CHAPTER 1

Introduction

As the world moves into the 21st century, our civilization is relying more and more on technology that is affected in some way by conditions in the space environment. To prepare to deal with the vulnerabilities of our technology, several U. S. government agencies have developed a program called the National Space Weather Program (NSWP) and documented the goals of that program in the National Space Weather Program Strategic Plan (FCM-P30-1995, Office of the Federal Coordinator For Meteorological Services and Supporting Research, Silver Spring, Md., 1995). "Space weather" refers to conditions on the Sun and in the solar wind, magnetosphere, ionosphere, and thermosphere that can influence the performance and reliability of space-borne and ground-based technological systems and can endanger human life or health. This document presents the Implementation Plan for the NSWP. It is the culmination of months of multiagency coordination and cooperation, and represents a dedicated effort by Federal agencies to improve capabilities in an area that has critical societal impacts.

1.1 Scope of the Program

The NSWP encompasses all activities necessary for the timely specification and forecast of natural conditions in the space environment that may have an impact on technical systems. The domain of primary interest to the program consists of Sun and solar wind, the magnetosphere, the ionosphere, and the thermosphere. Because of the vastness and complexity of the region of interest, all traditional areas of space sciences can contribute to achieving the program goals.

Space weather begins at the Sun's surface, the source of radiative and particle energy impacting Earth. Solar activity changes the radiative and particle output of the Sun, producing corresponding changes in the near-Earth space environment, as well as at Earth's surface. The most dramatic events on the Sun, insofar as space weather effects are concerned, are solar flares and coronal mass ejections. Although longer term variations in solar emissions do not produce dramatic space weather effects, they are important in helping us understand the underlying processes behind the short-term variations.

Changes in the radiative output from the Sun directly affect the state of the upper atmosphere and ionosphere through the excitation and ionization of atoms and molecules. Particle emissions from the Sun include both the energetic particles and the low-energy plasma that constitute the solar wind. Both particles and electromagnetic fields evolve as they flow outward from the Sun, especially as they create or interact with interplanetary shocks.

The solar wind moves outward from the Sun and impinges on Earth. The plasma and magnetic field of the solar wind interact with Earth's atmosphere and geomagnetic field, creating a tear-drop-shaped region called the magnetosphere. The surface of this region is referred to as the magnetopause. The magnetopause is usually found near 10 Earth radii (RE) in the sunward direction, although this distance is highly variable (roughly between 5 and 15 RE) in response to solar wind dynamic pressure. In the antisunward direction, the magnetopause extends to distances beyond the orbit of the moon. The magnetopause represents a barrier that prevents all but a fraction of the energy carried by the solar wind from entering the magnetosphere. Under normal conditions, the energy that does penetrate the magnetopause is stored in the form of the particles and fields of the magnetosphere, but under some conditions it is impulsively released into Earth's atmosphere. This impulsive release of energy is referred to as a magnetospheric substorm. It is characterized by the appearance of bright, dynamic aurora and the development of intense ionospheric currents. During a substorm the magnetic field in the magnetosphere suddenly assumes a new configuration; after the substorm there is a recovery period that takes many hours.

Substorms are a relatively short-lived response of the magnetosphere to solar wind stimulus. Geomagnetic storms are a sustained, long-lived (days to weeks) response to a prolonged period of solar wind flow characterized by a strong southward interplanetary magnetic field. Geomagnetic storms lead to a substantial energization of the ring current, a belt of quasi-trapped electrons, protons, and heavier ions, and significant geomagnetic fluctuations at low geographic latitudes. Magnetospheric particles precipitate into the polar caps, heating the neutral atmosphere (thermosphere and mesosphere) and launching ionospheric disturbances. Substorms may also occur during the course of geomagnetic storms. Once the solar wind returns to its undisturbed state, the magnetosphere and ionosphere require hours to days to recover.

Because Earth's magnetic field permeates the magnetosphere, most magnetospheric processes are manifested in some way by changes in the properties of the ionosphere and thermosphere. Magnetospheric processes produce electrical currents, auroral emissions, frictional heating, ionization, and scintillation. All these phenomena are elements of near-Earth space weather. The near-Earth space environment is also influenced by processes originating at lower altitudes, such as gravity waves, and direct energy deposition from solar radiation and cosmic rays. Space weather effects also include the electrical currents induced within Earth's surface as a result of changes in ionospheric currents.

This brief description of the space weather system demonstrates the vastness of the region of interest to the NSWP and the complexity of the physical processes that must be understood. Adding to this complexity is the high degree of coupling between the various regions. The program will emphasize the importance of dealing with the space environment as a seamless system in which processes occurring in one location cannot be understood without adequate knowledge of the way the entire system is linked.

