Cyprus Environment and Energy (2009)

 
   

Climate change, greenhouse effect and global warming

What's it all about?

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Introduction

In this essay, I'm going to try and provide an explanation about what this is all about, in the simplest terms, because politicians and the media have made such a complete mess that Joe Public has become totally misinformed or, at least, confused about what these terms really mean. To make this as clear as possible, I'll separate the related theories of global warming and climate change but, first, let me give you a few definitions.

What is weather?

Weather is the effect of a number of variables at a given place and at a given time. These variables include temperature, dew point or relative humidity, precipitation, wind speed and direction, clouds, sun, dust and other aerosols etc. Note that this has got nothing to do with climate; one can have a cool day in a place with a hot climate, such as when it drops to under a maximum of 25°C in a Nicosia July, for example.

What is climate?

Climate is the effect of the average weather over a period of time (commonly 30 years) and over a large area. For example, the Mediterranean climate, which we enjoy in Cyprus, is categorised by hot dry summers and cool wet winters, such as may be experienced along the whole north coast of Africa and the whole south coast of Europe. This has nothing to do with the weather of the region. Global climate is averaged over the whole earth.

What is a theory?

The average man, if asked this question, will reply that it is something for which there may be circumstantial evidence but for which there is no proof. This definition does not satisfy the scientist; he would call this a hypothesis. No, a theory is more than a hypothesis and requires substantial observations and calculations to confirm the known facts (and to try and find out more!)

There are many theories based on scientific fact, such as relativity and gravity. To take the latter, legend has it that Newton watched an apple fall from a tree. That is an observation. From this, he deduced that every mass attracts every other mass by a force pointing along the line intersecting the mass centres of both masses. The force is proportional to the product of the two masses and inversely proportional to the square of the distance between the point masses and can thus be expressed as an equation:


From http://en.wikipedia.org/wiki/Newton%27s_law_of_universal_gravitation

That Newton was able to discover this in the 17th century is rather amazing and is a tribute to his genius, but no one has yet been able to discover why gravity exists, what causes the actual force. For this reason, gravitational force is a theory. We can observe that the apple does not fly to the moon and we can mathematically prove it, provided we know the values of the variables.

Theory of global warming

We owe this theory to another great scientist, the Swede Svante Arrhenius. In 1896, yes, 113 years ago, he published a paper entitled On the Influence of Carbonic Acid in the Air upon the Temperature of the Ground. Initially, this was a hypothesis but he later published his work as a theory. His calculations were later refined but were remarkably accurate. What he did not foresee was that man would extract billions of tonnes of fossil fuels and burn them willy-nilly, so his predictions of climate change (see below) were not accurate.

So what did Arrhenius say? Essentially, that the sun heated the earth's surface because some of the energy in solar short-wave electromagnetic radiation, peaking in the light spectrum, was absorbed. The resultant rise in temperature caused the earth to re-radiate this energy, at a much longer wavelength, in the far infra-red part of the spectrum, out towards space. If the earth were to have an atmosphere of only transparent gases like oxygen and nitrogen, then the energy radiated outwards would be substantially equal to the incoming energy. The temperature of the earth's atmosphere would be very cold, averaging about -18°C, over the globe. So, why is the global average temperature about +15°C, what caused this global warming of 30-odd degrees?

Various scientists had previously suggested that small amounts of various gases could absorb black body radiation at 15°C. Arrhenius measured the absorption spectra of gases, notably water vapour and carbon dioxide (carbonic acid) and calculated that the radiation was absorbed sufficiently to explain the global warming. One particular point that he made and he disputed with Ångstrom was that absorption spectrum of carbon dioxide covered most of the radiation spectrum, so that small quantities of the gas were as important as the comparatively large quantities of water vapour present in the atmosphere. This absorbed only a comparatively narrow band towards the edge of the radiation spectrum. This compelled him to state that small variations of carbon dioxide levels would have important effects on global warming. His calculations showed that a decrease of carbon dioxide levels by a third would produce an average temperature drop of a little more than -3°C, creating an ice age, while a 50% increase would cause a temperature rise of about +3.5°C with latitudinal variations. Apart from these theoretical carbon dioxide variations, he also found that variations in water vapour concentrations would have a smaller effect from practical observations.

Greenhouse gases

Because carbon dioxide and water vapour absorb radiative energy from the earth's surface, causing the air temperature to rise, they have been likened to the glass in a greenhouse, which stops much of the heat radiated from the plant beds from escaping outside the structure. They have therefore been nicknamed greenhouse gases. Other important greenhouse gases are methane, some halocarbon gases and nitrous oxide.

Theory of climate change

The theory of global climate change is a very complex subject. It is not fully understood, but the major causes have been well documented in scientific literature. The climate of the Earth is constantly changing if looked at over long periods of time. Up to recently, the changes have been natural and occasionally very important such as during the ice ages and interglacial periods. There are a number of reasons why this happens including solar cycles, cataclysmic events, changes in the atmospheric composition etc.

