Free Real-Time Radiation Monitor & Solar Weather Dashboard_
Live NOAA SWPC Telemetry · Geomagnetic Storm Tracking · Ionizing Radiation Reporting
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Live NOAA data on top, modelled ground-level dose on the map.
The NOAA R, S and G scales show radio blackouts, radiation storms and geomagnetic storms on 0–5.
The 24-hour bar chart shows geomagnetic activity on 0–9. Kp 5 or more is a storm.
The speed dial turns yellow above 500 km/s and red above 700; a strongly negative Bz often comes before a storm.
Click any of the 61 locations for dose rate, yearly dose and comparisons, or jump by region or station.
Overlay NOAA’s live OVATION forecast and open the map full screen.
This free real-time radiation monitor provides live reporting on global ionizing radiation levels, solar weather conditions, and geomagnetic activity. All data is sourced directly from NOAA's Space Weather Prediction Center (SWPC), the world's authoritative source for space weather forecasting and solar event reporting. The space-weather data refreshes automatically every 2 minutes, giving you continuous access to live space weather telemetry without any registration, API keys, or fees.
The Kp Index chart displays the last 24 hours of planetary geomagnetic activity, measured on a 0 to 9 scale. This index is essential for understanding when geomagnetic storms may affect GPS accuracy, radio communications, power grid stability, and aurora visibility. A Kp value of 5 or above indicates a geomagnetic storm. The color-coded bar chart makes it easy to spot storm periods at a glance, and the status badge provides an instant summary of current geomagnetic conditions — from quiet to extreme storm levels.
The solar wind particle stream visualization shows real-time data from the DSCOVR and ACE spacecraft positioned at the L1 Lagrange point, approximately 1.5 million kilometres upstream of Earth. Particle speed and density are mapped directly to the animation — faster solar wind creates faster-moving particles, and higher proton density increases particle brightness. When solar wind speeds exceed 500 km/s, the display shifts from cyan to yellow, and above 700 km/s it turns red, providing an immediate visual warning of elevated conditions.
The magnetometer Bz timeline tracks the north-south component of the interplanetary magnetic field over the past six hours. When Bz turns negative (southward), it enables magnetic reconnection with Earth's magnetosphere, allowing solar wind energy to couple more efficiently into our magnetic field. Extended periods of strongly negative Bz are the primary driver of geomagnetic storms, making this one of the most important parameters for space weather forecasting.
The interactive world map displays modeled ground-level radiation for 61 locations worldwide — from major capitals to famous radiological anomalies: Pripyat (Chernobyl exclusion zone), Fukushima, Ramsar in Iran (the world's highest natural background, driven by radium-rich hot springs), Guarapari's monazite beaches in Brazil, and the thorium belts of Kerala and Yangjiang. Click any station for a full breakdown: dose rate, annual projection, cosmic-ray latitude and altitude factors, live geomagnetic modulation, geology notes, and everyday comparisons (bananas, chest X-rays, flight hours). A region selector jumps between continents, the station picker ranks locations by current level, and the NOAA OVATION aurora oval can be overlaid live. The map goes truly fullscreen with all controls available.
Ground-level radiation estimates are calculated using a physics-based model that combines known geological baselines per city with real-time cosmic ray modulation data. Higher geomagnetic latitude increases cosmic ray exposure due to weaker magnetic shielding, and elevated Kp index values modulate the cosmic ray intensity reaching Earth's surface. While these are modeled estimates rather than direct sensor readings, they use the same real NOAA data that drives professional space weather reporting systems.
This real-time radiation monitor is completely free to use with no account creation, no ads, and no data collection. It runs entirely in your browser using client-side JavaScript and public NOAA APIs. Whether you are a space weather enthusiast, a radio amateur monitoring HF propagation conditions, a researcher tracking geomagnetic storm impacts, or simply curious about current radiation levels around the world, this tool provides professional-grade radiation monitoring in an accessible, visually engaging format. It is one of over 100 free browser-based tools available at jasperbernaers.com — all built with the same commitment to real data, zero friction, and beautiful design.
Microsieverts per hour (μSv/h) is a dose rate: how much radiation dose a person would receive per hour at that spot. Natural background is typically 0.05 to 0.3 μSv/h, depending on the rocks underground, radon and altitude. Thresholds for an alarm differ per national network, so compare a reading with the usual level for that place rather than with one fixed number.
The worldwide average from natural sources is about 2.4 mSv a year (UNSCEAR): roughly 1.3 mSv from radon, 0.5 mSv from rocks and soil, 0.4 mSv from cosmic rays and 0.3 mSv from food and drink. Medical imaging adds about 0.6 mSv on average worldwide, and more in countries with heavy CT use. The occupational limit for radiation workers is 20 mSv a year, averaged over five years.
Below about 100 mSv the extra cancer risk is too small to measure directly; radiation protection assumes roughly 0.5% extra lifetime cancer risk per 100 mSv. An acute dose of about 1 Sv (1,000 mSv) causes radiation sickness, and around 4–5 Sv is fatal for about half of people without treatment. Even the highest point on this map, Ramsar at about 1 μSv/h, adds up to under 10 mSv a year.
