Showing posts with label nature. Show all posts
Showing posts with label nature. Show all posts

Interesting Facts about Tornado


What is a Tornado?
A Tornado is a column of air violently rotating  across the earth's surface.  The column of air most frequently attached to a cloud or thunderstorm overhead, which then extends down to the ground.  Tornadoes can form into any shape, but generally form the shape of a tunnel, narrow near the bottom and larger at the top.

What causes a Tornado?
The most common cause of a tornado is from a thunderstorm.  Tornadoes form when warm, moist air or air from a  thunderstorm meets cooler, dry air creating an unstable atmosphere. After creating an unstable atmosphere, changes in wind direction and wind speed creates a spinning effect near the earth's surface, eventually forming a tunnel of wind that rapidly grows and violently rotates along the earth's surface, destroying homes and uprooting trees that are in it's path.

Where are they  most likely  to  occur?
Tornadoes are likely to occur anywhere in the world, but most tornadoes occur in "Tornado Alley," which stretches from Texas to Oklahoma, Nebraska, Kansas and into the Dakotas.  The reasoning for "Tornado Alley," is because warm, moist air from the gulf of Mexico mixes with the cooler, dry air from the north creating dangerous tornadoes.  Tornadoes can occur during any time of the year, but typically happen during the spring.



What to do in case of a Tornado-  
If you find yourself in danger of a tornado, it's important that you take shelter to protect yourself.   The safest place to be in the case of a tornado is in the basement of your house or the building that you are in.
Do not go near the walls that face in the southern or western directions, this is generally the direction tornadoes move in.  You should seek shelter under a stair case, inside a closet or under a heavy table.  You should also use a heavy blanket or trash can for protection against debris.
You may also seek shelter in the bathtub, in many homes that have been destroyed by tornadoes, the bathtub plumbing is the only thing left standing.  This is because the plumbing is anchored into the ground.  If you driving near a tornado, you should leave your car and find shelter inside, you should not keep driving, you may not know what you may encounter on the road. It's also important to realize that a car cannot outrun a tornado.


15 Facts About Tornadoes

1. In order for a vortex to be classified as a tornado, the violently rotating column of air must be in contact with both the cloud above and the ground below.


2. Though tornadoes do occur on other continents, North America’s geography makes it more vulnerable to them. Bradley Smull, an atmospheric scientist at the National Science Foundation, explained yesterday in a Washington Post online chat: “In particular, the proximity of a major north-south mountain range…and the Gulf of Mexico…all in a latitude range frequented by strong upper-level jetstreams amounts to something of a “perfect storm” for severe (supercell-type) thunderstorm formation.”

3. Tornadoes are rated on the Enhanced F (EF) Scale (the old scale was called the Fujita (F) Scale), which assigns a number (0 to 5) based on estimates of 3-second wind gusts and damage. There have been more than 50 F5/EF5 tornadoes recorded in the United States since 1950.

4. Rain, wind, lightning and/or hail may accompany a tornado, but none of them is a reliable predictor of an oncoming tornado.


5. A tornado can last from a few seconds to more than an hour. On average, they persist for about 10 minutes.

6. It is a myth that a tornado cannot pass over features like valleys, mountains, lakes and rivers. When it passes over a lake or river, a tornado becomes a waterspout.

7. Tornado alley is the region in the middle of the United States where tornadoes are most frequent. However, every U.S. state and every continent (except Antarctica) has experienced a tornado.

8. A tornado watch means that conditions are ripe for a tornado; a warning means that a storm has been spotted on the ground or via radar (and you should take cover immediately).

9. Since the first tornado forecast was made in 1948, tornado warning lead times have been increasing and now average 13 minutes. However, they have a 70 percent false alarm rate, which may lead some people to take them less seriously than they should.

10. Mobile homes aren’t more likely to get hit by a tornado than any other type of building, but their flimsy structure provides little protection against strong winds and flying debris.


11. It’s also a bad idea to take shelter in a car—which can be easily tossed about—or under a bridge, where a person would be vulnerable to flying debris or a bridge collapse.

12. The single deadliest tornado killed 695 people in Missouri, Illinois and Indiana on March 18, 1925. The series of tornadoes that struck Tuscaloosa, Alabama and other Southern states in April 2011 set a new record. According to NOAA, there were 312 recorded tornadoes that touched down from 8 a.m. on April 27 through 8 a.m. on April 28. The death toll these storms was over 250 people, and did not break the 1925 record mentioned above.

13. A tornado that struck Washington, D.C. on August 25, 1814, is credited with driving the British invaders out of the city and preventing them from carrying out further destruction. They had burned the White House and much of the city the day before.