Of course, during global climate change phenomena, regional climates also change. It is important to note that some regional changes may not be in the same sense as global changes. This can mean, for example, that during a period of higher global temperature, some regions may have a lower temperature.

One natural phenomenon that popularly draws a lot of attention is the major volcanic eruption. For example, the 1991 Pinatubo eruption did affect world weather. Vast amounts of dust and sulfur dioxide were thrown into the lower stratosphere by the force of the explosion. This blocked almost 20% of the solar energy from reaching the earth's surface and air temperatures in the northern hemisphere dropped by an average of about 0.6°C and in the southern hemisphere by about 0.4°C. The energy that was blocked heated the lower stratosphere, of course. The aerosols from major eruptions have a relatively short lifetime and the drop in received radiation rises again in a very short time as the dust settles and rains out. The radiation block then follows an exponential curve back to normal levels in a 2 to 5 year time scale. The following graph shows the effect of four large eruptions on light levels in Hawaii.


From: http://www.cmdl.noaa.gov/albums/cmdl_overview/Slide18.sized.png

Of course, it is impossible to predict the frequency and magnitude of volcanic eruptions, so no accurate estimations can be included in the climate modelling. This is not terribly important because the effects are over a relatively short time scale. It is only if there were a continuous series of Volcanic Explosion Index 5 or 6 eruptions over decades that the global climate would be affected, causing a drop in temperatures with consequent side-effects. This is a similar scenario to the 1980s scaremongers' "nuclear winter", which would be unlikely to happen as the explosions would be unlikely to propel much dust into the stratosphere.

Another similar natural effect is that of massive forest fires. I was a student in Edinburgh in September 1950 and, one Wednesday afternoon, I noticed the sun was bright blue. That evening, the three-quarters moon was also very blue (and I've only seen it that colour once in my lifetime, so the adage may have some truth!). I could hardly believe my eyes! I later learnt that the cause was soot particles from massive forest fires in British Columbia carried by the jet stream many thousands of kilometres. The next day, the sun and moon appeared normal. I don't believe this phenomenon would have much climate influence because it was ephemeral and there would be little stratospheric mixing.

In very recent years, it is very likely that human activity has also started to cause a climate change, as the media constantly report, although they usually use the term global warming, even though climate includes many phenomena other than temperature, such as precipitation, wind speed and direction, cloud cover and so on. One of the popular media themes in southern Europe, and Cyprus especially, is potential desertification. Even though this includes a possible temperature change, it also means a considerable reduction in precipitation and humidity.

Over the past 150 years, we have extracted many billions of tonnes of coal, oil and gas which we have burnt without any thought about what it may entail. Every tonne of any of these fossil fuels that is combusted will produce between 2 3/4 and 4 1/2 tonnes of carbon dioxide. We are allowing this to escape into the atmosphere at the rate of about 26 billion tonnes per year. As it happens, nature is able to remove about half of this, mostly by absorption into the upper levels of the oceans, acidifying the water. The other half is simply accumulating, year by year, in an ever increasing quantity. For many centuries, the natural level of carbon dioxide in the atmosphere has been relatively constant at about 280 ppm. This has been an essential part of global warming enabling life as we know it. The current level of carbon dioxide in the atmosphere is about 385 ppm with projected trends up to 400 ppm within a decade or two. This is an increase of 43%. You will remember that Arrhenius predicted in 1896 that a 50% increase in carbon dioxide concentration would result in a global increase in temperature of 3.5°C. We are nearly there. This is therefore a man-made or anthropogenic manifestation of one type of climate change.

The graphs on the left, taken from the report of Working Group I of the Intergovernmental Panel on Climate Change, Summary for Policymakers, of the AR4, 2007, show how the three major greenhouse gases have had levels substantially constant for 10,000 years, until the last 100 or so years. Can there be any real doubt that it is too much of a coincidence for the increase in carbon dioxide to be anything other than largely due to the increase from burning fossil fuels in the same time frame? Of course, there are other contributory factors, such as the reduction of sinks by deforestation and urbanisation.

On the right hand side of these graphs, there is a scale of radiative forcing. Please let me digress and explain what this means. The radiative forcing of the surface-troposphere system due to the perturbation in or the introduction of an agent (say, a change in greenhouse gas concentrations) is the change in net (down minus up) irradiance (solar plus long-wave; in Wm-2) at the tropopause AFTER allowing for stratospheric temperatures to readjust to radiative equilibrium, but with surface and tropospheric temperatures and state held fixed at the unperturbed values. This definition sounds a little difficult to understand; more simply, it is the change in the difference between incoming and outgoing radiated energy at the tropopause since 1750 due to a given cause. For carbon dioxide, this amounts to an increase of about 1.5 Wm-2 in the last 259 years (mostly in the last 100 years). This change in energy levels is, in fact, what is driving the atmospheric temperature up, creating the conditions for climate change.

