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Статті в журналах з теми "Typhoons South China Sea Region"
Park, Seongjun, and Tae-Kyung Hong. "Typhoon-Induced Microseisms around the South China Sea." Seismological Research Letters 91, no. 6 (September 9, 2020): 3454–68. http://dx.doi.org/10.1785/0220190310.
Повний текст джерелаRen, Jia, Nan Xu, and Yani Cui. "Typhoon Track Prediction Based on Deep Learning." Applied Sciences 12, no. 16 (August 11, 2022): 8028. http://dx.doi.org/10.3390/app12168028.
Повний текст джерелаJin, Weifang, Chujin Liang, Junyang Hu, Qicheng Meng, Haibin Lü, Yuntao Wang, Feilong Lin, Xiaoyan Chen, and Xiaohui Liu. "Modulation Effect of Mesoscale Eddies on Sequential Typhoon-Induced Oceanic Responses in the South China Sea." Remote Sensing 12, no. 18 (September 18, 2020): 3059. http://dx.doi.org/10.3390/rs12183059.
Повний текст джерелаShang, Xiao-dong, Hai-bin Zhu, Gui-ying Chen, Chi Xu, and Qi Yang. "Research on Cold Core Eddy Change and Phytoplankton Bloom Induced by Typhoons: Case Studies in the South China Sea." Advances in Meteorology 2015 (2015): 1–19. http://dx.doi.org/10.1155/2015/340432.
Повний текст джерелаChen, Huei-Fen, Yen-Chu Liu, Chih-Wen Chiang, Xingqi Liu, Yu-Min Chou, and Hui-Juan Pan. "China's historical record when searching for tropical cyclones corresponding to Intertropical Convergence Zone (ITCZ) shifts over the past 2 kyr." Climate of the Past 15, no. 1 (February 13, 2019): 279–89. http://dx.doi.org/10.5194/cp-15-279-2019.
Повний текст джерелаShao, Weizeng, Yexin Sheng, Huan Li, Jian Shi, Qiyan Ji, Wei Tan, and Juncheng Zuo. "Analysis of Wave Distribution Simulated by WAVEWATCH-III Model in Typhoons Passing Beibu Gulf, China." Atmosphere 9, no. 7 (July 15, 2018): 265. http://dx.doi.org/10.3390/atmos9070265.
Повний текст джерелаXu, Yao, Hailun He, Jinbao Song, Yijun Hou, and Funing Li. "Observations and Modeling of Typhoon Waves in the South China Sea." Journal of Physical Oceanography 47, no. 6 (June 2017): 1307–24. http://dx.doi.org/10.1175/jpo-d-16-0174.1.
Повний текст джерелаLi, Pingyuan, Mingkun Li, Huayang Gan, and Zhen Xia. "A preliminary study on sediment records of possible typhoon in the northern South China Sea during the past 6500 years." Holocene 31, no. 7 (April 12, 2021): 1221–28. http://dx.doi.org/10.1177/09596836211003229.
Повний текст джерелаLi, R. H., S. M. Liu, Y. W. Li, G. L. Zhang, J. L. Ren, and J. Zhang. "Nutrient dynamics in tropical rivers, lagoons, and coastal ecosystems of eastern Hainan Island, South China Sea." Biogeosciences 11, no. 2 (January 30, 2014): 481–506. http://dx.doi.org/10.5194/bg-11-481-2014.
Повний текст джерелаHuong, Chu Thi Thu, Tran Dinh Linh, Dinh Tran Ngoc Huy, and Nguyen Binh Phong. "Changes of the temperature field during storms and Effects of Cold Air on Structure of Thermal Fields in Typhoons – Case in China and Vietnam Sea." International Journal of Rural Development, Environment and Health Research 6, no. 6 (2022): 25–29. http://dx.doi.org/10.22161/ijreh.6.6.5.
Повний текст джерелаДисертації з теми "Typhoons South China Sea Region"
Zhang, Zhongfeng. "Study of South China Sea typhoons between 1999 and 2002 /." View Abstract or Full-Text, 2003. http://library.ust.hk/cgi/db/thesis.pl?MATH%202003%20ZHANGZ.
