the average temperature will drop 0.05-0.35 ℃, average surface temperature will drop 0.1-0.8℃, average sensible heat flux will reduce 5-25w/m2, about 8-40% and average latent heat flux will increase 5-40w/m2, about 4-35%.
The reed wetland absorbed carbon about 13.32 t CO_2/hm~2 in 2005,and the values of diurnal mean sensible heat flux and latent heat flux were 2464 kJ/ m~2 and 3880 kJ/m~2 in 2005,respectively.
The differential scanning calorimetry (DSC) measurements indicate that the latent heat in phase transition changes from 0.852 to 2.381J/g and increases with the increase of the maximal absolute values of ( M/ T).
2°× 2° mean monthly COADS grid data (1970-1979) are used to compute the net longwave radiation and fluxes of sensible and latent heat over the tropical Pacific and Indian Ocean (30°S - 30°N) and their seasonal and annual variations.
the average temperature will drop 0.05-0.35 ℃, average surface temperature will drop 0.1-0.8℃, average sensible heat flux will reduce 5-25w/m2, about 8-40% and average latent heat flux will increase 5-40w/m2, about 4-35%.
The reed wetland absorbed carbon about 13.32 t CO_2/hm~2 in 2005,and the values of diurnal mean sensible heat flux and latent heat flux were 2464 kJ/ m~2 and 3880 kJ/m~2 in 2005,respectively.
The differential scanning calorimetry (DSC) measurements indicate that the latent heat in phase transition changes from 0.852 to 2.381J/g and increases with the increase of the maximal absolute values of ( M/ T).
Compared with the version coupled with SSiB land surface model,SAMIL-R42L26 coupled with CLM also has better performance in simulating the seasonal evolution of the surface sensitive heating and latent heating in Asian monsoon region,the results are very close to reanalysis data.
The more latent heating released in the ice phase processes associated with the freezing process leads to strengthening deep convection due to the vertical gradient of buoyancy, which results in a long life of the convective system.
Multi-year NCEP/NCAR reanalysis data were used to analyze the effects of the sensible heating flux and the latent heating on the seasonal evolution of the subtropical high belt during the onset-period of the Asia summer monsoon.
By means of daily reanalysis data of the South China Sea Monsoon Experiment in 1998,the influence of condensation latent heating on mid- and short-term activities of West Pacific Subtropical High(WPSH) during Meiyu period 1998 is studied.
This paper Presents a conversion of superheat steam for heating to sensible heating for heating feed water and uses hidden heat for heating System at low load heating state in order to increase the steam inlet of back pressure theme to reach the goal of increasing generating output
The paraffin wax (with melting temperature of 29°C, crystallizing temperature of 26°C and latent heat of 142 J/g) served as latent heat storage material and the silica as supporting material, which prevented the leakage of the melted paraffin wax.
According to the characteristics of quenching process, a new method of computing phase-transformation latent heat is presented to ensure the computation accuracy of temperature.
The latent heat is measured on these samples for the first time in the region of the spin-reorientation phase transition using differential scanning calorimetry.
The same qualitative results are obtained provided the threshold is more than unity for the corresponding SEIS model with no infectious force in the latent period.
However, after mid-April it changes into latent heating over Indo-China Peninsula due to the onset of convection, and the apparent heating ratio increases with height in mid-and lower troposphere.
Maxima in CCM-simulated precipitation correspond to the simulated outflow maxima and are generally larger than observational estimates, and the associated atmospheric latent heating appears to contribute to the stationary wave errors.
Quantitatively, sensitivity of evaporation to short-wave cloud absorption, when averaged over the whole tropics, can be described by an approximate balance of variations in atmospheric radiative cooling and latent heating.