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Academic literature on the topic 'South Red Sea'

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Published: 9 March 2023
Last updated: 10 March 2023

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Journal articles on the topic "South Red Sea"

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Abdelmoaty, Samir. "Workshop explores Red Sea region." Leading Edge 38, no. 5 (May 2019): 400–401. http://dx.doi.org/10.1190/tle38050400.1.

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When you select the right subject to be discussed by the right experts in the right place, you will get fantastic results. That is what the SEG Middle East Advisory Committee has done by forming an outstanding Technical Committee chaired by Maurice Nessim, president of WesternGeco, and Mohamed Abdel Azim, chairman of the South Valley Egyptian Petroleum Holding Company (GANOPE).
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Tsvieli, Y., and A. Zangvil. "Synoptic climatological analysis of Red Sea Trough and non-Red Sea Trough rain situations over Israel." Advances in Geosciences 12 (October 15, 2007): 137–43. http://dx.doi.org/10.5194/adgeo-12-137-2007.

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Abstract. Winter (October to April) rainfall in Israel is caused mostly by migrating Mediterranean cyclones but certain rain situations are accompanied by a low pressure trough extending northward from the southern Red Sea towards the Eastern Mediterranean (EM) and the Levant. This system, the Red Sea Trough (RST) is one of the most frequent surface atmospheric circulation patterns over the southeastern Mediterranean, but most of the RSTs are not accompanied by rain. This paper presents a synoptic climatological comparative analysis between rain situations associated with RSTs, and those not connected with RSTs (non-RST rain, NRR). The RST situations were identified objectively with the aid of a new algorithm applied to the GEOS-1 reanalysis gridded data set from NASA, for the period of March 1985–November 1995. Results show that RST rain is accompanied by a relatively narrow 500-hPa trough, located west of the Israeli coast-line and characterized by a deep southward penetration, while Non-RST-associated rain (NRR) is accompanied by a wider upper trough, located over the Israeli coast-line with a shallower southward penetration. We found a south-southwesterly wind vector anomaly at 200 hPa over Israel during RST rains, while during NRRs a similar wind vector anomaly pattern is observed east of Israel. There is a divergence center over, or a few degrees east of Israel during RST rains, while NRR is associated with a divergence value of nearly zero over Israel and a maximum divergence center located east of Israel. The moisture flux during NRR at 700 and 900 hPa is from the Mediterranean, while during RST rain there is a south-westerly moisture flux at 700 hPa from equatorial Africa to Israel and vicinity. A steeper temperature lapse-rate between 950–500 hPa was found during RST rain compared with NRR, resulting from a combination of cooling aloft together with heating near the surface.
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Wang, YingMin, Qiang Xu, Dong Li, JianHui Han, Ming Lü, YongFeng Wang, WeiGuo Li, and HaiRong Wang. "Late Miocene Red River submarine fan, northwestern South China Sea." Chinese Science Bulletin 56, no. 14 (May 2011): 1488–94. http://dx.doi.org/10.1007/s11434-011-4441-z.

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Righton, David, Jeremy Kemp, and Rupert Ormond. "Biogeography, Community Structure and Diversity of Red Sea and Western Indian Ocean Butterflyfishes." Journal of the Marine Biological Association of the United Kingdom 76, no. 1 (February 1996): 223–28. http://dx.doi.org/10.1017/s0025315400029167.

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Patterns of variation in the assemblage structure of butterflyfishes (Chaetodontidae) of the Red Sea and western Indian Ocean have been compared. There is a lower number of species in the Red Sea, a high proportion of which are endemic to the region, both features that have been attributed to the relatively recent origin of the Red Sea. In the Red Sea overall mean abundance of butterflyfish is greatest in the central part, decreasing both to north and south. Several species present in the southern Red Sea are absent from the north. By contrast, most western Indian Ocean species are widely distributed within the Indo-West Pacific. Comparative field studies in the northern Red Sea (Egypt) and western Indian Ocean (Kenya) showed that mean number of species was higher in the western Indian Ocean, but mean density of butterflyfishes was higher in the Red Sea. In both areas diversity of butterflyfish was related to mean substrate diversity (the number of coral growth forms). Mean spatial niche breadth of butterflyfish species was much higher in the Red Sea than in the western Indian Ocean, whereas the extent of microhabitat use was higher in the western Indian Ocean. It is suggested that these differences may be related to the more recent evolution of the Red Sea fauna.
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Abdulla, Cheriyeri P., Mohammed A. Alsaafani, Turki M. Alraddadi, and Alaa M. Albarakati. "Mixed layer depth variability in the Red Sea." Ocean Science 14, no. 4 (July 2, 2018): 563–73. http://dx.doi.org/10.5194/os-14-563-2018.

