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Diabatic heating rates

A more practical approach is simply to derive the net mean circulation directly from the diabatic heating rate, q, as suggested by Dunkerton (1978). From the thermodynamic equation (3.60) in which it is assumed that d /dt and (v/a)(dO/dheat fluxes are negligibly small, one can deduce that... [Pg.99]

Note that the eddy heat flux does not appear in the transformed thermodynamic equation (3.65). From these equations, vd and wb may be derived directly from a knowledge of the diabatic heating rate. We... [Pg.99]

A second issue is the transport of trace gases in the stratosphere. How do the polar vortices form How readily are air parcels exchanged between the vortex and midlatitudes and between altitudes at different latitudes and seasons What are the diabatic heating and cooling rates at different times... [Pg.188]

Figure 3.3. Net radiative heating rate associated with (1) absorption of ultraviolet radiation by molecular oxygen in the upper mesosphere and thermosphere, and by ozone in the stratosphere and mesosphere, and (2) emission of infrared radiation by atmospheric CO2, O3, and H2O. Values given in K/day and positive in the summer hemisphere (net diabatic heating) and negative (net diabatic cooling) in the winter hemisphere. Prom London (1980). Figure 3.3. Net radiative heating rate associated with (1) absorption of ultraviolet radiation by molecular oxygen in the upper mesosphere and thermosphere, and by ozone in the stratosphere and mesosphere, and (2) emission of infrared radiation by atmospheric CO2, O3, and H2O. Values given in K/day and positive in the summer hemisphere (net diabatic heating) and negative (net diabatic cooling) in the winter hemisphere. Prom London (1980).
The parametrization of cumulus cloud rainfall utilizes some form of one-dimensional cloud model. These are called cumulus cloud parametrization schemes. Then-complexity ranges from instantaneous readjustments of the temperature and moisture profile to the moist adiabatic lapse rates when the relative humidity exceeds saturation, to representations of a set of one-dimensional cumulus clouds with a spectra of radii. These parametrizations typically focus on deep cumulus clouds, which produce the majority of rainfall and diabatic heating associated with the phase changes of water. Cumulus cloud parametrizations remain one of the major uncertainties in mesoscale models since they usually have a number of tunable coefficients, which are used to obtain the best agreement with observations. Also, since mesoscale-model resolution is close to the scale of thunderstorms, care must be taken so that the cumulus parametrization and the resolved moist thermodynamics in the model do not double count this component of the and Sq.. [Pg.193]

In the diabatic distillation column, each element is small enough that equipartition of entropy production may be approximately achieved by adjusting the heat flows and thus the liquid and vapor flow rates. We assume that each element performs a specified duty of Ji0. The total cost function Ct for all N elements is... [Pg.298]

A reduction of 38% in the entropy production rate was obtained for a binary separation of benzene and toluene in an equimolar mixture. The heat added on each tray in the optimal diabatic column and the corresponding vapour flows are shown in Figure 7. [Pg.7]

The steady two-dimensional diabatic flow is described by the equations for mass, momentum and energy in conservation form (Schnerr and Dohrmann [7], Dohrmann [8]). Real gas effects are not yet included and inviscid fluids are assumed. Here the classical nucleation theory of Volmer [9] is used which gives a good qualitative representation of the behavior of condensing in the supersaturated state (Wegener [iO]). Oswatitsch [11] introduced this theory into the calculation of flow processes, a summary of all basic relationships for compressible flows with heat addition is given by Zierep [12]. To compute the nucleation rate J per unit time and volume, we take... [Pg.172]

Here two different airfoils are Investigated, the circular arc CA-0.1 (thickness ratio of 10 %) and the NACA-0012, Due to the approximately constant cooling rate at local Mach numbers close to one the circular arc airfoil allows some simplifications. The value at Mach number one, denoted by the star, represents the time scale at the entire transonic airfoil section, whereas the cooling rate at the NACA-0012 changes considerably. Condensation onset Mach numbers very close to one are correlated with higher cooling rates and vice versa (Table 1). Usually it is assumed that the temperature gradients in adiabatic flow and with heat addition are identical up to the condensation onset for free stream Mach numbers M < 1, too. However, the numerical results of diabatic flows show a more or less pronounced precompression... [Pg.175]

For the case of diabatic flow (involving heat input to the transfer line), Martinelli and Nelson showed that a modification of Eq. (7.76) can be used to relate the total pressure drop in the transfer line to that experienced by a flow that is only liquid with a total flow rate equal to the sum of and The modification has the form... [Pg.461]


See other pages where Diabatic heating rates is mentioned: [Pg.55]    [Pg.68]    [Pg.93]    [Pg.158]    [Pg.228]    [Pg.55]    [Pg.68]    [Pg.93]    [Pg.158]    [Pg.228]    [Pg.133]    [Pg.48]    [Pg.489]    [Pg.149]    [Pg.357]    [Pg.7]    [Pg.60]    [Pg.179]    [Pg.179]    [Pg.191]    [Pg.554]   
See also in sourсe #XX -- [ Pg.158 ]




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