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High-altitude nuclear explosion

High-altitude nuclear explosion is a physics 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 High-altitude nuclear explosion rather than just read about it. In short: High-altitude nuclear explosions are the result of nuclear weapons testing within the upper layers of the Earth's atmosphere and in outer space. Several such tests were performed at high altitudes by the United States and the Soviet Union between 1958 and 1962.

High-altitude nuclear explosion — main illustration
High-altitude nuclear explosion — illustration

Key takeaways

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

Reference excerpt

High-altitude nuclear explosions are the result of nuclear weapons testing within the upper layers of the Earth's atmosphere and in outer space. Several such tests were performed at high altitudes by the United States and the Soviet Union between 1958 and 1962. The Partial Test Ban Treaty was passed in October 1963, ending atmospheric and exoatmospheric nuclear tests. The Outer Space Treaty of 1967 banned the stationing of nuclear weapons in space, in addition to other weapons of mass destruction. The Comprehensive Nuclear-Test-Ban Treaty of 1996 prohibits all nuclear testing; whether over- or underground, underwater or in the atmosphere, but has yet to enter into force as it has been ratified by some of the states party to the Treaty.

EMP generation

The strong electromagnetic pulse (EMP) that results has several components. In the first few tenths of nanoseconds, about a tenth of a percent of the weapon yield appears as powerful gamma rays with energies of one to three mega-electron volts (MeV, a unit of energy). The gamma rays penetrate the atmosphere and collide with air molecules, depositing their energy to produce huge quantities of positive ions and recoil electrons (also known as Compton electrons). These MeV-energy Compton electrons then accelerate and spiral along the Earth's magnetic field lines. The resulting transient electric fields and currents generate electromagnetic emissions in the radio frequency range of 15 MHz to 250 MHz. This high-altitude EMP occurs between 30 and 50 kilometers (19 and 31 miles) above the Earth's surface. The potential as an anti-satellite weapon became apparent in August 1958 during Hardtack Teak. The EMP observed at the Apia Observatory at Samoa was four times more powerful than any created by solar storms, while in July 1962 the Starfish Prime test damaged electronics in Honolulu and New Zealand (approximately 1,300 kilometres (810 mi) away), fused 300 street lights on Oahu (Hawaii), set off about 100 burglar alarms, and caused the failure of a microwave repeating station on Kauai, which cut off the sturdy telephone system from the other Hawaiian islands. The radius for an effective satellite kill for the Compton radiation produced by such a nuclear weapon in space was determined to be roughly 80 kilometres (50 mi). Further testing to this end was carried out, and embodied in a Department of Defense program, Program 437.

Drawbacks

There are problems with nuclear weapons carried over to testing and deployment scenarios, however. Because of the very large radius associated with nuclear events, it was nearly impossible to prevent indiscriminate damage to other satellites, including one's own satellites. Starfish Prime produced an artificial radiation belt in space that soon destroyed three satellites (Ariel, TRAAC, and Transit 4B all failed after traversing the radiation belt, while Cosmos V, Injun I and Telstar 1 suffered minor degradation, due to some radiation damage to solar cells, etc.). The radiation dose rate was at least 0.6 Gy/day at four months after Starfish for a well-shielded satellite or crewed capsule in a polar circular earth orbit, which caused NASA concern with regard to its crewed space exploration programs.

Differences from atmospheric tests

In general, nuclear effects in space (or very high altitudes) have a qualitatively different display. While an atmospheric nuclear explosion has a characteristic mushroom-shaped cloud, high-altitude and space explosions tend to manifest a spherical 'cloud' until distorted by Earth's magnetic field. The charged particles resulting from the blast are accelerated along the Earth's magnetic field lines to create an auroral display at the conjugate point, which has led documentary maker Peter Kuran to characterize these detonations as 'the rainbow bombs'. The visual effects of a high-altitude or space-based explosion may last longer than atmospheric tests, sometimes in excess of 30 minutes. Heat from the Bluegill Triple Prime shot, at an altitude of 50 kilometers (31 miles), was felt by personnel on the ground at Johnston Atoll, and this test caused retina burns to two personnel at ground zero who were not wearing their safety goggles.

