Sea-Level Rise for the Coasts of California, Oregon, and Washington
Chambers et al, 2016, Evaluation of the Global Mean Sea Level Budget
between 1993 and 2014
French Space Agency, Satellite Altimetry Data website
NASA, New study finds sea level rise accelerating

Alaska and Arctic Climate Change
UAF Research
UAF International Arctic Research Center
Alaska Oceans Observing System
Arctic Research Consortium of the United States
Rick Thoman, at 2019 Weather and Climate Summit, (time marker 1:58 to 3:12)
Rick Thoman, A Century of Alaska Weather and Climate, Science for Alaska Lecture Series
Climatologists on Twitter:
Rick Thoman, IARC, https://twitter.com/AlaskaWx
Brian Brettschneider, UAF, https://twitter.com/Climatologist49
Zach Labe, UC Irvine, Cornell, https://twitter.com/ZLabe
Robert Rohde, Berkeley Earth, https://twitter.com/RARohde

Ocean and Food-Chain Stress
Seabird Die-off
Whale Deaths
Declining Humpback Migration and Calving
Seal Die-off
Krill and Mussel Die-off
Pink Salmon Die-off