Category Archives: History and philosophy of science

Science, philosophy and religion at Cambridge

I’m spending this week in St Edmund’s College of the University of Cambridge, attending the Faraday Institute summer school on science, philosophy and religion. So far, the course is a feast in the history and philosophy of science, just as last year (see posts on last year’s summer school in July 2008 section).

This morning started with an excellent talk on ‘The Reception of Darwinism’ by renowned historian Prof John Hedley Brooke that posed three main questions. What shifts in attitude resulted from Darwin’s work? What information exists to add to conventional accounts of debates such as the Huxley-Wilberforce debate? Does it make sense to say that Darwin’s theory led to the death of God? I won’t attempt to summarize the talk here, but a video of it will be available on the Faraday website in a few days.

Next we had a talk on ‘Rationality in Science and Religion’ by Roger Trigg, followed by a talk on ‘Islam and Science Yesterday’ by Prof Nidhal Guessom of the University of Sharjah, UAE. Roger’s talk was a highly appropriate for the first day, setting the stage with definitions of concepts such as realism, materialism, relativism, naturalistic methodology etc. Nidahl’s talk was a fascinating account of the history of Islamic science, not merely as curators of Greek classicism but as innovative scientists – accompanied by a careful discussion of the reasons for the gradual decline of Islamic science.

For me, the tour- de-force of the day was a fantastic talk on the history of mediaeval science by the Oxford historian Allan Chapman: ‘Mediaeval cosmology and the Church’. Essentially, Chapman’ s thesis was that the ‘Dark Ages’ is a misnomer, created by a revisionist Protestant view of Catholic science in the middle ages (‘those dark and monkish times’ – Hooke). Chapman made his case by giving a superb overview of science from 600 AD to 1400, describing the advances made from optics to astronomy, and the contributions of figures such as William of Ockham, d’Oresmene,  Nicholas of Cusa and Bernhardt Walther.

Of course, this thesis leads to an obvious question – if the Dark Ages were not so dark, why did it take so long for the heliocentric model to emerge? (my question). Chapman had a great answer – because no-one suspected the Ptolemy model was wrong! After all, most of the predictions of Ptolemny’s geocentric model were more or less accurate!!

I love this theme, and I’m sure it’s typical in science. The most difficult scientific theories to refute are those that are almost correct -or make predictions that re almost correct – simply because no-one suspects they need fixing! True from the limits of Newton’s gravity to the discovery of the elctroweak interaction!. Thought for the day…

Al in all, a super first day. As usual, each talk is a superb example of how to communicate science. After each talk, there is 30 mins of Q&A after every talk, leading to great discussions. After tea, there is a plenary panel discussion, with questions raised during the day discussed.

Course director Rodney Holder (far left) chairs a panel discussion with Allan, Niddaahl and Ernan (L-R)

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150th anniversary of Tyndall’s greenhouse effect

Every scientist knows that this year marks the 150th anniversary of the publication of Darwin’s ‘On the Origin of Species’, but not so many may be aware that another scientific breakthrough occurred that year. In 1859, the Irish physicist John Tyndall discovered that certain gases – carbon dioxide and water vapour in particular – absorb infra-red radiation. The discovery was established over a few short weeks, but it provided an explanation for the greenhouse effect, one of the great puzzles of science.

The Irish Times have accepted a piece I have written on Tyndall for their Irishman’s Diary slot next month. I like this column- it is a unique feature of The Irish Times, comprising an 800-word essay prominently displayed on the op-ed page, written by the house journalist 3 days a week and by a freelance writer on other days. I have written a few diaries on various Irish scientists in the past (see My Articles) and I hope one day to publish the ‘Science Diaries’ as a collection of essays.  Below is a draft of what I intend to say on Tyndall:

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John Tyndall: celebrated Irish scientist who discovered the greenhouse effect

Many readers will know that this year marks the 150th anniversary of the publication of Darwin’s ‘On the Origin of Species’. Another breakthrough occurred in science that fateful year, this one with an Irish connection. The discovery attracted much less attention than Darwin’s theory of evolution at the time, but it has become one of the hottest topics in science today (literally).

