Sentences with phrase «joules =»

Energy: Energy before atmospheric entry: 1.99 x 1021 Joules = 4.74 x 10 ^ 5 MegaTons TNT The average interval between impacts of this size somewhere on Earth during the last 4 billion years is 2.6 x 10 ^ 6 years

1 joule = 1 watt second 5.1 e +14 earth area m ^ 2 240 watts / m ^ 2 surface insolation 1.224 e +17 joules / second 31557600 sec / year 3.86265024 e +24 joules per year

Not exact matches

A 1 GW reactor running at 60 % efficiency will need 1 GW * 3600 second * 24 hours / 0.6 = 1.44 Joules worth of energy from fuel per day.

:) < a href = «http://stylebyjoules.com"> Style by Joules

Latent heat to melt ice: 355,000 joules / kg x 1,000 kg / cubic meter x 10 ^ 9 cubic meter / cubic km = 3.55 x 10 ^ 17 joules to melt one cubic kilometer of ice.

28 Earth's Heat Gain During the Past 50 years (10 21 Joules *) Oceans = 145 (84 %) Continents = 10.4 (6 %) Earth's Ice = 8.1 (5 %) Atmosphere = 6.6 (4 %) * A joule is a unit of heat energy

ΔT = q / C, where q is heat in joule an C is heat capacity.

Knowing that there is no escape from THE FOUR LAWS WITHOUT WHICH NOTHING WHATSOEVER IN THE UNIVERSE THAT HAPPENS, HAPPENS — there simply is no change in temperature of anything without input of energy = work = quantity of heat, requiring accountancy in joule, and not that «phlogiston» of «feedback» without any energy dimension.

From Energy Units we have (approximately) 1 calorie = 4.19 joules (J), 1J = 1 watt second and 1 calorie is sufficient to raise the temperature of 1 ml of water by 1 degree Celsius.

Divide that by the Hiroshima estimate above = 378,923,076 joules.

Since ARGO measurements started in 2003 the first estimate in 2008 showed slight upper ocean cooling; the corrected and extended estimate shows around 2 x10 ^ 22 Joules warming = around 0.02 C (0 - 700m)

Units: yr = year, J = joules, mm = millimeters.

paper that seems to have had such an effect on Joules Verne, some numbers might be useful: h = kb * T / (m * g) = 9.08 km for N2 at 300K λ = 68nm at 101325 Pa To get λ ~ 0.01 h where the deviation from the Fourier Law is ~ 10 % requires a reduction of pressure of 11 orders of magnitude to ~ 1E - 6Pa or an increase of g of a similar magnitude or some combination of both that increases λ and reduces h. I'm not going to touch the temperature gradient as that's even worse.

The total joules needed to do this is around 4660 J (E = mgh).

(ZJ = zettajoules = 1e21 joules).

That last attempt took the middle ground of allowing both P and V to increase, which I associated with a specific heat for air of 25 joules / mole / K, intermediate between cv = 21 and cp = 29 for air.

The latent heat of vaporization of water being 2260 J / g, condensation of 0.3 g releases 0.3 * 2260 = 678 joules.

Energy can't be measured closer than 1/2 (6.626) = 3.313 * 10 ^ -LRB--34) joule seconds.

10 Heat Storage: Mostly the Oceans 1955 - 1996; Levitus et al. 2001: Science World Ocean = 18.2 x10 22 Joules Atmosphere = 0.7 x10 22 Joules Land Ice = 0.8 x10 22 Joules observed Modeled Model includes forcing from Greenhouse Gases, Sulfate Aerosols Solar irradiance changes, and volcanic aerosols.

For the 2nd 4 - year model run in Figure 3, the value of heat flow into the ocean depths = 1.92 x 10 ^ 4 Joules / m ^ 2 per day — for both the solar increase and the equivalent DLR increase.

Mathematically this can be restated as ∆ Q (change in energy added, Joules / year) = ∆ U (change in energy lost, Joules / year) + ∆ Ocean (change in energy in / out of ocean, Joules / year), or