What We Study

Building on NASA’s rich history of exploration of Earth’s neighborhood and distant planetary systems, we are poised to provide a predictive understanding of our place in the solar system. While sunlight fundamentally enables and sustains life, our star can also produce radiation and magnetic energy that can disrupt planets’ atmospheres, satellites, and even life. We study this space environment in order to send spacecraft and astronauts through it safely. Closer to home, we seek knowledge of near-Earth space, because -- when extreme -- space weather can interfere with our communications, satellites and power grids.

Mapping out this interconnected system requires a holistic study of the Sun’s connection to Earth and other planets at both small and large scales. To accomplish this, heliophysics encompasses a vast range of research subjects, including but not limited to:

  • the sun's 11-year solar cycle
  • giant solar explosions such as solar flares and coronal mass ejections
  • the constant stream of solar particles called the solar wind
  • the magnetic environment near Earth
  • what drives change in the charged particles that surround Earth and inhabit the ionosphere
  • boundaries of the solar system as it travels through our interstellar neighborhood.


Solar Science

NASA studies the Sun for numerous reasons. The Sun’s variable radiation influences the habitability of Earth, which can be either be helpful or detrimental to life. The accompanying energy and plasma the Sun sends out, can create changes in the space weather around us and interfere with our space technology and communications systems. The Sun is the only star we can study up close, and can inform our research of other stars throughout the universe.  

Space Weather

The Sun’s constant outflow of solar wind fills space with a thin and tenuous wash of particles, fields, and plasma. This solar wind, along with other solar events like giant explosions called coronal mass ejections, influences the very nature of space and can interact with the magnetic systems of Earth and other worlds. Such effects also change the radiation environment through which our spacecraft – and, one day, our astronauts headed to the Moon and to Mars – travel.  Such space weather can interfere with satellite electronics, communications and GPS signals, and even – when extreme – utility grids on Earth. 


The magnetosphere is a bubble of magnetic fields that surrounds Earth, created by the natural magnetism of the planet. The magnetosphere protects humans on Earth from incoming energy from the Sun, however it does change shape and size in response to such space weather, and these fluctuations can degrade communication signals and cause unexpected electrical surges in power grids. NASA studies the magnetosphere to better understand its role in our space environment. By studying this space environment close to home, we can better understand the nature of space throughout the universe. Such research helps unravel the fundamental physics of space, which is dominated by complex electromagnetic interactions unlike what we experience day-to-day on Earth.

Artist rendition of the magnetosphere

Ionosphere, thermosphere, mesosphere

NASA studies the layers of the atmosphere, such as the ionosphere-thermosphere-mesosphere system where aurora and other space weather events manifest. The ionosphere is a layer in Earth's atmosphere that extends from about 50 to 300 miles above the surface of the planet. The layer is filled with electrically charged particles and overlaps with the neutral particles of the mesosphere and thermosphere. The ionosphere is sensitive to incoming material from the Sun, so it can respond dramatically to space weather. Since the ionosphere is home to low Earth-orbiting spacecraft, as well as the region of space through which radio communications travel, unexpected changes in the region can have a dramatic effect on human technology.

Graphic diagram of the Ionosphere
​Stretching from roughly 50 to 400 miles above the surface, this region, called the ionosphere, is an electrified layer of the upper atmosphere, generated by extreme ultraviolet radiation from the Sun. Understanding the ionosphere’s extreme variability is tricky because it requires detangling interactions between the different factors at play — interactions of which we don’t have a clear picture. That’s where airglow comes in. Airglow occurs when atoms and molecules in the upper atmosphere, excited by sunlight, emit light in order to shed their excess energy. The phenomenon is similar to auroras, but where auroras are driven by high-energy particles originating from the solar wind, airglow is sparked by day-to-day solar radiation.Airglow carries information on the upper atmosphere’s temperature, density, and composition, but it also helps us trace how particles move through the region itself. Vast, high-altitude winds sweep through the ionosphere, pushing its contents around the globe — and airglow’s subtle dance follows their lead, highlighting global patterns.Credit: NASA's Goddard Space Flight Center/Mary Pat Hrybyk-Keith


The Sun sends out a constant flow of charged particles called the solar wind, which ultimately travels past all the planets, extending out three times the distance to Pluto before being impeded by the interstellar medium. This forms a giant bubble around the Sun and its planets, known as the heliosphere. NASA studies the heliosphere to better understand the fundamental physics of the space surrounding us -- which, in turn, teaches us more about the nature of space throughout the rest of the universe, as well as regarding how it drives planetary atmospheres that contribute to planet habitability.