14. The city of Greensburg, Kansas was flattened by a tornado in 2007, but instead of abandoning the town, the people are rebuilding with an emphasis on green technology.

15. In 2009 and 2010, more than 100 scientists participated in VORTEX2 (funded by the National Science Foundation and National Oceanic and Atmospheric Administration), which set out to track tornadoes as they formed and moved across the landscape. The V2 researchers are trying to answer many basic questions about tornadoes, such as how, when and why they form, how strong the winds get near the ground, how they do damage, and how predictions can be improved. During the two years, they collected data from dozens of storms and tornadoes. In order for a vortex to be classified as a tornado, the violently rotating column of air must be in contact with both the cloud above and the ground below.

Interesting Video about Tornado

Tornado Destruction


Family's surveillance cameras rolling as tornado hits West

Largest tornado ever recorded? 2.5 miles wide! Hallam, Nebraska 2004

Tornado Watch - Girls Swimming - Baby Having Fun - VLOG - Beach Plan Fail - Bad Prank

BEAUTIFUL tornado in New Zealand!!

Planeta zywiolów - Tornado (Cz.1/5)

Australia Tornado 'Was Frightening'

Tornado en Tuscaloosa Familia Duarte

Australian driver races for his life against massive tornado in Victoria

Tornado Chasers Needs Your Help!

source: www.uvm.edu; blogs.smithsonianmag.com


Interesting Facts about Tsunami



  • On July 12, 1993 a magnitude 7.8 earthquake in the Sea of Japan produced tsunami that totally destroyed the southern half of Okushiri Island. Waves were greater than 30 feet and some could have been 100 feet. The earthquake was about 50 miles offshore and the tsunami arrived within minutes. 120 people died.
  • The states most at risk for Tsunami are California, Hawaii, Oregon and Washington. Hawaii is at greatest risk and they have about 1 tsunami a year and a dangerous tsunami about every 7 years.
  • On March 28, 1964 an extremely large earthquake (magnitude 8.4) struck Alaska. It caused tsunami waves that were very destructive in southeastern Alaska, in Vancouver Island, Canada, and in the States of Washington, California and Hawaii. Waves ranged in size from 6 to 21 feet. The tsunami killed more than 120 people and damages costing more than $106 million. It was the costliest tsunami ever to strike the Western United States and Canada.
  • Although a large asteroid impact is highly unlikely, scientists studying the possibility have decided that a moderately large asteroid or about 5-6 km in diameter falling in the middle of the Atlantic Ocean, would generate a tsunami that would travel all the way to the Appalachian Mountains in the upper two-thirds of the United States. Coastal cities would be wiped out by such a tsunami.
  • Nuclear explosions could possible create tsunami but none have ever been generated from testing yet. Furthermore, such testing is currently banned by international treaty.



 What causes a tsunami?
When an undersea earthquake or other major disturbance causes a section of the ocean floor to suddenly rise or sink, the mass of water above the affected area also rises or sinks. This unexpected movement of the water creates a series of powerful waves.
Undersea earthquakes that cause massive changes to the ocean floor and the displacement of a large volume of water are the most common cause of a tsunami.
Tsunami can also be caused by other undersea events such as volcanoes or landslides
A tsunami can also be caused from events above the ocean floor. These events could include a meteorite crashing into the ocean, major landslides near a coastline or material from an erupting volcano forming a landslide. The impacts of tsunami triggered this way tend to be localised.
More than 75 per cent of tsunami are caused by undersea earthquakes.


Where do tsunami occur?
Most tsunami occur in the Pacific and Indian Oceans. The boundary of the Pacific Ocean experiences frequent earthquakes. This boundary is commonly known as the Ring of Fire. There are two major subduction zones in the Indian Ocean that can also generate tsunami.
Subduction zone earthquakes are the most common source of destructive tsunami. These earthquakes are generated when two tectonic plates meet and one goes under the other, usually at a rate measured in centimetres. The sinking (subducting) plate drags against the upper plate, causing flexing. Continued stress on the plate boundary results in the upper plate rebounding to its original position, displacing the sea water above.
The Questacon Tsunami show includes a demonstration of this process (between the 8 and 16 minute mark). 


