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Sagamore Hill Radio Observatory

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The Sagamore Hill Solar Radio Observatory is a solar radio observatory located in Hamilton, Massachusetts , that operates on a daily basis to obtain scientific observations of the Sun . It is a functional component of the Radio Solar Telescope Network (RSTN).

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86-442: It became apparent in the early 1960s that certain space weather events might interfere with the U.S. objective of putting a man on the moon. Foremost among these concerns was the possibility of a geomagnetic storm of solar origin. Metric Type II radio bursts, signatures of coronal shock waves or coronal mass ejections , were known to be commonly associated with solar flares . The United States Air Force Research Laboratory (AFRL)

172-629: A "Carrington-class" solar superstorm (solar flare, CME, solar electromagnetic pulse ) was observed, but its trajectory narrowly missed Earth. During the May 2024 solar storms , the Aurora Borealis was sighted as far south as Puerto Rico. In June 2013, a joint venture from researchers at Lloyd's of London and Atmospheric and Environmental Research (AER) in the US used data from the Carrington Event to estimate

258-455: A LEO spacecraft falls out of orbit and towards the Earth's surface. Many spacecraft launched in the past few decades have the ability to fire a small rocket to manage their orbits. The rocket can increase altitude to extend lifetime, to direct the re-entry towards a particular (marine) site, or route the satellite to avoid collision with other spacecraft. Such maneuvers require precise information about

344-514: A clear strip of sky, which may be described as four fingers held at arm's length. The northern side from the zenith was also illuminated with beautiful colors, always curling round at the zenith, but were considered to be merely a reproduction of the southern display, as all colors south and north always corresponded. It was a sight never to be forgotten, and was considered at the time to be the greatest aurora recorded [...]. The rationalist and pantheist saw nature in her most exquisite robes, recognising,

430-435: A cooler climate, but these correlations have disappeared after deeper studies. The suggested link from changes in cosmic-ray flux causing changes in the amount of cloud formation did not survive scientific tests. Another suggestion, that variations in the extreme ultraviolet (EUV) flux subtly influence existing drivers of the climate and tip the balance between El Niño / La Niña events collapsed when new research showed this

516-556: A disturbed ionosphere. Space weather events that corrupt GPS signals can significantly impact society. For example, the Wide Area Augmentation System operated by the US Federal Aviation Administration (FAA) is used as a navigation tool for North American commercial aviation. It is disabled by every major space weather event. Outages can range from minutes to days. Major space weather events can push

602-458: A large solar storm has been found for the years 774–775 and 993–994 . Carbon-14 levels stored in 775 suggest an event about 20 times the normal variation of the Sun's activity, and 10 or more times the size of the Carrington Event. An event in 7176 BCE may have exceeded even the 774–775 event based on this proxy data. Whether the physics of solar flares is similar to that of even larger superflares

688-434: A mechanism for the generation of downward propagating atmospheric gravity waves (AGWs). As AGWs reach lower atmosphere , they may excite the conditional instability in the troposphere , thus leading to excessive rainfall. Observation of space weather is done both for scientific research and applications. Scientific observation has evolved with the state of knowledge, while application-related observation expanded with

774-627: A permanent region of luminescence 15 to 25° in latitude from the magnetic poles and 5 to 20° wide. In 1958, the Explorer I satellite discovered the Van Allen belts , regions of radiation particles trapped by the Earth's magnetic field. In January 1959, the Soviet satellite Luna 1 first directly observed the solar wind and measured its strength. A smaller International Heliophysical Year (IHY) occurred in 2007–2008. In 1969, INJUN-5 (or Explorer 40 ) made

860-526: A radio wave by the ionosphere depends on the signal frequency. Radio signals in the VHF band (30 to 300 MHz) can be distorted beyond recognition by a disturbed ionosphere. Radio signals in the UHF band (300 MHz to 3 GHz) transit a disturbed ionosphere, but a receiver may not be able to keep locked to the carrier frequency. GPS uses signals at 1575.42 MHz (L1) and 1227.6 MHz (L2) that can be distorted by

