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The Surface Latent Heat Flux anomalies related to major earthquake

机译:与大地震有关的地表潜热通量异常

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摘要

SLHF (Surface Latent Heat Flux) is an atmospheric parameter, which can describe the heat released by phase changes and dependent on meteorological parameters such as surface temperature, relative humidity, wind speed etc. There is a sharp difference between the ocean surface and the land surface. Recently, many studies related to the SLHF anomalies prior to earthquakes have been developed. It has been shown that the energy exchange enhanced between coastal surface and atmosphere prior to earthquakes can increase the rate of the water-heat exchange, which will lead to an obviously increases in SLHF. In this paper, two earthquakes in 2010 (Haiti earthquake and southwest of Sumatra in Indonesia earthquake) have been analyzed using SLHF data by STD (standard deviation) threshold method. It is shows that the SLHF anomaly may occur in interpolate earthquakes or intraplate earthquakes and coastal earthquakes or island earthquakes. And the SLHF anomalies usually appear 5-6 days prior to an earthquake, then disappear quickly after the event. The process of anomaly evolution to a certain extent reflects a dynamic energy change process about earthquake preparation, that is, weak-strong-weak-disappeared.
机译:SLHF(表面潜热通量)是一种大气参数,可以描述相变释放的热量,并且取决于诸如地面温度,相对湿度,风速等气象参数。海洋表面与陆地之间存在明显的差异表面。最近,已经开展了许多与地震前SLHF异常有关的研究。研究表明,地震前沿海地表与大气之间的能量交换增强,可以提高水热交换速率,从而导致SLHF明显增加。本文使用SLHF数据,通过STD(标准差)阈值方法分析了2010年的两次地震(海地地震和印度尼西亚苏门答腊西南地震)。结果表明,SLHF异常可能发生在内插地震,板内地震,沿海地震或岛屿地震中。 SLHF异常通常在地震发生前5-6天出现,然后在事件发生后迅速消失。异常演化的过程在一定程度上反映了地震准备过程中能量的动态变化过程,即弱强弱消失。

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