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    题名 作者 年代 出处 被引量
1Temporal Variations of the Frontal and Monsoon Storm Rainfall during the First Rainy Season in South China显示文摘The temporal variations in storm rainfall during the first rainy season (FRS) in South China (SC) are investigated in this study. The results show that the inter-annual variations in storm rainfall during the FRS in SC seem to be mainly influenced by the frequency of storm rainfall, while both frequency and intensity affect the inter-decadal variations in the total storm rainfall. Using the definitions for the beginning and ending dates of the FRS, and the onset dates of the summer monsoon in SC, the FRS is further divided into two sub-periods, i.e., the frontal and monsoon rainfall periods. The inter-annual and inter-decadal variations in storm rainfall during these two periods are investigated here. The results reveal a significant out-of-phase correlation between the frontal and monsoon storm rainfall, especially on the inter-decadal timescale, the physical mechanism for which requires further investigation.YUAN Fang WEI Ke CHEN Wen FONG Soi Kun LEONG Ka Cheng 2010Atmospheric and Oceanic Science Letters2010,3,5:10
2Numerical prediction experiment on Typhoon Maggie (9903)显示文摘The movement of Typhoon Maggie (9903) in June 1999 is one of the rare cases ever seen in the history. At 00U on June 6 Maggie was located at about 70 km to the southwest of Taiwan. When it arrived at the coastal region of Shanwei City (22.8N, 116.5E), it turned suddenly to move southwestward along the southern China coastal line. De June 7 Maggie finally turned to move northward, making landfall to the north of Shangchuan Island. The experimental numerical prediction system on typhoon movement that was designed based on MM5 is proved quite successful for the 48h prediction of Maggie’s movement and rainfall. The mean prediction error of typhoon track is 81 km for 0-24 h and 74 km for 24-48 h. The location of typhoon center in the initial field of the model is approximately 100 km away from the actual observations. In order to modify the location of typhoon center, a bogus typhoon was intro- duced into the model and the prediction of typhoon track was improved in 0-24 h time interval. But the prediction error was enlarged in 24-36 h. We also performed a sensitivity experiment of changing the land of southern China into the ocean. It is found that the orientation of South China coastal line and the topography have no obvious effect on the movement of Typhoon Maggie.Fong Soi Kun, Wu Chisheng, Hao I Pan, Lam Kin Hang Ku Chi Meng, Wang Anyu, Lin Wenshi (1. Macao Meteorological and Geophysical Bureau, Macao, China 2. Department of Atmospheric Sciences, Zhongshan University, Guangzhou 510275, China) 2001Acta Oceanologica Sinica2001,20,2:3
3Projection of the Zhujiang(Pearl) River Delta's potential submerged area due to sea level rise during the 21st century based on CMIP5 simulations显示文摘Projections of potential submerged area due to sea level rise are helpful for improving understanding of the influence of ongoing global warming on coastal areas. The Ensemble Empirical Mode Decomposition method is used to adaptively decompose the sea level time series in order to extract the secular trend component. Then the linear relationship between the global mean sea level(GMSL) change and the Zhujiang(Pearl) River Delta(PRD)sea level change is calculated: an increase of 1.0 m in the GMSL corresponds to a 1.3 m(uncertainty interval from1.25 to 1.46 m) increase in the PRD. Based on this relationship and the GMSL rise projected by the Coupled Model Intercomparison Project Phase 5 under three greenhouse gas emission