In July 1859, the Irish physicist John Tyndall, one of the great scientists of the 19th century, established that certain atmospheric gases absorb heat quite strongly. This innocuous-sounding discovery was established over a few short weeks, but it provided the solution to one of the great riddles of science: the famous ‘greenhouse effect’.

The greenhouse effect was first proposed by the French polymath Joseph Fourier, almost a century before Tyndall’s experiments. Fourier had wondered how the earth maintains its warm temperature, and he speculated that while heat from the sun passes easily through our atmosphere on the way to earth, heat radiated outwards by the warm earth must somehow be trapped in the atmosphere. The hypothesis was highly controversial, as it was widely assumed that gases are transparent to heat.

Tyndall, a fierce proponent of the new experimental method of science, devised a series of simple experiments to test Fourier’s hypothesis.  Working in the dusty basement of the Royal Institution in London in the summer of 1859, he soon established that, while most gases are indeed transparent to light and heat, some gases – carbon dioxide and water vapour in particular – can absorb heat energy at certain wavelengths. As traces of each gas were known to exist in the earth’s atmosphere, the puzzle of the earth’s temperature was solved.

How did an Irish scientist come to make such an important discovery? John Tyndall was born in Leighlinbridge, County Carlow in 1820, the son of an RIC officer and land agent. On completing his schooling under renowned local teacher John Conwill, he started his professional career as a surveyor for the Ordinance Survey of Ireland.  He was soon transferred to a position with the Ordinance Survey in Lancashire, England, but became interested in the new experimental sciences of physics and chemistry emerging in Germany. He moved to Germany in 1848 to study under the famous experimentalist Robert Bunsen at the University of Marburg, returning to England with a PhD in experimental science in 1851. By 1853, he had been appointed Professor of Natural Philosophy at the Royal Institution, a position previously held by the renowned scientist Micheal Faraday.

Tyndall remained at the Royal Institution for the rest of his career, making important discoveries in diverse areas of science, from magnetism to optics, from the physics of sound to the behaviour of bacteria. He is probably best known for ‘Tyndall scattering’, the scientific explanation for why the sky is blue. A keen mountaineer, he became interested in the science of glaciers and made several important discoveries concerning their behaviour. He became extremely well-known in Victorian England as a public communicator of science and was a prominent member of the ‘X Club’, an influential group of prominent scientists who defended evolution and other new scientific theories from religious dogma.

Tyndall’s verification of the greenhouse effect was accepted by the scientific establishment, but not regarded as a matter of vital importance. He and his colleagues were aware of the output of Victorian England’s factory chimneys, but no-one drew a link between this pollution and the greenhouse effect.

Nowadays, evidence has emerged that the average temperature of the earth and its oceans has been gradually rising since the industrial revolution. Despite many uncertainties, the scientific consensus is that this global warming is associated with an increase in carbon dioxide in the atmosphere, an increase that has been produced by human activities such as industry and transport. The discovery has led to concerted international efforts to agree on targets for reducing carbon emissions worldwide, a process that is only just beginning.

What would Tyndall make of today’s climate problems? Like most scientists of his era, he would probably find it difficult to grasp that humans could have such a global effect on nature. On the other hand, he would be greatly depressed by the shrinking of his beloved glaciers. Above all, he would be astonished to find that, of all the scientific discoveries he made, the work he did in the summer of 1859 has become a major preoccupation of 21st century science.

Today, the work of this great Irish scientist is commemorated by the annual Tyndall lecture of the Institute of Physics, the Tyndall Centre for Climate Change Research in the UK, the Tyndall National Institute in Cork, Mount Tyndall in California and the Tyndall glacier in Chile.

