# The low-frequency break observed in the slow solar wind magnetic spectra

## TL;DR

This study reveals that the low-frequency 1/f magnetic spectral break, previously observed only in fast solar wind streams, also exists in slow streams when sufficiently long intervals are analyzed, challenging prior assumptions.

## Contribution

The paper demonstrates, for the first time, that the 1/f magnetic spectral scaling is present in slow solar wind when long-lasting intervals are examined, extending previous findings.

## Key findings

- The 1/f magnetic spectral scaling exists in slow wind for long intervals.
- Velocity spectrum maintains Kolmogorov scaling regardless of interval length.
- Magnetic amplitude saturation may explain the 1/f scaling in slow wind.

## Abstract

Fluctuations of solar wind magnetic field and plasma parameters exhibit a typical turbulence power spectrum with a spectral index ranging between $\sim -5/3$ and $\sim -3/2$. In particular, at $1$ AU, the magnetic field spectrum, observed within fast corotating streams, also shows a clear steepening for frequencies higher than the typical proton scales, of the order of $\sim 3\times10^{-1}$ Hz, and a flattening towards $1/f$ at frequencies lower than $\sim 10^{-3}$ Hz. However, the current literature reports observations of the low-frequency break only for fast streams. Slow streams, as observed to date, have not shown a clear break, and this has commonly been attributed to slow wind intervals not being long enough. Actually, because of the longer transit time from the Sun, slow wind turbulence would be older and the frequency break would be shifted to lower frequencies with respect to fast wind. Based on this hypothesis, we performed a careful search for long-lasting slow wind intervals throughout $12$ years of Wind satellite measurements. Our search, based on stringent requirements not only on wind speed but also on the level of magnetic compressibility and Alfv\'enicity of the turbulent fluctuations, yielded $48$ slow wind streams lasting longer than $7$ days. This result allowed us to extend our study to frequencies sufficiently low and, for the first time in the literature, we are able to show that the $1/f$ magnetic spectral scaling is also present in the slow solar wind, provided the interval is long enough. However, this is not the case for the slow wind velocity spectrum, which keeps the typical Kolmogorov scaling throughout the analysed frequency range. After ruling out the possible role of compressibility and Alfv\'enicity for the 1/f scaling, a possible explanation in terms of magnetic amplitude saturation, as recently proposed in the literature, is suggested.