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基于多源测高数据建立平均海面高模型
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作者 宋昊天 文汉江 +2 位作者 程鹏飞 刘焕玲 于宏旭 《大地测量与地球动力学》 CSCD 北大核心 2023年第5期467-473,共7页
利用多源卫星测高数据构建9°~19°N、110°~116°E范围内分辨率为1′×1′的平均海面高模型,对ERM数据的共线平均、GM数据的时变改正、单星及多星间交叉点平差、格网化等方法进行阐述。实验结果表明,平均海面高模... 利用多源卫星测高数据构建9°~19°N、110°~116°E范围内分辨率为1′×1′的平均海面高模型,对ERM数据的共线平均、GM数据的时变改正、单星及多星间交叉点平差、格网化等方法进行阐述。实验结果表明,平均海面高模型与CLS15差值的平均值(mean)、均方根(RMS)、标准差(STD)分别为0.59 cm、 2.85 cm、2.79 cm,与DTU18差值的mean、RMS、STD分别为2.06 cm、4.17 cm、3.62 cm。利用独立于模型的测高数据(Sentinel-3B、HY-2B)验证模型的精度,建立MSS时使用HY-2A、Jason-3和Sentinel-3A卫星数据,再通过与T/P(TOPEX/Poseidon)数据的对比,分析新数据对MSS的提升作用。 展开更多
关键词 卫星测高 平均海面高模型 共线平均 CLS15
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Study of Nonpolaritons in a Kerr Nonlinear Optical Resonator
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作者 WAN Jin-Yin CHENG Ze 《Communications in Theoretical Physics》 SCIE CAS CSCD 2006年第6期1107-1111,共5页
We find that in a Kerr nonlinear optical resonator, the photon system possesses a new kind of quasiparticle, the nonpolariton. The existence of nonpolaritons should be testified by observing the energy density depende... We find that in a Kerr nonlinear optical resonator, the photon system possesses a new kind of quasiparticle, the nonpolariton. The existence of nonpolaritons should be testified by observing the energy density dependence of the velocity and squeezing of nonpolaritons. As we have investigated, the transition energy density of a Kerr nonlinear optical resonator is larger than that of a normal state. 展开更多
关键词 Kerr nonlinear resonator nonpolariton average energy density
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Terrestrial water variations in the North China Plain revealed by the GRACE mission 被引量:17
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作者 SU XiaoLi PING JinSong YE QiXin 《Science China Earth Sciences》 SCIE EI CAS 2011年第12期1965-1970,共6页
Using eight years of time-variant gravity measurements from the GRACE gravity satellite mission, we estimate monthly terrestrial water storage variations in the North China Plain between August 2002 and August 2010. W... Using eight years of time-variant gravity measurements from the GRACE gravity satellite mission, we estimate monthly terrestrial water storage variations in the North China Plain between August 2002 and August 2010. We find that during this period, the water storage is not constant but accelerate at a rate of -1.1 cm/yr over time. The study confirms that the relatively long-term trend of water storage in the North China Plain (by 13-point moving average) is consistent well with that by linear fitting. Two hydrological models, CPC and GLDAS, are adopted in calculating surface water variations, with results indicating that they agree with those of GRACE. Furthermore, rates of -0.6 cm/yr for surface water variations and -0.5 cm/yr for groundwater variations are found in the North China Plain during the study period. Decrease of rainfall and the groundwater over-exploitation are possibly the main causes for groundwater depletion in the North China Plain. The results will be helpful for better understanding climatic changes and provide reference for the management of water resources and the establishment of policies on preventing and alleviating natural hazards. 展开更多
关键词 GRACE gravity measurements GROUNDWATER the North China Plain
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