
NSF Org: |
AGS Division of Atmospheric and Geospace Sciences |
Recipient: |
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Initial Amendment Date: | August 28, 2020 |
Latest Amendment Date: | August 15, 2022 |
Award Number: | 2028154 |
Award Instrument: | Standard Grant |
Program Manager: |
Mangala Sharma
msharma@nsf.gov (703)292-4773 AGS Division of Atmospheric and Geospace Sciences GEO Directorate for Geosciences |
Start Date: | September 1, 2020 |
End Date: | February 28, 2025 (Estimated) |
Total Intended Award Amount: | $799,611.00 |
Total Awarded Amount to Date: | $799,611.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
301 SPARKMAN DR NW HUNTSVILLE AL US 35805-1911 (256)824-2657 |
Sponsor Congressional District: |
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Primary Place of Performance: |
320 Sparkman Drive Huntsville AL US 35805-1912 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | SOLAR-TERRESTRIAL |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Solar wind, a stream of charged particles emitted from the Sun, is a key driver of space weather at Earth and throughout the solar system. Extreme space weather events occur when disturbances in the Sun?s atmosphere, called coronal mass ejections (CMEs), reach the Earth?s magnetosphere. Space weather phenomena can create conditions hazardous for humans and instruments in space and on the ground. Accurately forecasting space weather is thus increasingly important for our technology-dependent society and will be critical while planning and operating missions to the Moon and Mars. This project will develop a new generation of software capable of near real-time modeling from the Sun to Earth's orbit (inner heliosphere) and predicting intense space weather events. The tools developed by this project can not only dramatically improve the accuracy and performance of currently operational space weather models, but also allow the broader scientific community to experiment with and extend these tools to create new capabilities that could eventually be transformational for operational activity. This work will also provide a leap forward in the computation and simulation of complex, turbulent plasma systems and is expected to have impact in several areas, including space physics and astrophysics. The project team includes both early-career and senior researchers at U.S. universities, NASA centers, national labs, and in the private sector; support for the non-academic collaborating institutions is to be provided by NASA.
The structuring of the solar wind into fast and slow streams is the source of recurrent geomagnetic activity. The largest geomagnetic storms are caused by CMEs propagating through and interacting with the solar wind. The connection of the interplanetary magnetic field to CME-related shocks and impulsive solar flares determines where solar energetic particles propagate. Therefore, data-driven modeling of stream interactions in the background solar wind, and CMEs propagating through it, is a necessary part of space weather forecasting. At present NOAA Space Weather Prediction Center forecasts the background solar wind and CME arrival times using empirically driven models. The goal of this project is to develop a data-driven, time-dependent model that will improve the current state of the art. The new model will consist of: 1) a surface flux transport model, 2) potential field solver, and 3) an MHD solar wind model. It will provide more accurate solutions and be scalable on massively parallel computing systems, including Graphic Processor Units. Products from this project will provide a leap forward in the computation and simulation of complex plasma systems involving multiple discontinuities. The developed software will also be useful for astrophysical problems possessing a distinct spherical geometry, including exoplanets, early sun, and sun-like stars.
This award is made as a part of the joint NSF-NASA pilot program on Next Generation Software for Data-driven Models of Space Weather with Quantified Uncertainties (SWQU). All software developed as a result of this award will be made available by the awardee free of charge for non-commercial use; the software license will permit modification and redistribution of the software free of charge for non-commercial use.
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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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.
Space Weather (SWx) is defined by the transients in the space environment traveling from the Sun, through the heliosphere, to Earth. In the past decade, the difficult task of understanding and predicting violent solar eruptions and their terrestrial impacts has become a strategic national priority, as it affects the daily life of humans, including communication, transportation, power supplies, national security, space travel, and more. It is also crucial to the development and operations of space exploration missions, including the future Moon and Mars initiatives. Although SWx broadly encompasses a wide range of effects, one of the primary concerns is the interaction of Coronal Mass Ejections (CME) with the Earth's magnetosphere, ionosphere, atmosphere, and lithosphere. The strength of the CME-Earth interaction is controlled to a large extent by the speed of arriving CME and the amount of southward-pointing magnetic field component it carries. CMEs propagate through the ambient solar wind, which is frequently characterized by the presence of high-speed streams (HSSs) that originate from the coronal holes. HSSs can be especially effective in coupling with the Earth's ionosphere/magnetosphere because of the long-lasting recovery of the storms they produce.
