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| Full Void Melee vs. other str bonus armour |
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HIGH DEF -add "&fmt=18" onto end of url
--Sorry about the lack-of-action... I didn't
want my video to be too long (I personally
hate the really long videos). A few editing
errors....
-=-=-=-=-=-DISCLAIMER-=-=-=-=-=-
[If you use this, please credit Fantikerz]
RuneScape is a registered trademark of JaGeX
Limited. I do not claim, or have any,
affiliation with JaGeX Ltd. This video was
not intended for any personal gain, only for
entertainment purposes. All comments by
others are their own and I do not take
responsibility for their actions. Consider
this, free advertising
http://www.runescape.com/
All other trademarks (such as music), are
property of their respected owners, I do not
claim to own any rights to the trademarks.
Music is simply used as the base of the
video, I do not own any rights to the tracks,
I tend to use music that I/others like, so
feel liked if your music has been used. If
you have any concerns, DONT HESITATE to
contact me! Thank you for reading this, and
enjoy the video!
Ignore this --
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Tags : RuneScape Void Melee Comparisons compare fullvoid jagex rs sexy lesbians fucking licking eachothers pussy while shitting on Cutter631's face whereafter Maxboison scoops it up with an ice cream cone |
|
Affichage : 3184
Durée : 190 s |
| Clinton 2.0 |
 |
Hello, Internet.
We are Clinton.
By Hugh Atkin.
http://hmatkin.blogspot.com
A Sledge Video.
http://abc.net.au/unleashed
Tags : gaunse esoterica whereafter |
|
Affichage : 62883
Durée : 150 s |
| Heat equation, take 2 |
 |
I've further implemented code to manage
different electron-beam events. Now you can
give it beam parameters at different times;
electron-beam energy and electron number is
converted to heat inside the slab at specific
geometrical coordinates with different
electron density distributions.
In this example, the electrons penetrate the
slab in a cylinder distribution form with
uniform density from the slab surface (z=0)
until z=zmax/2=16/2=8 units. 1E22 electrons
are converted to heat each second (ns
actually) in that cylindrical space between
t=10 and t=100, whereafter you can see it
even out by diffusion.
Blackbody radiation is there but the time is
much shorter than the last example and here
the initial temperature of the slab is close
to the ambient temperature, so BB effects are
not noticable.
Lastly, Temperature Strength is now an
average over z-axis.
Update: code now available -
http://www.geocities.com/wombofwoe/
Tags : heat diffusion equation 3D physics matlab |
|
Affichage : 897
Durée : 66 s |
| TNT Ella-Mugen #1: Dio/Sakura |
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Somewhere in a quiet village in Colorado,
there lived a six year old girl. She was
tormented by her parents in that miserable
home of hers, for she was what they call an
"accident". Her name was Ella.
One day, Ella sat on a half-torn sofa when
her father, Dio Brando, passed through with a
bag filled with firearms. He was planning a
robbery with Ella's mother, Sakura. "What's
that?" she asked, whereafter Dio hissed it's
none of her business. Then he tripped over
one of Ella's toy trains and dropped the bag,
causing one of the guns to go off.
Infuriated, Dio grabbed a chair and threw it
at the child, then rushed out to continue his
plan.
That should have been a fatal blow to Ella,
but just she was about to die (or just after?
Who knows), a dark force emnated from Ella's
body, shattering the chair and everything
else in the room. She was changing. Her
ability to think was changing. Consumed by
both hatred and fear, Ella rushed forth to
catch up with her parents and massacre them.
----------------
Gee wizz, I decided to join in the fad,
complete with elaborate intro and Movie Maker
effects. The first match consists of two
rounds, one against Sakura and one against
Dio (whose download link I will dig up if
it's highly requested). It's like a team
battle, except Ella has max health for each
round.
Sakura is just awesome. Kick-ass AI,
animation, supers, whatever. My only
complaint is that Hadouken that forms an
almost flawless keep-away barrier. It needs
more lag time.
Dio wasn't a challange, considering he has no
AI. Still, it was an awesome match overall.
The stage is from either Mugenfury,
Mugenation or Randomselect (sorry). The music
is Rayman 2 - Rocketrun, and if you don't
like it, you can take your whiny snivveling,
snotnose population, form a line behind me
and kiss my...wait...can't say that on
YouTube...
Tags : mugen ella |
|
Affichage : 2525
Durée : 140 s |
| the amusement park at wonder valley |
 |
the dangerous water ride, whereafter
whosoever rode it, complained of horrible
body pains, muscle pulls and neck catches ,
make any sense? no. I thought as much.
