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Comment Re:Do you really buy your own BS? (Score 1) 360

> > Since 1880, Earth’s average surface temperature has warmed by about 1.4 degrees Fahrenheit (0.8 degrees Celsius)
> In over 100 years the average has warmed 8/10's of a single degree.

This is actually a bit more than that because the chosen +0C is the average temperature during the 20th century that was reached around 1950, only 60-70 years ago:

http://static.berkeleyearth.or...

On that graph we are now at +0.8C but in 1910-20 we were around -0.4C so the last 100 year increase is more like 1.2C.

If the +0C was the average of the first measured century (1880-1980), it would be -0.2C or -0.3C.

Comment Re:No such thing in real gambling (Score 1) 340

I do not think that you realize how big is 3x10^48.
Let's imagine that a magic technology would allow you to store one permutation per atom of hydrogen.
One mole of hydrogen is 6x10^23 atoms or 12g.
So 3*10^48 atoms of hydrogen is 12*(3*10^48)/(6*10^23) = 6*10^25 g = 6*10^22 kg
That's is almost the mass of the moon (7.34*10^22 kg)

Comment Re:If you don't want to upgrade your box (Score 1) 100

Ramdisks are a not a stupid idea. They are just not useful in most cases.

Putting temporary files (e.g. /tmp) in a ram disk can be beneficial but only if you have significantly more ram than needed. That can significantly speed up tasks that are known to create lots of temporary files (e.g. compilation). This is also very interesting to prevent your (old) ssd or flash disk to wear-off too quickly.

On Linux, it is not uncommon for /run to be a ram disk (of type tmpfs). This is where most services will put small temporary and special files that need be accessed very quickly.

Comment Re:Starts to get reasonable (Score 3, Informative) 100

No! I would say: FORTUNATELY I don't think that's going to happen.

2000MB/s is still one or two orders of magnitude slower than DDR3/4 (between 20000 and 60000MB/s) so I clearly don't want direct mapping.
Let the OS cache the SSD sectors in RAM pages and everything will be fine (and from the user point of view, that won't change anything)

Comment Re:I downloaded the entire MAME library from them (Score 1) 198

MAME is a nice application but the problem is that most games were not designed for fun but to make you lose as fast as possible. Simply speaking, a cabinet game will be a lot harder than the same game for console or PC. When I was young, playing cabinet games was fun partly because I did not have a lot of money. In MAME, I can just play a few minutes, die, insert a "free" coin and continue the game to die even faster ... Boring!

MAME is still interesting for people trying to beat their high-score but not for casual gaming.

Comment Re:Investment oportunity (Score 1) 289

The more I think about it, the more I feel that this leap second system is bogus on the long term. The problem is that the 1.7 milliseconds are cummulative.

This is of course not true but for the sake of simplicity, let suppose that a second was defined according to the day length of 1900.

Around year 2000, so after 100 years, each day is now 1.7 ms longer so a whole year is 365*1.7ms = 0.62s longer. A leap second will be required every 1.6 years on average.
Around year 2100, so after 200 years, each day is now 3.4 ms longer so a whole year is 365*3.4ms = 1.24s longer. A leap second will be required every 0.8 years = 9 months on average.
Around year 2200, so after 300 years, each day is now 5.1 ms longer so a whole year is 365*3.4ms = 1.86s longer. A leap second will be required every 0.53 years = 6 months on average. ...
Around year 2900, so after 1000 years, each day is now 17ms longer so a whole year is 365*17ms = 6.2s longer. A leap second will be required every 0.16 years = 2 months on average.

There is of course no easy solution to that problem. Ideally, the second itself should be redefined regularly according to the day length.

Comment Re:Investment oportunity (Score 1) 289

According to http://en.wikipedia.org/wiki/T...

> If other effects were ignored, tidal acceleration would continue until the rotational period of Earth matched
> the orbital period of the Moon. At that time, the Moon would always be overhead of a single fixed place on
> Earth. Such a situation already exists in the Pluto–Charon system. However, the slowdown of Earth's
> rotation is not occurring fast enough for the rotation to lengthen to a month before other effects make
> this irrelevant: About 2.1 billion years from now, the continual increase of the Sun's radiation will likely
>cause Earth's oceans to vaporize,[11] removing the bulk of the tidal friction and acceleration. Even without
> this, the slowdown to a month-long day would still not have been completed by 4.5 billion years from now
> when the Sun will probably evolve into a red giant and likely destroy both Earth and the Moon.

Anyway, your formula is wrong for several reasons. The first being that slowing down the earth rotation does not reduce its day length but increases it.

So assuming that the rate of 1.7 milliseconds every 100 years will remain constant, daytime will increase by 17s every million years. That's about 1700s ~ 1/2 hour every 100 Million years or 5 hours every 1 billion years.

So when the Sun will destroy earth in 4.5 billion years, one (hot) day should take about 24+4.5*5 = 46.5 hours.

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