The fossil wind structures of Eta Carinae: changes across on 5.54-year cycle

TL;DR

This study uses HST/STIS observations over multiple cycles to map fossil wind-shell structures around Eta Carinae, revealing how wind interactions and ionization states change across its 5.54-year orbit.

Contribution

It provides the first detailed, time-resolved mapping of fossil wind-shells and their ionization states in Eta Carinae across multiple orbital cycles, offering new insights into wind interactions.

Findings

Fossil wind-shells are consistently observed across cycles.

Ionization states vary with orbital phase, especially during periastron.

Wind and photo-ionization properties remain stable over several cycles.

Abstract

Eta Carinae, the closest, active, massive binary containing a highly unstable LBV, exhibits expanding, compressed wind shells, seen in emission, that are spatially and spectrally resolved by \hst/\stis. Starting in June 2009, these structures were mapped across its 5.54-year, highly elliptical, binary orbit to follow temporal changes in the light of [Fe~III] 4659\AA\ and [Fe~II] 4815\AA. The emissions trace portions of fossil wind-shells, that were formed by wind-wind interactions across each cycle. Over the high-ionization state, dense arcs, photo-ionized by far ultraviolet radiation from the hot secondary, are seen in [Fe~III]. Other arcs, ionized by mid-ultraviolet radiation from the primary star, are seen in [Fe II]. The [Fe III] structures tend to be interior to [Fe II] structures that trace extensive, less disturbed primary wind. During the brief periastron passage when the secondary plunges deep into the primary's extremely dense wind, on the far side of primary star, high-ionization [Fe III] structures fade and reappear in [Fe II]. Multiple fossil wind-structures were traced across the 5.7-year monitoring interval. The strong similarity of the expanding [Fe II] shells suggests that the wind and photo-ionization properties of the massive binary have not changed substantially from one orbit to the next over the past several orbital cycles. These observations trace structures that can be used to test three-dimensional hydrodynamical and radiative-transfer models of massive, interacting winds. They also provide a baseline for following future changes in Eta Carinae, especially of its winds and photoionization properties.