New Article on ApJ: “Observation of magnetic switchback in the solar corona”

Observation of magnetic switchbacks in solar corona

Article in press on “Astrophysical Journal Letters” https://arxiv.org/pdf/2206.03090.pdf

The solar wind is a continuous flow of supersonic plasma particles generated at the level of the Solar Corona – the Sun’s atmosphere – that expands radially, reaching the planets of the solar system and creating a large bubble of plasma that extends well beyond Pluto’s orbit, called the heliosphere. Together with this plasma flux, the Sun generates also a large scale magnetic field that pervades the heliosphere, carried within the solar wind. In 2019 NASA has launched the Parker Solar Probe – PSS, a mission designed to explore magnetic, electric and velocity fields in the solar wind, performing the closest approaches to Sun ever made by a spacecraft.

Soon after its launch, PSS has discovered the existence in the Solar Corona of abundant clusters of S-like structures called “switchbacks (see the animation below). These are essentially short-term ‘flips’ in the polarity of the magnetic field frozen in the outflowing solar wind, which may actually play a critical role in the creation and acceleration of the solar wind. 

Parker Solar Probe observed switchbacks: traveling disturbances in the solar wind that caused the magnetic field
to bend back on itself. Credits: NASA’s Goddard Space Flight Center/Conceptual Image Lab/Adriana M. Gutierrez

 

 

 

While in the last couple of years, thanks to PPS, switchbacks have been widely observed near the Sun and the international community has worked on their characterizations, no theory has been put forward to date that explain their origin, as is reported in this recent articles on the NASA website:
https://www.nasa.gov/feature/goddard/2021/switchbacks-science-explaining-parker-solar-probe-s-magnetic-puzzle 
The main question concerning this very peculiar magnetic structures, essential to explain the dynamics of the solar wind is: do the switchbacks have a solar origin or they form locally in the solar wind, as it expands into the interplanetary space?
This puzzle has finally been solved thanks to the a breakthrough discovery made by a team of scientists working on the ESA Solar Orbiter – SolO mission (launched in the February 2020), based on the first direct observation of a magnetic switchback in the Solar Corona, done with the METIS coronographer on board of SolO. In an article that will soon appear on “The Astrophysical Journal Letters (ApJ)”, Daniele Telloni, from the Italian National Institute for Astrophysics, co-investigator of the METIS, in collaboration with Raffaele Marino, CNRS scientist at the LMFA /Ecole Centrale de Lyon, Co-investigator of the plasma suite SWA on SolO, together with a team of worldwide recognized scientists from many countries, propose indeed a theory that would explain the origin of the magnetic switchbacks.

Composite of the Metis-observed total brightness image of the solar corona (blue) and of the ultraviolet emission image (yellow) provided by the Extreme Ultraviolet Imager from the Solar Orbiter vantage point on March 25, 2022 at 20:39 UT. The switchback (in the rectangular box) propagates through the Solar Corona, above an active region of the Sun (white box).

 

 

 

Telloni and Marino say: “the novelty of our work relies on presenting to the community the first observation of a magnetic switchback in the Solar Corona, together with a rigorous evidence based explanation of the SBs origin. As we explain with solid arguments in the manuscript just accepted in ApJ, we were able to interpret the generation of the switchbacks in space plasmas as the result of the interchange reconnection occurring between closed magnetic structures developing above active regions of the Sun and the open magnetic field lines emerging from neighbor of coronal holes, which suggest a common genesis for the magnetic switchbacks and the slow solar wind streams”.   
The authors make the claim that the large scale S-like plasma structure observed in the Corona with the METIS instrument (shown in the figure above), in a region susceptible to contain the inversion of the local mean magnetic field, is indeed compatible with the existence of an underlying magnetic switchback. This is substantiated by a thorough spatio-temporal analysis performed using the METIS data, and by the outcome of (numerical and analytical) models of the coronal plasma and its magnetic field that have been ran in order to interpret the observations. According to Telloni and Marino, phenomenological evidence and quantitative assessments presented in their work provide critical elements leading to conclude that the observed plasma structure is supported by a large magnetic switchback in the Corona, occurring in a site where the probability for interchange reconnection to develop is high.