Soviet high-altitude tests The Soviets detonated four high-altitude tests in 1961 and three in 1962. During the Cuban Missile Crisis in October 1962, both the US and the USSR detonated several high-altitude nuclear explosions as a form of saber rattling. The worst effects of a Soviet high-altitude test occurred on 22 October 1962, in the Soviet Project K nuclear tests (ABM System A proof tests) when a 300 kt missile-warhead detonated near Dzhezkazgan at 290-kilometre (180 mi) altitude. The EMP fused 570 kilometres (350 mi) of overhead telephone line with a measured current of 2,500 A, started a fire that burned down the Karaganda power plant, and shut down 1,000 kilometres (620 mi) of shallow-buried power cables between Tselinograd and Alma-Ata.

List of high-altitude nuclear explosions

See also Nuclear weapons testing Nuclear electromagnetic pulse Operation Argus Operation Fishbowl Outer Space Treaty Partial Test Ban Treaty Project Highwater Soviet Project K nuclear tests

References

External links "High-altitude nuclear explosions" Peter Kuran's Nukes in Space: The Rainbow Bombs Archived 2016-10-10 at the Wayback Machine – documentary film from 1999 United States high-altitude test experiences – A Review Emphasizing the Impact on the Environment Measured EMP waveform data and actual effects from high-altitude nuclear weapons tests by America and Russia American and British official analyses of photography from high-altitude nuclear explosions US Government Films:

Operation Argus Operation Dominic Starfish Prime Operation Fishbowl Operation Dominic – Christmas Island Operation Dominic – Johnston Island High-Altitude Effects – Phenomenology High-Altitude Effects – Systems Interference

Illustrations

High-altitude nuclear explosion: Hardtack-Teak, 3.88 megatons of TNT (16.2 PJ). Deployment via PGM-11 Redstone.
Hardtack-Teak, 3.88 megatons of TNT (16.2 PJ). Deployment via PGM-11 Redstone.
High-altitude nuclear explosion: The mechanism for a 400 kilometres (250 mi) high-altitude burst EMP: gamma rays hit the atmosphere between 20 and 40 kilometres (12 and 25 mi) altitude, ejecting electrons that are then deflected sideways by the Earth's magnetic field.
The mechanism for a 400 kilometres (250 mi) high-altitude burst EMP: gamma rays hit the atmosphere between 20 and 40 kilometres (12 and 25 mi) altitude, ejecting electrons that are then deflected sideways by the Earth's magnetic field.
High-altitude nuclear explosion: Late phases of TEAK fireball and formation of Northern Branch of Aurora as viewed from aircraft flying northwest of explosion.
Late phases of TEAK fireball and formation of Northern Branch of Aurora as viewed from aircraft flying northwest of explosion.
High-altitude nuclear explosion: Hardtack I Orange
Hardtack I Orange
High-altitude nuclear explosion: View of Starfish Prime through thin cloud, as seen from Honolulu, 1,300 km away.
View of Starfish Prime through thin cloud, as seen from Honolulu, 1,300 km away.

Worked examples

Example 1 — a first encounter with High-altitude nuclear explosion

Start with the simplest possible case. Write down what High-altitude nuclear explosion claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In physics, 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 High-altitude nuclear explosion 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 High-altitude nuclear explosion 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 High-altitude nuclear explosion

In research
High-altitude nuclear explosion appears in physics 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 High-altitude nuclear explosion 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
High-altitude nuclear explosion is common in secondary-school and first-year university syllabi. It links to neighbouring topics Energy weapons, Exoatmospheric nuclear weapons testing, Nuclear weapons testing, so understanding it makes those chapters shorter.
In everyday life
Look for High-altitude nuclear explosion 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 High-altitude nuclear explosion in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what High-altitude nuclear explosion 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 High-altitude nuclear explosion out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is High-altitude nuclear explosion in simple terms?

High-altitude nuclear explosions are the result of nuclear weapons testing within the upper layers of the Earth's atmosphere and in outer space. Several such tests were performed at high altitudes by the United States and the Soviet Union between 1958 and 1962.

Why does High-altitude nuclear explosion matter?

Because it connects several physics 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 High-altitude nuclear explosion?

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 High-altitude nuclear explosion.

Tags

  • Energy weapons
  • Exoatmospheric nuclear weapons testing
  • Nuclear weapons testing

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