scenarios(representative concentration pathways, or RCPs, from low to high emission scenarios RCP2.6, RCP4.5, and RCP8.5), the PRD sea level is calculated and projected for the period 2006–2100. By around the year 2050, the PRD sea level will rise 0.29(0.21 to 0.40) m under RCP2.6, 0.31(0.22 to 0.42) m under RCP4.5, and 0.34(0.25 to 0.46) m under RCP8.5, respectively.By 2100, it will rise 0.59(0.36 to 0.88) m, 0.71(0.47 to 1.02) m, and 1.0(0.68 to 1.41) m, respectively. In addition,considering the extreme value of relative sea level due to land subsidence(i.e., 0.20 m) and that obtained from intermonthly variability(i.e., 0.33 m), the PRD sea level will rise 1.94 m by the year 2100 under the RCP8.5scenario with the upper uncertainty level(i.e., 1.41 m). Accordingly, the potential submerged area is 8.57×103 km2 for the PRD, about 1.3 times its present area.XIA Jiangjiang YAN Zhongwei ZHOU Wen FONG Soi Kun LEONG Ka Cheng TANG Iu Man CHANG S W LEONG W K JIN Shaofei 2015Acta Oceanologica Sinica2015,34,9:3
4Genetic adaptation to high altitude in the Ethiopian highlands显示文摘Scheinfeldt LB Soi S Thompson S 2012Genome Biol2012,13,1:1
5Intratympanic dexamethasone treatment for control of subjective idiopathic tinnitus: our clinical experience 显示文摘CESARANI A CAPOBIANCO S SOI D 2002Int Tinnitus J2002,8,:1
6Land Transport Policy and Public Transport in Singapore显示文摘SOI HOI LAM TRINH DINH TOAN 2006Transportation2006,33,:1
7Acidic and basic fibroblast growth factors are present in glioblastoma multiforme显示文摘Stefank DF Rizkalla LR Soi A 1991Cancer Res1991,51,:1
8Genetic adaptation to high altitude in the Ethiopian highlands显示文摘Scheinfeldt L B Soi S Thompson S Ranciaro A Woldemeskel D Beggs W 2012Genome Bi- ol2012,131,:1
9Intratympanic dexamethasone treatment for control of subjective idiopathic tiunitus:our clinical experience显示文摘Cesarani A Capobianco S Soi D 2002Int Tinnitus J2002,8,:1
10Game-theoretic analysis of cooperation among supply chain agents: Review and extensions显示文摘Nagarajan M Soi G 2008European Journal of Operational Research2008,187,3:1
11Titration of C60: A method for the synthesis of organofullerenes 显示文摘HIRSCH A SOI A KARFUNKEL H R 1992Angew Chem: Int Ed Eng1992,31,:1
12Land transport policy and public transport in Singapore显示文摘Soi Hoi Lam Trinh Dinh Toan 2006Transportation2006,,33:1
13Game-theoretic analysis of cooperation among supply chain agents: Review and extensions显示文摘Nagarajan M Soi G 2008European Journal of Operational Research2008,187,3:1
14Polyimide (PI) films by chemical vapor deposi- tion (CVD): Novel design, experiments and characterization显示文摘JAIME PUIG-PEY GONZALEZ ALAIN LAMURE FRAN- SOIS SENOCQ 2007Surface and Coatings Technology2007,201,2223:1
15Temperature distribution in composite bridges显示文摘KENNEDY J B SOI 1MAN M H 1987Journal of Structural Engineering1987,113,3:1
16Genetic adaptation to high altitude in the Ethiopian highlands显示文摘Scheinfeldt LB Soi S Thompson S 2012Genome Biol2012,13,1:1
17Transit path choice models using RP and SP data显示文摘Feng Xie Soi Hoi Lan 2002Trans Research Record2002,,1799:1
18Effects of Shrinkage Reducing Admixture in Shrinkage Compensating Concrete显示文摘COLLEPARDI M BOR SOI A COLLEPARDI S Troli ENCO Engineering concrete Ponzano Veneto (TV)0,,:1
19Low-Protein diet suppresses serum insulin--like growth factor--1 and decelerates the progression of growth hormone-induced glomerulosclerosis显示文摘Doi Soi Rasaiah S Tack I Mysore J 2001Am J Nephrol2001,21,4:1
20Nano -emulsions prepared by the phase inversion composition method: Preparatinn variables and scale up 显示文摘ISABEL SOI E PEY C M ALICIA MAESTRO 2010Journal of Colloid and Interface Science2010,344,:1
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