Schematics of the interchange reconnection mechanism [from Zank et al. 2020, ApJL, 903,1] proposed to explain the origin of the magnetic switchbacks. a) a coronal loop (massive closed magnetic structure developing over the  Sun’s surface) approaches a region with open magnetic field lines; b) the first magnetic field line “reconnect” asshown, producing a S-shaped open magnetic field line; c) the switchback is then pushed both upward and downward (as the arrows indicate in the sketch), while a new reconnection event starts on the subsequent neighbor field line, interacting with the same coronal loop. 

R. Marino and R. Foldes joined the ISSI team on “Cross-Scale Energy Transfer in Space Plasmas”, Bern (SWI)

Raffaele Marino and Raffaello Foldes joined the ISSI team: “Cross-Scale Energy Transfer in Space Plasmas

Raffaele Marino and Raffaello Foldes joined the International Space Science Institute (ISSI) team organized by Kieokaew R. (Institut de Recherche en Astrophysique et Planétologie, IRAP, France) and Yang Y. (University of Delaware, USA) and approved by ISSI the last May, 24th. A series of two to three one-week meetings over a period of 12 to 18 months with subject “Cross-Scale Energy Transfer in Space Plasmas“.

Find out more @ISSI

Harikrishnan Charuvil Asokan PhD Thesis defense (09/2023)

Harikrishnan Charuvil Asokan PhD thesis defense: Investigations of Mesosphere and Lower Thermosphere Mesoscale Dynamics Using Ground-based Measuring Techniques

Thesis advisors

CHAU Jorge Luis, Research Director (Leibniz Institute for Atmospheric Physics)
MARINO Raffaele, Head of Research (CNRS)

Summary

Mesoscale dynamics in the mesosphere and lower thermosphere (MLT) region are mainly due to atmospheric gravity waves (GWs) and stratified turbulence. GWs are assumed to be the dominant drivers of MLT mesoscale dynamics. However, characterising and observing these scales is challenging due to their scales and intermittent nature. This thesis investigates the mesoscale dynamics of the MLT region using ground-based observations. The main dataset used in this work is from multistatic specular meteor radars (SMRs). The study is complemented with observations from airglow imagers and satellites and with direct numerical simulations as well as high-resolution model data. This thesis uses a novel second-order statistics approach to investigate the correlation functions in temporal and spatial scales from one-dimensional projections of three-dimensional wind velocities. In a case study, we found that unexpected large horizontal scales dominate the dynamics. Intriguing high vertical velocity estimates using multistatic SMRs at different latitudes are also addressed through a validation study by constructing virtual multistatic radar systems based on winds from a high-resolution general circulation model.

 

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Meet Us @ EGU General Assembly 2022, 23-27/05, Wien (Aus)

Meet Us @ EGU General Assembly 2022, 23-27/05, Wien (Aus)

The European Geophysical Union General Assembly 2022 will bring together geoscientists from all over the world for one meeting covering all disciplines of the Earth, planetary, and space sciences. The EGU aims to provide a forum where scientists, especially early career scientists, can present their work and discuss their ideas with experts in all fields of geoscience.

Find out more @ EGU official website

LETMA – CeLyA Spring School 2022: Waves & geosciences

LETMA – CeLyA Spring School 2022: Waves & geosciences

General Information

The spring school is proposed in the framework of LETMA, which is a joint laboratory between CEA, Sorbonne University and Centrale Lyon. LETMA studies the propagation of low frequency waves in the atmosphere. In order to raise awareness of the subjects studied in relation to environmental issues, LETMA’s partners propose a spring school Waves & geosciences: Infrasound and beyond for students and researchers.

The spring school will take place from 28 March 2022 to 1 April 2022 at the Valpré seminar centre in Ecully near Lyon, France. The number of participants is expected to be around 50.

This spring school, in the format of a research school, is aimed at students, researchers and engineers. The objective is to present the state-of-the-art on different topics: physics of the atmosphere and propagation, statistical methods and machine learning, quantification of uncertainties, etc. An important aspect will be dedicated to the presentation of dual problems (identification of acoustic sources for environmental problems, contribution to climate modelling, etc.). Some of the lectures will be complemented by practical sessions. Collaborative work and scientific presentations will allow exchanges between participants.