The second graph is for methane and it can be seen that the concentrations have more than doubled in the last 100 years or so, even though the radiative forcing is less than that of carbon dioxide. If this increase continues, it could catch up on the latter. It is important to realise where this methane comes from, because there are both natural and man-made sources. Amongst the natural ones, there is the anaerobic decomposition of organic matter in wetlands (the true natural gas), decomposition due to termites and the enteric fermentation in herbivores, notably in Africa. The sudden increase over the last 100 or so years is due largely to the increased human population requiring increased areas of rice paddies, more cattle, more landfills and, above all, an insatiable greed for fossil natural gas. Most methane reacts, sooner or later, with free hydroxyl radicals, from atmospheric humidity, releasing a molecule of carbon dioxide for each molecule of methane, a kind of double whammy!

The third graph shows a similar progression for nitrous oxide. The natural sources are mostly from microbes in the soil and in the ocean, from lightning strikes and from forest fires. The main man-made ones are from nitrogen fertilisers, fossil fuel combustion and biomass burning. It has a long lifetime because it decomposes mainly only after it has reached the stratospheric ozone layer, where it contributes to ozone depletion, another double whammy!

Other man-made greenhouse gases are from halocarbons. There are virtually no natural sources of these, so any found in the atmosphere must be of human origin. A halocarbon is any organic substance where one or more hydrogen atoms are replaced by atoms of fluorine, chlorine, bromine or iodine (ignoring astatine) or combinations of them. The more stable a halocarbon is, the greater is its effect on trapping the radiation from the earth, simply because it can do so for longer periods of time before it decomposes. As a rule, substances containing fluorine last longer than those containing chlorine, in turn lasting longer than those containing bromine and so on. Some gases containing only carbon and fluorine may last 10,000 years before they break down, so you can imagine the damage they would cause for tens of future generations if they were released in quantity (fortunately they aren't). However, large quantities of substances known as HFCs and HCFCs are used for refrigeration, aerosol propellants, solvents etc. and these are much worse than carbon dioxide or even methane per unit weight emitted.

The above chart, also taken from the report of Working Group I of the Intergovernmental Panel on Climate Change, Summary for Policymakers, of the AR4, 2007, shows the positive and negative effects on radiative forcing (i.e., the potential climate change) from each of the major man-made sources and the major natural one of variations in the solar cycle. On the graphic bars, there are extreme maximum and minimum limits shown by H-shaped bars, with the same data between parentheses in the RF values column. The aggregate, at the bottom obviously sums the limits, as well as average values, and it shows that we are responsible, up to 2005, for a radiative forcing of 0.6 to 2.4 W/m² with a likely value of 1.6 W/m². It is perhaps important to note that the tolerances of the values for the major gases is quite small.

One influence that is very difficult to model accurately is the positive feedback loop. A couple of examples will illustrate this. Some arctic regions have thick peat layers on or close to the surface which are perennially frozen (permafrost). These contain large quantities of gases resulting from centuries of peat formation from sphagnum moss. Amongst these gases is methane, free, dissolved or as clathrates. As the global climate increases in temperature, the permafrost melts, allowing the methane to escape, causing more climate change, causing more permafrost to melt, and so on. Another example is the decrease of glacial cover due to ice melt, laying bare darker rocks, reducing the albedo (reflectivity of the solar radiation as outgoing short-wave radiation) causing larger areas absorbing more energy. These positive feedback mechanisms may "snowball", almost unpredictably, until a new equilibrium is reached.

Equally, some phenomena may induce negative feedback mechanisms. These always tend towards increased stability, but the new equilibrium state is difficult to predict. One example is that increased ocean temperatures, causing more evaporation of water, creating more clouds whose high albedo will reflect more solar energy back to space, thus reducing warming of the earth and the oceans, in turn, creating less evaporation. This is why the cloud albedo effect in the above chart has the widest margin of error.

How can the masses of global data of what has happened in the past be used to predict future climate change? Scientists have little faith in crystal balls, so groups around the world used estimates of the amplitude of known causes over the past century, including episodic phenomena like El Niño, volcanic eruptions as well as meteorological data and natural causes, such as variations in the sunspot cycle, orbital changes etc. and they tried to model the exact mathematical curve that would provide the best fit to the observations of temperature. It would then be possible to extrapolate the different models to continue the trends forward. So, how well have these models performed?

The above graphs, again taken from the report of Working Group I of the Intergovernmental Panel on Climate Change, Summary for Policymakers, of the AR4, 2007, show the observations (black line) of global temperature, the blue areas show the modelled results using only natural phenomena on the input, while the pink shows that the natural plus the man-made phenomena, combined, provide the best fit, although there is an anomaly about 1940, especially for ocean data. For simplification, these curves are simplified to the averages for each decade, to avoid unnecessary busy-ness on the small dimensions. I emphasise that the ranges for the blue curves cover the stated limits of 19 different simulations with 5 different models while the pink ones use 58 simulations from 14 models. The correlation between the models all seem remarkably close.

The IPCC used these models for predicting future trends, using different scenarios. They are reasonably confident about what may happen over the next decades, even up to the end of the century. However, the purpose of this essay is to provide as simple a demonstration as is possible that climate change has already started and that it is largely, but not entirely, due to human activities. I do not propose, therefore, to discuss what may or may not happen in the future. Quod erat demonstrandum.



 
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