Alpha particles (helium nuclei) are stopped by paper or skin but are harmful when inhaled or swallowed. Beta particles (electrons) pass through skin but are stopped by a few millimetres of aluminium. Gamma rays need lead or thick concrete. Environmental monitors mostly measure gamma, the main external dose. At flight altitude, neutrons from cosmic rays add a significant share.
Yes: a small fraction of the potassium in a banana is radioactive potassium-40. Eating one gives about 0.1 μSv, the informal “banana equivalent dose”. A day of normal background is about 20 bananas, a chest X-ray about 200, and a transatlantic flight about 400. The station panel on the map shows each city’s dose rate in bananas per day.
The solar flux index measures the Sun’s radio output at 2,800 MHz (10.7 cm), measured daily at the Dominion Radio Astrophysical Observatory in Penticton, Canada. It runs from about 65 sfu at solar minimum to 200–300 sfu or more around solar maximum, and tracks the Sun’s ultraviolet output, which matters for HF radio propagation and satellite drag.
Kp is a 0–9 measure of global geomagnetic disturbance, derived every three hours from 13 magnetometer stations between 44° and 60° geomagnetic latitude. Kp 5 is a minor storm (G1), Kp 7 a strong storm (G3), Kp 8 severe (G4) and Kp 9 extreme (G5). Storms can degrade GPS accuracy, HF radio and satellite operations and, in extreme cases, power grids.
NOAA rates space weather on three 0–5 scales: R for radio blackouts caused by X-ray flares, S for solar radiation storms caused by energetic protons (relevant to astronauts and polar flights), and G for geomagnetic storms, the same activity the Kp index measures. 0 means no event in progress.
Not on the ground: the atmosphere and the Earth’s magnetic field absorb it, which is why the ground estimates on the map barely move during storms. The risk is for astronauts and for crews on polar flights during solar particle events, and for infrastructure such as GPS, radio, satellites and power grids — the 1989 Québec blackout was caused by a geomagnetic storm.
It depends on Kp. At Kp 3 the aurora usually stays at high latitudes (Iceland, northern Norway, Alaska). At Kp 5 it can reach Scotland, Denmark and southern Canada, and at Kp 7 or more it can be seen in parts of central Europe and the northern United States. Turn on the aurora oval layer on the map for NOAA’s live OVATION forecast, and look north from a dark place.
Ramsar, Iran holds the record: radium-rich hot springs give some residents up to about 260 mSv a year. Other well-known areas are the monazite-sand beaches of Guarapari in Brazil, the thorium-rich coast of Kerala in India (up to about 70 mSv a year), Yangjiang in China, and high-altitude cities such as Denver and Bogotá, where more cosmic radiation reaches the ground.
Yes. The 1986 accident spread caesium-137 and strontium-90, both with half-lives of about 30 years, so a little over half of that contamination has decayed since. Central Pripyat typically reads around 1 μSv/h, with hotspots such as the Red Forest far higher, and parts of the exclusion zone will stay restricted for a very long time.
Most of Fukushima prefecture is back to near-normal levels and most evacuation orders have been lifted. Monitoring posts in towns near the plant mostly read a few tenths of a μSv/h, the remaining restricted zones more, and Tokyo around 0.04 μSv/h. Levels keep falling a few percent a year through decay and weathering. Japan runs thousands of public real-time monitoring posts.
Cosmic radiation roughly doubles every 1,500–2,000 metres you climb. At sea level it contributes about 0.03 μSv/h; at cruise altitude (10–12 km) the total dose rate is about 3–8 μSv/h, depending on latitude and solar activity. A transatlantic flight gives roughly 30–60 μSv. In the EU, airlines must assess the dose of aircrew who are likely to receive more than 1 mSv a year.
Solar flux, solar wind, Kp, Bz, the R/S/G scales and alerts come from NOAA’s Space Weather Prediction Center and refresh every 2 minutes. The ground-level values on the map are modelled: a known geological and altitude baseline per location, adjusted with the live NOAA data, because official ground networks such as EURDEP and RadNet do not offer a free browser API for individual stations. Use them for context, not as measurements.
Official readings come from national networks: Europe’s EURDEP (thousands of stations across about 39 countries), the US EPA RadNet, Germany’s BfS ODL network and Belgium’s FANC TELERAD. The CTBTO’s International Monitoring System also measures airborne radioactivity worldwide. Community projects such as Safecast publish millions of open Geiger-counter measurements. In an emergency, always follow your national radiation protection agency.
Markers are coloured and sized by modelled dose rate, from green (low) through cyan, yellow and orange to red; known hotspots such as Chernobyl, Fukushima and Ramsar are flagged. Use the region and station drop-downs to jump around, click a marker for details, and use the full-screen button above the map.
The dashboard is free, with no signup, no ads and no tracking cookies.