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Space weather is the concept of changing environmental conditions in outer space. It is distinct from the concept of weather within a planetary atmosphere, and deals with phenomena involving ambient plasma, magnetic fields, radiation and other matter in space. "Space weather" often implicitly means the weather in outer space close to the Earth, but it is also studied in interplanetary and occasionally interstellar space). 1 Within our own solar system, space weather is greatly influenced by the speed and density of the solar wind and the interplanetary magnetic field (IMF) carried by the solar wind plasma. A variety of physical phenomena are associated with space weather, including geomagnetic storms and substorms, energization of the Van Allen radiation belts, ionospheric disturbances and scintillation, aurora and geomagnetically induced currents at Earth's surface. Coronal Mass Ejections and their associated shock waves are also important drivers of space weather as they can compress the magnetosphere and trigger geomagnetic storms. Solar Energetic Particles, accelerated by coronal mass ejections or solar flares, are also an important driver of space weather as they can damage electronics onboard spacecraft through induced electric currents,citation needed and threaten the life of astronauts. Space weather exerts a profound influence in several areas related to space exploration and development. Changing geomagnetic conditions can induce changes in atmospheric density causing the rapid degradation of spacecraft altitude in Low Earth orbit. Geomagnetic storms due to increased solar activity can potentially blind sensors aboard spacecraft, or interfere with on-board electronics. An understanding of space environmental conditions is also important in designing shielding and life support systems for manned spacecraft. There is also some concern that geomagnetic storms may also expose conventional aircraft flying at high latitudes to increased amounts of radiation.2
Satellites observing space weatherSince 1995, the joint NASA-European Space Agency Solar and Heliospheric Observatory (SOHO) spacecraft is the main source of near-real time solar data for space weather prediction. It was joined in 1998 by the NASA Advanced Composition Explorer (ACE), which carries a space weather beacon for continuous transmission of relevant in situ space environment data. SOHO and ACE are located near the L1 Lagrangian point, 1% of the earth-sun distance upstream of the earth where it measures solar wind plasma and magnetic field approximately one hour before it reaches the earth. Most recently, the launch of the NASA-ESA Solar-Terrestrial Relations Observatory (STEREO) added an additional space weather data stream that covers the region between the sun and the earth with stereoscopic imagery. The two STEREO spacecraft drift away from the earth by about 22 degrees per year, one leading and the other trailing the earth in its orbit. Modeling effortsMajor modelling efforts to simulate the space environment from the Sun to the Earth and beyond using three-dimensional magnetohydrodynamics frameworks have been undertaken since the 1990s. In the United States, the two major centers are the Center for Space Environment Modeling (CSEM) 3 and the Center for Integrated Space weather Modeling (CISM).4 Examples of space weather events
Space weather at the Earth’s surfaceThe best known ground-level consequence of space weather is geomagnetically induced currents, or GIC. These are damaging electrical currents that can flow in power grids, pipelines and other conducting networks. Rapid magnetic changes on the ground - that occur during geomagnetic storms and are associated with space weather - can also be important for activities such as geophysical mapping and hydrocarbon production. Geophysical explorationAir and ship borne magnetic surveys can be affected by rapid magnetic field variations during geomagnetic storms. Storms can cause data interpretation problems where the magnetic field changes due to space weather are of similar magnitude to those of the sub-surface crustal magnetic field in the survey area. Accurate geomagnetic storm warnings, including an assessment of the magnitude and duration of the storm, allows for an economic use of survey equipment. Geophysics and hydrocarbon productionFor economic and other reasons, oil and gas production often involves the directional drilling of well paths many kilometers from a single wellhead in both the horizontal and vertical directions. The accuracy requirements are strict, due to target size – reservoirs may only be a few tens to hundreds of meters across – and for safety reasons, because of the proximity of other boreholes. Surveying by the most accurate gyroscopic method is expensive, since it can involve the cessation of drilling for a number of 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 the drilling direction and nearby magnetic observatories prove vital (Clark and Clarke, 2001; Reay et al, 2006). Magnetic data and storm forecasts can also be helpful in clarifying unknown sources of drilling error on an on-going basis. Further reading
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