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Fig. 1

Fig. 1 Refer to the following caption and surrounding text.

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Comparison of the wind temperature profiles, T(r), commonly used in the atomic calculations of the force multiplier factor (Eq. (4)). As can be seen, it is important to approximate the temperature profile throughout the wind, given its variation along the radial coordinate, rather than relying on the two fixed values typically adopted in the isothermal treatment.

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