Find out more @Centre for Acoustic Research

Fabio Feraco PhD Thesis defense

Fabio Feraco PhD thesis defense: Dynamics driven by emerging vertical drafts in stratified turbulent flows

Committee

Bertoglio Jean-Pierre, Research Director (CNRS, Emeritus) – Thesis Supervisor
Marino Raffaele, Head of Research (CNRS) Thesis Supervisor
Primavera Leonardo, Professor (University of Calabria, Italy) – Thesis Supervisor
Lanotte Alessandra, Researcher (CNR, Italy) – Rapporteur
Liu Hanli, Senior Scientist and Professor (NCAR-CU Boulder, US) – Rapporteur
Moisy Frédéric, Professor (University of Paris-Saclay) – Examiner
Bourgoin Mickaël, Head of Research (CNRS, École Normale Supérieure of Lyon) – Examiner
Folini Doris, Senior scientist at Lecturer (ETH) – Examiner

Summary

Intermittency is a characteristic feature of turbulent flows.
Typically observed as the localized enhancement of small-scale field fluctuations, it is at the origin of the bursty behavior of the energy dissipation in fluids. However, the intermittent character of the velocity and of the temperature fields has been reported in many observations in geophysical flows also in the large scales.

The purpose of this thesis is precisely to characterize the emergence of large-scale intermittent vertical velocity drafts and temperature bursts in stratified turbulent flows of geophysical interest, as detected in the atmosphere and the oceans. In particular, using direct numerical simulations (DNSs) of the Boussinesq equations (with or without rotation), I explore the parameter space with the aim of investigating dynamics and energetics in stratified flows in which the interplay of internal waves and turbulent motions produces powerful enhancements of the vertical velocity and temperature at large-scale. This phenomenon, resulting from a resonant mechanism that I describe through a simple one-dimensional model, feeds back on the energy transport and dissipation property of the flow, influencing mixing. The large-scale intermittency detected in stratified flows has been investigated here by means of high order statistics of the prognostic fields, and in particular through the kurtoses of the vertical velocity and temperature, which are found to have a non-monotonic behavior with the Froude number, that is, the control parameter of the turbulent system viewed as a superposition of waves and nonlinear eddies.

The Eulerian fields are used to characterize the distribution of the energy across the scales and the exchanges between kinetic and potential energies within the resonant regime. Lagrangian tracers have also been released in DNSs to investigate their dispersion in stratified turbulent flows developing extreme vertical drafts.
The first radar observation of an extreme event in the vertical velocity field in the mesosphere and lower thermosphere, interpreted here as a “super-bore”, is finally presented together with a study of the diffusion of a passive scalar in a turbulent flow, preliminary to future characterizations of the passive scalar diffusion in a stratified environment in the resonant regime identified as before in terms of the Froude number.

Keywords: stratified turbulence, waves, geophysical flows, mixing, intermittence, rotation, Lagrangian particles

New Article on EOS Vol. 103

New Article on EOS (Science News by AGU) Vol. 103: A New Journey Around (and Around) the Sun

 
Daniele Telloni, Francesco Valentini and Raffaele Marino
 
The Solar Orbiter just completed its commissioning phase while en route to the Sun. It has already provided valuable looks at solar campfires and Venus’s magnetic fields, and it promises much more.
 
Find out more on EOS

New Article on Physics Review Fluids Vol. 7 (3), p. 033801

New Publication on Physical Review Fluids, Vol. 7 (3), p. 033801: Turbulence generation by large-scale extreme vertical drafts and the modulation of local energy dissipation in stably stratified geophysical flows

R. Marino, F. Feraco, L. Primavera, A. Pumir, A. Pouquet, D. Rosenberg, P. Mininni

We observe the emergence of strong vertical drafts in direct numerical simulations of the Boussinesq equations in a range of parameters of geophysical interest. These structures, which appear intermittently in space and time, generate turbulence and enhance kinetic and potential energy dissipation, providing a possible explanation for the observed variability of the local energy dissipation in the bulk of oceanic flows and the modulation of its probability distribution function. We show how, due to the extreme drafts, in runs with Froude numbers observable in geophysical scenarios, roughly 10% of the domain flow can account for up to 50% of the global volume dissipation, reminiscent of estimates based on oceanic models.

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