946-466: A result of solar energetic particle events but can be due to terrestrial events such as forest fires, and correlate with other chemical signatures of known forest fire plumes. Nitrate events in cores from Greenland and Antarctica do not align, so the hypothesis that they reflect proton events is now in significant doubt. A 2024 study analysed digitized magnetogram readings from magnetic observatories at Kew and Greenwich . "Initial analysis suggests

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1032-470: A signal can be transmitted around the curvature of the Earth beyond the line of sight. During the 20th century, HF communications was the only method for a ship or aircraft far from land or a base station to communicate. The advent of systems such as Iridium brought other methods of communications, but HF remains critical for vessels that do not carry the newer equipment and as a critical backup system for others. Space weather events can create irregularities in

1118-580: A single wellhead. Accuracy requirements are strict, due to target size – reservoirs may only be a few tens to hundreds of meters across – and safety, because of the proximity of other boreholes. The most accurate gyroscopic method is expensive, since it can stop drilling for hours. An alternative is to use a magnetic survey, which enables measurement while drilling (MWD) . Near real-time magnetic data can be used to correct drilling direction. Magnetic data and space weather forecasts can help to clarify unknown sources of drilling error. The amount of energy entering

1204-496: A space weather component. For example, 46 of the 70 failures reported in 2003 occurred during the October 2003 geomagnetic storm. The two most common adverse space weather effects on spacecraft are radiation damage and spacecraft charging . Radiation (high-energy particles) passes through the skin of the spacecraft and into the electronic components. In most cases, the radiation causes an erroneous signal or changes one bit in memory of

1290-421: A spacecraft's electronics ( single event upsets ). In a few cases, the radiation destroys a section of the electronics ( single-event latchup ). Spacecraft charging is the accumulation of an electrostatic charge on a nonconducting material on the spacecraft's surface by low-energy particles. If enough charge is built up, a discharge (spark) occurs. This can cause an erroneous signal to be detected and acted on by

1376-472: Is a measure of how strongly space weather magnetic fields, such as coronal mass ejections, couple with the Earth's magnetic field. This is determined by the direction of the magnetic field held within the plasma that originates from the Sun. New techniques measuring Faraday rotation in radio waves are in development to measure field direction. A host of research spacecraft have explored space weather. The Orbiting Geophysical Observatory series were among

1462-483: Is a measure of the ionosphere over a given location. TEC is the number of electrons in a column one meter square from the base of the ionosphere (around 90 km altitude) to the top of the ionosphere (around 1000 km altitude). Many TEC measurements are made by monitoring the two frequencies transmitted by GPS spacecraft. Presently, GPS TEC is monitored and distributed in real time from more than 360 stations maintained by agencies in many countries. Geoeffectiveness

1548-557: Is advance warning of coronal mass ejections. Space weather models are simulations of the space weather environment. Models use sets of mathematical equations to describe physical processes. These models take a limited data set and attempt to describe all or part of the space weather environment in or to predict how weather evolves over time. Early models were heuristic; i.e ., they did not directly employ physics. These models take less resources than their more sophisticated descendants. Solar storm of 1859 The Carrington Event

1634-425: Is an estimate of the magnetic field change at the Earth's magnetic equator due to a ring of electric current at and just earthward of the geosynchronous orbit . The index is based on data from four ground-based magnetic observatories between 21° and 33° magnetic latitude during a one-hour period. Stations closer to the magnetic equator are not used due to ionospheric effects. The Dst index is compiled and archived by

1720-623: Is believed that the relatively high speed of this CME was made possible by a prior CME, perhaps the cause of the large aurora event on 29 August that "cleared the way" of ambient solar wind plasma for the Carrington Event. Just before noon on 1 September 1859, the English amateur astronomers Richard Carrington and Richard Hodgson independently recorded the earliest observations of a solar flare. Carrington and Hodgson compiled independent reports which were published side by side in Monthly Notices of

1806-413: Is compiled from geomagnetic disturbances at 12 geomagnetic observatories in and near the auroral zones and is recorded at 1-minute intervals. The public AE index is available with a lag of two to three days that limits its utility for space weather applications. The AE index indicates the intensity of geomagnetic substorms except during a major geomagnetic storm when the auroral zones expand equatorward from

