Sentences with phrase «average over time =»

In any case, the «positive feedback» you're alluding to becomes an equal «negative feedback» as it moves away from the Sun once more — average over time = zero.

Not exact matches

Amount = Over 32 ounces (nearly 1 1/2 times the amount of the average bottle of store bought dish washing soap)

Time series of the observed amplitudes (in meters per second) of zonal wave numbers m = 6 (black), m = 7 (red), and m = 8 (blue) for the 15 - d running means of the meridional wind velocity at 300 hPa averaged over 37.5 ° N − 57.5 ° N for May − September 2012 and 2013, based on daily reanalysis data (41).

So in an equilibrium atmosphere with T = 300 K, when averaged over long periods of time, a molecule of N2 in such an atmosphere will have an average altitude of 9 km.

If we want to obtain a function T (x, y, z, t) obeying certain non linear PED / ODE we will look for a PARTICULAR type type of solution: T (x, y, z, t) = Ta (x, y, z) + u (x, y, z, t) where Ta (x, y, z) is a time average of T (x, y, z, t) over a certain period L (eventually a bit space averaged around the point (x, y, z)-RRB- AND u (x, y, z, t) is a random variable with a known probability density distribution.

The fundamental hypothesis is that at some time in the past and over some unspecified time - averaging period that on a whole - planet basis radiative energy transport attained a state of equilibrium; out - going energy = in - coming energy.

10 Temperature change over past 22,000 years Agriculture established Temperature change (C °) End of last ice age Average temperature over past 10,000 years = 15 °C (59 °F) Figure 20.2 Science: estimated changes in the average global temperature of the atmosphere near the earth's surface over different periods oAverage temperature over past 10,000 years = 15 °C (59 °F) Figure 20.2 Science: estimated changes in the average global temperature of the atmosphere near the earth's surface over different periods oaverage global temperature of the atmosphere near the earth's surface over different periods of time.

The rates averaged over the last three decades very closely give an exponential with a doubling time of 33.3 years, i.e. eightfold in a century, meaning starting with 370 in 2000 (90 +280) gives exactly 1000 in 2100 (= 720 +280).

From Equation (7), Y = A ˜ / (X) b, if we divide the average weighted level curve of satisfaction by A ˜, we obtain the average adjusted weighted level curve of satisfaction over time:

By dividing each country's weighted level curve by the average weighted level curve of satisfaction over time in Equation (7), Y = A ˜ / (X) b, we obtain