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Simulations were performed to quantify the thermal improvement effect of the cooling system in terms of surface temperature reduction, mean radiative temperature (MRT), heat island potential (HIP), indoor air temperature, and cooling load reduction.
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The measured average radiative temperature difference between the bionic and natural leaves is less than 1.0 °C.
Canopy radiative temperature was also monitored on the same plots by means of infrared thermometers, while wind and temperature profiles were measured separately at a central location.
The mean radiative emission is underestimated if turbulent fluctuations are fully ignored and overestimated if only temperature fluctuations are considered, while neglecting fluctuations of the absorption coefficient of the medium, the error being generally higher in the latter case.
The time variation of global mean radiative damping is therefore determined by the time-invariant local feedback parameter λ(r) and the time-varying spatial pattern of surface temperature change ΔT r,t).
Finally, predictions of the mean radiative emission spectra from these flames are presented.
The results indicated differences between nadir and off-nadir radiative temperature of up to 5 K.
Figure 5 shows the difference in the vertical profile of global annual mean radiative cooling by CO2 from that observed in 2002.
In this section, the transient response of the global mean surface temperature to radiative perturbation is reviewed in a classical global feedback framework.
If the injection were ever halted suddenly, it could result in a sudden rise in the global mean surface temperature by unmasking radiative forcing of greenhouse gases.
In this review article, we focus on the transient response of the global mean surface temperature to external radiative perturbation, because the magnitudes of many climatic impacts can be scaled proportionally to this global mean variable relatively well (e.g., Ishizaki et al. 2012; Ishizaki et al. 2013; Yoshimori and Abe-Ouchi 2012).
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