Skip to main content

Space Weather Academy

Guides

A structured library covering space weather from first principles all the way to reading live NOAA data and planning a night out under the aurora. Six categories, all cross-linked to the live tools on this site.

Space Weather Fundamentals

Start here. What space weather actually is, how the Sun couples to Earth's magnetosphere, and why geomagnetic storms happen at all.

What Is a Geomagnetic Storm?

Magnetospheric compression phases and NOAA's G-scale classifications, from G1 to G5.

What Is Space Weather? The Heliospheric Environment

The continuous stream of radiation and magnetic plasma emitted by the Sun that interacts directly with Earth's atmosphere.

Space Weather vs. Earth Weather

Key structural differences — how each moves energy, and why rain gauges can't measure aurora visibility.

Why the Sun Has an 11-Year Cycle

The internal solar dynamo engine — differential rotation, magnetic winding, and pole reversal.

How the Sun Affects Earth

Heliospheric coupling — how solar activity reaches across space to interact with our planet.

Understanding the Magnetosphere

Earth's cosmic defense shield — how it deflects solar radiation and charged particles.

Earth's Magnetic Field Explained

The core geodynamo engine that generates and sustains our planet's magnetic field.

What Is Space Weather?

A plain-English intro to the shifting Sun-Earth environment: solar wind, flares, CMEs, and their real-world effects.

What Is Solar Wind?

The continuous stream of charged particles flowing from the Sun, its typical speed and density, and its role in shaping Earth's magnetosphere.

How Geomagnetic Storms Are Classified (G1–G5)

NOAA's five-step scale, what each level means for aurora, power grids, and satellites.

Space Weather

A complete guide to space weather: what it is, what causes it, how it's monitored, and why it matters for power grids, satellites, aviation, GPS, and the aurora.

Earth & Magnetosphere

Learn how Earth's magnetic field forms, why it protects us from solar wind, and how it drives the aurora.

The Solar System

Learn about the layout of the solar system, the eight planets, dwarf planets, and the boundary where the Sun's influence ends.

Reading Live Space Weather Data

How to interpret every number on the live dashboards — Kp, Bz, Bt, solar wind speed, X-ray flux, and NOAA alerts.

Decoding Live Magnetometer Charts

Read real-time ground-based magnetometer deflection data, faster than the lagging Kp index.

What Is the Kp Index?

The universal 0-to-9 scale used to measure global geomagnetic storm intensity and aurora visibility.

What Is the Solar Wind?

The continuous stream of ionized plasma blowing from the Sun — speed, density, and why it matters.

What Is the Bz Component?

Why a negative, southward-pointing interplanetary magnetic field is the key to aurora visibility.

How to Read a Space Weather Forecast

Decode NOAA's 3-day forecast — Kp grid, R/S/G scales, and the written discussion.

How to Read the Kp Index

What each Kp value means, how it maps to your geomagnetic latitude, and its real limitations.

How to Read the Solar Wind

Speed, density, and temperature from DSCOVR — how to spot a CME shock arrival in real time.

How to Read the Bz Magnetic Field

Why a southward (negative) Bz is the single most important trigger for aurora activity.

How to Understand NOAA Space Weather Alerts

Watch vs warning vs alert, and the R/S/G category system for radio, radiation, and geomagnetic storms.

How to Predict Aurora Visibility

Combine Kp, Bz, cloud cover, moon phase, and geomagnetic latitude to know if tonight is worth it.

Kp Index

Learn what the Kp index is, how it's measured, typical values, and why it's the single most-used number for predicting aurora visibility.

Solar Wind

Learn what solar wind is, how fast it typically travels, how it's measured, and why its speed matters for aurora and space weather.

Bz (IMF Bz)

Learn what Bz is, why its direction matters more than its strength, and why it's considered the best real-time predictor of aurora activity.

Bt (Total Magnetic Field)

Learn what Bt is, how it relates to Bz, typical values, and why the total field strength sets the ceiling on geomagnetic storm intensity.

Interplanetary Magnetic Field (IMF)

Learn what the interplanetary magnetic field is, how it's structured, and why its Bz and Bt components are central to space weather forecasting.