Повний текст джерелаCheng, Kuo-Feng. "Typhoon effects on the South China Sea wave characteristics during winter monsoon." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2006. http://library.nps.navy.mil/uhtbin/hyperion/06Mar%5FCheng.pdf.
Повний текст джерелаDenny, Martin Anthony. "Regional strategic considerations in the Spratly Islands dispute." Thesis, Hong Kong : University of Hong Kong, 1997. http://sunzi.lib.hku.hk/hkuto/record.jsp?B18061515.
Повний текст джерела"The study on upper ocean responses to typhoon Cimaron and eddy heat flux in the South China Sea." 2013. http://library.cuhk.edu.hk/record=b5549853.
Повний текст джерела通過衛星海表溫度資料和氣候態海洋溫度資料反演颱風西馬侖引起的混合層加深的問題。反演結果顯示,2006年11月3日,對應海表溫度降低了4.4度,混合層則由颱風前的43.2米加深了104.5米,該結果與一維混合層模型(GOTM)的類比結果一致。此外,颱風引起的海表面溫度梯度可用來計算斜壓地轉流場和渦度。負渦度顯示了反氣旋斜壓迴圈在混合層底部最強,在50米水深處地轉流速可達到0.2米每秒。2006年11月3日,颱風西馬侖在最大的海表溫度降低的附近,向西南方向轉彎,此時行進速度比較緩慢(1.7 米每秒)進而導致在亞臨界條件弗勞德數(颱風的平移速度與第一斜壓相速度的比值)為0.6,在颱風尾區因缺少慣性重力波從而促進了海表溫度冷卻和混合層加深。通過比較Argo浮標觀測資料和氣候態資料的溫度剖面,混合層加深程度估算的誤差在10米以內。
三維海洋數值模型ROMS 用來研究颱風期間海洋物理動力和生態回應。海表溫度類比值同衛星觀測值比對得到的相關係數高達84%以上,表明ROMS基本上可以模擬在颱風期間南海的海表面溫度變化情況。但是深入研究發現由於垂向混合強度不夠,模式結果低估了海表面溫度冷卻和混合層加深,混合層深度被低估。通過增加波致混合效應(Bv)改進KPP混合方案,可以提高海表面溫度冷卻和混合層加深的模擬精度。類比結果顯示在颱風尾區,葉綠素的大規模爆發則發生在颱風經過的1周以後。透光層葉綠素濃度由颱風前的0.1 mg m⁻³ 增加到11月9日的1.9 mg m⁻³。衛星觀測顯示在颱風尾區,葉綠素濃度在11月16日仍高達0.85 mg m⁻³。
高度計的海表面高度異常值與海表面溫度的衛星觀測資料可以用來計算南海渦度熱通量。南海表層渦度熱通量的年變化趨勢表明,在南海西邊的熱通量表現出北向輸送特徵,其強度甚至與黑潮延伸區域的強熱通量相當。渦熱通量在冬季最強,熱量由南海南部流入,並且從呂宋海峽流出,甚至通過臺灣海峽進入東海海域。冬季熱通量的輻合帶主要分佈在南海東部近呂宋海峽附近海域和越南東南海域,而夏季主要集中在越南東南海域。研究表明,冬季和夏季的海表面渦度熱通量對海洋上層熱收支平衡的調整有顯著影響。
This dissertation focuses on the investigation of the upper ocean response to typhoon Cimaron (2006) and annual variations of horizontal eddy fluxes in the South China Sea (SCS) through the methods both of satellite remote sensing and numerical ocean modeling.