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Abstract. For the first time, a monthly climatology of mixed layer depth (MLD) in the Red Sea has been derived based on temperature profiles. The general pattern of MLD variability is clearly visible in the Red Sea, with deep MLDs during winter and shallow MLDs during summer. Transitional MLDs have been found during the spring and fall. The northern end of the Red Sea experienced deeper mixing and a higher MLD associated with the winter cooling of the high-saline surface waters. Further, the region north of 19° N experienced deep mixed layers, regardless of the season. Wind stress plays a major role in the MLD variability of the southern Red Sea, while net heat flux and evaporation are the dominating factors in the central and northern Red Sea regions. Ocean eddies and Tokar Gap winds significantly alter the MLD structure in the Red Sea. The dynamics associated with the Tokar Gap winds leads to a difference of more than 20 m in the average MLD between the north and south of the Tokar axis.
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Melnikova, Elena, and Natalya Kuzminova. "Influence of Abiotic Environmental Factors on the Growth Rate of Red Mullet." Croatian Journal of Fisheries 80, no. 2 (June 1, 2022): 87–95. http://dx.doi.org/10.2478/cjf-2022-0009.

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Abstract A study of the interannual variability of the size-age composition of M. barbatus ponticus, inhabiting the south-western shelf of the Crimea, was carried out over a five-year period (between 2016 and 2020). The influence of habitat temperature on growth rate is considered. Equations obtained characterize the size-weight growth of M. barbatus ponticus. The influence of the sea temperature on the development of individuals is considered. It is shown that with an increase in the average annual water temperature, the average annual length (correlation coefficient r = 0.97), weight (r = 0.96) and condition factor (r = 0.93) of individuals increase. It was found that red mullet has a positive allometric growth in the study area. The analysis showed that there was a close correlation between changes in the average annual temperature and the allometric growth rate b (r = 0.97). The equations of length growth of M. barbatus ponticus showed retarded linear growth of the fish living on the south-western shelf of the Crimea in comparison with other areas, Sinop region (Black Sea) and the Aegean Sea. The comparison of the effect of temperature on the size and weight parameters of M. barbatus ponticus living in the south-eastern part of the Black Sea (Sinop region) and the Aegean Sea is carried out; general patterns and differences are noted.
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EL-SHATER, A., and M. ABOU-AUF. "Beachrock in South Jeddah, The Red Sea Coast of Saudi Arabia." Journal of King Abdulaziz University-Marine Sciences 6, no. 1 (1995): 53–65. http://dx.doi.org/10.4197/mar.6-1.5.

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Abdulla, Cheriyeri P., and Abdullah M. Al-Subhi. "Is the Red Sea Sea-Level Rising at a Faster Rate than the Global Average? An Analysis Based on Satellite Altimetry Data." Remote Sensing 13, no. 17 (September 2, 2021): 3489. http://dx.doi.org/10.3390/rs13173489.

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Satellite altimetry sea-level data was taken for nearly three decades (1993–2020) and is used to understand the variability and associated dynamics in the Red Sea sea-level. Seasonally, the sea-level is higher during December–January and lower during August, with a consistent pattern from south to north. The interannual fluctuations in sea-level have a close agreement with the variability in the global climate modes, i.e., El-Nino Southern Oscillation events, East Atlantic-West Russian oscillation, and the Indian Ocean Dipole. The impact of the El-Nino Southern Oscillation mode on sea-level is higher than other climate modes. The Red Sea sea-level was seen to rise at a rate of 3.88 mm/year from 1993–present, which was consistent with the global rate of 3.3 ± 0.5 mm/year. However, a noticeably faster rate of 6.40 mm/year was observed in the Red Sea sea-level from 2000-present.
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Bland, Robert D. "“A GRIM MEMORIAL OF ITS THOROUGH WORK OF DEVASTATION AND DESOLATION”: RACE AND MEMORY IN THE AFTERMATH OF THE 1893 SEA ISLAND STORM." Journal of the Gilded Age and Progressive Era 17, no. 2 (April 2018): 297–316. http://dx.doi.org/10.1017/s1537781417000846.