Proton Flux

Learn what proton flux measures, the NOAA S-scale for radiation storms, and why it matters for astronauts, satellites, and polar flights.

Electron Flux

Learn what electron flux measures, why energetic electrons matter for satellites, and how it relates to Earth's radiation belts.

X-ray Flux

Learn what X-ray flux is, how it's used to classify solar flares, and why it causes radio blackouts on Earth.

F10.7 Solar Radio Flux

Learn what the F10.7 solar radio flux index measures, why it's used as a solar activity proxy, and how it affects satellite orbits.

Solar Events

Flares, CMEs, coronal holes, and the 11-year solar cycle — the drivers behind every geomagnetic storm on the dashboard.

Aurora & Northern Lights

Everything about the aurora — the physics behind the colors, how to photograph them, and why a high Kp doesn't always mean a visible sky.

Night Sky & Observing

The everyday sky. Moon phases, visible planets, meteor showers, stars, and how to actually find them from your backyard.

How to See Planets Tonight

How to identify Venus, Mars, Jupiter, and Saturn in the night sky, why planets don't twinkle, and common beginner mistakes.

What Is a Star?

How nuclear fusion powers stars, why they don't 'burn' like fire, and why star color reveals surface temperature.

Moon Phases for Beginners

How and why the Moon's phases change over its 29.5-day synodic cycle, plus Earthshine.

What Is a Planet?

The real IAU definition, why Pluto was reclassified, and how planets differ from moons and exoplanets.

The Moon

The Moon explained: how it formed, why it always shows the same face, its phases, and how moonlight affects stargazing and aurora viewing.

Stars & Stellar Evolution

Learn how stars form, how they generate energy through nuclear fusion, and how they die.

Eclipses (Solar & Lunar)

Learn how solar and lunar eclipses happen, what totality means, and how to observe them safely.

Comets

Learn how comets form, why their tails always point away from the Sun, and where they come from.

Asteroids

Learn about the asteroid belt, Near-Earth Objects, and how NASA tracks and defends against potential impacts.

Meteor Showers

Learn what causes meteor showers, how to find the radiant point, and when major annual showers peak.

Stargazing & Astrophotography

Learn how to choose a telescope, find dark skies, and set up your camera for astrophotography.

James Webb Space Telescope

How JWST works, its instruments, its position near L2, and what it studies -- from the early universe to exoplanet atmospheres.

How to Read an Aurora Forecast

What the Kp index, IMF Bz direction, and solar wind speed mean together — and when it's actually worth going outside.

How a Solar Storm Travels From the Sun to Earth

The complete real journey of a solar storm: eruption, CME launch, interplanetary travel, L1 detection, magnetosphere impact, and the resulting aurora and technology effects.

How Long Does a CME Take to Reach Earth?

Real CME travel times from the Sun to Earth, why slow and fast CMEs differ so much, and how DSCOVR detects the incoming disturbance before it arrives.

What Happens When a CME Hits Earth?

The real sequence from CME arrival to aurora: solar wind shock, magnetosphere compression, southward Bz, magnetic reconnection, and geomagnetic storming.

What Is Light Pollution and How Does It Affect Stargazing?

The Bortle scale, sky brightness, urban vs rural skies, moonlight, and artificial light -- and why faint aurora and stars disappear in bright skies.

How Does the Moon Affect What You Can See Tonight?

How lunar illumination changes observing conditions: moon phase, moonrise and moonset, deep-sky observing, meteor watching, and aurora viewing.

How to Photograph the Northern Lights

A practical guide to photographing aurora: smartphone photography, camera settings, shutter speed, ISO, focus, tripods, and why cameras see more than your eyes.

How to Photograph a Solar Eclipse Safely

Safe solar eclipse photography: certified solar filters, camera safety, smartphone limitations, wide-angle vs telephoto, and totality filter timing.

Why Does the Aurora Turn Green, Red, Purple and Blue?

The real atomic physics behind aurora colors: oxygen and nitrogen emission, altitude, wavelength, why green dominates, and why cameras see colors your eyes can't.

