To get
total Joules for the planet, we need to multiply that answer by 5.1 E14 square metres, to include the total surface area.
The total joules needed to do this is around 4660 J (E = mgh).
Venus doesn't even «have a lot of energy» - in terms of
total joules of heat in it atmosphere, assuming one find a lot something which is colder one couldn't create an extraordinary amount of energy.
Use
total Joules instead of temperatures.
By the way, it is the same quantity whether it's measured in
total Joules or converted to W / m ^ 2.
Not exact matches
As the beams move through a series of amplifiers, their energy increases exponentially: From beginning to end, the beams»
total energy grows from one - billionth of a
joule to four million
joules, increasing by a factor of more than a quadrillion.
The
total energy released must have been about 3 x 1049
joules — an enormous figure compared with the Sun's output of 1026
joules per second, or the output of all the stars of our Galaxy combined, which is 1037
joules per second.
This falls well short of the
total 145 x 1020
joules per year (although the error bars do overlap).
These various contributions
total between 45 to 115 x 1020
joules per year.
Full of color, prints and great style
Joules offers quality and
total - Brit style.
In
total, one kilogram of molten basalt at a temperature of 1,350 degrees releases 2,19 million
joules of heat into the surrounding atmosphere.
One large tropical storm can release a
total heat energy from the ocean of the order of 10 ** 20
joules.
The reason is that the greater
total heat in
joules applied to the hemisphere more oriented towards the Sun during perihelion (near Sun) turns out to be cancelled by the greater heat applied to the other hemisphere during aphelion (distant from Sun).
The
total heat accumulation in the environment from 1961 to 2003 is estimated as 15.9 x 1022
Joules.
So 4.59 x 10 ^ 23
joules is about
total energy of atmosphere, but less than this is useful.
The 24X1022
Joules represent, in the scheme of things, a tiny warming of the oceans - a barely measurable
total of +0.09 C degrees over 55 years.
Have you worked out how much energy it takes to increase the
total ocean area by that many
Joules over 45 years?
To compute the effect of the interaction of changing seasonal insolation and albedo, he uses albedo data from NASA's Terra satelite, finding a
total of 3.674 x 10 ^ 24
Joules of solar energy absorbed over the Gaussian year (equivalent to 228.25 W / m ^ 2 averaged over the globe.
When I do this computation, the result is that the
total absorbed solar energy is 3.652 x 10 ^ 24
joules, and the average terrestrial albedo 0.332.
Total ocean warming pre-2000 is in the order of 5 × 10 ^ 22
Joules — apparently.
You need to look at
total HEAT (
joules), not power (watts —
joules / sec).
I do note from the Nature study «When Mount St Helens erupted in 18 May 1980, it released more than 10 ^ 18
joules of heat at once — about 20 times the
total heat flow from all the volcanoes studied in 2001»
Total Energy — Joules and ergs — The total amount of energy in various forms (kinetic, potential, magnetic, thermal, gravitati
Total Energy —
Joules and ergs — The
total amount of energy in various forms (kinetic, potential, magnetic, thermal, gravitati
total amount of energy in various forms (kinetic, potential, magnetic, thermal, gravitational)