Let us consider now the case of an isothermal cloud, for which the density in the cloud varies as a function of the position in the following way (Binney & Tremaine (1997)):
where is a constant of proportionality. In other words, because the jet and cloud are maintained in pressure balance, the pressure acting on the jet is given by:
For this isothermal case, it is easy to verify that the factors in the expansions for the gravitational potential and the pressure as defined by eqs.(17.12)-(17.13) are given by:
This solution corresponds to that found by Raga & Cantó (1996) for the case in which no gravity is present, i.e. . From the solutions obtained above in eq.(17.14) and eq.(18.3) it follows that the dimensionless parameter defined as:
is a number that parametrises the required solution.
The deflection of jets in isothermal clouds may be important for interstellar molecular clouds and the jets associated with Herbig-Haro objects. For this case we can obtain a value for the parameter . If we adopt a particle number density of , and a temperature for a cloud with radius (Hartmann, 1998; Spitzer, 1998), then
The same calculation can be made for the cases of radio jets interacting with the gas inside a cluster of galaxies. For this case, typical values are (Longair, 1992; Longair, 1998). With these values, the parameter , exactly as eq.(18.5).
The fact that jets are formed in various environments such as giant molecular clouds and the gaseous haloes of clusters of galaxies with the same values of the dimensionless parameter provides a clue as to why the jets look the same in such widely different environments.
From its definition, the parameter can be rewritten as , where is the mass within a sphere of radius . This quantity is roughly the ratio of the gravitational potential energy from the cloud acting on a fluid element of the jet, to its kinetic energy at the initial position . The parameter is thus an indicator of how large the deflections due to gravity are going to affect the trajectory of the jet. The bigger the number , the more important the deflection caused by gravity will be. In other words, when the parameter the jet becomes ballistic and bends towards the centre of the cloud. When the deflections are dominated by the pressure gradients in the cloud and the jets bend away from the centre of the cloud.
Fig.(III.3) shows plots for three different values of with initial Mach numbers of and . A comparison with a numerical integration of eq.(17.14) using a fourth-order Runge-Kuta method is also presented in the figures by dashed lines. This comparison shows that as long as the deflections are sufficiently small, or as long as the Mach number of the flow in the jet is sufficiently large, the analytic approximations discussed above are a good approximation to the exact solution.
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