McComas et al. - Interstellar Pickup Ions from 20 to 40 AU Interstellar Pickup Ion Observations to 38 AU D.J. McComas1,2, E.J. Zirnstein1, M. Bzowski3, H.A. Elliott2, B. Randol4, N.A. Schwadron5, J.M. Sokół3, J.R. Szalay1, C. Olkin6, J. Spencer6, A. Stern6, H. Weaver7 1Department of Astrophysical Sciences, Princeton University, Princeton, NJ 08544, USA (
[email protected]) 2Southwest Research Institute, San Antonio, TX 78228, USA 3Space Research Centre of the Polish Academy of Sciences, Warsaw, Poland 4Goddard Space Flight Center, Greenbelt, MD 20771, USA 5University of New Hampshire, Space Science Center, Durham, NH 03824, USA 6Southwest Research Institute, Boulder, CO 80302, USA 7Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA ABSTRACT This study provides the first direct observations of interstellar H+ and He+ pickup ions in the solar wind from 22 AU to beyond 38 AU. We use the functional form of the Vasyliunas and Siscoe model, including pickup ion isotropization, convection, and adiabatic cooling, to fit to SWAP pickup ion observations. We are able to fit most observed distributions, although the fit parameters generally lie outside their physically expected ranges. None- the-less, this functional form allows fits that quantify the pickup H+ density, temperature, and pressure over this range of distances. By ~20 AU, the pickup ions already provide the dominant internal pressure in the solar wind. We determine the radial trends of the pickup H+ parameters, and extrapolate them to the termination shock at ~90 AU. There, the inferred ratio of the pickup H+ to core solar wind density of ~0.14.