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1892-598: Is diverted. Measurements of the radiation environment at commercial aircraft altitudes above 8 km (26,000 ft) have historically been done by instruments that record the data on board where the data are then processed later on the ground. However, a system of real-time radiation measurements on-board aircraft has been developed through the NASA Automated Radiation Measurements for Aerospace Safety (ARMAS) program. ARMAS has flown hundreds of flights since 2013, mostly on research aircraft, and sent

1978-405: Is still unclear. The Sun may differ in important ways such as size and speed of rotation from the types of stars that are known to produce superflares. Ice cores containing thin nitrate -rich layers have been analysed to reconstruct a history of past solar storms predating reliable observations. This was based on the hypothesis that solar energetic particles would ionize nitrogen, leading to

2064-875: The Dominion Radio Astrophysical Observatory at Penticton, BC, Canada and reported once a day at local noon in solar flux units (10 W·m ·Hz ). F10.7 is archived by the National Geophysical Data Center. Fundamental space weather monitoring data are provided by ground-based magnetometers and magnetic observatories. Magnetic storms were first discovered by ground-based measurement of occasional magnetic disturbance. Ground magnetometer data provide real-time situational awareness for postevent analysis. Magnetic observatories have been in continuous operations for decades to centuries, providing data to inform studies of long-term changes in space climatology. Disturbance storm time index (Dst index)

2150-502: The L 1 Sun-Earth Lagrangian point , 235 Earth radii above the surface (about 1.5 million km, or 924,000 miles) and continuously monitored the solar wind from 1978 to 1982. The next spacecraft to monitor the solar wind at the L 1 point was WIND from 1994 to 1998. After April 1998, the WIND spacecraft orbit was changed to circle the Earth and occasionally pass the L 1 point. The NASA Advanced Composition Explorer has monitored

2236-622: The POES series, the DMSP series, and the Meteosat series. The GOES spacecraft have carried an X-ray sensor (XRS) which measures the flux from the whole solar disk in two bands – 0.05 to 0.4 nm and 0.1 to 0.8 nm – since 1974, an X-ray imager (SXI) since 2004, a magnetometer which measures the distortions of the Earth's magnetic field due to space weather, a whole disk EUV sensor since 2004, and particle sensors (EPS/HEPAD) which measure ions and electrons in

2322-608: The Rocky Mountains in the United States was so bright that the glow woke gold miners, who were reported to have begun to prepare breakfast because they thought it was morning. It was also reported that people in the north-eastern United States could read a newspaper by the aurora's light. The aurora was also visible from the poles to low latitude areas such as south-central Mexico , Cuba , Hawaii , Queensland , southern Japan and China, and even at lower latitudes very close to

2408-711: The STEREO mission. The Yohkoh spacecraft at LEO observed the Sun from 1991 to 2001 in the X-ray portion of the solar spectrum and was useful for both research and space weather prediction. Data from Yohkoh inspired the Solar X-ray Imager on GOES. Spacecraft with instruments whose primary purpose is to provide data for space weather predictions and applications include the Geostationary Operational Environmental Satellite (GOES) series of spacecraft,

2494-509: The interplanetary magnetic field carried by the solar wind plasma . A variety of physical phenomena is associated with space weather, including geomagnetic storms and substorms , energization of the Van Allen radiation belts , ionospheric disturbances and scintillation of satellite-to-ground radio signals and long-range radar signals, aurorae , and geomagnetically induced currents at Earth's surface. Coronal mass ejections are also important drivers of space weather, as they can compress

2580-467: The solar wind , especially on the Earth's magnetosphere , ionosphere , thermosphere , and exosphere . Though physically distinct, space weather is analogous to the terrestrial weather of Earth's atmosphere ( troposphere and stratosphere ). The term "space weather" was first used in the 1950s and popularized in the 1990s. Later, it prompted research into " space climate ", the large-scale and long-term patterns of space weather. For many centuries,

2666-511: The 1990s along with the belief that space's impact on human systems demanded a more coordinated research and application framework. The purpose of the US National Space Weather Program is to focus research on the needs of the affected commercial and military communities, to connect the research and user communities, to create coordination between operational data centers, and to better define user community needs. NOAA operates