The NSWP is primarily concerned with naturally occurring phenomena in the space environment. Thus, the program does not specifically address the possible impact of orbital debris on satellite systems. However, the program will contribute to the accurate tracking of objects in space by improving the specification and prediction of variations in atmospheric density, which affect the drag on orbiting objects.

Similarly, the NSWP does not deal directly with the engineering aspects that enter into the design and development of technical systems. Here again, the program can be of benefit to the community by providing detailed information about the space environment so that engineers can better design these systems. Often accurate specification of the range in environmental parameters to which a piece of equipment will be subjected can result in significant cost savings.

The goal of the NSWP is to provide products to a community of customers that is continually changing. Each of these customers may have different requirements, making it a formidable task to provide customized products. The routine production of information tailored to meet specific customer requirements is not within the scope of the NSWP. The specification and forecast information provided by the forecast centers will be sufficient to allow such tailored products to be developed either by the customers themselves or by others offering to provide these services. In particular, the need for these services provides opportunities for small businesses or other profit-making enterprises. In the case of Department of Defense (DoD) customers, it is expected that DoD will take responsibility for its own tailored products. Agency representatives and customers involved in the NSWP will routinely evaluate the status of NSWP products and agree upon the level of information falling within the scope of the program.

1.2 Relevance to the Nation

Space weather is working its way into the national consciousness as we see an increasing number of problems with parts of our technological infrastructure, such as satellite failures and widespread electric power brownouts and blackouts. As our society grows more dependent on advanced technology systems, we become increasingly more vulnerable to malfunctions in those systems.

For example, long-line power networks connecting widely separated geographic areas have increased the probability of power grids absorbing damaging electric currents induced by geomagnetic storms; the miniaturization of electronic components on satellites makes them potentially more susceptible to damage by high-energy particles; aircraft designed to fly at 60,000 feet (18.3 kilometers) have increased human risk to radiation exposure during severe space weather. Figure 1-1 lists sample significant space weather events and their impacts over the past several years.

System and human vulnerabilities to space weather effects include the following:

Engineering Aspects. Engineers use space environment information to specify the extent and types of protective measures that are to be designed into a system and to develop operating plans that minimize space weather effects. However, engineering solutions to some problems may be very costly or impossible to implement. After the fact, engineers use space environment information to determine the source of failures and develop

March 24, 1940. A "great" geomagnetic storm rendered inoperative 80% of all long-distance telephone connections out of Minneapolis, Minnesota. Electric service was temporarily disrupted in portions of New England, New York, Pennsylvania, Minnesota, Quebec, and Ontario.

February 9-10, 1958. A geomagnetic storm caused severe interruptions on Western Union's North Atlantic telegraph cables and made voice communications very difficult on the Bell System transatlantic cable from Newfoundland to Scotland. Toronto, Canada, experienced a temporary blackout.

August 4, 1972. A severe geomagnetic storm caused a 30-minute shutdown of the Bell System coaxial cable link between Plano, Illinois, and Cascade, Iowa. A power transformer failed at the British Columbia Hydro and Power Authority.

November 26, 1982. The Geostationary Operational Environmental Satellite (GOES) 4 visible and infrared spin-scan radiometer, which maps cloud cover, failed 45 minutes after the arrival of high-energy protons from a major solar flare. The untimely failure occurred as a series of intense storms hit the California coast.

March 13-14, 1989. A severe geomagnetic storm caused a system-wide power failure in Quebec, Canada, resulting in the loss of over 20,000 megawatts. The blackout cut electric power to several million people. Time from onset of problems to system collapse was about 90 seconds. High frequency (HF) radio frequencies were virtually unusable worldwide, while very high frequency (VHF) transmissions traveled unusually long distances and created interference problems. A Japanese communications satellite lost half of its dual-redundant command circuitry. A National Aeronautics and Space Administration (NASA) satellite dropped 3 miles (4.8 kilometers) in its orbit due to the increase in atmospheric drag.

April 29, 1991. A transformer at the Maine Yankee Nuclear Plant catastrophically failed within a few hours of a severe geomagnetic storm onset.

January 20-21, 1994. Two Canadian communications satellites failed, interrupting telephone, television, and radio service for several hours. The failures occurred after an extended period of high electron levels in the satellite environment.

Figure 1-1. Impacts of Significant Space Weather Events

corrective actions. Significant economic and societal benefits can be realized if designers of emerging technology can (1) anticipate the properties of the space environment to which the hardware will be subjected, (2) depend on accurate and timely predictions of space weather, and (3) take advantage of post-event analysis to determine the source of system anomalies and failures and to build a database for future planning.

Satellite Systems. Space weather affects satellite missions in a variety of ways, depending on the orbit and satellite function. Our society depends on satellites for weather information, commercial television, communications, navigation, exploration, search and rescue, research, and national defense. The impact of satellite system failures is more far-reaching than ever before, and the trend will almost certainly continue at an increasing rate.

