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Sunrise: 08:22Sunset: 16:48
8h 25m 45sof daylight today which is 3 min longerthan yesterday
All weather on Earth, from the surface of the planet out into space, begins with the Sun. Space weather and terrestrial weather (the weather we feel at the surface) are influenced by the small changes the Sun undergoes during its solar cycle. These changes can also potentially impact GPS systems, along with radio and satellite communications.
Various government and non-governmental agencies around the world study space weather changes in order to understand and predict their impacts going forward, and often make this data freely available.
The data on this page has been taken from these freely available sources.
The sun is constantly monitored for sun spots and coronal mass ejections. EIT (Extreme ultraviolet Imaging Telescope) images the solar atmosphere at several wavelengths, and therefore, shows solar material at different temperatures. In the images taken at 304 Angstrom the bright material is at 60,000 to 80,000 degrees Kelvin. In those taken at 171 Angstrom, at 1 million degrees. 195 Angstrom images correspond to about 1.5 million Kelvin, 284 Angstrom to 2 million degrees. The hotter the temperature, the higher you look in the solar atmosphere.
LASCO (Large Angle Spectrometric Coronagraph) is able to take images of the solar corona by blocking the light coming directly from the Sun with an occulter disk, creating an artificial eclipse within the instrument itself. The position of the solar disk is indicated in the images by the white circle. The most prominent feature of the corona are usually the coronal streamers, those nearly radial bands that can be seen both in C2 and C3. Occasionally, a coronal mass ejection can be seen being expelled away from the Sun and crossing the fields of view of both coronagraphs. The shadow crossing from the lower left corner to the center of the image is the support for the occulter disk.
C2 images show the inner solar corona up to 8.4 million kilometers (5.25 million miles) away from the Sun.
C3 images have a larger field of view: They encompass 32 diameters of the Sun. To put this in perspective, the diameter of the images is 45 million kilometers (about 30 million miles) at the distance of the Sun, or half of the diameter of the orbit of Mercury. Many bright stars can be seen behind the Sun.
Real-Time Solar Wind data refers to data from any spacecraft located upwind of Earth, typically orbiting the L1 Lagrange point, that is being tracked by the Real-Time Solar Wind Network of tracking stations. The NOAA DSCOVR satellite became the operational RTSW spacecraft on July 27, 2016 at 1600UT (noon EDT, 10am MDT).
SWPC maintains the ability to instantaneously switch the spacecraft that provides the RTSW data. During times of outages in DSCOVR data or problems with the data, this page may instead display the data from the NASA/ACE spacecraft.
WSA-Enlil is a large-scale, physics-based prediction model of the heliosphere, used by the Space Weather Forecast Office to provide 1-4 day advance warning of solar wind structures and Earth-directed coronal mass ejections (CMEs) that cause geomagnetic storms. Solar disturbances have long been known to disrupt communications, wreak havoc with geomagnetic systems, and to pose dangers for satellite operations.
The Solar Cycle is observed by counting the frequency and placement of sunspots visible on the Sun. The forecast comes from the Solar Cycle Prediction Panel representing NOAA, NASA and the International Space Environmental Services (ISES). The Prediction Panel forecasts the sunspot number expected for solar maximum and has predicted a maximum of 115 occurring in July, 2025. The error bars (high/low) on this prediction mean the panel expects the cycle maximum could be between 105-125 with the peak occurring between November 2024 and March 2026, as shown in the chart below.
Data sourced and prepared by the U.S. Dept. of Commerce, NOAA, Space Weather Prediction Center (SWPC). Data source file
This forecast provides a short-term glimpse into the location and intensity of the aurora. Developed using the OVATION model, it offers a 30 to 90-minute projection of where and how intense the aurora will be. The forecast lead time corresponds to the duration it takes for solar wind to travel from the L1 observation point to Earth.
The two maps below depict Earth’s North and South poles. The aurora’s brightness and position are typically represented as a green oval centered around Earth’s magnetic pole. When the aurora is expected to intensify, these green ovals transition to red. Meanwhile, the sunlit side of Earth is indicated by lighter blue ocean hues and the continents’ paler colors. Auroras can be witnessed somewhere on Earth shortly after sunset or just before sunrise. However, they remain invisible during daylight hours. Remarkably, the aurora need not be directly overhead; it can be seen from distances of up to 1000 km when conditions align and its brilliance shines.
The aurora serves as an indicator of current geomagnetic storm conditions, offering situational awareness for various technologies. It directly affects HF radio communication and GPS/GNSS satellite navigation. Additionally, it’s closely linked to ground-induced currents that impact electric power transmission.
Instruments on board the NOAA Polar-orbiting Operational Environmental Satellite (POES) continually monitor the power flux carried by the protons and electrons that produce aurora in the atmosphere. SWPC has developed a technique that uses the power flux observations obtained during a single pass of the satellite over a polar region (which takes about 25 minutes) to estimate the total power deposited in an entire polar region by these auroral particles. The power input estimate is converted to an auroral activity index that ranges from 1 to 10.
The D-Region Absorption Product addresses the operational impact of the solar X-ray flux and SEP events on HF radio communication. Long-range communications using high frequency (HF) radio waves (3 - 30 MHz) depend on reflection of the signals in the ionosphere. Radio waves are typically reflected near the peak of the F2 layer (~300 km altitude), but along the path to the F2 peak and back the radio wave signal suffers attenuation due to absorption by the intervening ionosphere. The D-Region Absorption Prediction model is used as guidance to understand the HF radio degradation and blackouts this can cause.
Product: 3-Day Forecast - Issued: 2026 Jan 21 1230 UTC Prepared by the U.S. Dept. of Commerce, NOAA, Space Weather Prediction Center.
The greatest observed 3 hr Kp over the past 24 hours was 8 (NOAA Scale G4). The greatest expected 3 hr Kp for Jan 21-Jan 23 2026 is 7.33 (NOAA Scale G3).
Rationale: G1-G3 (Minor-Strong) geomagnetic storms are expected on 21 Jan due to a halo CME compounded with CH HSS influences, with isolated G1 (Minor) expected on 22 Jan.
Solar radiation, as observed by NOAA GOES-18 over the past 24 hours, was above S-scale storm level thresholds.
Rationale: S1 (Minor) or greater solar radiation storms are expected on 21 Jan and possible on 22 Jan, decreasing to a slight chance on 23 Jan.
Radio blackouts reaching the R1 levels were observed over the past 24 hours. The largest was at Jan 21 2026 0712 UTC.
Rationale: R1-R2 (Minor-Moderate) radio blackouts are likely, with a slight chance for R3 (Strong) events, on 21-23 Jan.
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