The Post

Eighty amazing years of Dobson No 17

- Paul Gorman

It looks like it could have come out of the Tardis of the first Doctor Who – an attempt at appearing technologi­cally modern that long ago became an anachronis­m.

But the Dobson spectropho­tometer goes much further back than early 1960s British television. And the heavy – it takes two people to move it – yet fragile block of cast iron remains an accurate and reliable way of measuring atmospheri­c ozone levels.

In the 1980s, Dobson instrument­s in the Antarctic registered dropping ozone values in the stratosphe­re, evidence that the springtime ozone hole had become a reality.

Those measuremen­ts propelled a concerned world to adopt the Montreal Protocol, to protect the ozone layer, in 1988. It took another decade before ozone-depleting chlorofluo­rocarbons peaked, but they have been declining since.

This is the story of Dobson No 17, now nearly 80 years old and still in fine working order at Arrival Heights near Scott Base, Antarctica.

A Dobson spectropho­tometer measures the total amount of ozone in a column of air between the instrument on the ground and the top of the atmosphere.

It does this using quartz prisms to compare the absorption of ultraviole­t of different intensitie­s that are either strongly or weakly absorbed by ozone.

The amount of ozone is measured in Dobson Units, DUs, with 100DU equal to a 1mm-thick sliver of ozone at standard temperatur­e and pressure.

The instrument was invented in the late 1920s by Oxford University physicist and meteorolog­ist Dr Gordon Dobson.

The National Institute of Water and Atmospheri­c Research (Niwa) looks after

New Zealand’s two Dobsons. The original, No 17, is on the ice and its younger sibling, No 72, is at Lauder in Central Otago. There are about 100 Dobsons worldwide.

‘‘The Dobson is still highly regarded because they have been running for so long,’’ says Niwa atmospheri­c scientist Dr Sylvia Nicol. ‘‘It’s quite a simple instrument in some respects. Like a lot of meteorolog­ical equipment, it hasn’t changed much over the years.’’

Writing in Weather and Climate, Nicol says the

New Zealand Meteorolog­ical Service was invited to buy one of the first 20 units because Christchur­ch was one of five internatio­nal sites already measuring ozone using a borrowed Fery quartz spectrogra­ph.

Approval was given to buy a Dobson in 1937, but it was another 13 years before the instrument landed in New Zealand.

First, there were delays with calibratio­n and then it was requisitio­ned for ‘‘urgent defence investigat­ions’’ by the British Meteorolog­ical Office during World War II.

On No 17’s arrival in 1950, it was installed at Gracefield in Wellington, and then at Kelburn in July 1951. The first measuremen­ts were taken by Elizabeth Porter, who died in the Tangiwai train disaster on Christmas Eve 1953.

The work was then taken on by Edith Farkas, a scientist who had arrived from Hungary as a refugee a few years earlier. She then became leader of the Dobson No 17 programme from 1965 until her retirement in 1986.

Meanwhile, however, the unit was shifted to the met service’s Invercargi­ll airport office in June 1970.

When No 72 was installed at Lauder in January 1987, the old instrument was sent to the Antarctic, where it made contributi­ons to burgeoning ozone-hole studies.

That is where No 17 remains to this day, 31 years after moving south, an incongruou­s slab of metal still taking intricate daily ozone readings with its periscope through the roof of the observator­y.

‘‘The Dobson is still highly regarded because they have been running for so long.’’ Dr Sylvia Nicol, Niwa

 ??  ?? Dobson 17 at Arrival Heights, Antarctica. From left, Kate McKenzie from Antarctica New Zealand, Sylvia Nicol and Wills Dobson from Niwa and Koji Miyagawa from the US National Oceanic and Atmospheri­c Administra­tion.
Dobson 17 at Arrival Heights, Antarctica. From left, Kate McKenzie from Antarctica New Zealand, Sylvia Nicol and Wills Dobson from Niwa and Koji Miyagawa from the US National Oceanic and Atmospheri­c Administra­tion.

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