Titlebook: Wave Propagation; Lectures given at a Giorgio Ferrarese Book 2011 Springer-Verlag Berlin Heidelberg 2011 partial differential equations

Colossal

書(shū)目名稱(chēng)Wave Propagation影響因子(影響力)




書(shū)目名稱(chēng)Wave Propagation影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Wave Propagation網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Wave Propagation網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱(chēng)Wave Propagation被引頻次




書(shū)目名稱(chēng)Wave Propagation被引頻次學(xué)科排名




書(shū)目名稱(chēng)Wave Propagation年度引用




書(shū)目名稱(chēng)Wave Propagation年度引用學(xué)科排名




書(shū)目名稱(chēng)Wave Propagation讀者反饋




書(shū)目名稱(chēng)Wave Propagation讀者反饋學(xué)科排名

墊子

gospel

期滿(mǎn)

裝入膠囊

Giuseppe Grioliess. Recovery plan could facilitate the local-level participation and support bottom-up approaches. Such approaches strengthen self-reliance and efficiency at the local level..Second is to find out the opportunities and challenges of resilient-based recovery for affected communities. Although resili

motor-unit

ffects of the fault crossing angle that causes compression to the pipeline are also examined. Finally, the small-scale tests conducted at NTU Athens in a special-purpose soil box are presented. The box simulates vertical differential motion due to fault rupture or soil subsidence. In all experiments

恩惠

A. JeffreyMadinah—and also hosts the youngest volcanoes in the Kingdom of Saudi Arabia, which have historical and cultural significance (Fig.?3.1). Harrat Al Madinah is the northern part of the Harrat Rahat and the best studied in the Harrat Rahat. The distinction between Harrat Rahat and Harrat Al Madinah is

有惡臭

Tristano Manacordaoration of all geosites was carried out. Seven geosites have reached the stage of usage values and are to be exploited for geoeducational and geotourism purposes out of a total of 23 geosites, which represents 30.4% of the sites listed. Three geosites (Bizi, Taffert and Taferdoust) have been chosen

能量守恒

百科全書(shū)

Guy Boillat-atmospheric processes induced by the BWI oscillation in the SCS SST results in enhanced sea level pressure and surface shortwave radiation flux during the summer monsoon. Besides, it is observed that the SCS BWI oscillation in the changes of SST causes a feedback in the atmosphere by modifying the