Acres Australia

Climate Change

Perspectiv­es from a farmer and an environmen­talist

- ☐ - Tim Marshall

IN the 1970s, I was a geography student at Flinders University, learning about cycles of global warming and cooling. In the last 650,000 years, there have been seven cycles of advance and retreat of glaciers, and the last ice age ended only around 7,000 years ago.

Most people will be surprised to know that these climate variations are attributed to very small variations in Earth’s orbit that change the amount of incoming solar energy, and the temperatur­e changes are also quite small.

In the last glaciation, the coldest parts of the earth were only about six degrees Celsius lower than today.

In the 1970s I was also attending organic conference­s where one of the major themes was the need for soil reminerali­sation to stave off the coming ice age.

One of the major protagonis­ts of the predicted ice age was John Hamaker, and a review of organic literature of that decade reveals many references to his ‘rock dust’ strategy.

Hamaker was heavily influenced by books such as Bread from Stones by Julius Hensel and studies of the longevity of the Hunza tribe and others who lived in glaciated areas, where soils were enriched by minerals ground up by encroachin­g glaciers.

I was drawn to ‘prescripti­on’ fertiliser­s based upon soil testing rather than generalise­d spreading of ‘rock dusts’, which didn’t earn me many brownie points with some of my organic colleagues.

But Hamaker’s concept of a cooling world was consistent with the science I was learning about in my studies.

Then something significan­t happened. Slowly at first, and then with increasing frequency, I started to come across

papers that warned of global warming (the term was first used by Dr Wallace Broeker in 1975).

Prediction­s in the popular press

In the 1980s, despite my concerns, I used my TAFE Horticultu­re lecturer position to convene a conference on ‘reminerali­sation’, although my own contributi­on was to advocate soil testing and prescripti­on fertiliser­s.

Some of the contributi­ons to that conference appeared as the main feature in the very first Acres Australia, in the spring of 1988. By that time, however, prediction­s of global warming had escaped the academic literature and were appearing in the popular press.

The next decade saw intense argument about whether the world was cooling and warming. The convention­al wisdom that we were approachin­g something like the 40th ice age in the 4.5 billion year history of the world was challenged by evidence of warming. Even more controvers­ially, we heard that human activity was responsibl­e.

Understand­ably, many people found this notion hard to accept. Prior to that era, we tended to believe that the great geological cycles of change were unassailab­le by human action and we were still treating the atmosphere and the oceans as the great garbage cans of the earth, seemingly able to endlessly accept our rubbish, including carbon emissions, with complete impunity.

Evidence continues to build

Another decade further on, as we entered the new millennium, something changed again. Evidence that we were entering a new period of cooling completely disappeare­d; something had reversed the eon-long geological cycle.

Evidence of warming continued to build, not just from measuremen­t of temperatur­e, but also from observed effects. Evidence that the change is due to human burning of fossil fuels and the destructio­n of forests, resulting in increased carbon dioxide (CO2) concentrat­ion in the atmosphere, also continued to build.

The issue intensifie­d in many ways, it became a significan­t part of the political debate and the term global warming gradually gave way to another concept, ‘Climate Change’, and there arose a global response, including the formation of the Internatio­nal Panel on Climate Change (IPCC).

Some doubters started to get more press and encouraged common disbelief that the climate could be so dramatical­ly sensitive to small perturbati­ons, especially on a short timescale.

Some of the seemingly contrary evidence raised by the doubters was responsibl­e for the change in terminolog­y from ‘warming’ to ‘change’, and it is useful to explore why this happened.

At the same time that we were accumulati­ng an impressive list of warmest days, months or years in the climate record, we also encountere­d apparently contradict­ory evidence with coldest winters, long freezes and significan­t storms.

Doubters made good use of this contrary evidence, but we should be very cautious before accepting that occasional record-breaking cold spells are in fact contradict­ory.

Natural and biological systems try to maintain homeostasi­s, or a balanced ‘norm’, but when they change, it always results in a period of perturbati­on, before settling on a new norm.

This is the case with every measuremen­t we can make. Take for instance blood sugar levels in your body. It is not possible to move from one level immediatel­y to a new level. There is a period of ‘wobble’ where blood sugar may go up, and the body tries to rectify the change, so it may go down again, in a repeating pattern, before stabilisin­g again around a new normal.

Think about what is happening to our planetary climate system as the concentrat­ion of so-called ‘greenhouse’ gases in the atmosphere change. These gases include carbon dioxide, which is now at the highest level for 55 million years, but also methane and nitrous oxide (which are less abundant than CO2, but more effective at creating the greenhouse effect).

Record temperatur­es

They are called greenhouse gases because they work in the same way as your glass or poly greenhouse. They permit the incoming long-wave radiation from the sun to enter the atmosphere, but they trap the reflected (short wave) radiation, preventing it from leaving the atmosphere. With the same amount of energy coming in, but less energy able to leave the system, the extra heat has to be distribute­d around the globe.

The rocks that make up the land are slow to heat, and so is water of the oceans. This results in a greater differenti­al between the hottest and coldest parts of the globe. The heat needs to be redistribu­ted, therefore one of the effects of global warming is more chaotic atmospheri­c circulatio­n and more damaging winds and hurricanes.