Tags : dangerous |
|
Affichage : 2404
Durée : 16 s |
| Hurricane Dean - 2007 |
 |
Hurricane Dean was a powerful tropical
cyclone of the 2007 Atlantic hurricane
season. It was the most intense Atlantic
hurricane since Hurricane Wilma of 2005, and
tied for seventh most intense Atlantic
hurricane ever recorded as well as the third
most intense Atlantic hurricane ever at
landfall. A Cape Verde-type hurricane, Dean
took a west-northwest path through the
Caribbean Sea, passing just to the south of
Jamaica on August 20, making landfall in the
Yucatán on August 21, and a second landfall
near Tecolutla, Mexico, on August 22 after
crossing the Bay of Campeche. At least 42
deaths have been reported and insured damage
is estimated at about $6.6 billion (USD).
Dean was the first hurricane to make landfall
in the Atlantic basin at Category 5 intensity
in 15 years; the last storm to do so was
Hurricane Andrew on August 24, 1992. Although
Dean was much larger than Andrew, its
Category 5 landfall was in a more sparsely
populated area and thus far less damaging.
-- Storm History --
On August 11, 2007, a tropical wave moved off
the west coast of Africa, and, encountering
favorable conditions, quickly developed into
Tropical Depression Four about 520 miles (835
km) west-southwest of Cape Verde. The
depression moved briskly westward, and was
upgraded to Tropical Storm Dean at 1500 UTC
on August 14. The storm's intensity continued
to build although dry air and cooler air
inflow from the north were slowing structural
development. Ragged bands formed on August 15
and the formation of a partial eyewall was
observed later that day.
Intensification continued and the storm was
upgraded to Hurricane Dean at 5 a.m. EDT
(0900 UTC) August 16. The deep-layered ridge
to the north continued to steer the system
west, towards the Caribbean Sea. The storm
quickly strengthened to a Category 2
hurricane on the Saffir-Simpson Hurricane
Scale. The storm's development slowed
slightly but a reconnaissance aircraft
discovered a closed eyewall on August 17 as
the storm passed through the Lesser Antilles.
Data from the aircraft indicated that
Hurricane Dean had strengthened to a Category
3 hurricane and its trailing bands were still
over the Lesser Antilles. During the evening
of August 17 Dean strengthened into a
Category 4 hurricane and continued to
steadily grow in both size and intensifying
through the night. On August 18 the presence
of a double eyewall was noted, indicating an
eyewall replacement cycle and causing short
term fluctuations in intensity. These
fluctuations did not affect the storm's well
defined satellite presentation.
Operationally, Dean was thought to have only
been a Category 4 on the 18th, but post-storm
analysis shows that Dean had become a 165 mph
(266 km/h) Category 5 that day before
weakening. Dean weakened very slightly on
morning of August 19 as it finished the
eyewall replacement cycle and began to
interact with the island of Jamaica
Hurricane Dean passed south of Jamaica on the
evening of August 19 and began to intensify
again that night. Its eyewall replacement
cycle was thought to be completed. A
concentric eyewall was briefly observed again
on the morning of August 20, but did not last
long. The hurricane, still tracking
west-northwest under the influence of a
strengthening deep-layered high pressure
system to the north, moved over waters with
extremely high heat content and began to
strengthen once again. The eyewall became
even better defined throughout the day, and,
at 8:35 p.m. AST on August 20 (0035 August
21, UTC), Dean restrengthened to a Category 5
hurricane, the highest rating on the
Saffir-Simpson Hurricane Scale. It made
landfall as a Category 5 storm in Quintana
Roo's Costa Maya region, some 65 km (40 mi)
northeast of the border between Mexico and
Belize, and weakened on its way over land,
reemerging on the western side of Yucatán as
a Category 1 storm. Dean regained strength as
it crossed the Gulf of Mexico, and made its
second landfall as a Category 2 storm on 22
August, at around 11:30 CDT, near Tecolutla,
Veracruz, to the south of Tuxpan, whereafter
it moved westward, losing strength and mostly
disintegrating over central Mexico. A small
remnant circulation did enter the far east
Pacific, eventually moving northwestward
around an anticyclone, roughly parallel to
the Mexican coast and finally back inland
over the southwestern United States, where it
completely dissipated on 27 August.
Most intense Atlantic hurricanes
Intensity is measured solely by central
pressure Rank
Hurricane Season Min. pressure
1 Wilma 2005 882 mbar (hPa)
2 Gilbert 1988 888 mbar (hPa)
3 "Labor Day" 1935 892 mbar (hPa)
4 Rita 2005 895 mbar (hPa)
5 Allen 1980 899 mbar (hPa)
6 Katrina 2005 902 mbar (hPa)
7 Camille 1969 905 mbar (hPa)
7 Mitch 1998 905 mbar (hPa)
7 Dean 2007 905 mbar (hPa)
10 Ivan 2004 910 mbar (hPa)
Tags : Hurricane Dean Lesser Antilles Greater 2007 Belize Honduras Mexico Dominica Dominican Republic Haiti Jamaica Nicaragua |
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Durée : 54 s |
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