The mixed layer deepening induced by typhoon Cimaron is derived based on satellite observed sea surface temperature (SST) and climatological temperature profiles in the SCS. Corresponding to the SST drop of 4.4ÅC on November 3, 2006, the mixed-layer deepened by 104.5 m relative to the undisturbed depth of 43.2 m, which is consistent with the simulation results from the one-dimensional mixed-layer model (GOTM). Furthermore, baroclinic geostrophic velocity and vorticity are calculated from the surface temperature gradient caused by the typhoon. The negative vorticity, associated with the typhoon cooling, indicated an anti-cyclonic baroclinic circulation strongest at the base of the mixed-layer, and at the depth of 50 m, the geostrophic speed reached as high as 0.2 m s⁻¹. Typhoon Cimaron proceeded slowly (1.7 m s⁻¹) when it was making a southwestward turn on November 3, 2006, resulting in a subcritical condition with a Froude number (the ratio of typhoon translation speed to first baroclinic mode speed) of 0.6 around the maximum SST drop location and facilitating high SST cooling and mixed-layer deepening due to absence of inertial-gravity waves in the wake of the typhoon. Comparison of Argo buoy data with the climatological temperature suggests that the average uncertainty in the mixed-layer deepening estimation caused by the difference between Argo and climatological temperature profiles is less than 10 m.
The physical dynamic and biological responses to typhoon Cimaron are investigated through a three-dimensional ocean model, the Regional Ocean Modeling System (ROMS). The correlation between simulated sea surface temperature (SST) and the satellite observations is over 84%, which indicates ROMS can generally simulate the sea surface temperature in the South China Sea during typhoon process. However, detailed analysis shows that the ROMS model underestimates the sea surface temperature cooling and mixed layer deepening because of insufficient mixing in the modeling. The wave-induced mixing term (Bv) added into the nonlocal K-Profile Parameterization (KPP) scheme can increase the simulation accuracy of surface temperature cooling and mixed layer depth deepening in response to the typhoon forcing. The simulation results show that the blooming of phytoplankton in the wake of storm appeared one week later after typhoon’s passage. The concentration of chlorophyll is 0.1 mg m⁻³ at pre-typhoon time and increase to 1.9 mg m⁻³ on November 9. Satellite Observation indicates the concentration of chlorophyll in wake of typhoon Cimaron was also in a high value of 0.85 mg m⁻³ on November 16.
The eddy heat flux in the SCS is derived from the satellite data including the altimeter surface height anomalies and optimally interpolated sea surface temperature. The long term heat flux shows a northward heat transport on the west side of the SCS, comparable to that in other strong flux regions such as the Kuroshio extension. The eddy flux becomes the strongest in winter with the inflow flux in the south and the outflow through the Luzon, and the eddy heat can flux through the Taiwan Strait into the East China Sea. The convergence of the flux indicates that heat accumulation in the eastern SCS close to Luzon Strait in winter and also to southeast of Vietnam in winter and summer. The eddy heat flux is more significant in adjusting the ocean upper layer heat budget flux in winter and summer.
Detailed summary in vernacular field only.
Detailed summary in vernacular field only.
Detailed summary in vernacular field only.
Detailed summary in vernacular field only.
Sun, Yujuan.
Thesis (Ph.D.)--Chinese University of Hong Kong, 2013.
Includes bibliographical references (leaves 101-111).
Abstracts also in Chinese.
Abstract --- p.ii
摘要 --- p.v
Acknowledgements --- p.vii
Table of Contents --- p.viii
List of Tables --- p.x
List of figures --- p.xi
Chapter 1. --- Introduction --- p.1
Chapter 1.1 --- Ocean responses to typhoons (or tropical storms and hurricanes) --- p.4
Chapter 1.2 --- Eddy Heat Transport --- p.9
Chapter 2. --- The one-dimension remote sensing model (the mixed-layer deepening) --- p.11
Chapter 2.1 --- Introduction --- p.11
Chapter 2.2 --- Data and Methodology --- p.11
Chapter 2.3 --- Results --- p.16
Chapter 2.4 --- One-dimensional mixed-layer model --- p.17
Chapter 2.5 --- Discussions --- p.20