To address Objective II of the National Space Weather Strategy and Action Plan to "Develop and Disseminate Accurate and Timely Space Weather Characterization and Forecasts" and US Congress PROSWIFT Act 116-181, our team has developed a new set of open-source software that ensures substantial improvements of SWx forecasts. On the one hand, our focus has been on the development of data-driven solar wind models. On the other hand, each individual component of our software has been designed to have accuracy higher than any existing SWx prediction tools with a dramatically improved performance. This has been done by the application of new computational technologies and enhanced data sources. The development of such software paves way for improved SWx predictions accompanied with an appropriate uncertainty quantification. This makes it possible to forecast hazardous SWx effects on the space-borne and ground-based technological systems, and on human health. Our models include (1) a new, open-source solar magnetic flux model (OFT), which evolves information to the back side of the Sun and its poles, and updates the model flux with new observations using data assimilation methods; (2) a new potential field solver (POT3D) associated with the Wang-Sheeley-Arge (WSA) coronal model, resulting in SWiG and (3) a new adaptive, 4-th order of accuracy solver (HelioCubed) for the Reynolds-averaged MHD equations implemented on mapped multiblock grids (cubed spheres). The tests show that our software is formally more accurate and performs much faster than its predecessors used for SWx forecasts. All components in the POT3D-OFT-SWiG-HelioCubed toolkit work on both CPUs and GPUs and have been made publicly available:
(1) POT3D: https://github.com/predsci/pot3d
(2) OFT/MagMAP: https://github.com/predsci/magmap
(3) OFT/HipFT: https://github.com/predsci/oft
(4) Magnetic field tracer MAPFL: https://github.com/predsci/mapfl
(5) SWiG: https://github.com/predsci/swig
(6) HelioCubed: https://github.com/dhami1234/HelioCubed.
In addition, they have been either implemented (OFT, WSiG) or submitted for implementation (HelioCubed) at the NASA Community-Coordinated Modeling Center (CCMC).
To quantify uncertainty in simulation results and, consequently, SWx forecasts, the team preformed extensive ensemble simulations and analyzed their performance using the WSA metrics. New uncertainty quantification procedures have been applied in simulations involving multiple spacecraft data, including Parker Solar Probe (PSP), Solar Orbiter (SolO), STEREO, and OMNI data base. These analyses have been applied both to the ambient (background) solar wind and to CMEs. From the forecasting perspective, the ensemble modeling approach significantly improves our ability to assess and communicate uncertainties in the ambient SW. By simulating a range of solar wind realizations, we were able to quantify the confidence bounds for each specific prediction. Our study represented the first step towards understanding of how uncertainties in the input synchronic maps propagate through the model chain. Importantly, such modeling also helped distinguish between the features that are robust across the ensemble members and those that are sensitive to boundary uncertainties, enabling forecasters to better assess the associated risks.
Our team directly demonstrated that a 12-hour, on the average, prediction window for the CME time of arrival may be directly related to subjective uncertainties in the identification of initial parameters of CMEs inserted into the background SW. This means that (1) theoretical CME models require further improvements and (2) more observational data is required for be used in the above-mentioned models. It has been demonstrated convincingly that application of ML/AI techniques is critically important for improving SWx forecasts at the current state of the art. By way of example, we used the time-elongation CME maps available from STEREO (now also from SolO) spacecraft for this purpose. As a result, we have been able to improve CME time of arrival predictions 2-3 times. Although our pioneering study involved a few dozens of CMEs, the proposed approach is certainly very promising and productive.
Last Modified: 06/24/2025
Modified by: Nikolai V Pogorelov
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