Award Abstract # 1834822
Understanding Wave Energy Transport Through the Complex Chromosphere and Transition Region

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: THE TRUSTEES OF COLUMBIA UNIVERSITY IN THE CITY OF NEW YORK
Initial Amendment Date: May 3, 2019
Latest Amendment Date: May 3, 2019
Award Number: 1834822
Award Instrument: Standard Grant
Program Manager: Lisa Winter
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: May 15, 2019
End Date: April 30, 2023 (Estimated)
Total Intended Award Amount: $418,387.00
Total Awarded Amount to Date: $418,387.00
Funds Obligated to Date: FY 2019 = $418,387.00
History of Investigator:
  • Michael Hahn (Principal Investigator)
    mhahn@astro.columbia.edu
  • Daniel Wolf Savin (Co-Principal Investigator)
Recipient Sponsored Research Office: Columbia University
615 W 131ST ST
NEW YORK
NY  US  10027-7922
(212)854-6851
Sponsor Congressional District: 13
Primary Place of Performance: Columbia University
2960 Broadway
New York
NY  US  10027-6902
Primary Place of Performance
Congressional District:
13
Unique Entity Identifier (UEI): F4N1QNPB95M4
Parent UEI:
NSF Program(s): SOLAR-TERRESTRIAL
Primary Program Source: 01001920DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 152300
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Plasma waves appear to be responsible for much of the heating of the chromosphere, transition region, and corona of the Sun. Fluid motions in the photosphere provide power for the waves, but the precise excitation mechanism is yet unknown. Once excited, the wave energy must be transmitted to the corona. However, recent observations have shown that the interface region between the photosphere and corona (i.e., the chromosphere and transition region) is complex. Thus, it is known how wave energy propagates through the interface region. These issues hinder the development of coronal heating models, which are limited by our poor understanding of the wave properties at the base of the corona. To tackle these important science problems for solar physics, this three-year project will use data from the Interface Region Imaging Spectrometer (IRIS) to measure the properties of waves in the interface region of the solar atmosphere. The main science objectives of the project are to: (1) identify where plasma waves are generated; (2) determine how wave energy propagates from the photosphere to the corona; and, (3) specify the wave boundary conditions at the base of the corona.

During this three-year research project, archival data from IRIS will be analyzed to address the following three major issues. First, determine where MHD waves are generated. It is currently unknown whether waves are generated mainly in the photosphere and propagate up through the interface region or whether the waves are generated within the interface region. The photosphere exhibits various fluid motions that can generate waves, such as the buffeting of magnetic field lines by granular motions. But, the waves can be reflected by the strong density gradients at the transition region and so not reach the corona. Global acoustic p-modes at the photosphere could launch acoustic waves, but they must undergo mode conversion if they are the source of the Alfvenic waves observed in the corona. Alternatively, waves may be generated in the chromosphere, for example, by reconnection. The IRIS data will be used to determine the wave modes and sources and sinks of wave power through varying heights in the interface region and thereby identify signatures of these processes and other possible ones. Second, measure the propagation of waves from the photosphere into the corona. Wave reflection and damping may prevent much of the wave power from reaching the corona. This project will determine how waves are transmitted through the interface region by observing the propagation of waves along structures and by measuring the power spectrum of the waves. These measurements will then be compared to existing observations and spectra of lower lying photospheric fluctuations and of Alfvenic waves in the higher lying corona. The analysis will determine where Alfvenic waves are reflected, if there is conversion of wave power from longitudinal to transverse modes or vice versa, and where wave energy is dissipated. Results will be compared to theories for the propagation, reflection, and damping of waves throughout this complex region. Third and final, characterize the wave modes and power at the base of the corona in order provide the critical boundary conditions needed for models of coronal heating. By comparing the amplitudes and phases of velocity and intensity fluctuations one can constrain the relative contribution of compressible versus incompressible waves. IRIS has sufficient spatial resolution to see torsional oscillations and thereby estimate the Alfvenic wave energy content of torsional versus kink waves. By studying the power spectrum of the waves, it will be determined whether the fluctuations are already turbulent at the base of the corona or whether the turbulence develops in the corona at larger heights.

This research project will have broader impacts through postdoctoral training and public outreach. The project will train a postdoctoral research scientist in the field of solar physics and in techniques for the analysis of spectroscopic observations. The research and EPO agenda of this project supports the Strategic Goals of the AGS Division in discovery, learning, diversity, and interdisciplinary research.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Hahn, Michael and Fu, Xiangrong and Savin, Daniel Wolf "Evidence for Parametric Decay Instability in the Lower Solar Atmosphere" The Astrophysical Journal , v.933 , 2022 https://doi.org/10.3847/1538-4357/ac7147 Citation Details
Hahn, Michael and Ho, Brandon and Savin, Daniel Wolf "Characteristics of Nanoflare Heating in a Coronal Bright Point" The Astrophysical Journal , v.936 , 2022 https://doi.org/10.3847/1538-4357/ac897f Citation Details

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The outer layer of the Sun, visible during solar eclipses, is called the corona. This layer of the Sun has a temperature of a million degrees, much hotter than the underlying photosphere, the layer we normally see, which is only a few thousand degrees. One of the major problems, the Coronal Heating Problem, is to understand why the corona is so hot. One possibility is that energy is carried into the corona by waves generated at the photosphere that travel outward. The most important type of waves that may do this are called Alfven waves. These waves are transverse waves in which a hot plasma and a magnetic field move together. We know that Alfven waves originate inside the Sun and carry enough energy to heat the corona, but we do not know why this energy turns into heating in the corona. 


The main outcome of this project has been to find observational evidence that the Alfven waves undergo a parametric decay instability (PDI) in the Sun. In this process, an outward traveling Alfven wave breaks apart into an outward traveling sound wave and a backward-traveling Alfven wave. This makes it possible to heat the corona efficiently because the outward and backward Alfven waves collide with each other to generate turbulence, which allows energy to go into heating particles. 


This grant also supported an undergraduate student research project. That student studied the heating of small hot loops in the corona, called bright points. Most people who study coronal heating have looked at very complicated active regions, which are the hottest regions of the corona. Even though bright points are not quite as hot, because they are simpler we might have a better chance of understanding them. By comparing spectroscopic observations to a model, the student was able to determine the heating rate for these structures. The student who performed the work has gone to graduate school to pursue robotics. 


The funds also supported a postdoctoral research scientist who is comparing plasma waves in the Sun to similar waves seen in laboratory plasmas. The Sun allows us to study conditions that are difficult to replicate on Earth. By studying waves in the Sun, we can gain a deeper understanding of their behavior, which may have applications to laboratory plasmas. 


Last Modified: 06/30/2023
Modified by: Michael Hahn

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