| 1. | The radar pulse is generated from the bullet's kinetic energy by a process known as magnetic flux compression.
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| 2. | Consider a radar pulse emanating from a radar beacon traveling downwards and interacting with a flat ocean surface.
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| 3. | The radar altimeter measures the return power of the radar pulse that's reflected off the land / ocean surface.
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| 4. | A beam 1 ^ o wide will illuminate millions of square feet of surface by the time the radar pulse reaches.
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| 5. | The bullet emits a radar pulse as it grinds to a halt, offering a safe and efficient way of finding landmines.
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| 6. | Unfortunately, it is exceedingly difficult to verify that we have detected an ET radar pulse as opposed to a human-generated transmission.
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| 7. | The radar pulse train is used to modulate a radar carrier, the typical spectrum shown on the left will be obtained.
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| 8. | The following figure shows an illustration of the vertical cross-section and top-down view of the radar pulse ( adapted from ).
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| 9. | In its ultimate incarnation, each radar pulse is sent out on a different frequency and therefore renders single-frequency jamming almost impossible.
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| 10. | First, the radar footprint is covering less area so it so the radar pulse emitted by the satellite requires much less power.
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