Energetic particles that originate from the Sun, from interplanetary space, and from Earth's magnetosphere continually impact the surfaces of spacecraft. Highly energetic particles penetrate electronic components, causing changes in electronic signals that can result in spurious commands within the spacecraft or erroneous data from an instrument. These spurious commands have caused major satellite system failures that might have been avoided if ground controllers had had advance notice of impending particle hazards. Less energetic particles contribute to a variety of spacecraft surface charging problems, especially during periods of high geomagnetic activity. In addition, energetic electrons responsible for deep dielectric charging can degrade the useful lifetime of internal components. Overall radiation dose can ultimately determine satellite lifetime.

Highly variable solar ultraviolet radiation continuously modifies terrestrial atmospheric density and temperature, affecting spacecraft orbits and lifetimes. Major geomagnetic storms result in heating and expansion of the atmosphere, causing significant perturbations in low-altitude satellite trajectories. At times, these effects may be severe enough to cause premature re-entry of orbiting objects, such as Skylab in 1979. It is important that satellite controllers be warned of these changes and that accurate models are in place to realistically predict the resulting atmospheric effects. The Space Shuttle is also vulnerable to changes in atmospheric drag; re-entry calculations for the orbiter are highly sensitive to atmospheric density, and errors can threaten the safety of the vehicle and its crew.

Power Systems. Modern power grids are extremely complex and widespread. The long power lines that traverse the Nation are susceptible to electric currents induced by the dramatic changes in high-altitude ionospheric currents that occur during geomagnetic storms. "Surges" in power lines from induced currents can cause massive network failures and permanent damage to multimillion-dollar equipment in power generation plants. Considering the significant national dependence on reliable electrical power, the resulting social chaos, economic impact, and threat to safety during widespread power outages are far more serious than the simple cost of repairing the systems.

The electric power distribution system has developed an increased susceptibility to the phenomenon of geomagnetically induced currents because of widespread grid interconnections, complex electronic controls and technologies, and large interarea power transfers. The phenomenon occurs globally and simultaneously, and industry operations allow for little redundancy or operating margin to absorb the effects. Mitigation of such effects is fairly straightforward provided advance notice is given of an impending storm; specific strategies currently exist within the power industry. Advanced warnings of storms are needed, but of equal economic importance to industry is that the forecasts be reliable. Forecasts that incorrectly "cry wolf," known as false alarms because the storm never actually occurs, are counterproductive and must be minimized.

Navigation Systems. The accuracy of maritime navigation systems using very low frequency signals, such as Long-Range Navigation (LORAN) and OMEGA (not a acronym), depends on knowing accurately the altitude of the bottom of the ionosphere. Rapid vertical changes in this boundary during solar flares and geomagnetic storms can introduce errors of several kilometers in location determinations.

The Global Positioning System (GPS) operates by transmitting radio waves from satellites to receivers on the ground, aircraft, or other satellites. These radiowave signals are used to calculate location very accurately. However, significant errors in positioning can result when the signals are refracted and slowed by ionospheric conditions. In addition, receivers can experience loss of GPS signal lock when the signal traverses an ionospheric disturbance (scintillation). Future high-resolution applications of GPS technology will require better space weather support to compensate for these induced errors. Accurate specification and prediction of the properties of the ionosphere will aid in the design and operation of emerging systems.

Communications. Radiowave communications over a broad range of frequencies are affected by space weather. HF radio wave communication is more routinely affected because this frequency depends on reflection from the ionosphere to carry signals great distances. Ionospheric irregularities contribute to signal fading; highly disturbed conditions, usually near the aurora and across the polar cap, can absorb the signal completely and make HF propagation impossible. Accurate forecasts of these effects can give operators more time to find an alternative means of communication. Telecommunication companies increasingly depend on higher frequency radio waves, such as ultrahigh frequency (UHF), which penetrate the ionosphere and are relayed via satellite to other locations. Signal properties can be changed by ionospheric conditions so that they can no longer be accurately received at Earth's surface. This may cause degradation of signals, but more important, can prohibit critical communications, such as those used in search and rescue efforts and military operations.

Manned Space Flight. Besides being a threat to satellite systems, energetic particles present a hazard to astronauts on space missions. On Earth we are protected from these particles by the geomagnetic shielding and the atmosphere. The geomagnetic field shields Earth's atmosphere from all particles of MeV energy except in the polar regions. The atmosphere absorbs all but the most energetic cosmic ray particles. During space missions, astronauts performing extra-vehicular activities are relatively unprotected at high latitudes in the spacecraft orbit. This could be particularly problematic during the upcoming construction of the space station during solar maximum. The fluxes of energetic particles can increase hundreds of times following an intense solar flare or to dangerous levels during a large geomagnetic storm. Timely warnings are essential to give astronauts sufficient time to return to their spacecraft prior to the arrival of such energetic particles. High altitude aircraft crews and passengers on polar routes, e.g., on Supersonic Transports (SSTs) or U-2s, are also susceptible to radiation hazards during similar events.