What Is Solar Wind Speed -- and What Is a Dangerous Speed?

What solar wind speed numbers like 350, 500, 700 and 1,000+ km/s actually mean, and why speed alone never determines whether aurora or a geomagnetic storm happens.

What Is a Solar Storm Shockwave?

The real physics of a CME-driven interplanetary shock front: why solar wind speed, density, magnetic field and temperature all jump at once when it arrives.

How Scientists Predict a Geomagnetic Storm

The real forecasting pipeline behind a geomagnetic storm prediction, from watching the Sun to L1 confirmation, and the crucial difference between forecast, nowcast, and observation.

Why Space Weather Can Affect GPS

How ionospheric disturbances from space weather cause real GPS positioning errors, and why a solar storm doesn't simply turn GPS off.

Can Solar Storms Affect Airplanes?

The real effects of space weather on aviation: polar routes, HF radio, radiation exposure, navigation, communication, and why passengers rarely need to worry.

How to Read SpaceWeatherTracker Like a Scientist

The master tutorial for reading this site's live data together -- Kp, Bz, Bt, solar wind speed, density, X-ray flux, proton flux and CME data as one connected story.

What Is the Solar Cycle?

The real 11-year cycle of solar activity: solar minimum vs maximum, sunspots, flares and CMEs, where we are now, and why it matters for aurora watchers.

What Is a Sunspot and Why Does It Matter?

Why sunspots look dark, how their magnetic fields work, what sunspot groups and active regions are, and how complex fields produce flares and CMEs.

What Is an Active Region on the Sun?

How NOAA numbers active regions, why magnetic complexity drives flare and CME production, and how scientists monitor these regions in real time.

What Is a Solar Flare?

What physically happens during a solar flare, the X/M/C classification scale, X-ray radiation, radio effects, and why flare strength doesn't equal storm strength.

What Is a Radio Blackout?

How solar X-rays disrupt HF radio, the R-scale classification, effects on aviation and maritime communication, and why blackouts are geographically dependent.

What Are Solar Energetic Particles?

High-energy protons and electrons accelerated by solar eruptions: solar particle events, why spacecraft and astronauts care, and Earth's real protection.

What Is a Solar Radiation Storm?

NOAA's S-scale explained: S1 through S5, high-energy protons, satellite impacts, aviation radiation, and how radiation storms differ from geomagnetic storms.

What Is the Magnetosphere?

Earth's magnetic bubble explained: solar wind pressure, the magnetopause, magnetotail, bow shock, and why the magnetosphere protects Earth.

What Is Magnetic Reconnection?

How magnetic field lines reconnect and release energy, connecting solar wind, Earth's magnetic field, particle acceleration, and the aurora in one real chain.

What Is the Magnetotail?

Earth's magnetic tail stretched by the solar wind: magnetic lobes, the plasma sheet, substorms, and how stored energy powers auroral activity.

What Is an Auroral Substorm?

The real physics behind sudden auroral brightening: energy storage, magnetotail reconnection, expansion phase, and why aurora can suddenly explode across the sky.

Why Does the Aurora Move and Dance?

The real physics of auroral motion: charged particles, Earth's magnetic field, magnetic-field changes, curtains, and why some displays appear almost alive.

What Would Happen During a Carrington-Level Solar Storm Today?

What an extreme, Carrington-level solar storm would realistically mean today for satellites, GPS, radio, aviation, power grids and aurora -- without the sensationalism.

The Parker Spiral

Why the Sun's rotation twists the interplanetary magnetic field into a spiral -- and why that shape governs how particles and storms actually reach Earth.

The Ionosphere

The electrically charged upper-atmosphere layer where space weather directly disrupts GPS, HF radio, and aviation communications.

Earth's Radiation Belts

The Van Allen belts explained -- trapped particles, spacecraft exposure, and why they're a genuinely different hazard from solar energetic particles or cosmic rays.

The Solar Dynamo and Tachocline

How differential rotation and the tachocline deep inside the Sun are believed to generate the magnetic field behind sunspots, flares, and the 11-year cycle.

