# Element Abundances: A New Diagnostic for the Solar Wind

**Authors:** J. Martin Laming, Angelos Vourlidas, Clarence Korendyke, Damien Chua,, Steven R. Cranmer, Yuan-Kuen Ko, Natsuha Kuroda, Elena Provornikova, John C., Raymond, Nour-Eddine Raouafi, Leonard Strachan, Samuel Tun-Beltran, Micah, Weberg, and Brian E. Wood

arXiv: 1905.09319 · 2019-07-24

## TL;DR

This paper investigates element abundance variations in the solar corona and solar wind, proposing a new diagnostic based on FIP fractionation influenced by wave-driven processes in the chromosphere.

## Contribution

It introduces a novel diagnostic method using element abundances affected by FIP fractionation to understand the solar wind's origin and reconnection processes.

## Key findings

- FIP effect causes element abundance differences in corona and solar wind.
- Intermediate FIP elements behave differently in closed loops versus solar wind.
- Wave types influence element fractionation in the chromosphere.

## Abstract

We examine the different element abundances exhibited by the closed loop solar corona and the slow speed solar wind. Both are subject to the First Ionization Potential (FIP) Effect, the enhancement in coronal abundance of elements with FIP below 10 eV (e.g. Mg, Si, Fe) with respect to high FIP elements (e.g. O, Ne, Ar), but with subtle differences. Intermediate elements, S, P, and C, with FIP just above 10 eV, behave as high FIP elements in closed loops, but are fractionated more like low FIP elements in the solar wind. On the basis of FIP fractionation by the ponderomotive force in the chromosphere, we discuss fractionation scenarios where this difference might originate. Fractionation low in the chromosphere where hydrogen is neutral enhances the S, P and C abundances. This arises with nonresonant waves, which are ubiquitous in open field regions, and is also stronger with torsional Alfven waves, as opposed to shear (i.e. planar) waves. We discuss the bearing these findings have on models of interchange reconnection as the source of the slow speed solar wind. The outflowing solar wind must ultimately be a mixture of the plasma in the originally open and closed fields, and the proportions and degree of mixing should depend on details of the reconnection process. We also describe novel diagnostics in ultraviolet and extreme ultraviolet spectroscopy now available with these new insights, with the prospect of investigating slow speed solar wind origins and the contribution of interchange reconnection by remote sensing.

## Full text

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## Figures

13 figures with captions in the complete paper: https://tomesphere.com/paper/1905.09319/full.md

## References

131 references — full list in the complete paper: https://tomesphere.com/paper/1905.09319/full.md

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Source: https://tomesphere.com/paper/1905.09319