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2752-483: The 20th century, the interest in space weather expanded as military and commercial systems came to depend on systems affected by space weather. Communications satellites are a vital part of global commerce. Weather satellite systems provide information about terrestrial weather. The signals from satellites of a global positioning system (GPS) are used in a wide variety of applications. Space weather phenomena can interfere with or damage these satellites or interfere with

2838-519: The American telegraph line between Boston, Massachusetts , and Portland, Maine , on the night of 2 September 1859 and reported in the Boston Evening Traveler : Boston operator (to Portland operator): "Please cut off your battery [power source] entirely for fifteen minutes." Portland operator: "Will do so. It is now disconnected." Boston: "Mine is disconnected, and we are working with

2924-555: The Earth in its orbit. Together they compile information about the solar surface and atmosphere in three dimensions. The Van Allen probes record detailed information about the radiation belts, geomagnetic storms, and the relationship between the two. Some spacecraft with other primary missions have carried auxiliary instruments for solar observation. Among the earliest such spacecraft were the Applications Technology Satellite (ATS) series at GEO that were precursors to

3010-403: The Earth. Kristian Birkeland explained the physics of aurorae by creating artificial ones in his laboratory, and predicted the solar wind. The introduction of radio revealed that solar weather could cause extreme static or noise. Radar jamming during a large solar event in 1942 led to the discovery of solar radio bursts, radio waves over a broad frequency range created by a solar flare. In

3096-525: The National Weather Service's Space Weather Prediction Center . The concept was turned into an action plan in 2000, an implementation plan in 2002, an assessment in 2006 and a revised strategic plan in 2010. A revised action plan was scheduled to be released in 2011 followed by a revised implementation plan in 2012. Within the Solar System , space weather is influenced by the solar wind and

3182-690: The Radio Interference Monitoring Sets (RIMS) and the Solar Radio Spectrograph (SRS). The RIMS system consists of three dishes observing at eight different frequencies, while the SRS system consists of two antennas observing two different frequency bands. The site previously included a 150-foot fully steerable antenna, which was installed in 1963 and moved to Millstone Hill in Westford, Massachusetts in 1978. In 1967, this parabolic dish

3268-672: The Royal Astronomical Society and exhibited their drawings of the event at the November 1859 meeting of the Royal Astronomical Society . Because of a geomagnetic solar flare effect (a "magnetic crochet") observed in the Kew Observatory magnetometer record by Scottish physicist Balfour Stewart , and a geomagnetic storm observed the following day, Carrington suspected a solar–terrestrial connection. However, he

3354-596: The World Data Center for Geomagnetism, Kyoto. Kp/ap index: 'a' is an index created from the geomagnetic disturbance at one midlatitude (40° to 50° latitude) geomagnetic observatory during a 3-hour period. 'K' is the quasilogarithmic counterpart of the 'a' index. Kp and ap are the average of K and an over 13 geomagnetic observatories to represent planetary-wide geomagnetic disturbances. The Kp/ap index indicates both geomagnetic storms and substorms (auroral disturbance). Kp/ap data are available from 1932 onward. AE index

3440-466: The ability to exploit such data. Space weather is monitored at ground level by observing changes in the Earth's magnetic field over periods of seconds to days, by observing the surface of the Sun, and by observing radio noise created in the Sun's atmosphere. The Sunspot Number (SSN) is the number of sunspots on the Sun's photosphere in visible light on the side of the Sun visible to an Earth observer. The number and total area of sunspots are related to

3526-415: The atmosphere and create measurable radiation. All aircraft flying above 8 km (26,200 feet) altitude are exposed to these particles. The dose exposure is greater in polar regions than at midlatitude and equatorial regions. Many commercial aircraft fly over the polar region. When a space weather event causes radiation exposure to exceed the safe level set by aviation authorities, the aircraft's flight path

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3612-444: The atmosphere, atomic interactions occur that cause a shower of lower-energy particles to descend into the atmosphere and to ground level. The presence of cosmic rays in the near-Earth space environment can be detected by monitoring high-energy neutrons at ground level. Small fluxes of cosmic rays are present continuously. Large fluxes are produced by the Sun during events related to energetic solar flares. Total Electron Content (TEC)

