The steps to convert heat
flux over a depth interval to temperature change over that interval involves integration of Fourier's equation of heat conduction.»
Not exact matches
By integrating a global database of terrestrial heat
flux measurements with another database of temperature versus
depth within boreholes and with the twentieth - century instrumental record of surface temperature, Huang et al. reconstruct the surface temperature history
over the past 20,000 years.
In a linear approximation (that the blackbody spectral
flux as a function of local temperature changes linearly
over optical thickness going down from TOA, down to a sufficient optical
depth), a doubling of CO2 will bring the
depth of the valley halfway towards half of the OLR (the OLR at 15 microns will decrease by 25 % per doubling — remember this is before the temperature responds).
For some entries (more than 6,000), there was additional information about the
depth range
over which the heat
flux determination was made.»
On the 2000 meter
depth graph
over 2006 - 2014 of Poitou & Bréon, the yearly minima increased from 10 units to 16 units of 1022 J that is 0.41 W / m ²; but there is every year some oceanic heat storage during six months and a release of this heat the following six months: the maximum of the global outgoing longwave radiation is in July, shifted by 6 months w.r.t. the solar
flux hat is maximum in January (1412 W / m ²) and minimum in July (1321 W / m ²).