Chapter 2.5.1 --- Horizontal baroclinic pressure gradient and vorticity --- p.20
Chapter 2.5.2 --- Effects of subsurface temperature variation on the mixed-layer deepening --- p.22
Chapter 2.6 --- Summary --- p.28
Chapter 3. --- Three-dimensional numerical ocean model --- p.29
Chapter 3.1 --- Model description --- p.29
Chapter 3.1.1 --- Physical model --- p.30
Chapter 3.1.2 --- Biological model --- p.34
Chapter 3.2 --- Model setting --- p.40
Chapter 3.2.1 --- Initial and lateral boundary conditions --- p.41
Chapter 3.2.3 --- Bio-module setting --- p.47
Chapter 3.3 --- Model result validation --- p.51
Chapter 3.3.1 --- Satellite observations --- p.51
Chapter 3.3.2 --- Validations of observations and simulations --- p.54
Chapter 3.4 --- Model results analysis --- p.56
Chapter 3.4.1 --- Ocean temperature --- p.56
Chapter 3.4.2 --- Ocean current --- p.62
Chapter 3.4.3 --- bio-results of simulation --- p.70
Chapter 3.4.4 --- Effect of the wave-induced mixing --- p.77
Chapter 3.5 --- summary --- p.83
Chapter 4. --- Annual Variations of Horizontal Eddy Heat Flux in the South China Sea --- p.84
Chapter 4.1 --- Introduction --- p.84
Chapter 4.2 --- Methodology and data --- p.86
Chapter 4.3 --- Results --- p.89
Chapter 4.4 --- Summary --- p.96
Chapter 5. --- Conclusion --- p.97
Chapter 6. --- Future work --- p.100
Bibliography --- p.101
Huang, Szu-yu, and 黃思瑜. "Impacts of typhoons and winter monsoons on biogeochemical processes in the northern South China Sea." Thesis, 2014. http://ndltd.ncl.edu.tw/handle/f7y35r.
Повний текст джерела國立中山大學
海洋科學系研究所
102
Both satellite and field observations have shown that extreme weather events (EWEs), such as typhoons and winter storms, enhance chlorophyll a (chl a) concentrations in the South China Sea (SCS). However, detailed hydrographic and particulate organic carbon (POC) flux data are usually hard to obtain because of sampling difficulties on the sea shortly before and after an EWE. To better understand the biogeochemical responses (including concentrations of nutrients, chl a, POC and POC flux) in the SCS to the passage of typhoons and winter storms, hydrographic data were collected during the period of 13 cruises conducted from September 2012 to June 2014 by R/V Ocean Researcher III or V in the northern SCS. Floating sediment traps were used to collect sinking particles at the bottom of the euphotic zone, and the samples collected were used to estimate POC export fluxes. I analyzed seasonal variations in biogeochemical parameters and investigated the effects of typhoons and winter storms on these parameters. The results indicate that POC fluxes did not show distinct seasonal variations, the average POC flux was 48 ± 6 mg-C m−2 d−1 without EWE effects. The POC fluxes after the passage of typhoons Tembin and Soulik, and the passage of several winter storms were 78 ± 12、115 ± 16 and 95 ± 13 mg-C m−2 d−1, respectively. These values were 1.6- to 2.4-fold higher than those obtained without EWE effects. The average surface chl a concentrations in spring, autumn and winter in the northern South China Sea were 0.34, 0.10 and 0.54 μg L−1, respectively. The highest chl a concentration occurred in winter, suggesting that the strong vertical mixing and nutrient entrainment from subsurface water to the euphotic zone induced by strong wind enhance phytoplankton growth. When compared to field chl a data, we found that chl a data obtained by Moderate Resolution Imaging Spectroradiometer (MODIS) exhibited a tendency to underestimate chl a concentrations. In coastal waters, however, the MODIS chl a concentrations were overestimated. The error between field observations and satellite MODIS data may be strongly affected by dissolved organic matter and suspended particles in the water column. Therefore, satellite MODIS chl a data need to be validated using more field data. The results presented in this thesis provide clear evidence that EWEs can trigger elevated organic particle export from the euphotic zone to the deeper ocean in the northern SCS. Regarding the affected area and period (winter storm &;gt; typhoon), a winter storm seems to sequester more carbon in the ocean as compared to a typhoon.
Chen, Peng-Jen, and 陳鵬任. "Diurnal variation of convection over South China Sea region during summer monsoon onset." Thesis, 2016. http://ndltd.ncl.edu.tw/handle/20443866219417607570.
