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Tsunami

March 2005

Speed and power of a long tsunami wave, from Bernoulli's Theorem

Imagine that you're sitting in a low-flying jet just keeping pace with the tsunami in mid-ocean. You can see the ocean surface rushing past you at a speed of about 500 miles per hour. (We'll call the speed $U$.) You can't see the tsunami itself, however. Even a tsunami as energetic as the December 26th tsunami would be invisible.

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Tsunami


March 2005

Speed and power of a long tsunami wave, from Bernoulli's Theorem

Imagine that you're sitting in a low-flying jet just keeping pace with the tsunami in mid-ocean. You can see the ocean surface rushing past you at a speed of about 500 miles per hour. (We'll call the speed $U$.) You can't see the tsunami itself, however. Even a tsunami as energetic as the December 26th tsunami would be invisible.

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Tsunami

March 2005

The source of the tsunami

The real ocean-floor motion is complicated, and generates waves of many wavelengths. The December 26th tsunami was generated by a sudden large-scale vertical displacement over an earthquake area over a thousand kilometres long in the north-south direction, and a few hundred kilometres wide in the east-west direction. That is easily large enough to generate long waves.

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Exploring the Enigma


March 2005

Cryptography terminology

Plaintext: Everyday language; e.g. "This is plaintext"
Ciphertext: Enciphered language; e.g. "rgua ua xuogwerwzr"

A code is a system of secret communication in which each word in a message is replaced with another word, letter, sentence or symbol. For example:

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