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Satelite Meter
ΠΕΔΙΟΜΕΤΡΟ SATELITE METER
Ensuring Early Detection of Tsunamis and Acquiring Data Critical to Real-Time Forecasts - Protect Yourself From The Japanese Radiation Leak
It sounds like the stuff of a tragic fictional tale - a giant wave from out of nowhere comes crashing onto shore, sweeping away whole communities as if they were made of playing cards and tooth picks and leaving behind many dead and injured citizens. Unfortunately, these killer waves are a reality. They are called tsunami, which means "harbor wave" in Japanese. Tsunamis are oftentimes confused with tidal waves, and although, their severity has a link to tidal schedules, tsunamis are strictly caused by seismic activity.
Although most tsunamis occur in the Pacific Ocean, they can occur in any ocean. Tsunamis, which can move through the open ocean at speeds greater than 500 mph, can savagely attack coastlines, causing devastating property damage and loss of life. Areas at greatest risk are less than 25 feet above sea level and within
one mile of the shoreline. Most deaths caused by a tsunami are because of drowning. Associated risks include flooding, contamination of drinking water, fires from ruptured tanks or gas lines, and the loss of vital community infrastructure (police, fire, and medical facilities). Tsunamis can travel upstream in coastal estuaries and rivers, with damaging waves extending farther inland than the immediate coast. A tsunami can occur during any season of the year and at any time, day or night.
By definition a tsunami is a wave train, or series of waves, generated in a body of water by an impulsive disturbance that vertically displaces the water. Earthquakes, landslides, volcanic eruptions, explosions, and even the impact of cosmic bodies, such as meteorites, can generate tsunamis. Shortly after one of these events occur on the ocean floor, the water is displaced, and a tsunami is born. As a tsunami leaves the deep water of the open ocean and travels into the shallower water near the coast, it transforms. A tsunami travels at a speed that is related to the water depth - hence, as the water depth decreases, the tsunami slows, and grows in height. A ship traveling in deeper waters may not even notice a tsunami, due to its lenghened wavelength (sometimes hundreds of miles long), and amplitude of only a few feet. This also makes it unnoticable from the air.
Tsunamis have great erosional potential, stripping beaches of sand that may have taken years to accumulate and undermining trees and other coastal vegetation. Capable of inundating, or flooding, hundreds of meters inland past the typical high-water level, the fast-moving water associated with the inundating tsunami can crush homes and other coastal structures. Tsunamis may reach a maximum vertical height onshore above sea level, often called a runup height, of 10, 20, and even 30 meters.
From an initial tsunami generating source area, waves travel outward in all directions much like the ripples caused by throwing a rock into a pond. As these waves approach coastal areas, the time between successive wave crests varies from 5 to 90 minutes. The first wave is usually not the largest in the series of waves, nor is it the most significant. Furthermore, one coastal community may experience no damaging waves while another, not that far away, may experience destructive deadly waves. Depending on a number of factors, some low-lying areas could experience severe inland inundation of water and debris of more than 1,000 feet.
Twenty-four tsunamis have caused damage in the United States and its territories during the last 204 years. Just since 1946, six tsunamis have killed more than 350 people and caused a half billion dollars of property damage in Hawaii, Alaska, and the West Coast. Scientists throughout the world are continually improving tsunami warning systems as technology advances. One such system is called DART, an early detection system consisting of a surface buoy and an ocean floor device that transmit information up to a space satelite. As part of the U.S.National Tsunami Hazard Mitigation Program (NTHMP), the DART Project is an ongoing effort to develop and implement a capability for the early detection and real-time reporting of tsunamis in the open ocean. DART is essential to fulfilling NOAA's national responsibility for tsunami hazard mitigation and warnings. Project goals are:
1) Reduce the loss of life and property in U.S. coastal communities.
2) Eliminate false alarms and the high economic cost of unnecessary evacuations.
DART stations are sited in regions with a history of generating destructive tsunamis to ensure early detection of tsunamis and to acquire data critical to real-time forecasts.
You know the government isn't telling you everything! You know that the radiation from the Japanese Nuclear Reactors is getting spread across the entire planet!
Defense and Protection from Nuclear Threats (3 different books on this!)
Ways to Shield Yourself and your Family from Radiation
What Health Service Workers should do in the event of Radiation Disasters – shouldn't you know this information too?
Click Here => Radiation Safety Handbook
About the Author
This site will help you protect yourself from the Japanese Radiation Leak!
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Frequently Asked Questions...
Another Gravity Problem?
A satellite of mass 5500 kg orbits the Earth (mass = 6.0X10^24 kg) and has a period of 6500 s.
(a) Find the magnitude of the Earth's gravitational force on the satellite.
Answer in Newtons of course.
(b) Find the altitude of the satelite.
Answer in meters.
Answer:
Fc = (4pi^2mr) / T^2
Fc = (6.67x10^-11 Mm)/r^2
since the the gravity force of the earth is also the centripedal force. Set the two equation equal to each other
(4pi^2mr) / T^2 = (6.67x10^-11 m1m2)/r^2
one of the mass cancel out.
solve for r
r = cubed root of (6.67x10^-11 * m * T^2) / (4pi^2)
after you get the radius, use the second equation to find the force.