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“‘A Grim Memorial of Its Thorough Work of Devastation and Desolation’: Race and Memory in the Aftermath of the 1893 Sea Island Storm” explores the political struggle that ensued in the aftermath of the August 1893 hurricane. The storm, which decimated the predominantly African American South Carolina Sea Islands, required a nine-month relief effort to assist the region's citizens in their time of need. Led by the American Red Cross, the relief effort became a new proxy for a long-standing debate over the legacy of Reconstruction and the meaning of black citizenship. This battle, waged by leaders in South Carolina's Democratic Party, Red Cross officials, writers in the national press, former abolitionists, and African Americans living in the South Carolina Sea Islands, exposed growing fissures in how Americans understood notions of charity and self-help. More than a battleground for still-nascent ideas of disaster relief, the political turmoil that followed the 1893 Sea Island Storm played a critical role in redefining the racial boundaries of the United States on the eve of the Jim Crow era.
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Yokkaichi, Yasuhiro. "The Maritime and Continental Networks of Kīsh Merchants under Mongol Rule: The Role of the Indian Ocean, Fārs and Iraq." Journal of the Economic and Social History of the Orient 62, no. 2-3 (March 18, 2019): 428–63. http://dx.doi.org/10.1163/15685209-12341484.

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AbstractBased on a variety of literary and archaeological sources, notably the tariff lists produced in Rasulid Yemen, this study reconstructs the trade routes of the Kīsh merchants, demonstrating that the Persian Gulf route—between South and West India (Coromandel, Malabar, and Gujarat) and Iraq via the Persian Gulf—and the Red Sea route—between South and West India and Egypt via the Red Sea—were closely connected in the Mongol period. This not only manifests aspects of the proto-globalization in Mongol Eurasia but also argues against the supposed economic decline of post-1258 Baghdad and the economic centrality of Cairo in the post-Abbasid Muslim world.
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Dissertations / Theses on the topic "South Red Sea"

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Durrani, Nadia. "The Tihamah coastal plain of South West Arabia in its regional context : c. 6000 BC - AD 600." Thesis, University College London (University of London), 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.368203.

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Bowman, Emilie Elisabeth. "North-south variations in structure, topography, and melting regime along the ultra-slow spreading Red Sea Ridge." Thesis, Massachusetts Institute of Technology, 2019. https://hdl.handle.net/1721.1/122237.

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Thesis: S.M. in Geology, Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2019
Cataloged from PDF version of thesis.
Includes bibliographical references (pages 88-98).
The Red Sea rift is a nascent ultra-slow spreading ridge superimposed on the Afar plume. Based on high-resolution seismic data, the southernmost (south of the Danakil rift at 17.05°N), southern (17.05-19.75°N), and central (19.75-23.8°N) segments display seafloor spreading that is anomalously magma-rich compared to other ultra-slow spreading centers. In contrast, the northern segment (23.8-28°N) exhibits magma-poor extension along large-offset east- and west-dipping detachments. Sediment-corrected basement depths along the northern Red Sea reveal an axial valley as deep as the Gakkel Ridge (4200-5100 m). South of 19.75°N, plume-supported axial shoaling matches that of adjacent parts of Arabia, Africa, and the Gulf of Aden. Geochemically, the southernmost Red Sea is the locus of plume-ridge interaction. Here, E-MORBs are enriched in alkali, incompatible, and light rare-earth elements.
High mantle potential temperatures (T[subscript p]; 1326±5°C), melting pressures (12±0 kbars) and temperatures (1306±6°C), and fractionation pressures (5.3±1.6 kbars) calculated using the reverse fractional crystallization model of Brown (2019) suggest thickened oceanic crust created by high-degree partial melting of a plume-like source. North of the Danakil rift, T[subscript p] (1307± 11°C) spans a narrow range and is within the range of ambient mantle. The southern Red Sea contains N- to E-MORB depleted in alkali, incompatible, and light rare-earth elements indicating limited mixing with Afar plume material, while the central segment is host to the most depleted magmas along the ridge (La/Sm[subscript N] < 0.8). Within the southern and central regions, fractionation pressures (2.0±1.2 and 4.8±2.1 kbars, respectively) indicate lithosphere (5-15 km) thinner than that of normal ultra-slow spreading ridges (15-35 km).
In the northern Red Sea, high Na₈ and deep pressures of melting (10.4±1.4 kbars) suggest thickened lithosphere, undulations in which induce melt focusing into volcanic deeps. Based on these results, we propose that the Red Sea south of at least 26.5°N is an oceanic spreading center. We find that anomalously magma-rich spreading in the central and southern segments cannot be related to the Afar plume. Instead, the Danakil rift diverts plume-related mantle flow northeast beneath Arabia. Thus, the southern and central Red Sea must be characterized by vigorous mantle upwelling that causes heightened melt production and lithospheric thinning.
by Emilie Elisabeth Bowman.
S.M. in Geology
S.M.inGeology Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences
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Zhu, Mangzheng. "Offshore Red River fault and slope sediments in northern South China Sea : implications for paleoceanography and uplift of the tibet plateau /." May be available electronically:, 2007. http://proquest.umi.com/login?COPT=REJTPTU1MTUmSU5UPTAmVkVSPTI=&clientId=12498.

