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单词 South Atlantic Anomaly
释义

South Atlantic Anomaly

中文百科

南大西洋异常区

范艾伦辐射带
Los cinturones de radiación Van Allen y el punto donde se encuentra la Anomalía del Atlántico Sur.
La AAS a una altura aproximada de 560 km de la superficie terrestre.[2]
Ilustración de AAS y mapa de flujo de protones (n.º de protones registrados por un detector de estado sólido) con un factor geométrico de 9.5×10-3 cm²/s.

南大西洋异常区(South Atlantic Anomaly)是地球上一片地磁最弱的区域,覆盖范围遍及南美洲南部及南大西洋海域。由于该区的地磁较其他地区弱,阻挡太阳粒子的范艾伦辐射带在该区域上空形成一凹陷部份,容让粒子可以到达更接近地球的位置,导致穿越该区域上空的人造卫星受粒子影响而出现运作异常。

英语百科

South Atlantic Anomaly 南大西洋异常区

The anomaly at an altitude of approximately 560 kilometers[1]
A cross-sectional view of the Van Allen radiation belts, noting the point where the South Atlantic Anomaly occurs
范艾伦辐射带
Los cinturones de radiación Van Allen y el punto donde se encuentra la Anomalía del Atlántico Sur.

The South Atlantic Anomaly (SAA) is an area where the Earth's inner Van Allen radiation belt comes closest to the Earth's surface dipping down to an altitude of 200 km (124 mi). This leads to an increased flux of energetic particles in this region and exposes orbiting satellites to higher-than-usual levels of radiation. The effect is caused by the non-concentricity of the Earth and its magnetic dipole, and the SAA is the near-Earth region where the Earth's magnetic field is weakest relative to an idealized Earth-centered dipole field.

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更新时间:2025/6/23 7:31:17