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astronomy

John H. Mercer

John H. Mercer is a astronomy topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand John H. Mercer rather than just read about it. In short: John H. Mercer (19 October 1922 – 3 July 1987) was a British glaciologist, chiefly known for his theoretical work on, and field studies of Antarctic ice streams, especially in the Transantarctic Mountains and in West Antarctica.

John H. Mercer — main illustration
John H. Mercer — illustration

Key takeaways

  • John H. Mercer belongs to astronomy; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect John H. Mercer to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of John H. Mercer from memory before moving on to harder problems.

Reference excerpt

John H. Mercer (19 October 1922 – 3 July 1987) was a British glaciologist, chiefly known for his theoretical work on, and field studies of Antarctic ice streams, especially in the Transantarctic Mountains and in West Antarctica. Following John T. Hollin's work (1962) suggesting that climatic warming and rising sea-level cause Antarctic ice shelves to retreat, Mercer postulated that the West Antarctic ice sheet, being grounded well below sea-level and terminating in floating ice shelves, was vulnerable to these changes and may have collapsed altogether during the last interglacial when Antarctica may have been warmer and sea-level may have been higher. In 1978, in the science magazine Nature, Mercer pointed out that "green-house" warming from burning fossil fuel could have the same effect during the present interglacial. Two studies published 12 May 2014 confirm Mercer's assumption. Climate scientist James Hansen has coined the term, "John Mercer effect." After Mercer published his paper suggesting that the West Antarctic ice sheet could collapse in response to warming, he struggled to get funding. Others, including Hansen, had similar problems. Many climate scientists censor their own work to avoid losing funding, especially regarding prospects for limiting warming to 2 °C above pre-industrial temperatures. John H. Mercer was born in Cheltenham, England in 1922, the third child of Harriet and John W. Mercer. He was educated at private schools in Cheltenham and, later, at Gordonstoun in Scotland. During World War II he served in the British Merchant Marines (1940–46) as a radio man. After the war he went to University of Cambridge and studied geography. At that time he came under the influence of William Vaughan Lewis. After finishing his B.A. in 1949 Mercer went to Canada, where he received his PhD in geography from McGill University in 1954. He was a Research Scholar from 1954 to 1956 at the Australian National University in Canberra, where he studied land use and population in western Samoa. He returned to Canada and worked in the Canadian Hydro-graphic Office in Ottawa as a geographer in 1957 and 1958. During 1959–60, 1961–62, 1964, and 1966, the American Geographical Society employed him at its World Data Center A for Glaciology in New York. The turning point in his career as a glaciologist was in 1960, when he became a research associate at The Ohio State University, in the Institute of Polar Studies (renamed the Byrd Polar Research Center). He remained at The Ohio State University until his death, becoming its first senior research scientist. Mercer died in Columbus, Ohio in 1987.

Legacy Mercer Ridge in Antarctica is named for him

Bibliography Southern Hemisphere Glacier Atlas (1967) Glacier Resurgence at the Atlantic/sub-Boreal Transition (1967) Antarctic Ice and Sangamon Sea Level (1968) Holocene Glacier Variations in Southern South America (1982) Cenozoic Glaciation in the Southern Hemisphere (1983)

References

External links John H. Mercer papers at The Ohio Library and Information Network, OhioLINK

Illustrations

John H. Mercer: Profile showing that most of the West Antarctic ice sheet is grounded below sea level which makes it sensitive to sea level rise. If contact of ice to bottom rocks is lost seaward of the grounding line, the ice sheet becomes significantly thinner (some 100 m), forming a shelf ice.
Profile showing that most of the West Antarctic ice sheet is grounded below sea level which makes it sensitive to sea level rise. If contact of ice to bottom rocks is lost seaward of the grounding line, the ice sheet becomes significantly thinner (some 100 m), forming a shelf ice.

Worked examples

Example 1 — a first encounter with John H. Mercer

Start with the simplest possible case. Write down what John H. Mercer claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In astronomy, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to John H. Mercer before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about John H. Mercer ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of John H. Mercer

In research
John H. Mercer appears in astronomy research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses John H. Mercer in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
John H. Mercer is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1922 births, 1987 deaths, Alumni of the University of Cambridge, so understanding it makes those chapters shorter.
In everyday life
Look for John H. Mercer outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study John H. Mercer in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what John H. Mercer means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain John H. Mercer out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is John H. Mercer in simple terms?

John H. Mercer (19 October 1922 – 3 July 1987) was a British glaciologist, chiefly known for his theoretical work on, and field studies of Antarctic ice streams, especially in the Transantarctic Mountains and in West Antarctica.

Why does John H. Mercer matter?

Because it connects several astronomy ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study John H. Mercer?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on John H. Mercer.

Tags

  • 1922 births
  • 1987 deaths
  • Alumni of the University of Cambridge
  • British Merchant Navy personnel of World War II
  • British expatriates in Australia
  • British expatriates in Canada
  • British expatriates in the United States
  • British glaciologists
  • McGill University alumni
  • People educated at Gordonstoun

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