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首页> 外文期刊>Journal of geophysical research >Coseismic Traveling Ionospheric Disturbances during the M-w 7.8 Gorkha, Nepal, Earthquake on 25 April 2015 From Ground and Spaceborne Observations
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Coseismic Traveling Ionospheric Disturbances during the M-w 7.8 Gorkha, Nepal, Earthquake on 25 April 2015 From Ground and Spaceborne Observations

机译：Coseismic Traveling Ionospheric Disturbances during the M-w 7.8 Gorkha, Nepal, Earthquake on 25 April 2015 From Ground and Spaceborne Observations

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abstract_textpCoseismic traveling ionospheric disturbances (CTIDs) and their propagation characteristics during M-w 07.8 Gorkha earthquake in Nepal on 25 April 2015 have been investigated using a suite of ground-based GPS receivers and broadband seismometers along with the spaceborne radio occultation observations over the Indian subcontinent region. Depletion in vertical total electron content, a so called ionospheric hole, is observed near the epicenter similar to 9-11 min after the onset of earthquake. A positive pulse preceding the depletion, similar to N-shaped perturbation, propagating with an apparent velocity of similar to 2.4 km/s is observed on the south. Further, the CTIDs in the southward direction are found to split in to fast (similar to 2.4-1.7 km/s) and slow (similar to 680-520 m/s) propagating modes at epicentral distances greater than similar to 800 km. However, the velocities of fast mode CTIDs are significantly smaller than the surface Rayleigh wave velocity (similar to 3.7 km/s), indicating that they are not the true imprint of Rayleigh wave, instead, can probably be attributed to the superimposed wave front formed by the mixture of acoustic waves excited by main shock and propagating Rayleigh wave. The southward CTIDs are found to propagate at F-2 region altitudes of similar to 300-440 km captured by Constellation Observing System for Meteorology, Ionosphere and Climate radio occultation observations. The CTIDs with periods of similar to 4-6 min are observed in all directions with significantly larger amplitudes and faster propagation velocities in south and east directions. The observed azimuthal asymmetry in the amplitudes and velocities of CTIDs are discussed in terms of the alignment with geomagnetic field and nature of surface crustal deformation during the earthquake./p/abstract_text

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