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CARAGNANO, ANNALISA. "Lithopyllum spp. as proxy of climate variability in the nw indian ocean." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2013. http://hdl.handle.net/10281/41553.

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A previously unexplored subfamily of coralline algae, the Lithophylloideae, was investigated as potential paleoclimatic archive. For the first time, seasonal changes in Mg/Ca, Li/Ca and Ba/Ca composition of Lithophyllum spp. from the Gulf of Aden (Balhaf, Yemen), the Arabian Sea (Socotra, Yemen), and the South of Red Sea (Kamaran, Yemen) were investigated by Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS). For the first time in coralline algae, the Li/Ca composition was analyzed and showed a highly significant and positive correlation with Mg/Ca and SST. Monthly algal Mg/Ca and Li/Ca variations indicate a positive correlation with sea water temperature (SST). Although no correlation between monthly algal Ba/Ca and local (SST) was found, fluctuations in Ba/Ca indicate the influence of nutrients introduced by seasonal upwelling, and record an increase of sediment at the sampling sites. From the age model of Mg/Ca the annual algal extension rates were measured in all specimens of Lithophyllum spp., and they resulted highly variable, mainly influenced by light and occasional burial. The elementary ratio of Mg/Ca, Li/Ca and Ba/Ca, and annual extension rate were successfully used in historical reconstruction of the climate and oceanographic variability of the study area.
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Aqili, Ahmed. "L'information télévisée et la géopolitique de l'Arabie saoudite : le cas particulier des informations diffusées par la chaîne publique Al Saudiya entre 1989 et 2000 concernant les pays du sud de la mer Rouge (Djibouti, l’Érythrée, la Somalie et le Yémen)." Thesis, Paris 2, 2019. http://www.theses.fr/2019PA020080.

