Space Weather Laboratory (SWL)
Researching the physical processes that trigger space weather and their effects on Earth and throughout the solar system
Learn MoreOur Mission
The Space Weather Laboratory performs research and analysis of the physical processes underlying space weather. It conducts space-based, ground-based, theoretical, and modeling studies of the chain of events that triggers space-weather effects of interest to NASA, other U.S. government agencies, and the general public. Laboratory staff lead the development of space environment projects and missions, and provide project scientists for NASA flight missions with space weather applications. The Laboratory communicates NASA research results to the scientific community, various space weather interests, and the general public.
Strategic Priorities
Our key research goals and objectives.
- Understanding the physics of space weather (SW) activity, from initiation of solar eruptions to geomagnetically induced currents on Earth
- Using our insights to improve SW models and develop new ones
- Validating and prototyping SW models for research-to-operations transitions
- Conveying critical SW information to users with innovative, effective products
- Enabling community SW research through access to models, tools, and data streams
Development Areas and Core Activities
Our expertise and ongoing research activities.
- State-of-the-art theory/modeling of the solar atmosphere and wind, including eruptions on all scales
- In-depth analysis and interpretation of solar, heliospheric, and geospace data
- Instruments flown on sounding rockets, to measure fields and particles in geospace
- Miniaturized geospace instruments to be flown on Cubesats and other small satellites
- Spaceborne lidar for observing the mesospheric sodium layer (wind diagnostics)
- Electric-field boom design and construction
- Novel methods for remote sensing and in-situ sampling of the magnetosphere and ITM
- Space weather impacts on the power grid (GICs) and on locations throughout the Heliosphere, including extreme (Carrington-type) SW events
- Basic physics of magnetic reconnection
Flight Missions
Our active and upcoming space missions.
- ARTEMIS
- C/NOFS
- Firefly
- Geotail
- THEMIS
- TIMED
- Van Allen Probes
- GOLD
- ICON
Research Highlights
Recent discoveries and ongoing investigations.
A very fast CME was observed on January 7, 2014. Preliminary data analysis and all 8 community forecasts reported in GSFC's Space Weather Scoreboard indicated rapid arrival at Earth and a major geo-magnetic storm. However, the CME arrived at Earth ~19 hr after the predicted time, and the geo¬magnetic storm was weak (Kp < 3). What happened?
Detailed analysis by the CCMC/SWRC team identified possible causes for the gap between predicted vs. actual outcome.
The solar wind coming from the nearby coronal holes was extremely fast – 950 km/s at Earth (very rare!) and deflected the CME away from the Earth. However, the solar wind speed assumed at the lower boundary of the CME transport model (WSA-ENLIL) was too low – 750 km/s (maximum allowed value). Therefore the model CME propagated to Earth much too slowly. Previously the same coronal hole did not produce such high speed wind, so the strong deflection was a surprise. We know that CMEs can be deflected by a coronal hole, so a CME that seems to be Earth-directed can be deflected from the Earth-Sun line. The simulations did not predict that the deflection would be so large that the CME only hit a glancing blow to the Earth.
Theory predicts that the interplanetary magnetic field (IMF) flattens the circular near-Earth magnetotail cross-section into an oblate cross-section far from the Earth.
Sibeck et al. [JGR, 2014] used the BATS-R-US global magnetospheric model, run at GSFC's CCMC, to show how rotating the IMF orientation from vertical to horizontal flattens the cross-section of the Earth's magnetotail.
The 674 team is now ready to test these model predictions with recent ARTEMIS observations at lunar distances.