摘要
计算2010年4月14日发生在青海玉树Ms7.1地震前后潮汐力位变化,并以潮汐力位变化为时间指示,处理美国NOAA提供的大气温度(AT)、地面长波辐射(OLR)数据资料,结果显示:玉树地震发生时正处于震中所受引潮力较大的极值附近;在震中附近,大气温度和地面长波辐射遥感影像,都呈现出震前增温、震后衰减的清晰过程。
The celestial body tidal force niche of the sun and the in Qinhai on April 14^th, 2010 was calculated, and took the cycle indicator, the paper analyzed the air temperature （AT） and the moon for Yushu Ms7. 1 earthquake occurred of celestial body tidal force niche as the time out-long-radiation （OLR） data which were collected from the NOAA. The results showed that the earthquake occurred at the time when the tidal force of celestial body appeared went through the enhan near the maximum value. Around the epicenter, both the AT and the OLR images cement before earthquake and the attenuation after the shock.
出处
《高原地震》
2015年第A12期22-26,共5页
Plateau Earthquake Research
基金
地震科技星火计划项目(编号:XH153704)资助
关键词
玉树地震
潮汐力位
大气温度
长波辐射
Yushu Ms7, 1 earthquake
Celestial body tidal force niche
Air temperature
Out-long-radiation