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L’objectif de cette recherche est de mettre en évidence la manière dont les médias d'information de l’Arabie saoudite participent au rayonnement du Royaume dans la région du Sud de la mer Rouge et dans le monde. L’efficacité politique, économique et culturelle du pays repose sur une combinaison intelligente, le smart power selon Joseph Nye, qui allie le hard power, la richesse économique due au pétrole et le soft power (la puissance douce), c’est-à-dire la richesse culturelle et l’influence dans les relations internationales. Dans ce sens, notre recherche a essayé d’identifier les dimensions de ce soft power dans le discours des médias publics en Arabie saoudite, en particulier dans celui de la première chaîne nationale saoudienne Al Saudiya (anciennement Aloula), en se concentrant sur l’analyse des informations diffusées pour couvrir les événements et les actions politiques, économiques, culturelles et humanitaires dans la région du sud de la mer Rouge. La complexité de notre recherche a nécessité de multiples approches. L’investigation empirique s’est appuyée sur des approches d’analyse récentes appliquées au domaine de l’information et de la communication, appelée analyse de contenu médiatique, qui a récemment fait l’objet de grands développements et a connu de nombreuses améliorations méthodologiques.Les résultats de cette thèse montrent que la première chaîne publique a intégré la religion dans son message médiatique, non seulement pour renforcer la position et la place de l’Arabie saoudite comme détenteur des lieux saints de l’islam, la Mecque et Médine, mais aussi pour représenter le monde arabo-musulman dans les relations internationales
The purpose of this research is to highlight how the Saudi Arabian news media are contributing to the Kingdom's outreach in the Southern Red Sea region and around the world. The political, economic and cultural efficiency of the country is based on a smart combination, Nye's smart power, which combines hard power, economic wealth due to oil and soft power, that is, to say cultural wealth and influence in international relations. In this sense, our research has tried to identify the dimensions of this soft power in the public media discourse in Saudi Arabia, especially in that of the first Saudi national channel Al Saudiya (formerly Aloula), focusing on the analysis information disseminated to cover political, economic, cultural and humanitarian events and actions in the Southern Red Sea region.The complexity of our research required multiple approaches. The empirical investigation has relied on recent analytical approaches applied to the field of information and communication, called media content analysis, which has recently undergone major developments and has undergone many methodological improvements. The results of this thesis show that the first public channel incorporated religion into its media message, not only to strengthen the position and place of Saudi Arabia as the holder of the holy places of Islam, Mecca and Medina, but also to represent the Arab-Muslim world in international relations
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Hozumi, Aya. "Environmental Factors Affecting the Whale Shark Aggregation site in the South Central Red Sea." Diss., 2015. http://hdl.handle.net/10754/583276.

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Motivation behind the spring whale shark (Rhincodon typus) aggregation in Al-Lith, on the Saudi Arabian coast of the South Central Red Sea, is uncertain. A plausible hypothesis is that whale sharks gather to feed on high prey density, leading to questions about the cause of the prey density. A bottom-up process fueled by nutrient input or accumulation from physical advection could create a peak in prey biomass. Wastewater discharged from an aquaculture facility could affect productivity or provide a chemosensory cue for whale sharks. Yet, basic physico-biological oceanography of this region is unresolved. Monthly profiles, long-term moorings, and spatial surveys were used to describe the temporal variability of potential prey biomass and water masses in this region for the first time. Plankton abundance of individuals larger than ~0.7 cm did not peak during whale shark season. Rather, a decrease coinciding the trailing end of whale shark detections was observed. Sites 180 m apart had differences in acoustic backscatter, suggesting small-scale biomass patchiness, supporting the small-scale variability in whale shark habitat selectivity. Red Sea Deep Water, a nutrient-rich water mass formed in the northern Red Sea, appeared in July at the same time the Tokar wind jet from the Sudanese mountain gap is the highest. Gulf of Aden Water, a nutrient-rich water mass from the Indian Ocean, arrived as episodes from May to September, contrary to previous expectations that the water arrives continuously. It is unlikely that these natural nutrient sources are directly responsible for the high prey density attracting the whale sharks. The aquaculture plume, observed at the aggregation site, had a distinct seasonality from the ambient waters. The plume’s highest salinity (>48) approached the extreme limits of coral tolerances. Nutrient concentrations (nitrate, nitrite, phosphate, silica), suspended particulate matter, phytoplankton biomass, bacteria and cyanobacteria cell counts, total nitrogen, and relative abundance of genera associated with opportunistic pathogenic species (e.g., Arcobacter) were significantly higher in the plume. This study was the first to estimate the nutrient flux and spatial variability of the aquaculture plume.
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Wei-LanLiao and 廖韋嵐. "Authigenic and Detrital REE, Sr and Nd Isotopes in the South China Sea Sediments: Implications of Paleoclimatic Change During the Past 32 ka." Thesis, 2012. http://ndltd.ncl.edu.tw/handle/27161725727318869876.