3698-545: The auroral current. How do you receive my writing?" Portland: "Better than with our batteries on. – Current comes and goes gradually." Boston: "My current is very strong at times, and we can work better without the batteries, as the aurora seems to neutralize and augment our batteries alternately, making current too strong at times for our relay magnets. Suppose we work without batteries while we are affected by this trouble." Portland: "Very well. Shall I go ahead with business?" Boston: "Yes. Go ahead." The conversation

3784-526: The brightness of the Sun in the EUV and X-ray portions of the solar spectrum and to solar activity such as solar flares and coronal mass ejections. The 10.7 cm radio flux (F10.7) is a measurement of RF emissions from the Sun and is roughly correlated with the solar EUV flux. Since this RF emission is easily obtained from the ground and EUV flux is not, this value has been measured and disseminated continuously since 1947. The world standard measurements are made by

3870-418: The capability to maneuver out of the path of Cosmos 2251 and could have evaded the crash, if a credible collision prediction had been available. The exposure of a human body to ionizing radiation has the same harmful effects whether the source of the radiation is a medical X-ray machine , a nuclear power plant , or radiation in space. The degree of the harmful effect depends on the length of exposure and

3956-428: The cost of a similar event in the present to the US alone at US$ 600 billion to $ 2.6 trillion (equivalent to $ 774 billion to $ 3.35 trillion in 2023 ), which, at the time, equated to roughly 3.6 to 15.5 percent of annual GDP. Other research has looked for signatures of large solar flares and CMEs in carbon-14 in tree rings and beryllium-10 (among other isotopes) in ice cores. The signature of

4042-744: The data to the ground through Iridium satellite links. The eventual goal of these types of measurements is to data assimilate them into physics-based global radiation models, e.g., NASA's Nowcast of Atmospheric Ionizing Radiation System ( NAIRAS ), so as to provide the weather of the radiation environment rather than the climatology. Magnetic storm activity can induce geoelectric fields in the Earth's conducting lithosphere . Corresponding voltage differentials can find their way into electric power grids through ground connections , driving uncontrolled electric currents that interfere with grid operation, damage transformers, trip protective relays, and sometimes cause blackouts. This complicated chain of causes and effects

4128-444: The disturbed polar ionosphere 10° to 30° of latitude toward the equator and can cause large ionospheric gradients (changes in density over distance of hundreds of km) at mid and low latitude. Both of these factors can distort GPS signals. Radio waves in the HF band (3 to 30 MHz) (also known as the shortwave band) are reflected by the ionosphere. Since the ground also reflects HF waves,

4214-595: The divine immanence, immutable law, cause, and effect. The superstitious and the fanatical had dire forebodings, and thought it a foreshadowing of Armageddon and final dissolution. Because of the geomagnetically induced current from the electromagnetic field , telegraph systems all over Europe and North America failed, in some cases giving their operators electric shocks . Telegraph pylons threw sparks. Some operators were able to continue to send and receive messages despite having disconnected their power supplies. The following conversation occurred between two operators of

4300-409: The effect of high-energy charged particles on atmosphere. If proven, this may suggest a link between space weather (in the form of solar particle events ) and cloud formation. Most recently, a statistical connection has been reported between the occurrence of heavy floods and the arrivals of high-speed solar wind streams (HSSs). The enhanced auroral energy deposition during HSSs is suggested as

4386-589: The effects of space weather were noticed, but not understood. Displays of auroral light have long been observed at high latitudes. In 1724, George Graham reported that the needle of a magnetic compass was regularly deflected from magnetic north over the course of each day. This effect was eventually attributed to overhead electric currents flowing in the ionosphere and magnetosphere by Balfour Stewart in 1882, and confirmed by Arthur Schuster in 1889 from analysis of magnetic observatory data. In 1852, astronomer and British Major General Edward Sabine showed that

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4472-621: The energy range of 50 keV to 500 MeV. Starting sometime after 2015, the GOES-R generation of GOES spacecraft will replace the SXI with a solar EUV image (SUVI) similar to the one on SOHO and STEREO and the particle sensor will be augmented with a component to extend the energy range down to 30 eV. The Deep Space Climate Observatory (DSCOVR) satellite is a NOAA Earth observation and space weather satellite that launched in February 2015. Among its features

