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Introduction The unexpected December 26, 2004, off the west coast of northern Sumatra, Indonesia, MW=9.0 earthquake, which caused devastating tsunami around the Indian Ocean, reminds seis-mologists of the difficulty of earthquake forecast and/or prediction. For seismologists this earth-quake is almost completely unexpected, because there was neither forecasting (which means the estimation of the future earthquake rate as a function of location, time, and magnitude) nor predic-tion (forecasti… 相似文献
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该文介绍了基于MapXtremeforNT的WebGIS应用专题系统———大庆供水管网信息系统的设计与实现 ,阐述该系统的体系结构、功能设计 ,并对MapXtreme的实现机理进行分析 ,同时研究客户端和服务器端通讯技术及智能关阀等功能的实现方法。 相似文献
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R. Rajaraman S. Joseph Winston T. S. Murty Hema Achyuthan N. Nirupama 《Marine Geodesy》2006,29(3):167-178
The State of Tamil Nadu was the most affected region in India during the tsunami of December 26, 2004, in the Indian Ocean, in terms of loss of life and damage. Numerical simulation was made for three tsunamis, the December 26, 2004, event, the Sumatra tsunami of 1833, and a hypothetical tsunami originating in the Andaman-Nicobar region. Since inundation is not included in these simulations, the tsunami amplitudes were deduced at the 10m depth contour in the ocean, off several locations on the coast of Tamil Nadu. The computed amplitudes appear reasonable as compared to known tsunami amplitudes from past events. 相似文献
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Bogusław M. Domański 《Acta Geophysica》2007,55(3):267-287
An analysis of source parameters of the two unexpected earthquakes from the Kaliningrad (Russia) area is presented. The earthquakes
occurred on 21 September 2004 at 11:05:01 and 13:32:31 UT, respectively. The first event was located at the latitude φ = 54.924°N and the longitude λ = 20.120°E, with a depth h = 16 km, and the second event at φ = 54.876°N, λ = 20.120°E and h = 20 km.
Magnitudes Mw of the two events were very similar: 5.1 and 5.2. The magnitude values reported by various international data centers have
been meaningfully different. The reason is the presence of high-frequency components in Z velocity component of the S wavefield.
They were observed along the direction defined by two stations, BLEU in Sweden and SUW in Poland, located in opposite sides
of the source. Along the direction perpendicular to it, the effects are relatively very small. The high-frequency waves are
understood to mean components in the 6–8 Hz band for event 1 and 2-4 Hz for event 2. The effects in question are also clearly
visible on displacement spectrograms. The magnitude values calculated at such stations from S-wave amplitudes or from seismic
spectra are clearly overestimated and are close to 6. Therefore, we made a careful selection of channels in order to determine
the spectral parameters and, on this basis, the source parameters.
The size of the source is relatively small, of about 2 km. The closest seismic station is at 100 source radii from the source.
One can clearly see the effect of the TT zone which markedly reduces the seismic moment value for seismic stations laying
on the opposite sides of the source. Both events have very similar spatial distributions of the source parameters: magnitude,
seismic moment and radius. 相似文献
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Emile A. Okal 《Pure and Applied Geophysics》2007,164(2-3):325-353
Following the recent reports by Yuan et al. (2005) of recordings of the 2004 Sumatra tsunami on the horizontal components of coastal seismometers in the Indian Ocean
basin, we build a much enhanced dataset extending into the Atlantic and Pacific Oceans, as far away as Bermuda and Hawaii,
and also expanded to five additional events in the years 1995–2006. In order to interpret these records quantitatively, we
propose that the instruments are responding to the combination of horizontal displacement, tilt and perturbation in gravity
described by Gilbert (1980), and induced by the passage of the progressive tsunami wave over the ocean basin. In this crude approximation, we
simply ignore the island or continent structure, and assume that the seismometer functions de facto as an ocean-bottom instrument. The records can then be interpreted in the framework of tsunami normal mode theory,and lead
to acceptable estimates of the seismic moment of the parent earthquakes. We further demonstrate the feasibility of deconvolving
the response of the ocean floor in order to reconstruct the time series of the tsunami wave height at the surface of the ocean,
suggesting that island or coastal continental seismometers could complement the function of tsunameters. 相似文献
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基于MapXtreme的校园WebGIS系统实现 总被引:3,自引:0,他引:3
万维网地理信息系统(WebGIS)是利用互联网(Internet)来扩展和完善地理信息系统功能的一项新技术,是由地理信息系统和互联网技术相结合而产生的一种新方法。目前,用于开发WebGIS的方法有许多种,文章研究基于MapXtreme的WebGIS实现方法,把MapXtreme与JavaScript及ASP相结合开发WebGIS系统,并将其应用于校园信息查询中。实现基于MapXtreme的校园WebGIS系统。 相似文献
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