Waves in the Inner Magnetosphere and their Effects on Radiation Belt Electrons
This project aims to develop comprehensive wave models using multi-satellite data to understand the dynamics of Earth's radiation belts and their response to geomagnetic storms.
Projectdetails
Introduction
The magnetosphere is a natural plasma laboratory. Radiation belts in the magnetosphere are full of high-energy particles. The energetic electrons in the Earth’s radiation belts can be hazardous to Earth-orbiting satellites and astronauts in space. Many of the space systems on which modern human society depends operate in this region.
Dynamics of Radiation Belt Electrons
The fluxes of radiation belt electrons are very dynamic, which is not fully understood due to the delicate balance between various acceleration and loss processes. Wave-particle interactions are believed to play a crucial role in the acceleration and loss of these particles.
Need for Comprehensive Wave Models
To quantify the effect of different waves on the dynamics of radiation belt electrons, comprehensive wave models are needed. Currently, there are some wave models based on satellite measurements. However, the space coverage of these wave models is not sufficient due to the orbit limit of satellites.
Project Objectives
In this project, combining state-of-the-art measurements from multiple satellites, comprehensive wave models will be developed. The objectives include:
- Improving our sophisticated physics-based radiation belt dynamic model by using the wave models developed in this project.
- Calculating diffusion coefficients using more realistic background magnetic field and plasma density models for the first time.
- Quantifying fundamental acceleration and loss of energetic electrons caused by different waves in the Earth's radiation belts.
Validation of Results
We will systematically validate simulation results against satellite measurements to understand the competition between acceleration and loss caused by various mechanisms.
Scientific Importance
All these improvements will be critically important for answering the overarching scientific question: Why do the Earth’s radiation belts respond differently to geomagnetic storms which have approximately the same intensity? The knowledge gained in this project can be useful for basic plasma physics and astronomy physics because similar fundamental processes exist.
Financiële details & Tijdlijn
Financiële details
Subsidiebedrag | € 1.999.415 |
Totale projectbegroting | € 1.999.415 |
Tijdlijn
Startdatum | 1-6-2024 |
Einddatum | 31-5-2029 |
Subsidiejaar | 2024 |
Partners & Locaties
Projectpartners
- HELMHOLTZ ZENTRUM POTSDAM DEUTSCHES GEOFORSCHUNGSZENTRUM GFZpenvoerder
Land(en)
Vergelijkbare projecten binnen European Research Council
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Impact of foreshock transients on near-Earth space
The WAVESTORMS project aims to investigate the role of foreshock transients in collisionless shocks and their effects on particle acceleration and wave storms in Earth's magnetosphere.
Waves for energy in magnetized plasmas
SMARTWAVES aims to develop a novel plasma regime for fusion devices by enhancing wave-particle interaction understanding, improving diagnostics, and bridging fusion, space, and astrophysical research.
Dynamic Magnetosphere Ionosphere Thermosphere coupling
DynaMIT aims to revolutionize our understanding of space-atmosphere coupling in the polar ionosphere by integrating 3D modeling with innovative data assimilation techniques to enhance space weather predictions.
Solving the Bz problem in heliospheric weather forecasting
This project aims to enhance solar wind predictions at the Sun-Earth L1 point using advanced models to improve space weather forecasts, benefiting technology and society's resilience to extreme conditions.
Mercury in the solar wind: adaptive kinetic model for space weather at solar system's innermost planet
Develop a high-performance global plasma simulation model to study Mercury's unique solar wind interaction and enhance understanding of space weather processes through BepiColombo mission observations.