Повний текст джерела國立臺灣大學
大氣科學研究所
104
The South China Sea (SCS) summer monsoon is the bridge between the south Asia and East Asia systems. The better understanding of the evolution of precipitation and cloud patterns during monsoon onset period can help to understand the relationships between convection and environment, as well as the physical mechanisms of the Asian monsoon transition. Precipitation over the SCS exhibits significant diurnal variation during both pre- and post-onset periods. The post-onset southwesterly winds and land-sea breeze enhances the convergence at the low level and generates the convection. To better understand the changes of diurnal variation of convection during monsoon onset period, this study analyzed multiple datasets including the reanalysis data, the TRMM precipitation estimates, and the DARDAR-MASK and 2B-FLXHR-LIDAR cloud products. Climatological statistics for analyzed periods were derived for (1) temporal and spatial distribution of precipitation diurnal cycle, (2) the vertical cloud frequency, cloud types, and size of convection clouds, and (3) the cloud radiative effects. The post-onset precipitation diurnal cycle (DC) exhibits enhanced amplitude and the peak time over ocean becomes more synchronized. After monsoon onset, over the northern SCS, the cloud frequency, number, and size of convective cloud shows a significant increase. The cloud radiative effect becomes stronger. Over the southern SCS, the change in cloud frequency is more significant than the change in rainfall. The number and size of convective cloud both decrease. The present results indicate a change in convection organization after the monsoon onset. Future study can be focused on the investigation of the mechanisms of such organization, including the roles of environmental moisture and vertical wind shear, the interactions between local land-sea breeze and mean wind, and effects of topography.
Hsieh, Wei-Peng, and 謝瑋芃. "Taxonomy of Acrothoracican barnacles in the Western-Pacific and the South China Sea region." Thesis, 2012. http://ndltd.ncl.edu.tw/handle/15167964950278824346.
Повний текст джерела國立臺灣海洋大學
海洋生物研究所
100
Acrothoracican barnacles, also known as the boring barnacles, bores into the marine calcareous structures, including corals, gastropod and hermit crab shells, and the limestone rocks. At present, Kolbasov (2009) indicate acrothoracican barnacles consists of 65 species in 11 genera, three families and two orders of acrothoracican barnacles have been record worldwide. However, almost most of the studies in Acrothoracica were about its taxonomy. There were not many papers about its ecology. Diversity study of acorthoracican barnacles in Western Pacific Region is especially rare. In the past taxonomic studies in Taiwan, only Balanodytes taiwanus was described by Utinomi (1950) in Kaohsiung, and little information was known about the ecology and distribution pattern in Taiwan. This study focus on the identification and taxonomic studies of acrothoracican barnacles in the Western Pacific Region and South China Sea including Taiwan, Hong Kong, Vietnam, Philippines. We found eight genera Balanodytes, Auritoglyptes, Berndtia, Kochlorine, Lithoglyptes, Weltneria, Trypetesa, Cryptophialus and 15 species. 4 new species were identified and with 7 new record for Taiwan.
Valeček, Nikola. "The territorial disputes in the region of South China Sea - case study of selected countries in the region." Master's thesis, 2016. http://www.nusl.cz/ntk/nusl-250967.
Повний текст джерелаChuang, Hsueh-Lung, and 莊學龍. "Spatiotemporal Variation, Chemical Fingerprint, and Source Identification of Atmospheric Fine Particles Long-range Transported toward the Intersectional Region of Taiwan Strait and South China Sea." Thesis, 2016. http://ndltd.ncl.edu.tw/handle/60059408257754927981.