Corotating Interaction Regions (CIRs)

Not every geomagnetic storm comes from a CME -- how fast solar wind from coronal holes creates recurring storms as the Sun rotates.

Spacecraft Charging

How energetic particles build up dangerous electric charge on and inside satellites -- surface charging and deep dielectric charging explained.

Satellite Drag

How geomagnetic storms heat and expand Earth's upper atmosphere, increasing drag on low-Earth-orbit satellites and altering their orbits.

Planets

The planets explained: what defines a planet, the rocky and gas giant families, and how to spot them in tonight's sky.

Why Do Stars Twinkle? Atmospheric Scintillation & Planet Stargazing

Stars twinkle because Earth's turbulent atmosphere bends and refracts their pinpoint light in constantly shifting directions. Learn the physics of scintillation and why planets don't twinkle the same way.

Can You See the Aurora With the Naked Eye? Camera vs Human Vision

Yes, the aurora is often visible to the naked eye, but cameras routinely capture far more color and detail than human vision can perceive in low light. Learn why, and what to realistically expect.

Why Is the Moon Red? Lunar Eclipses, Rayleigh Scattering & Blood Moons

The Moon turns red during a total lunar eclipse because Earth's atmosphere bends sunlight into its shadow, filtering out blue light through Rayleigh scattering and letting only red light through — the same physics behind a sunset.

What Is a Solar Flare? X-Class Flares, Radio Blackouts & Solar Dynamics

A solar flare is a sudden, intense burst of radiation from the Sun caused by magnetic reconnection above sunspots. Learn the A-B-C-M-X classification, radio blackout effects, and how flares are tracked in real time.

Why Do Satellites Flare? Starlink Glints, Solar Arrays & Night Sky Streaks

Satellites flare when their flat, reflective solar panels or antennas briefly catch and mirror sunlight directly toward an observer on the ground, producing a sudden bright glint as they cross the night sky.

Why Is the Sky Blue? Rayleigh Scattering, Solar Spectra & Sunset Colors

The sky is blue because Earth's atmosphere scatters shorter blue wavelengths of sunlight far more strongly than longer red wavelengths, a phenomenon called Rayleigh scattering — and the same physics turns sunsets red.

What Is a Geomagnetic Storm? G1–G5 Scales, Solar CME Impacts & Grid Risks

A geomagnetic storm is a temporary, measurable disturbance of Earth's magnetic field caused by solar wind or CME impacts. Learn the G1-G5 NOAA storm scale, real infrastructure risks, and how storms are forecast.

What Causes the Northern Lights? Magnetosphere, Solar Wind & Atmospheric Glow

The northern lights are caused by charged particles from the Sun colliding with gases in Earth's upper atmosphere near the poles, exciting oxygen and nitrogen atoms that release light as they return to their normal state.

Noctilucent Clouds (NLCs): How to Spot Polar Mesospheric Clouds

Noctilucent clouds are rare, electric-blue ice clouds forming 76-85 km high in the mesosphere, visible only during deep summer twilight when the sun illuminates them from below the horizon.

What Is STEVE? Strong Thermal Emission Velocity Enhancement

STEVE is a rare, mauve-purple ribbon of light in the night sky, distinct from the aurora, caused by a fast-moving, hot river of charged particles in the upper atmosphere called a subauroral ion drift.

Can I See the International Space Station Tonight? Pass Times & Viewing Guide

Yes — the ISS is visible to the naked eye as a bright, steadily moving point of light during specific pass windows shortly after sunset or before sunrise. Learn how to find tonight's exact pass time.

How to Identify Planets in the Night Sky: Steady Light vs Twinkle & Ecliptic Paths

Identify planets in the night sky by their steady, non-twinkling light, their position along the ecliptic path, and their characteristic colors and brightness — no telescope required for the five brightest.

Space & Missions

Beyond aurora — how space weather affects satellites and launches, plus the missions and objects that shape modern astronomy.

Deep Space

Beyond our solar system — nebulae, stellar evolution, pulsars, exoplanet atmospheres, supernovae, and the cosmic microwave background.