Jon Shanklin

Last updated

Jonathan David Shanklin
Jonathan Shanklin.jpg
Jonathan Shanklin in Antarctica, summer 2012
Born (1953-09-29) 29 September 1953 (age 69)
NationalityBritish
Known for Ozone Hole Discovery
Awards The Chree Medal and Prize (2001)
Scientific career
Fields Physics, Meteorology (Professional)
Botany, Hepatics, Astronomy (Amateur)
Institutions British Antarctic Survey
Website www.theozonehole.com/jonathanshanklin.htm

Jonathan Shanklin is a meteorologist who has worked at the British Antarctic Survey since 1977. Together with Joe Farman and Brian G. Gardiner he discovered the "Ozone Hole" in the 1980s. [1] [2]

Shanklin has described his role at the BAS as being that of a "general dogsbody" at the time of the discovery of the "ozone hole". [3] He calibrated an instrument called the Dobson Ozone Spectrophotometer which provided data on atmospheric ozone.

In an article discussing the discovery, the BBC quotes him as saying

Perhaps the most startling lesson from the ozone hole is just how quickly our planet can change. Given the speed with which humankind can affect it, following the precautionary principle is likely to be the safest road to future prosperity. [4]

Shanklin maintains the ozone pages at BAS. He plays cricket, is a bell-ringer, an active local naturalist and is a keen amateur astronomer, being Director of the British Astronomical Association's Comet Section .

In December 2020 it was announced that the UK Antarctic Place-names Committee had named a glacier on the Antarctic Peninsula after Shanklin, in part to mark the 200th anniversary of the discovery of the continent. [5]

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The Montreal Protocol is an international treaty designed to protect the ozone layer by phasing out the production of numerous substances that are responsible for ozone depletion. It was agreed on 16 September 1987, and entered into force on 1 January 1989. Since then, it has undergone nine revisions, in 1990 (London), 1991 (Nairobi), 1992 (Copenhagen), 1993 (Bangkok), 1995 (Vienna), 1997 (Montreal), 1998 (Australia), 1999 (Beijing) and 2016 (Kigali) As a result of the international agreement, the ozone hole in Antarctica is slowly recovering. Climate projections indicate that the ozone layer will return to 1980 levels between 2040 and 2066. Due to its widespread adoption and implementation, it has been hailed as an example of successful international co-operation. Former UN Secretary-General Kofi Annan stated that "perhaps the single most successful international agreement to date has been the Montreal Protocol". In comparison, effective burden-sharing and solution proposals mitigating regional conflicts of interest have been among the success factors for the ozone depletion challenge, where global regulation based on the Kyoto Protocol has failed to do so. In this case of the ozone depletion challenge, there was global regulation already being installed before a scientific consensus was established. Also, overall public opinion was convinced of possible imminent risks.

<span class="mw-page-title-main">Ozone layer</span> Region of the stratosphere

The ozone layer or ozone shield is a region of Earth's stratosphere that absorbs most of the Sun's ultraviolet radiation. It contains a high concentration of ozone (O3) in relation to other parts of the atmosphere, although still small in relation to other gases in the stratosphere. The ozone layer contains less than 10 parts per million of ozone, while the average ozone concentration in Earth's atmosphere as a whole is about 0.3 parts per million. The ozone layer is mainly found in the lower portion of the stratosphere, from approximately 15 to 35 kilometers (9 to 22 mi) above Earth, although its thickness varies seasonally and geographically.

<i>Nature</i> (journal) British scientific journal since 1869

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Ozone depletion consists of two related events observed since the late 1970s: a steady lowering of about four percent in the total amount of ozone in Earth's atmosphere, and a much larger springtime decrease in stratospheric ozone around Earth's polar regions. The latter phenomenon is referred to as the ozone hole. There are also springtime polar tropospheric ozone depletion events in addition to these stratospheric events.

The Dobson unit (DU) is a unit of measurement of the amount of a trace gas in a vertical column through the Earth's atmosphere. It originated, and continues to be primarily used in respect to, atmospheric ozone, whose total column amount, usually termed "total ozone", and sometimes "column abundance", is dominated by the high concentrations of ozone in the stratospheric ozone layer.

The year 1985 in science and technology involved many significant events, listed below.

<span class="mw-page-title-main">Antarctic ice sheet</span> Earths southern polar ice cap

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Joseph Charles Farman CBE was a British geophysicist who worked for the British Antarctic Survey. Together with Brian Gardiner and Jon Shanklin, he published the discovery of the ozone hole over Antarctica, having used Dobson ozone spectrophotometers. Their results were first published on 16 May 1985.

The following events occurred in May 1985:

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The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on behalf of the UK. It is part of the Natural Environment Research Council (NERC). With over 400 staff, BAS takes an active role in Antarctic affairs, operating five research stations, one ship and five aircraft in both polar regions, as well as addressing key global and regional issues. This involves joint research projects with over 40 UK universities and more than 120 national and international collaborations.

John Adrian Pyle is a British atmospheric scientist, Director of the Centre for Atmospheric Science in Cambridge, England. He is a Professor in the Department of Chemistry at the University of Cambridge, and since 2007 has held the 1920 Chair of Physical Chemistry in the Chemistry Department. He is also a Fellow of the Royal Society and of St Catharine's College, Cambridge.

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<span class="mw-page-title-main">Antarctica</span> Continent

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<span class="mw-page-title-main">Institute of Physics Edward Appleton Medal and Prize</span> Award made for distinguished research in environmental physics

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Brian Gerard Gardiner is a retired British meteorologist, formerly working for the British Antarctic Survey. Together with Joe Farman and Jonathan Shanklin he discovered the "Ozone Hole". Their results were first published on 16 May 1985. They won the Chree medal and prize in 2001.

In astronomy, a calcium-rich supernova is a subclass of supernovae that, in contrast to more well-known traditional supernova classes, are fainter and produce unusually large amounts of calcium. Since their luminosity is located in a gap between that of novae and other supernovae, they are also referred to as "gap" transients. Only around 15 events have been classified as a calcium-rich supernova – a combination of their intrinsic rarity and low luminosity make new discoveries and their subsequent study difficult. This makes calcium-rich supernovae one of the most mysterious supernova subclasses currently known.

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References

  1. Farman, J. C.; Gardiner, B. G.; Shanklin, J. D. (1985). "Large losses of total ozone in Antarctica reveal seasonal ClOx/NOx interaction". Nature. 315 (6016): 207. Bibcode:1985Natur.315..207F. doi:10.1038/315207a0. S2CID   4346468.
  2. Shanklin, J. (2010). "Reflections on the ozone hole". Nature. 465 (7294): 34–35. Bibcode:2010Natur.465...34S. doi:10.1038/465034a. PMID   20445611. S2CID   4413691.
  3. Thirty years on...
  4. Richard Black (2010), Deep reflections on the ozone story
  5. Amos, Jonathan (3 December 2020). "Antarctic place names recognise 'modern explorers'". BBC News. Retrieved 5 December 2020.