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11篇 您的检索式：作者名="Peter Gerstoft"

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		题名	作者	年代	出处	被引量
	1	Ocean Acoustic Inversion with Estimation of a PosterioriProbability Distributions 显示文摘	Peter Gerstoft Christoph F Mecklenbr/iuker	1998	JASA1998，104，2：	1
	2	Tracking Refractivity from Clutter Using Kalman and Particle Filters显示文摘	Caglar Yardim Peter Gerstoft WILLIAM S		0，，4：	1
	3	Inversion for refractivity parameters from radar sea clutter显示文摘	Peter Gerstoft L Ted Rogers Jeffrey L Krolik William S Hodgldss	2003	Radio Sci2003，32，2：	1
	4	Inversion for refractivity parameters from radar sea clutter显示文摘	Peter Gerstoft L Ted Rogers Jeffrey L Krolik		0，，02：	1
	5	Ocean acoustic inversion with estimation of a posteriori probability distributions 显示文摘	Peter Gerstoft Christoph F Mceklenbrauker	1998	JASA1998，104，2：	1
	6	Tracking Refractivity from Clutter Using Kalman and Particle Filters 显示文摘	Caglar Yardim Peter Gerstoft WILLIAM S	2008	IEEE Transactions on Antennas and Propagation2008，56，4：	1
	7	Objective functions for ocean acoustic inversion derived by likelihood methods 显示文摘	Christoph F Mecklenbrauker Peter Gerstoft	2000	Journal of Computational Acoustics (S0218-396)2000，8，2：	1
	8	Phenomenological and global optimization inversion 显示文摘	Peter Gerstoft William S Hodgkiss William A Kuperman Heechun Song	2003	IEEE JOURNAL OF OCEANIC ENGERRING2003，28，3：	1
	9	Peer-Reviewed Technical Communication-An OverviewofSequential Bayesian Filtering in Ocean Acoustics显示文摘	Yardim Caglar Michalopoulou Zoi-Heleni Gerstoft Peter	2011	IEEE Journal of Oceanic Engneering2011，36，1：	1
	10	Tracking Refractivity from Clutter Using Kalman and Particle Filters 显示文摘	Caglar Yardim Peter Gerstoft William S	2008	IEEE Transactions on Antennas and Propagation2008，56，4：	1
	11	Local-scale cross-correlation of seismic noise from the Calico fault experiment显示文摘Most studies of seismic noise cross-correlation(NCC) have focused on regional/continental scale imaging using empirical surface-wave Green's functions extracted from primary(0.05–0.08 Hz) and secondary(0.1–0.16 Hz)microseisms.In this work,we present the NCC results at higher frequencies([0.5 Hz) from 6 months seismic noise recorded by a local array(4 km aperture) deployed along the Calico fault in the Mojave Desert,California.Both fast and slow propagating waves are observed from the NCC record-sections.We compare the NCCs from sensor pairs that share a common sensor with the records of a borehole shot located very close to this common sensor.The result shows a good match of the slow surface-wave arrivals,indicating that the NCC method is able to recover unbiased surface-wave Green's functions at local scales.The strong body-wave NCC component is caused by the P waves generated offshore California.Along a SW–NE profile across the fault,we observe apparent P-wave arrivals and their reflections,which can be explained by a low-velocityzone(LVZ) along the Calico fault.We calculate the LVZ width to be 2.3 km,and the P-wave velocity reduction within the LVZ to be *35 %.These estimates are consistent with other evidence for a relatively wide LVZ along the Calico fault.	Jian Zhang Peter Gerstoft	2014	Earthquake Science2014，27，3：	0

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