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碩士
國立成功大學
地球科學系碩博士班
100
South China Sea (SCS) as the marginal sea is, via river sediment discharges, the major source of a number of elements to the ocean. Thus, SCS plays a role of a source and/or a sink of elements for the ocean. Water mass circulation in the SCS has been widely studied; however information of the margin/ocean interactions and their influence on the oceanic isotopic chemistry is still sparse. Here, we present the REE concentrations, Nd and Sr isotopic data in Fe-Mn oxyhydroxides (authigenic phase) and detrital phase of the core MD05-2901, which developed during the last 32 ka. Moreover, 87Sr/86Sr and εNd analysis of sediments were combined to trace the elemental sources, and to evaluate the relative proportions of different end-members. All of the authigenic phases yielded 87Sr/86Sr values varying from 0.709262 and 0.709313 that are offset from the seawater value of 0.70918, which suggested that some detrital contamination involved in Core MD05-2901. The εNd values in authigenic and detrital phases vary with the abrupt climatic events. During the Bølling/Allerød period, εNd value was as low as -12.10 and -9.6 in detrital and authigenic phases, respectively. In contrast, the εNd value becomes slightly high (-10.28 and -6.3 in detrital and authigenic phases, respectively) during the Younger Dryas event. The paleoclimatic changes affect sediment transport pathways to SCS have been further clarified.
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Mduma, Regina Mshinwa. "Admiralty jurisdiction and party autonomy in the marine insurance practice in South Africa / Regina Mshinwa Mduma." Thesis, 2013. http://hdl.handle.net/10394/11847.

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An increase in international trade has resulted in an increase in the carriage of goods by sea, which has also promoted the business of marine insurance on a very huge scale. Marine insurance contracts fall within both the admiralty jurisdiction where admiralty laws apply and special contract law where the rules and principles of contract law apply. In certain circumstance this has left the courts with a dilemma in deciding in particular cases which law should apply; whether maritime law, contract law or marine insurance law. There are certain principles under the law of contract that are said to be profound and cannot be ousted easily by substantive law. The principle of party autonomy is one of these principles and it has gained international recognition through a number of cases. However, to date, courts are faced with difficulties in deciding whether to uphold the choice of law on jurisdiction and governing law exercised by parties or resort to substantive law, either by virtue of admiralty law or any other statutes in a country, which provisions may be contrary to the clause on choice of law under the contract. In South Africa practice has shown that courts are always reluctant to apply the clause on choice of law if they believe such application is against the public policy and interest in South Africa. This begs the question as to the precise meaning and effect of “public policy and interest” and how this principle influences the long-standing and well-established principle of party autonomy in admiralty jurisdiction. This dissertation is aimed at providing a legal response to this problem by analysing case law and the different viewpoints of various writers. It is imperative to investigate if their decisions and views answer all the uncertainties with regard to the meaning and the effect of the concept of “public policy and interest” on the principle of party autonomy.
LLM (Import and Export Law), North-West University, Potchefstroom Campus, 2014
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Books on the topic "South Red Sea"

1

Lieske, Ewald. Coral reef guide: Red Sea to Gulf of Aden, South Oman. London: HarperCollins, 2004.

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Office, Great Britain Hydrographic, ed. Red Sea and Gulf of Aden pilot: Suez Canal, Gulf of Suez and Gulf of ʻAqaba, Red Sea, Gulf of Aden, south-east coast of Arabia -- Raʻs Fartak to Raʻs al Junayz, coast of Africa -- Raas Caseyr to Raas Binna, Suquţrá and adjacent islands. [Taunton, Somerset]: United Kingdom Hydrographic Office, 2007.

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Office, Great Britain Hydrographic, ed. Red Sea and Gulf of Aden Pilot: Suez Canal, Gulf of Suez and Gulf of ʻAqaba, Red Sea, Gulf of Aden, south-east coast of Arabia from Raʼs Bā Ghashwah to Raʼs al Junayz, coast of Africa from Raas Caseyr to Raas Binna, Suquțrá and adjacent islands. Taunton, Somerset [England]: United Kingdom Hydrographic Office, 2002.

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Great Britain. Hydrographic Dept., ed. Red Sea and Gulf of Aden pilot: Suez Canal, Gulf of Suez and Gulf of ʻAqaba, Red Sea, Gulf of Aden, south-east coast of Arabia from Raʼs Bā Ghashwah to Raʼs Junayz, coast of Africa from Raas Caseyr to Raas Binna, Suquțrá and adjacent islands. [London]: Hydrographer of the Navy, 1987.

