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We start with an equilibrium state in which the global mean net radiation at the top of the atmosphere (TOA) is zero.
Therein, the annual mean net radiation and the latent heat flux of the green park were 14.33 W/m2and 14.56 W/m2 higher than the architectural complex area, respectively.
The study was motivated by curiosity as to whether non-linearity of the surface boundary conditions implies the existence of a non-vanishing mean signal even when mean forcing (i.e. mean net radiation) vanishes.
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See the text for the details Fig. 4 Relation between global mean surface air temperature and TOA net radiation changes from the preindustrial control simulation in the MIROC3.2 (medres) AOGCM experiments.
Over the range of conditions for which validation data were available (variable air temperature and wind with negligible net radiation), sensors predicted the mean net heat production of live animals to within ±0.023 W (equivalent to ±1°C at Tes=15°C).
Monthly mean data for five near-surface climate variables (net radiation RN, air temperature TA, relative humidity RH, wind speed WS and surface pressure P) are analysed and compared using visual inspection, hypothesis testing and principal component analysis.
Unlike boreal deep lakes, the monthly mean sensible and latent heat flux was tightly coupled with seasonal variations in net radiation at this large (size 2400 km2), subtropical (30.9 31.6°N) shallow (mean depth 1.9 m) Lake Taihu.
It could be concluded that net radiation can be estimated by means of a linear expression with incident global solar radiation depending on the type of vegetation.
Both methods require net radiation, air temperature, humidity and monthly mean wind velocity values plus ground heat fluxes when employed on a daily basis.
The net radiation heat flux is calculated by means of the fluctuational electrodynamics.
The TSMSM was run using fields of near-surface soil moisture from microwave imagery collected by aircraft on six days during the experiment, yielding a root mean square difference (RMSD) between model estimates and tower measurements of net radiation (Rn) and soil heat flux (G) of approximately 20 W m− 2, and 45 W m− 2 for sensible (H) and latent heating (LE).
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