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Hypercane: Difference between revisions

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==Physical description==
==Physical description==
Hypercanes would have wind speeds of over {{convert|800|km/h|mph}}, and would also have a central pressure of less than {{convert|700|hPa|inHg|abbr=off|lk=on}}, giving them an enormous lifespan.<ref name="MIT" /> The extreme conditions needed to create such a storm could conceivably produce a system up to the size of [[North America]], creating [[storm surge]]s of {{convert|18|m|ft|abbr=off|lk=off}} and an eye nearly {{convert|300|km|mi|abbr=off|lk=off}} across. The waters could remain hot enough for weeks, allowing more hypercanes to be formed. A hypercane's clouds would reach {{convert|30|km|mi}} into the [[stratosphere]]. A hypercane would also damage the earth's [[ozone]].<ref name="MIT" /> The reason for this is the water molecules sent up into the [[ozone]] layer merge with the [[ultraviolet light]] repelling particles and disintegrate the particles, creating a hole in the vicinity. Other scientists  have theorized that the system, compared to a normal [[hurricane]], would be considerably smaller, about 10 miles in diameter. This would more comparable to a [[tornado]], which can top out to about a mile and a half in diameter.
Hypercanes would have wind speeds of over {{convert|800|km/h|mph}}, and would also have a central pressure of less than {{convert|700|hPa|inHg|abbr=off|lk=on}}, giving them an enormous lifespan.<ref name="MIT" /> The extreme conditions needed to create such a storm could conceivably produce a system up to the size of [[North America]], creating [[storm surge]]s of {{convert|18|m|ft|abbr=off|lk=off}} and an eye nearly {{convert|300|km|mi|abbr=off|lk=off}} across. The waters could remain hot enough for weeks, allowing more hypercanes to be formed. A hypercane's clouds would reach {{convert|30|km|mi}} into the [[stratosphere]]. A hypercane would also damage the earth's [[ozone]].<ref name="MIT" /> The reason for this is the water molecules sent up into the [[ozone]] layer merge with the [[ultraviolet light]] repelling particles and disintegrate the particles, creating a hole in the vicinity. Other scientists  have theorized that the system, compared to a normal [[hurricane]], would be considerably smaller, about 10 miles in diameter. This would more comparable to a [[tornado]], which can top out to about a mile and a half in diameter.
==Controversy==
As many theories circulate about the demise of the [[dinosaurs]], only one holds true.  The most popular, however, is that a meteor, spanning the size of [[North America]], struck mid land pre continental drift. The impact drove debris and dust particles into the atmosphere, causing a blackout.  The lack of [[sun]] lead to the decay of most if not all of the earth’s [[biomass]].  Any prehistoric beings that had not died  during the initial impact, soon gave way to starvation.
The discovery of [[meteorites]] off the coast of [[Africa ]]disputes this.  With the newly found evidence, it is now believed that the meteor instead struck the [[ocean]].  The dramatic rise in temperature set forth optimal conditions for the creation of the only known hypercane in existence.  As the hypercane tore through the [[continents]], the debris it pulled into the atmosphere caused a blackout effect.  Most of the worlds biomass, and living inhabitants fell prey to the hypercane itself, and not the ensuing [[ice age]], which prevented life from inhabiting our planet for quit some time.


==References==
==References==

Revision as of 16:06, 26 August 2008

A hypercane is a hypothetical class of extreme tropical cyclone that could form if ocean temperatures reached around Template:Convert/°C —15° higher than the warmest ocean temperature ever recorded[1]— which could in turn be caused by a large asteroid or comet impact, a large volcanic or supervolcanic eruption, or very extensive global warming.[2] There is some speculation that some dinosaurs might have been killed off by a series of hypercanes, resulting from an asteroid or comet crashing into Earth.[3] The term was coined by atmospheric scientist Kerry Emanuel in 1994, at MIT.[4][5]

Physical description

Hypercanes would have wind speeds of over Template:Convert/km/h, and would also have a central pressure of less than Template:Convert/hPa, giving them an enormous lifespan.[4] The extreme conditions needed to create such a storm could conceivably produce a system up to the size of North America, creating storm surges of 18 metres ({{rnd/cTemplate:Rnd/b|59|(1−1)|0}} ft) and an eye nearly 300 kilometres ({{rnd/cTemplate:Rnd/b|190|(1−2)|0}} mi) across. The waters could remain hot enough for weeks, allowing more hypercanes to be formed. A hypercane's clouds would reach 30 kilometres ({{rnd/cTemplate:Rnd/b|19|(1−1)|0}} mi) into the stratosphere. A hypercane would also damage the earth's ozone.[4] The reason for this is the water molecules sent up into the ozone layer merge with the ultraviolet light repelling particles and disintegrate the particles, creating a hole in the vicinity. Other scientists have theorized that the system, compared to a normal hurricane, would be considerably smaller, about 10 miles in diameter. This would more comparable to a tornado, which can top out to about a mile and a half in diameter.

References


Template:Tcportal

Template:Weather-stub