1.3 Summary of the Strategic Plan

Recognizing the need for a more coordinated effort to improve present capabilities in specifying and forecasting conditions in the space environment, Federal agencies representing the research, operations, and user communities initiated the NSWP, as outlined in The National Space Weather Program Strategic Plan. The overarching goal of the program is to achieve an active, synergistic, interagency system to provide timely, accurate, and reliable space weather warnings, observations, specifications, and forecasts within the next 10 years. By building on existing capabilities and establishing an aggressive, coordinated process to set national priorities, focus agency efforts, and leverage resources, the NSWP provides the path to attain this goal. The activities that the NSWP will conduct are listed in Figure 1-2 and the specific goals of the program are enumerated in Figure 1-3.

National Space Weather Program Activities

· Assess and document the impacts of space weather

· Identify customer needs

· Set priorities

· Determine agency roles

· Coordinate interagency efforts and resources

· Ensure exchange of information and plans

· Encourage and focus research

· Facilitate transition of research results into operations

· Foster education of customers and the public

Figure 1-2. National Space Weather Program Activities

The key elements of the NSWP are described as follows:

Forecast and Specification Services. The predominant driver of the program is the value of space weather forecasting services to the Nation. The accuracy, reliability, and timeliness of space weather specification and forecasting must become comparable to that of conventional weather forecasting. Early warning capabilities of impending dangerous conditions must become equally reliable to be valuable for mitigation purposes. The strengthening of services includes modernization of facilities; implementation of new models and other analysis and forecast techniques; improved education and training; improved production, design, and dissemination of forecast products; and improved communication with the users of the services. Proposed operational models, instrumentation, and techniques will be evaluated according to their potential to improve forecasting services.

The National Space Weather Program Goals

To advance

· observing capabilities

· fundamental understanding of processes

· numerical modeling

· data processing and analysis

· transition of research into operational techniques and algorithms

· forecasting accuracy and reliability

· space weather products and services

· education on space weather


To prevent or mitigate

· under- or over-design of technical systems

· regional blackouts of power utilities

· early demise of multimillion-dollar satellites

· disruption of communications by satellite, HF, and VHF radio

· disruption of long-line telecommunications

· errors in navigation systems

· excessive radiation doses, dangerous to human health

Figure 1-3. National Space Weather Program Goals

Research. This will include intensive efforts in understanding the fundamental physical processes that affect the state of the Sun, solar wind, magnetosphere, ionosphere, and atmosphere, with a focus on answering research questions that impede progress in improving forecasting capability. Radiative, dynamical, electrical, and chemical coupling between different regions will be studied using data from existing ground- and space-based instrumentation. Theoretical investigations in these areas will help to define the needed observations and will aid the development of operational models.

Observations. The program will build on existing observational capabilities and determine the value of current data and new data needs. Observations in support of research and forecasting are expected to grow as critical parameters for forecasting are identified, measurement techniques are defined, and new space- and ground-based platforms are developed. The initial focus will be on better coverage of data-void or data-sparse regions, and on the deployment of systems that will provide data with appropriate accuracy, resolution, and timeliness. Because instrumentation development is an evolutionary process, the program will emphasize rapid exploitation of observational capabilities and efficient communication between data analysts, researchers, and instrument designers.

Modeling. These efforts for specifying and predicting the space environment have been under way for several years, but operational benefits have not yet been realized. The program will coordinate modeling and integration activities to ensure the consistency and optimal performance of the models. A primary goal is to develop physics-based specification and forecast models covering the forecast period out to 72 hours for solar events and 48 hours for near-Earth space weather phenomena. These models will be evaluated in close collaboration with research and observation efforts and with regard to user requirements. Gaps and deficiencies in these models will be identified and used to set requirements for future models.

Education. The education activities supported by the program will enhance public awareness of space weather and its impacts; will help ensure a sufficient supply of educated scientists and engineers to maintain expertise in all space-weather-related fields; and will improve training of forecasters, observers, and system operators. An educated public and commercial sector will be better able to utilize space environment forecasting services; student research will supply fresh ideas to explore; and knowledgeable government officials and the media will help realize the socioeconomic benefits.

Technology Transition and Integration. These processes must be improved and focused to facilitate the transfer of tools, techniques, and knowledge from the research or commercial communities to the operational forecasting activities. This effort, now often a bottleneck, is critical to the success of the program. Innovative means must be explored to establish a dynamic process for technology exploitation and transition to improve forecasting capability, utilize all relevant research, and rapidly realize benefits.


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