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De me tre s G. Letsios. Vyzantio kai Erythra Thalassa: Scheseis me te Nouvia, Aithiopia kai Notia Aravia o s te n Aravike katakte se = Byzantium and the Red Sea : relations with Nubia, Ethiopia and South Arabia until the Arab conquest. Athe na: Istorikes Ekd.Vasilopoulos, 1988.

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Blanchette, Jude. China's New Red Guards. Oxford University PressNew York, 2022. http://dx.doi.org/10.1093/oso/9780197577554.001.0001.

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Abstract China’s New Red Guards details two worrying trends in contemporary China that point to the revival of Maoism. First, an increasingly popular hard-edged form of nationalism that is reflexively anti-Western has taken root. The second is an unapologetic embrace of extreme authoritarianism that draws inspiration from the Maoist era. China’s assertive stance in the South China Sea and anti-Japanese rhetoric represents the former, and the massive crackdown on liberal thought since Xi Jinping assumed the presidency represents the latter. The result is plain to see: a more authoritarian and more militaristic China. The book goes further than this, though, arguing that what we’re seeing is a full-fledged Maoist revival. The book centers its story around a cast of nationalist intellectuals and activists who have helped unleash a wave of populist enthusiasm and nostalgia for the Great Helmsman’s policies. That, combined with Xi’s quick implementation of a range of authoritarian policies, suggests that the Maoist revival is neither epiphenomenal nor a passing fad. The ramifications, the book suggests, are clear: those in the West who have been predicting waves of democratization and liberalization are living in a dream world, blithely unaware of either the Communist Party’s commitment to authoritarianism or the degree of its residual veneration for the CCP’s founding leaders. In sum, this book demonstrates how ideologies can survive and prosper despite pervasive rumors of their demise.
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Admiralty distance tables, Indian Ocean: Covering Indian Ocean and part of the Southern Ocean from South Africa to New Zealand, Red Sea, Persian Gulf, Malay Archipelago. 3rd ed. [Taunton, England]: United Kingdom Hydrographic Office, 2008.

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Admiralty distance tables, Indian Ocean: Covering Indian Ocean and part of the Southern Ocean from South Africa to New Zealand, Red Sea, Persian Gulf, Malay Archipelago. 2nd ed. [Taunton, England]: United Kingdom Hydrographic Office, 2007.

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Toponymy on the Periphery: Placenames of the Eastern Desert, Red Sea, and South Sinai in Egyptian Documents from the Early Dynastic until the End of the New Kingdom. BRILL, 2020.

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London, Jack. South Sea Tales: Must Read Classics. Independently Published, 2022.

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Book chapters on the topic "South Red Sea"

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Sakellariou, Dimitris, Grigoris Rousakis, Ioannis Panagiotopoulos, Ioannis Morfis, and Geoff N. Bailey. "Geological Structure and Late Quaternary Geomorphological Evolution of the Farasan Islands Continental Shelf, South Red Sea, SW Saudi Arabia." In Geological Setting, Palaeoenvironment and Archaeology of the Red Sea, 629–52. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99408-6_28.

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Mohriak, Webster. "Rifting and Salt Deposition on Continental Margins: Differences and Similarities Between the Red Sea and the South Atlantic Sedimentary Basins." In Geological Setting, Palaeoenvironment and Archaeology of the Red Sea, 159–201. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99408-6_8.

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Chazot, G., M. A. Menzies, and J. Baker. "Pre-, syn- and post-rift volcanism on the south-western margin of the Arabian plate." In Sedimentation and Tectonics in Rift Basins Red Sea:- Gulf of Aden, 50–55. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-4930-3_4.

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Ibrahim, Tarek, Gouda Dabour, Minghua Ren, Gad El-Qady, Philip Goodell, Ibrahim Gaafar, Luis Sandoval, and Munazzam Ali. "Potential Heavy Mineral-Enriched Black Sand Deposits South Ras Banas Red Sea Coast (Egypt)." In Petrogenesis and Exploration of the Earth’s Interior, 129–32. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01575-6_31.

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Perrin, C., J. C. Plaziat, and B. R. Rosen. "Miocene coral reefs and reef corals of the south-western Gulf of Suez and north-western Red Sea: distribution, diversity and regional environmental controls." In Sedimentation and Tectonics in Rift Basins Red Sea:- Gulf of Aden, 296–319. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-4930-3_17.