Повний текст джерела國立中山大學
環境工程研究所
104
The deterioration of ambient air quality across the Taiwan strait, including Chinese haze, Asian duststorms and Indochina biomass burning, is highly correlated with industrial emissions, natural soil weathering and swidden agriculture. Under certain meteorological conditions, air pollutants could be blown to the downwind countries/regions and cause poor ambient air quality. Previous literature reported that the northern prevailing winds commonly blow the haze originated from northern China to central and southern China, Taiwan, and even Dongsha Islands. Therefore, the intersectional region of Taiwan Strait and South China Sea is an important air quality monitoring site for long-range transportation. This study selected two PM2.5 sampling sites (i.e. Penghu Islands and Dongsha Islands) located at the intersectional region of Taiwan Strait and South China Sea. Twenty-four hour sampling of PM2.5 was simultaneously collected at Penghu Islands and Dongsha Islands for continuous 14 days in four seasons from summer 2015 to spring 2016. PM2.5 samples were simultaneously collected with BGI-PQ200. After sampling, PM2.5 samples were carried back to the laboratory for conditioning, weighing, and chemical analysis. The chemical composition of PM2.5 including water-soluble ionic species, metallic elements, carbonaceous contents, and anhydrosugar. Moreover, the potential sources of PM2.5 and their contribution were further identified by principal component analysis (PCA) and chemical mass balance (CMB) receptor model. Field sampling results indicated that the spatial distribution of PM2.5 concentration increased from south to north. The lowest seasonal averaged PM2.5 concentrations were observed in summer at both Penghu Islands and Dongsha Islands. PM2.5 concentrations increased gradually since fall, which might be influenced by the northeastern monsoons since air masses could be transported from the north toward Penghu Islands and Dongsha Islands. Air masses blown from South China Sea in summer were much cleaner than those blown from the north in fall, winter, and spring. Chemical analysis results showed that the most abundant water-soluble ionic species of PM2.5 were secondary inorganic aerosols (SIAs) including SO42-, NO3-, and NH4+ which accounted for 50~70% of water-soluble ions (WSIs). The most abundant metallic elements of PM2.5 were crustal elements (Mg, K, Ca, Fe, and Al), while anthropogenic elements (V, Cr, Mn, Ni, As, Cd, and Pb) concentration increased since fall. Organic carbon (OC) was the main species in all seasons, and OC/EC ratios increased during the northeastern monsoon periods. The levoglucosan concentrations in summer and fall were commonly lower than those in winter and spring, showing that PM2.5 concentrations were highly influenced by biomass burning in winter and spring. Correlation analysis results obtained from paired t test showed that the p values of PM2.5 concentration and chemical composition were 0.001 and 0.004, respectively, between two subtropic islands, showing that they had high correlation. In addition to spring, both PM2.5 concentration and chemical composition had high correlation in summer, fall, and winter, because the transportation routes toward these two Islands were not similar in spring. The correlation of PM2.5 concentration for different routes showed that the southern routes were generally lower than the northern routes. Oppositely, the correlation of chemical composition for different routes showed that the northern routes were higher than the southern routes and the southern routes was not correlated, showing that the transportation routes were different toward the two Islands for the southern routes. Results from PCA and CMB receptor modeling showed that major sources of PM2.5 concentrations were at Penghu Islands and Dongsha Islands were sea salts, soil dusts, fuel burning, mobile sources, and secondary aerosols. Since fall, both pollutant sources and their contributions increased, especially for anthropogenic sources including petrochemical plants, steel plants, biomass burning and etc. The contributions of industrial sources (e.g. incinerators, petrochemical, steel, and cement industries) increased almost twice from summer to fall. In winter and spring, biomass burning caused different seasonal trends between Penghu Islands and Dongsha Islands. Levoglucosan concentrations in spring were higher than those in winter at Penghu Islands, while levoglucosan concentrations in winter were higher than those in spring at Dongsha islands, showing that the sources of biomass burning might be different at Penghu Islands and Dongsha Islands. Overall, cross-boundary transport accounted for 28.4~61.0% at Penghu Islands and 36.4~76.8% at Dongsha Islands, respectively, showing that both islands were highly influenced by the cross-boundary transport, especially at Dongsha Islands.
Petrtýl, Martin. "Čína v globální a regionální politice v 21.století - geopolitický střet s Japonskem, Indií, USA, Ruskem a Evropou." Doctoral thesis, 2014. http://www.nusl.cz/ntk/nusl-356368.
Повний текст джерелаКниги з теми "Typhoons South China Sea Region"
China Sea. New York: St. Martin's Press, 2000.
Знайти повний текст джерелаThe survival of empire: Portuguese trade and society in China and the South China Sea, 1630-1754. Cambridge: Cambridge University Press, 1986.
