Abstract

Abstract. It has been found that pick-up ions at their dynamical incorporation into the solar wind modify the original conditions of the asymptotic solar wind plasma flow. In this respect, it has meanwhile been revealed in many papers that these type of solar wind modifications, i.e. deceleration and decrease of effective Mach number, are not only due to the pick-up ion loading effects, but also to the action of pick-up ion pressure gradients. Up to now only the effects of radial pick-up ion pressure gradients were considered, however, analogously but latitudinal pressure gradients also appear to be important. Here we study the effects of radial and latitudinal pick-up ion pressure gradients, occurring especially during solar minimum conditions at mid-latitude regions where slow solar wind streams change to fast solar wind streams. First, we give estimates of the latitudinal wind components connected with these gradients, and then after revealing its importance, present a more quantitative calculation of solar wind velocity and density perturbations resulting from these pressure forces. It is shown that the relative density perturbations near and in the ecliptic increase with radial distance and thus may well explain the measured non-spherically symmetric density decrease with distance. We also show that the solar wind decelerations actually seen with Voyager-1/2 are in conciliation with interstellar hydrogen densities of nH∞≥0.1cm-3, in contrast to earlier claims for nH∞=0.05cm-3.

Highlights

  • For quite some time it has been recognized that the solar wind dynamics at larger distances is not determined by its own right, but is influenced by the process of incorporating newly created pick-up ions into the solar wind plasma bulk

  • The effective Mach number and the wind deceleration are fairly well calculated by making use of an expression for the pick-up pressure, Ppui = αρpuiVw2, which has been justified in papers by Fahr (2002) and Fahr and Chashei (2002)

  • In the preceding sections of this paper we have developed a theoretical description of the three-dimensional solar wind outflow under the action of radial and latitudinal pick-up ion pressure gradients

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Summary

Introduction to pick-up ion pressures

For quite some time it has been recognized that the solar wind dynamics at larger distances is not determined by its own right, but is influenced by the process of incorporating newly created pick-up ions into the solar wind plasma bulk. Α represents a weak function of the solar distance r, and ρpui and Vw are the pick-up ion mass density and the solar wind bulk velocity, respectively. Scherer: Perturbations of the solar wind flow by pick-up ion pressure gradients pick-up ion distribution function and supporting a representation of the pick-up pressure in the above mentioned form, i.e. Ppui = αρpuiVw2. With this expression the decelerated solar wind is described by (see Fahr and Rucinski, 2001):.

Estimated effect of latitudinal PUI pressure gradients
Approximated continuity equation
Towards a more quantitative solution
Momentum flow continuity equations ρVr
Linearization
Latitudinal gradients
Solution of the differential equations
The magnetic pressure
Findings
Discussion and concluding remarks
Full Text
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