Sentences with phrase «c water =»

The overall calorie content is probably a bit lower because I used only about half of the prunes (2/3 c prunes + 1 1/2 c water = more than 3/4 c prune paste).

Not exact matches

On day 6 of pregnancy, rats were randomly divided into 4 groups (n = 20 per group): control and hypoxic pregnancy, with and without vitamin C treatment (5 mg.ml − 1 maternal drinking water freshly prepared every day).

Part of the increase in energy expenditure may have been due to the energy required to heat the water from room temperature to body temperature (500 ml × 15 C = 7500 cal = 30 kJ).

The energy need to melt a volume of ice is equal to the energy needed to warm water by 80 C. Thus the energy that can produce 0.6 C of warming would cause the melting of 0.6 / 80 = 0.75 % of the ice cover per year.

The surface heat capacity C (j = 0) was set to the equivalent of a global layer of water 50 m deep (which would be a layer ~ 70 m thick over the oceans) plus 70 % of the atmosphere, the latent heat of vaporization corresponding to a 20 % increase in water vapor per 3 K warming (linearized for current conditions), and a little land surface; expressed as W * yr per m ^ 2 * K (a convenient unit), I got about 7.093.

1 An infinite pond that has water creatures that absorb excess heat by the relation E (excess heat) = M (increase in mass of creatures) * C ^ 2.

Greenhouse Effect = +33.00 ⁰ C Water Vapour causes 95 % of the effect = 31.35 ⁰ C Other Greenhouse gases cause 5 % of the Effect = 1.65 ⁰ C CO2 is about 75 % of the Effect of all GHGs = 1.24 ⁰ C

This climate - adjusted sensitivity of 0.73 C / 3.7 W / m ^ 2 = 0.20 C / Wm ^ -2 is very similar to what comes from 33 C / 155 W / m ^ 2 = 0.21 C / Wm ^ -2 implied by the response of climate to GHG forcing when water vapor is present and clouds can form.

c is the specific heat of sea water, D = 50m is the typical depth of the ocean - mixed layer, and t = 10 days is the restoring timescale.

I can see two effects — reduced need for A / C (one estimate I saw was 6 - 10 tons of A / C (12,000 BTU = 1 ton) from spraying a flat black rubber roof with water in a dry environment and letting it evaporate — but a white roof wouldn't need spraying in the first place), and the other is from increasing reflection into space?

Here, we report mean areal (per unit surface area) CH4 fluxes from reservoir water surfaces that are approximately 25 % larger than previous estimates (120.4 mg CH4 - C per m2 per day, SD = 286.6), CO2 flux estimates that are approximately 30 % smaller than previous estimates (329.7 mg CO2 - C per m2 per day, SD = 447.7), and the first - ever global mean estimate of reservoir N2O fluxes (0.30 mg N2O - N per m2 per day, SD = 0.9; table 1).

(Rule of Thumb: 27.5 ZJ = 0.01 deg C for the 0 - 2000 meter water column).

I calculate Delta GT carbon = 6.5 * Delta T + 0.48 * emitted carbon, which I make to convert to 2.8 ppmv per degree C. That's much less than your figure, but given the timescales one would expect much more outgassing over a longer period because a greater quantity of water will warm.

This gives $ T = Q / (c * m) = 0.00005 K for the increase of the average bulk temperature of water (from surface and up to 5 cm deep) due to the increase of the back radiation by 0.062 W / m ^ 2.

From Trebeth's figures, there's an additional 22 watts eaten up in convection, and 78 watts in latent heat for water vapor, so the actual figure may be 250/150 * 0.22 C = 0.37 C with 40 % of the heat being absorbed in latent heat and convection.

(c) 100 Watts / m ^ 2 = Net convective and water cycle input from the Surface to the Atmosphere (Claim # 9).