4558-419: The entire flight. Diverting such a flight is estimated to cost about $ 100,000. The magnetosphere guides cosmic ray and solar energetic particles to polar latitudes, while high-energy charged particles enter the mesosphere, stratosphere, and troposphere. These energetic particles at the top of the atmosphere shatter atmospheric atoms and molecules, creating harmful lower-energy particles that penetrate deep into

4644-510: The equator, such as in Colombia . On Saturday 3 September 1859, the Baltimore American and Commercial Advertiser reported that Those who happened to be out late on Thursday night had an opportunity of witnessing another magnificent display of the auroral lights. The phenomenon was very similar to the display on Sunday night, though at times the light was, if possible, more brilliant, and

4730-427: The first direct observation of the electric field impressed on the Earth's high-latitude ionosphere by the solar wind. In the early 1970s, Triad data demonstrated that permanent electric currents flowed between the auroral oval and the magnetosphere. The term "space weather" came into usage in the late 1950s as the space age began and satellites began to measure the space environment . The term regained popularity in

4816-451: The first of these was the IMP-8 (Interplanetary Monitoring Platform). It orbited the Earth at 35 Earth radii and observed the solar wind for two-thirds of its 12-day orbits from 1973 to 2006. Since the solar wind carries disturbances that affect the magnetosphere and ionosphere, IMP-8 demonstrated the utility of continuous solar wind monitoring. IMP-8 was followed by ISEE-3 , which was placed near

4902-558: The first spacecraft with the mission of analyzing the space environment. Recent spacecraft include the NASA-ESA Solar-Terrestrial Relations Observatory (STEREO) pair of spacecraft launched in 2006 into solar orbit and the Van Allen Probes , launched in 2012 into a highly elliptical Earth orbit. The two STEREO spacecraft drift away from the Earth by about 22° per year, one leading and the other trailing

4988-593: The ionosphere that scatter HF signals instead of reflecting them, preventing HF communications. At auroral and polar latitudes, small space weather events that occur frequently disrupt HF communications. At mid-latitudes, HF communications are disrupted by solar radio bursts, by X-rays from solar flares (which enhance and disturb the ionospheric D-layer) and by TEC enhancements and irregularities during major geomagnetic storms. Trans polar airline routes are particularly sensitive to space weather, in part because Federal Aviation Regulations require reliable communication over

5074-449: The largest geomagnetic storms (as recorded by ground-based magnetometers ) occurred. Estimates of the storm strength ( Dst ) range from −0.80 to −1.75  μT . The geomagnetic storm is thought to have been caused by a big coronal mass ejection (CME) that traveled directly toward Earth, taking 17.6 hours to make the 150 × 10 ^  km (93 × 10 ^  mi) journey. Typical CMEs take several days to arrive at Earth, but it

5160-525: The magnetosphere and trigger geomagnetic storms. Solar energetic particles (SEP) accelerated by coronal mass ejections or solar flares can trigger solar particle events , a critical driver of human impact space weather, as they can damage electronics onboard spacecraft (e.g. Galaxy 15 failure), and threaten the lives of astronauts , as well as increase radiation hazards to high-altitude, high-latitude aviation. Some spacecraft failures can be directly attributed to space weather; many more are thought to have

5246-403: The modern Geostationary Operational Environmental Satellite (GOES) weather satellite and many communication satellites. The ATS spacecraft carried environmental particle sensors as auxiliary payloads and had their navigational magnetic field sensor used for sensing the environment. Many of the early instruments were research spacecraft that were re-purposed for space weather applications. One of

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5332-485: The observatories. Radio noise bursts are reported by the Radio Solar Telescope Network to the U.S. Air Force and to NOAA. The radio bursts are associated with solar flare plasma that interacts with the ambient solar atmosphere. The Sun's photosphere is observed continuously for activity that can be the precursors to solar flares and CMEs. The Global Oscillation Network Group (GONG) project monitors both

5418-527: The observatory to the Air Force in October 1978. The observatory is now officially Detachment 2, 2nd Weather Squadron of the 2nd Weather Group of the 557th Weather Wing . The 2nd Weather Squadron currently operates other RSTN observatories at Kaena Point , Hawaii; San Vito dei Normanni , Italy; and Learmonth , Western Australia . Instruments currently located at the Sagamore Hill RSTN site include