Знайти повний текст джерелаPacific, United States Congress House Committee on Foreign Affairs Subcommittee on Asia and the. Reaffirming the peaceful and collaborative resolution of maritime and jurisdictional disputes in the South China Sea and the East China Sea as provided for by universally recognized principles of international law, and reaffirming the strong support of the United States Government for freedom of navigation and other internationally lawful uses of sea and airspace in the Asia-Pacific region: Markup before the Subcommittee on Asia and the Pacific of the Committee on Foreign Affairs, House of Representatives, One Hundred Thirteenth Congress, second session on H. Res. 714, September 17, 2014. Washington: U.S. Government Printing Office, 2014.
Знайти повний текст джерелаNavy Dept. Bureau of Yards and Docks. Native Woods for Construction Purposes in the South China Sea Region. University Press of the Pacific, 2006.
Знайти повний текст джерелаKeyuan, Zou. 28 The South China Sea. Oxford University Press, 2015. http://dx.doi.org/10.1093/law/9780198715481.003.0028.
Повний текст джерелаWang, QunPeng, ZhengRong Sha, JinShui Zhang, and AnQi Wang. Innovative Research on the Classification of Merchant Ships in the South China Sea of Prevention Typhoons: ???????????????? LONGMAN PRESS LTD, 2022.
Знайти повний текст джерелаElleman, Bruce. China’s Naval Operations in the South China Sea. Renaissance Books, 2017. http://dx.doi.org/10.5117/9781898823674.
Повний текст джерелаSouza, G. B. Survival of Empire: Portuguese Trade and Society in China and the South China Sea 1630-1754. Cambridge University Press, 2009.
Знайти повний текст джерелаSouza, G. B. The Survival of Empire: Portuguese Trade and Society in China and the South China Sea 16301754. Cambridge University Press, 2004.
Знайти повний текст джерелаSouza, G. B. Survival of Empire: Portuguese Trade and Society in China and the South China Sea, 1630-1754. Cambridge University Press, 2011.
Знайти повний текст джерелаЧастини книг з теми "Typhoons South China Sea Region"
Perez-Garcia, Manuel. "Silver, Rogues, and Trade Networks: Sangleyes and Manila Galleons Connecting the Spanish Empire and Qing China." In Palgrave Studies in Comparative Global History, 123–70. Singapore: Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-7865-6_4.
Повний текст джерелаWang, Dawei, Shiguo Wu, Genshun Yao, Fuliang Lü, and Michael Strasser. "Analysis of Quaternary Mass Transport Deposits Based on Seismic Data in Southern Deep-Water Region of Qiongdongnan Basin, South China Sea." In Landslide Science for a Safer Geoenvironment, 575–81. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04996-0_88.
Повний текст джерелаWu, Chunming. "Searching for the Prehistoric Seafaring Craft Between Southeast Coast of China and the Pacific Islands." In The Archaeology of Asia-Pacific Navigation, 161–85. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-4079-7_7.
Повний текст джерелаWu, Chunming. "Searching for the Prehistoric Seafaring Craft Between Southeast Coast of China and the Pacific Islands." In The Archaeology of Asia-Pacific Navigation, 161–85. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-4079-7_7.
Повний текст джерелаWu, Chunming. "The Inheritance of Island Yi and the Acculturation of Maritime Fan in the Han People on Southeast Coast of China." In The Archaeology of Asia-Pacific Navigation, 119–41. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-4079-7_5.
Повний текст джерелаWu, Chunming. "The Inheritance of Island Yi and the Acculturation of Maritime Fan in the Han People on Southeast Coast of China." In The Archaeology of Asia-Pacific Navigation, 119–41. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-4079-7_5.
Повний текст джерелаWu, Zhiyuan, and Mack Conde. "Response of the Coastal Ocean to Tropical Cyclones." In Current Topics in Tropical Cyclone Research. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.90620.
Повний текст джерела"I: THE GEOLOGY AND PHYSIOGRAPHY OF THE REGION." In South China Sea Oil, 7–18. ISEAS Publishing, 1997. http://dx.doi.org/10.1355/9789814376648-003.