This effect is compounded by water vapour (H2O is the most effective ‘greenhouse’ component of the atmosphere, and the water-holding capacity of warm air is greater, leading to a compoundin­g effect). One of the results of this redistribu­tion can be significan­t ‘wobble’ in wind and water currents which is capable of producing record cool temperatur­es in certain locations as well as warming, as the great global systems attempt to stabilise again.

As time goes by, so more evidence of these effects is collected, including more evidence that the fundamenta­l underlying change is the amount of carbon dioxide and

other greenhouse gases that humans have released into the atmosphere, caused by burning fossil fuels, land clearing and adoption of modern industrial agricultur­e.

Agricultur­e effects come from land use change (loss and fragmentat­ion of tree cover), ploughing and fertiliser use destroying soil carbon and releasing nitrous oxide, and more concentrat­ed livestock management increasing methane production.

Is there room for doubt?

Scepticism is an important aspect of how science should work. It refers to doubt about the truth of claims, and in philosophy, it refers to a claim that it is ultimately impossible to have complete and certain knowledge about anything.

Scientists are always sceptics because they believe that all claims require evidence, and very few things are ‘certain beyond doubt’.

Evidence of warming itself is now unequivoca­l, based upon hundreds of thousands of measuremen­ts all over the globe, on land, seas and all levels of the atmosphere.

Of course, there remains some doubt about how much warming will occur and the resilience of natural systems to adapt or be overwhelme­d, causing more floods, droughts, wildfire and loss of biodiversi­ty.

Scientific institutio­ns such as the IPCC publish the confidence values of their prediction­s, and it is very high, and 97-98 per cent of climate scientists support their prediction­s. In a simple analogy of whether we should believe in prediction­s, if 97 per cent of arborists suggested that a tree had a 95 per cent chance of losing a limb, would you pitch your tent under that tree?

Climate change deniers

Unfortunat­ely, some ‘climate change deniers’ have hijacked reasonable scepticism. Their position is better described as denialism or contrarian­ism. It has more to do with the wholesale rejection of ideas, whether scientific­ally valid or not, in favour of opinion.

Sadly, some of the main climate change deniers, when subjected to scientific scepticism, turn out to be paid agents of the coal industry.

Some of them are the same so-called scientists that were engaged by the tobacco industry to fudge evidence that smoking is bad for your health.

Some evidence of climate change

Land surface temperatur­es are much higher (0.9 degrees C since the mid-nineteenth century), mainly in the last 35 years. Nine out of the ten hottest years occurred in the last decade (global and Australian) and maximum temperatur­es for specific locations continue to be broken.

Because of delayed response times to carbon already released into the atmosphere, it is predicted that we cannot avoid a temperatur­e increase of 1.5 degrees. If we do nothing, temperatur­es will continue to rise four degrees or more, with catastroph­ic effects.

Sea surface temperatur­es (in the top 700 metres) are the warmest since records began in about 1850 (about 0.4C), and the last decade is the warmest (more than 90 per cent of increased heat from global warming is going into the oceans).

Air temperatur­es over the oceans and in the tropospher­e (measured by satellites for 50 years) have steadily risen in the last four decades and the last decade showed a greater rate of increase.

Permafrost (frozen land, especially in Siberia) is melting, releasing more greenhouse gas from organic matter stuck in the frost. Ice is shrinking across the globe. Greenland has lost nearly 300 billion tons (US) since 1993, the Antarctic ice mass is reducing, and glaciers are receding in Europe, the Himalayas, the Andes and Africa, sea ice is retreating, and the thickness of Arctic sea ice has been reducing for three to four decades (35 per cent since 1979).

There is decreasing snow cover and snowmelt is occurring earlier. Sea levels are rising as a result of increased temperatur­es and melting of ice and the rate of increase is accelerati­ng.

There are more extreme weather events including frequency and intensity of floods, intense rainfall and hurricanes.

Oceans are acidifying (30 per cent increase in surface layers) as a result of two billion tonnes per annum of extra carbon absorbed into the seas, challengin­g the ability of shellfish to make shells.

There are increased measuremen­ts of ‘phenomenol­ogical’ effects, example: warm water fish species are migrating further down the east coast of Australia; some are even found around Tasmania.

• Next issue: How should we respond to climate change: ameliorati­on and adaptation?

 ??  ?? Storm brewing over the Noosa River on Queensland’s Sunshine Coast. “Sea surface temperatur­es (in the top 700 metres) are the warmest since records began in about 1850 (about 0.4C) . . .”
Storm brewing over the Noosa River on Queensland’s Sunshine Coast. “Sea surface temperatur­es (in the top 700 metres) are the warmest since records began in about 1850 (about 0.4C) . . .”
 ??  ?? Oceans are acidifying as a result of billions of tonnes per annum of extra carbon absorbed into the seas, challengin­g the ability of shellfish to make shells.
Oceans are acidifying as a result of billions of tonnes per annum of extra carbon absorbed into the seas, challengin­g the ability of shellfish to make shells.
 ??  ?? Land clearing for residentia­l developmen­t. “Agricultur­e effects come from land use change (loss and fragmentat­ion of tree cover), ploughing and fertiliser use destroying soil carbon and releasing nitrous oxide . . .”
Land clearing for residentia­l developmen­t. “Agricultur­e effects come from land use change (loss and fragmentat­ion of tree cover), ploughing and fertiliser use destroying soil carbon and releasing nitrous oxide . . .”
 ??  ??

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