Sumatra earthquake and tsunami, 26 December 2004
In the case of the December 2004 earthquake off Indonesia, the tsunami was generated 10 minutes after the event when the displaced sea surface spread outward from the epicentre as a tsunami. In this illustration, the red arrows indicate the direction in which the upper plate is deformed due to drag and release of the lower plate. (Copyright Geoscience Australia)

A Tsunami can really move!
In the deep water of the ocean, the waves that are created have a large wavelength but are not usually bigger than one metre tall. A tsunami wave may be hundreds of kilometres in length and it moves at a high speed across great distances without losing much of its energy.
Tsunami waves move out from where a large body of water has been disturbed, similar to the way ripples move away from the place where a rock has been dropped into a pond.
In the open ocean, a tsunami can travel as fast as 950 kilometres per hour, which can be represented by the speed of a passenger jet. It loses speed as it approaches land, but it does not lose much of its energy. As it slows down, the height of the waves build.

How big is a tsunami?
In the open ocean it can be difficult to notice a tsunami wave. However, as a tsunami wave approaches land and moves into more shallow water, the leading edge of the wave slows down but the back of the wave is still travelling at its original speed. This causes the water to bunch up and increase the wave height. This is known as ‘shoaling’. When it reaches land, it may behave like a series of breaking waves or a large, powerful wave.
The tremendous energy of the wave can cause great quantities of water to surge inland, far beyond where even the highest of tides would commonly reach.
Some of the largest tsunami waves have been generated by the volcanic eruption of Krakatoa in 1883. This tsunami reached a height of 37 m. In 1737, a tsunami was estimated to be 64 m high as it struck Cape Lopatka in northeast Russia
.

Tsunami waves are different from normal waves
Tsunami are different from normal waves. Normal waves are generated by the wind and it is only the water near the surface that is moving. In a tsunami all the water from surface to sea bed is moving and the movement has been generated by something (usually an earthquake) that has displaced water. In the open ocean, tsunami create little movement and little threat to shipping.
When a tsunami wave reaches the shore, its wavelength might be more than 100 km.  Tsunami can last for several hours or even days depending on location. This is much different to the waves that we are used to seeing at the beach. Typical ocean waves usually last for less than a minute and have a wavelength of 100 m.
The energy behind a tsunami can strip sand off beaches, undermine trees, and crush buildings.
People and boats are powerless against the force of a tsunami. The amount of water carried inland is capable of inundating vast areas of normally dry land.

Case studies

Chile tsunami 27 Feb 2010
This tsunami followed an earthquake measuring 8.8 on the Richter Scale. The epicentre of the earthquake was 115 km NNE of Concepcion. The epicentre of this quake was 230 km north of the largest earthquake ever recorded (9.5 in 1960). This quake was the result of movement between the Nazca Plate on the eastern side of the Pacific Ocean and the South American Plate. The first waves hit about 34 minutes after the earthquake. Properties and businesses were damaged and over 200 lives were lost.

Samoa tsunami 29 September 2009
At 6.49am an earthquake measuring 8.0 on the Richter Scale triggered this tsunami. The earthquake epicentre was located on the Pacific tectonic plate near its boundary with the Australian Plate approximately 200 km south of Samoa. Dozens of magnitude 4 and 5 aftershocks followed the initial earthquake, continuing through the next day. This area, near the Tonga Trench, is one of the most active earthquake regions in the world. The tsunami struck the islands of Savi’i, Upola, and Tutuila minutes later with waves that were approximately 3 m high. Smaller tsunami hit other Pacific islands farther away from the earthquake’s epicentre. The tsunami caused a great amount of damage to property and the natural environment and caused the death of over 100 people.


Solomon Islands tsunami 2 April 2007
On 2 April 2007 an earthquake measuring 8.1 on the Richter Scale had its epicentre 350 km NW of Honiara. The earthquake occurred in shallow water in the early morning and was quickly followed by a tsunami. The waves were up to 10 m high. Over 50 deaths were reported and thousands were left homeless. A tsunami warning was issued for Australia and Alaska 15 minutes after the earthquake. 

Indian Ocean tsunami, 26 December 2004
This event was one of the most devastating caused by a natural hazard in recent years. The earthquake that triggered the tsunami occurred west of the Indonesian island of Sumatra and measured 9.0 on the Richter Scale, making it the largest earthquake worldwide in 40 years. The death toll in March 2005 was over 273 000 people, with many still missing.

Papua New Guinea tsunami 17 July 1998
An earthquake measuring 7.0 on the Richter Scale just off the northern coast generated a destructive tsunami. Waves up to 10 m high hit the villages in the Aitape region extremely quickly. More than 2000 people were killed and there was great damage to buildings and farmland.

Tsunami Thailand (Koh Phi Phi) - 2004


Japan 2011 Tsunami Video - See The power !!


Khao Lak Tsunami

source: www.ema.gov.au;  library.thinkquest.org; youtube.com