Повний текст джерелаZhang, Lei. "Environmental security in the South China Sea region." In The 21st Century Maritime Silk Road, 148–61. Routledge, 2019. http://dx.doi.org/10.4324/9780429058585-10.
Повний текст джерела"8. Energy and Geopolitics in the South China Sea." In Energy Issues in the Asia-Pacific Region, 174–200. ISEAS Publishing, 2010. http://dx.doi.org/10.1355/9789814279291-012.
Повний текст джерелаТези доповідей конференцій з теми "Typhoons South China Sea Region"
Botao, Xie, Ren Xuhe, Li Jiagang, and Huang Bigui. "The Application of Extreme Value Calculation Model Based on Deductive Method in South China Sea." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-78335.
Повний текст джерелаLi, Lixiao, Ahsan Kareem, Yiqing Xiao, Lili Song, and Peng Qin. "Wind Profile and Spectra in Typhoon-Prone Regions in South China." In ATC & SEI Conference on Advances in Hurricane Engineering 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412626.081.
Повний текст джерелаXie, Botao, Xuhe Ren, Jiagang Li, Wenyang Duan, Junrong Wang, and Binbin Zhao. "Study on Gust Parameters and Wind Spectrum of South China Sea." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95779.
Повний текст джерелаShang, Jihong, Jiabiao Li, and Fanlin Yang. "Study of Tectonic Evolutionary History in Region of Northeast South China Sea." In OCEANS 2007 - Europe. IEEE, 2007. http://dx.doi.org/10.1109/oceanse.2007.4302229.
Повний текст джерелаLi, Ya. "Fundamental Engineering Characteristics of Cohesive Sediments in the Northern Region of South China Sea." In IFCEE 2018. Reston, VA: American Society of Civil Engineers, 2018. http://dx.doi.org/10.1061/9780784481639.013.
Повний текст джерелаLi, Shuzhao, Xu Jia, Zhigang Li, and Jiagang Li. "Fundamental Engineering Characteristics of Cohesive Sediments in the Northern Region of South China Sea." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-96599.
Повний текст джерелаYang, Qiulong, Kunde Yang, Chunlong Huang, Hong Liu, and Ying Zhang. "Seasonal statistics of experimental oceanic noise observed in the deep region of the South China Sea." In Global Oceans 2020: Singapore - U.S. Gulf Coast. IEEE, 2020. http://dx.doi.org/10.1109/ieeeconf38699.2020.9389115.
Повний текст джерелаDeng, Tianan, Huan-Feng Duan, Jinghua Wang, and Alireza Keramat. "Spatio-temporal analysis of wave energy capacity in the Northern South China Sea Region using the SWAN model." In Proceedings of the 39th IAHR World Congress From Snow to Sea. Spain: International Association for Hydro-Environment Engineering and Research (IAHR), 2022. http://dx.doi.org/10.3850/iahr-39wc252171192022684.
Повний текст джерелаWu, Qingsong, and Xiao-Hua Zhu. "Determination of temperature profile from an acoustic method in the region northeast of the South China Sea." In 2011 4th International Congress on Image and Signal Processing (CISP). IEEE, 2011. http://dx.doi.org/10.1109/cisp.2011.6100768.
Повний текст джерелаTung, Aaron, and Claus Otto. "Lessons Learnt from Ospar and the North Sea: The Importance of Establishing a Regional Decommissioning Agreement in the South China Sea Region." In SPE Symposium: Decommissioning and Abandonment. Society of Petroleum Engineers, 2019. http://dx.doi.org/10.2118/199207-ms.
Повний текст джерелаЗвіти організацій з теми "Typhoons South China Sea Region"
St. Laurent, Louis. Internal Wave Generation Processes at Deep-Sills in the Luzon Passage Region of the South China Sea. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada590524.
Повний текст джерелаMiller, Mark S. Maintaining Peace in the South China Sea and the Spratly Islands: Are there Acceptable Alternatives to the US Naval Forces Forward Deployed in the Asia Pacific Region? Fort Belvoir, VA: Defense Technical Information Center, April 2002. http://dx.doi.org/10.21236/ada401689.
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