Award Abstract # 1622413
SHINE: Using the Solar Wind as a Turbulence Laboratory to Investigate the Role of Intermittency and Shear

NSF Org: AGS
Division of Atmospheric and Geospace Sciences
Recipient: UNIVERSITY SYSTEM OF NEW HAMPSHIRE
Initial Amendment Date: June 7, 2016
Latest Amendment Date: May 17, 2018
Award Number: 1622413
Award Instrument: Continuing Grant
Program Manager: Lisa Winter
AGS
 Division of Atmospheric and Geospace Sciences
GEO
 Directorate for Geosciences
Start Date: July 1, 2016
End Date: June 30, 2021 (Estimated)
Total Intended Award Amount: $370,649.00
Total Awarded Amount to Date: $370,649.00
Funds Obligated to Date: FY 2016 = $119,507.00
FY 2017 = $123,507.00

FY 2018 = $127,635.00
History of Investigator:
  • Charles Smith (Principal Investigator)
    Charles.Smith@unh.edu
Recipient Sponsored Research Office: University of New Hampshire
51 COLLEGE RD
DURHAM
NH  US  03824-2620
(603)862-2172
Sponsor Congressional District: 01
Primary Place of Performance: University of New Hampshire
Durham
NH  US  03824-2600
Primary Place of Performance
Congressional District:
01
Unique Entity Identifier (UEI): GBNGC495XA67
Parent UEI:
NSF Program(s): SOLAR-TERRESTRIAL
Primary Program Source: 01001617DB NSF RESEARCH & RELATED ACTIVIT
01001718DB NSF RESEARCH & RELATED ACTIVIT

01001819DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1323, 9150, EGCH
Program Element Code(s): 152300
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

A range of interplanetary studies, including energetic particle acceleration and modulation, are hindered by an incomplete, or misleading understanding of the spectrum of interplanetary turbulence. In this regard, the main purpose of this 3-year SHINE project is to gain a deeper understanding of the nonlinear dynamics that distribute energy throughout the interplanetary spectrum, and the use of the solar wind as a wind tunnel to ask fundamental physics questions pertaining to magnetohydrodynamic (MHD) turbulence. Thus, the main goal of the project is to provide an improved understanding of MHD turbulence, in general, seeding the future application of the project results to other space plasmas. The project will support an undergraduate student at the UNH, and it will promote strong international collaborations for the benefit of advancing space weather research both in the USA and worldwide.

This 3-year SHINE project is aimed at continuing the productive and successful research of the project team on the third-moment theory of the turbulence. The third-moment theory of the turbulence in the solar wind provides a tool, which is highly model-independent and can serve as benchmark for modelers. The investigators will continue to expand their research in this area by including wind tunnel data, the anisotropy of the energy-cascade, turbulence between 0.3 and 1 AU, intermittent structures, shear flows, turbulence in downstream shock regions, and expansion effects. The project is directly relevant to the NSF's SHINE program, because it will provide important knowledge about the nature of turbulence in space and astrophysical plasmas. Such knowledge is critical for accurate modeling and prediction of the space weather conditions from the solar surface to the Earth and beyond. The research and EPO agenda of this project supports the Strategic Goals of the AGS Division in discovery, learning, diversity, and interdisciplinary research.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Smith, et al. "Correlation Scales of the Turbulent Cascade at 1 AU" The Astrophysical Journal , v.858 , 2018 , p.21 doi.org/10.3847/1538-4357/aabb00
Smith, Vasquez, Coburn, Forman and Stawarz "Correlation scald of the turbulent cascade at 1 au" Proceedings of the 17th Annual International Astrophysics Conference, Journal of Physics: Conference Series , v.1100 , 2018 , p.012023 doi :10.1088/1742-6596/1100/1/012023
Smith, Vasquez, Coburn, Forman and Stawarz "Correlation scales of the turbulent cascade at 1 AU" The Astrophysical Journal , v.858 , 2018 , p.21 doi.org/10.3847/1538-4357/aabb00
Vasquez, et al. "The Turbulent Cascade for High Cross-Helicity States at 1 AU: II. Minor Energy" The Astrophysical Journal , v.867 , 2018 , p.156 doi.org/10.3847/1538-4357/aae6c6

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.

Work during the final few years of the grant were plagued by delays and inefficiencies due to COVID.  We (the PI, Co-I and students working on the grant) were unable to sit face-to-face to work out the details of a complex computer code.  Early results compute using a code written for this project (we will call this Code2) demonstrated that the correlation scale of third-moment functions describing the turbulent cascade in the solar wind for the first time, and this placed much of the previous research we have already performed onto a much firmer footing.  We found that the correlation scale is far shorter for third moments than it is for the primitive variables (velocity, density, and magnetic field) and this leads to two implications: (1) that the cascade is not correlated across the inertial-range scales, and (2) the nonlinear dynamics are much stronger than previously argued leading to spectral transfer in both direction to larger and smaller scales.  The more traditional estimations of the energy cascade rate represent the average rate only, which is germane to the heating rate, but underestimates the nonlinear dynamics of the inertial range.  It was decided that Code2 should not be modified to perform the remainder of the proposed analysis.  Also, the original code that had published our original results which were used as motivation for this proposal (we will call this Code1) had passed through too many hands to be editable.  We therefore decided that we needed to write a new third code to perform the remainder of the proposed research.  We will call this Code3.  This new code required numerous functional abilities that Code 2 did not possess and that Code1 could not perform.  We spent the remainder of our efforts developing this code and testing it against our previous results.  It was problematic.  Code3 contains processing decisions that were not present in either Code1 or Code2.  Some of these decisions were central to the analysis and could not be removed.  It was only in the weeks leading up to filing our final report that we finally decided we were getting correct results from Code3.  Much of this would have been more efficient if we had been able to meet and review the code together.  This is a source of great frustration to us.  However, we believe we now have a working Code3, and we can now complete the addition of the necessary functionality needed to perform the remainder of the proposed research.  It disturbs the PI greatly that we have not completed our promises, but using internal funds we are determined to perform the remainder of the proposed research and complete our promises.  A more detailed listing of our results, papers published, and talks given is available in the more extensive final report.


Last Modified: 01/24/2022
Modified by: Charles W Smith

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