Boy, there's nothing like good fiction!
And that was nothing like good fiction.
Transport layer winds along the U.S. East coast run predominately West to East, save for localized circulation around fronts. Depending on the heat (aka yield) of the above-ground device, the plume could also reach the jet stream, which, again, runs West to East, albeit considerably faster.
Given a week's worth of transport, the debris plume from a small non-boosted device, say in the yield range of 5-10KT, would most likely transit far out into the Atlantic Ocean after detonation in Manhattan. Note the movement of the debris cloud after this above-ground nuclear test in Nevada on 1 April 1952. The numbers represent midnight GMT on that given day:
Can you guess what branch of the DoD gets paid to simulate and run domestic events of nuclear terrorism over and over again, using meteorological modeling and data accumulated during previous nuclear events? Then I get to go intercept the cloud repeatedly. And we practice the latter part of the mission exhaustively. Funny thing is, depending on the dispersion and transport rate, we're often concerned that the plume doesn't stay concentrated long enough for us to get a good sample.
And that was nothing like good fiction.
The radioactive cloud continues southward, along the Atlantic seaboard.
Transport layer winds along the U.S. East coast run predominately West to East, save for localized circulation around fronts. Depending on the heat (aka yield) of the above-ground device, the plume could also reach the jet stream, which, again, runs West to East, albeit considerably faster.
Given a week's worth of transport, the debris plume from a small non-boosted device, say in the yield range of 5-10KT, would most likely transit far out into the Atlantic Ocean after detonation in Manhattan. Note the movement of the debris cloud after this above-ground nuclear test in Nevada on 1 April 1952. The numbers represent midnight GMT on that given day:
Can you guess what branch of the DoD gets paid to simulate and run domestic events of nuclear terrorism over and over again, using meteorological modeling and data accumulated during previous nuclear events? Then I get to go intercept the cloud repeatedly. And we practice the latter part of the mission exhaustively. Funny thing is, depending on the dispersion and transport rate, we're often concerned that the plume doesn't stay concentrated long enough for us to get a good sample.