Weapons of Mass Destruction and Global Climate Change Prof. Lynn R. Cominsky SSU Department of Physics & Astronomy.

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Presentation transcript:

Weapons of Mass Destruction and Global Climate Change Prof. Lynn R. Cominsky SSU Department of Physics & Astronomy

Talk Outline Hiroshima and Nagasaki Nuclear Weapons Proliferation Nuclear Weapons Effects Regional Nuclear Conflicts Nuclear “Autumn”? Conclusions

Hiroshima and Nagasaki Approximately 15 kilotons of equivalent TNT were dropped by the U.S. on each city during World War II This is “small” by today’s standards - modern warheads are ~100 kTons 13 square kilometers were burned in Hiroshima Ground level view of Hiroshima cloud

Hiroshima after the bomb August 6, 1945 – Courtesy of Richard Turco, UCLA

Who has nuclear weapons? US (1800) Russia (2700) UK (55.5) France (91.5) China(400) All numbers in Mtons India(tests) Pakistan(tests) Thermonuclear Fission N. Korea Israel (tests)

Who can make nuclear weapons? Brazil (200) Argentina (1100) North Korea (10-20) South Korea (4400) Pakistan (100+) India (1000+) Up to 45 countries have the potential or are already nuclear states Assumes Hiroshima-sized atomic weapon

Iraq Iran Libya Algeria Syria Chechnya (old USSR?) Other players… Belarus Ukraine Kazakhstan South Africa May want weaponsRenounced weapons

Physical Effects of Nuclear Weapons 15 kTons by automobile 15 kTons by airplane Google “Nuclear Weapons Effects Calculator” – provided by the Federation of American Scientists

Physical Effects of Nuclear Weapons Thermal (Red circle) Intense heat from the explosion will likely cause widespread fires within this region. Pressure Blast Wave Blue circle: Most homes are completely destroyed and stronger commercial buildings will be severely damaged due to the high pressure blast wave in this region. Yellow Circle: Moderate damage to buildings causing some risk to people due to flying debris is caused by the blast wave in this region.

Abandoned area from Cherynobyl accident This wasn’t even a bomb! From Toon et al km

Regional Nuclear Conflicts Based on work presented at AGU 2006 by Toon, Robock, Turco, Fromm, Jensen et al. Imagine a scenario where two nuclear powers start a regional war – e.g. India and Pakistan Each country sends about 50 Hiroshima-sized nukes at the others’ largest cities At least 5 million people die immediately -- as many fatalities as once projected for a full scale “strategic” war between the superpowers The deaths per kTon are 100 times greater for small yield weapons than for large ones

Regional Nuclear Conflicts Up to 5 million tons of soot loft into the atmosphere from the resulting firestorms Soot spreads around the world, darkening the skies and lowering the temperature by 1.25 o for up to a decade, disrupting food supplies and the ozone layer Although not as dramatic as the original Nuclear Winter predicted by an all-out war between super-powers, this type of regional war would still have significant environmental impacts

Combustible material in cities Bangalore, India inner city Nashville, TN suburb Each image is 1 square km = 1/13 of area destroyed in Hiroshima Each person in a mega-city contributes about 11 tons of combustibles From Turco et al. 2006

Soot spreading around the world From models by Alan Robock, Rutgers University 0.1 means 90% of sunlight gets through

Anti-greenhouse effect Smoke layer From Toon et al. 2006

Global cooling Time in years From Robock et al. 2006

Mass starvation Lower temperatures  less evaporation from oceans  less rainfall  drought  food supply disruption all over the world From Robock et al. 2006

Conclusions Nuclear weapons capabilities continue to spread throughout the world, despite existing non-proliferation treaties Even a “small” regional nuclear war can have catastrophic consequences that affect the entire globe Nuclear proliferation must be stopped and access to nuclear materials must be controlled and monitored

Additional Resources Carnegie Endowment for International Peace Federation of American Scientists The Why Files: Cold Cuts Science News: Sudden Chill A. Robock, L. Oman, G. L. Stenchikov, O. B. Toon, C. Bardeen, and R. P. Turco “Climatic consequences of regional nuclear conflicts” Atmospheric Chemistry and Physics Discussions 6 (Nov. 22, 2006): Available at: pdf pdf

Additional Resources Owen B. Toon, Richard P. Turco, Alan Robock, Charles Bardeen, Luke Oman, Georgiy L. Stenchikov “Atmospheric Effects And Societal Consequences Of Regional Scale Nuclear Conflicts And Acts Of Individual Nuclear Terrorism” Atmospheric Chemistry and Physics Discussions 6 (Nov. 22, 2006): Available from: pdf pdf Nuclear weapons effects calculator from the Federation of American Scientists: d=367 d=367

Backup Slides

Enriching Uranium in Iran As of 2003, Iran was developing an extensive, underground enrichment facility for Uranium Most of the centrifuges (up to 50,000) are underground, in order to withstand aerial attack – only 1-2% would be needed to make sufficient quantities of highly enriched U for a weapons program Iran’s stated goal for this facility is production of sufficient low-enriched U to generate 6000 MW electricity through power plants

2003 Image of Natanz, Iran

North Korean Nuclear Test On October 10, 2006 North Korea reported its first underground nuclear test, indicated by a small (~4 th magnitude) earthquake Estimates are that this blast measured only ~0.5 kilotons – very small compared to other first weapons tests Likelihood is that it was a “fizzle” or even a conventional weapons blast – only time will tell if radio-isotopes emerge.

Are we in danger from N Korea? In order to threaten the US, North Korea must have: Working nuclear warhead (uncertain) Working long range delivery system – yet Taepodong-2 missile test failed in July – and if it worked, could only hit Alaska Working electronics triggering for bomb (no evidence yet) Intent to actually bomb another country (no clear evidence but entirely possible)