*********************************

John Tyndall: celebrated Irish scientist who discovered the greenhouse effect

Many readers will know that this year marks the 150th anniversary of the publication of Darwin’s ‘On the Origin of Species’. Another breakthrough occurred in science that fateful year, this one with an Irish connection. The discovery attracted much less attention than Darwin’s theory of evolution at the time, but it has become one of the hottest topics in science today (literally).

In July 1859, the Irish physicist John Tyndall, one of the great scientists of the 19th century, established that certain atmospheric gases absorb heat quite strongly. This innocuous-sounding discovery was established over a few short weeks, but it provided the solution to one of the great riddles of science: the famous ‘greenhouse effect’.

The greenhouse effect was first proposed by the French polymath Joseph Fourier, almost a century before Tyndall’s experiments. Fourier had wondered how the earth maintains its warm temperature, and he speculated that while heat from the sun passes easily through our atmosphere on the way to earth, heat radiated outwards by the warm earth must somehow be trapped in the atmosphere. The hypothesis was highly controversial, as it was widely assumed that gases are transparent to heat.

Tyndall, a fierce proponent of the new experimental method of science, devised a series of simple experiments to test Fourier’s hypothesis. Working in the dusty basement of the Royal Institution in London in the summer of 1859, he soon established that, while most gases are indeed transparent to light and heat, some gases – carbon dioxide and water vapour in particular – can absorb heat energy at certain wavelengths. As traces of each gas were known to exist in the earth’s atmosphere, the puzzle of the earth’s temperature was solved.

How did an Irish scientist come to make such an important discovery? John Tyndall was born in Leighlinbridge, County Carlow in 1820, the son of an RIC officer and land agent. On completing his schooling under renowned local teacher John Conwill, he started his professional career as a surveyor for the Ordinance Survey of Ireland. He was soon transferred to a position with the Ordinance Survey in Lancashire, England, but became interested in the new experimental sciences of physics and chemistry emerging in Germany. He moved to Germany in 1848 to study under the famous experimentalist Robert Bunsen at the University of Marburg, returning to England with a PhD in experimental science in 1851. By 1853, he had been appointed Professor of Natural Philosophy at the Royal Institution, a position previously held by the renowned scientist Micheal Faraday.

Tyndall remained at the Royal Institution for the rest of his career, making important discoveries in diverse areas of science, from magnetism to optics, from the physics of sound to the behaviour of bacteria. He is probably best known for ‘Tyndall scattering’, the scientific explanation for why the sky is blue. A keen mountaineer, he became interested in the science of glaciers and made several important discoveries concerning their behaviour. He became extremely well-known in Victorian England as a public communicator of science and was a prominent member of the ‘X Club’, an influential group of prominent scientists who defended evolution and other new scientific theories from religious dogma.

Tyndall’s verification of the greenhouse effect was accepted by the scientific establishment, but not regarded as a matter of vital importance. He and his colleagues were aware of the output of Victorian England’s factory chimneys, but no-one drew a link between this pollution and the greenhouse effect.

Nowadays, evidence has emerged that the average temperature of the earth and its oceans has been gradually rising since the industrial revolution. Despite many uncertainties, the scientific consensus is that this global warming is associated with an increase in carbon dioxide in the atmosphere, an increase that has been produced by human activities such as industry and transport. The discovery has led to concerted international efforts to agree on targets for reducing carbon emissions worldwide, a process that is only just beginning.

What would Tyndall make of today’s climate problems? Like most scientists of his era, he would probably find it difficult to grasp that humans could have such a global effect on nature. On the other hand, he would be greatly depressed by the shrinking of his beloved glaciers. Above all, he would be astonished to find that, of all the scientific discoveries he made, the work he did in the summer of 1859 has become a major preoccupation of 21st century science.

Today, the work of this great Irish scientist is commemorated by the annual Tyndall lecture of the Institute of Physics, the Tyndall Centre for Climate Change Research in the UK, the Tyndall National Institute in Cork, Mount Tyndall in California and the Tyndall glacier in Chile.

Dr Cormac O’Raifeartaigh is the author of the science blog ANTIMATTER

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