5504-474: The orbit. A geomagnetic storm can cause an orbit change over a few days that otherwise would occur over a year or more. The geomagnetic storm adds heat to the thermosphere, causing the thermosphere to expand and rise, increasing the drag on spacecraft. The 2009 satellite collision between the Iridium 33 and Cosmos 2251 demonstrated the importance of having precise knowledge of all objects in orbit. Iridium 33 had

5590-408: The prismatic hues more varied and gorgeous. The light appeared to cover the whole firmament, apparently like a luminous cloud, through which the stars of the larger magnitude indistinctly shone. The light was greater than that of the moon at its full, but had an indescribable softness and delicacy that seemed to envelop everything upon which it rested. Between 12 and 1 o'clock, when the display

5676-460: The probability of the occurrence of geomagnetic storms on Earth was correlated with the number of sunspots , demonstrating a novel solar-terrestrial interaction. The solar storm of 1859 caused brilliant auroral displays and disrupted global telegraph operations. Richard Carrington correctly connected the storm with a solar flare that he had observed the day before near a large sunspot group, demonstrating that specific solar events could affect

5762-458: The production of nitric oxide and other oxidised nitrogen compounds, which would not be too diluted in the atmosphere before being deposited along with snow. Beginning in 1986, some researchers claimed that data from Greenland ice cores showed evidence of individual solar particle events , including the Carrington Event. More recent ice core work, however, casts significant doubt on this interpretation and shows that nitrate spikes are likely not

5848-623: The radiation's energy density . The ever-present radiation belts extend down to the altitude of crewed spacecraft such as the International Space Station (ISS) and the Space Shuttle , but the amount of exposure is within the acceptable lifetime exposure limit under normal conditions. During a major space weather event that includes an SEP burst, the flux can increase by orders of magnitude. Areas within ISS provide shielding that can keep

5934-404: The radio signals with which they operate. Space weather phenomena can cause damaging surges in long-distance transmission lines and expose passengers and crew of aircraft travel to radiation , especially on polar routes. The International Geophysical Year increased research into space weather. Ground-based data obtained during IGY demonstrated that the aurorae occurred in an auroral oval ,

6020-466: The solar wind at the L 1 point from 1997 to present. In addition to monitoring the solar wind, monitoring the Sun is important to space weather. Because the solar EUV cannot be monitored from the ground, the joint NASA - ESA Solar and Heliospheric Observatory (SOHO) spacecraft was launched and has provided solar EUV images beginning in 1995. SOHO is a main source of near-real time solar data for both research and space weather prediction and inspired

6106-414: The space weather-related magnetic field changes are similar in magnitude to those of the subsurface crustal magnetic field in the survey area. Accurate geomagnetic storm warnings, including an assessment of storm magnitude and duration, allows for an economic use of survey equipment. For economic and other reasons, oil and gas production often involves horizontal drilling of well paths many kilometers from

6192-429: The spacecraft computer. A recent study indicated that spacecraft charging is the predominant space weather effect on spacecraft in geosynchronous orbit . The orbits of spacecraft in low Earth orbit (LEO) decay to lower and lower altitudes due to the resistance from the friction between the spacecraft's surface ( i.e. , drag) and the outer layer of the Earth's atmosphere (or the thermosphere and exosphere). Eventually,

6278-499: The surface and the interior of the Sun by using helioseismology , the study of sound waves propagating through the Sun and observed as ripples on the solar surface. GONG can detect sunspot groups on the far side of the Sun. This ability has recently been verified by visual observations from the STEREO spacecraft. Neutron monitors on the ground indirectly monitor cosmic rays from the Sun and galactic sources. When cosmic rays interact with

6364-464: The tent saw a great reflection in the southern heavens at about 7 o'clock p.m., and in about half an hour, a scene of almost unspeakable beauty presented itself: Lights of every imaginable color were issuing from the southern heavens, one color fading away only to give place to another if possible more beautiful than the last, the streams mounting to the zenith, but always becoming a rich purple when reaching there, and always curling round, leaving

6450-408: The total dose within safe limits. For the Space Shuttle , such an event would have required immediate mission termination. The ionosphere bends radio waves in the same manner that water in a pool bends visible light. When the medium through which such waves travel is disturbed, the light image or radio information is distorted and can become unrecognizable. The degree of distortion (scintillation) of

6536-489: The troposphere and stratosphere from space weather phenomena is trivial compared to the solar insolation in the visible and infrared portions of the solar electromagnetic spectrum. Although some linkage between the 11-year sunspot cycle and the Earth's climate has been claimed., this has never been verified. For example, the Maunder minimum , a 70-year period almost devoid of sunspots, has often been suggested to be correlated to

6622-444: Was associated with a very bright solar flare on 1 September 1859. It was observed and recorded independently by British astronomers Richard Carrington and Richard Hodgson —the first records of a solar flare. A geomagnetic storm of this magnitude occurring today has the potential to cause widespread electrical disruptions, blackouts and damage due to extended cuts of the electrical power grid . On 1 and 2 September 1859, one of

6708-506: Was at its full brilliancy, the quiet streets of the city resting under this strange light, presented a beautiful as well as singular appearance. In 1909, an Australian gold miner named C. F. Herbert retold his observations in a letter to the Daily News in Perth , I was gold-digging at Rokewood, about four miles [6 km] from Rokewood township (Victoria) . Myself and two mates looking out of

6794-422: Was carried on for around two hours using no battery power at all and working solely with the current induced by the aurora, the first time on record that more than a word or two was transmitted in such manner. Another strong solar storm occurred in February 1872. Less severe storms also occurred in 1921 (this was comparable by some measures), 1938 , 1941, 1958, 1959 and 1960, when widespread radio disruption

6880-687: Was demonstrated during the magnetic storm of March 1989 , which caused the complete collapse of the Hydro-Québec electric-power grid in Canada, temporarily leaving nine million people without electricity. The possible occurrence of an even more intense storm led to operational standards intended to mitigate induction-hazard risks, while reinsurance companies commissioned revised risk assessments . Air- and ship-borne magnetic surveys can be affected by rapid magnetic field variations during geomagnetic storms. Such storms cause data-interpretation problems because

6966-440: Was not possible. As such, a linkage between space weather and the climate has not been demonstrated. In addition, a link has been suggested between high energy charged particles (such as SEPs and cosmic rays ) and cloud formation . This is because charged particles interact with the atmosphere to produce volatiles which then condense, creating cloud seeds . This is a topic of ongoing research at CERN , where experiments test

7052-405: Was not sure whether the two phenomena were related, writing that "one swallow does not make a summer". Worldwide reports of the effects of the geomagnetic storm of 1859 were compiled and published by American mathematician Elias Loomis , which support the observations of Carrington and Stewart. Auroras were seen around the world in the northern and southern hemispheres. The aurora borealis over

7138-518: Was reported. The flares and CMEs of the August 1972 solar storms were similar to the Carrington event in size and magnitude; however, unlike the 1859 storms, they did not cause an extreme geomagnetic storm. The March 1989 geomagnetic storm knocked out power across large sections of Quebec , while the 2003 Halloween solar storms registered the most powerful solar explosions ever recorded. On 23 July 2012 ,

7224-451: Was the most intense geomagnetic storm in recorded history, peaking on 1–2 September 1859 during solar cycle 10 . It created strong auroral displays that were reported globally and caused sparking and even fires in telegraph stations. The geomagnetic storm was most likely the result of a coronal mass ejection (CME) from the Sun colliding with Earth's magnetosphere . The geomagnetic storm

7310-446: Was thus assigned the task of developing and validating a network of ground-based solar observatories. AFRL established a worldwide network of sweep frequency recorders from which estimates of the shock speed in the corona could be made. The prototype was assembled and operated at Sagamore Hill during the early 1960s. The observatory began operating solar patrols in 1966. The Air Force Geophysics Laboratory (AFGL) transferred operation of

7396-505: Was used to receive data from the solar research satellite OV1-5 , and to conduct ionospheric research by receiving transmissions from the Intelsat 1 and ATS-1 satellites. Space weather Space weather is a branch of space physics and aeronomy , or heliophysics , concerned with the varying conditions within the Solar System and its heliosphere . This includes the effects of

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