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"Red Sea, Arabian Sea, South China Sea: The Maritime Silk Road." In A World History of the Seas. Bloomsbury Academic, 2021. http://dx.doi.org/10.5040/9781350269064.ch-3.

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De Romanis, Federico. "Epilogue." In The Indo-Roman Pepper Trade and the Muziris Papyrus, 321–24. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198842347.003.0018.

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The epilogue summarizes what the two texts of the Muziris papyrus tell us about the pepper and ivory production of the ancient Cēra kingdom, South Indian commercial connections with the Ganges Valley, the logistics of the Red Sea–Alexandria transports, the complex relationships between the South India traders and the contractors of the Red Sea tax, and the assessment and payment of the import and export customs duties. It also looks at what the two texts do not mention—the part of pearls and precious stones in the South India trade of the mid-second century ad. Furthermore, a speculative estimate of the commercial venture final balance is attempted.
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Rijsdijk, Ian-Malcolm. "Between Sherwood Forest and the Red Sea: Settler Colonial South Africa in early Hollywood." In Cinematic Settlers, 189–202. Routledge, 2020. http://dx.doi.org/10.4324/9781003057277-15.

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Emery, K. O., and David Neev. "General Geology." In The Destruction of Sodom, Gomorrah, and Jericho. Oxford University Press, 1995. http://dx.doi.org/10.1093/oso/9780195090949.003.0005.

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The Dead Sea occupies a linear down-dropped region between two roughly parallel faults along the central segment of the major northsouth- trending crustal rift that extends about 1,100 km from the Red Sea through the Gulf of Elath to Turkey. This rift or geosuture separates the Arabian crustal sub-plate on the east from the Sinai one on the west. An origin as early as Precambrian is possible (Bender, 1974; Zilberfarb, 1978). Crystalline crust along the north-south trough of the Sinai sub-plate is about 40 km thick in contrast with a thickness of half as much above ridges along both flanks (Ginsburg and Gvirtzman, 1979). Toward the north the ridges appear to converge (Neev, Greenfield, and Hall, 1985). Since the Miocene period the Arabian plate has moved north about 105 km relative to the Sinai plate. This sort of crustal movement along either side of a rift is termed strike-slip faulting. One result of it was the opening of the Red Sea relative to the Gulf of Suez. The Dead Sea graben, a down-dropped block between two roughly parallel faults, occupies the central segment of the long crustal rift. The boundary between these is rather sharp along the east shore of the sea (Frieslander and Ben-Avraham, 1989). Actual post-Miocene movement was along not just a single major fault but was distributed among numerous sub-parallel faults that form a 100-km-wide belt in which movements were transferred from one fault to another (Eyal et al., 1981; Gilat and Honigstein, 1981). Recent movements have occurred along the south segment of the north-south-trending Arava fault south of the Amazyahu transverse fault (Zak and Freund, 1966). These strike-slip movements probably did not continue after Miocene along the main East fault of the Dead Sea, which is the north extension of the Arava wrench fault. In contrast, recent movements have been present along the north-northeast- trending Jordan or Dead Sea fault (Ben-Menahem et al., 1977, fig. 1). The movements extend south from east of Jericho in the north along the base of the west submarine slope of the sea and the elongate salt diapir of Mount Sedom as far as the Amazyahu fault in the south.
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Thomson, Peter. "The Great Circle." In Sacred Sea. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195170511.003.0019.

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The Port of San Francisco, once one of the world’s most celebrated ports of call, has been reduced to this: a quarter-mile of bare, worn asphalt between a chain link fence and the bay, a couple dozen oblong cargo containers stacked like a set of playroom blocks, and one huge gray cargo crane that looms over the water like the skeleton of some Stanford student’s monstrous robotic dog. A few miles to the north, the Embarcadero and its ripsaw ridge of angled piers, once the pulsing heart of the city’s commercial port, is today a palm-tree-lined recreational waterfront of restaurants, bars, condos, and t-shirt vendors, while here to the south of downtown, huge swaths of abandoned waterfront lie fallow, awaiting the next wave of redevelopment. The San Francisco Bay itself remains a major Pacific port, but virtually all of its cargo traffic now moves through the modern container terminals of Oakland, across the bay. In the city of San Francisco itself, there remains only a single active cargo pier, and this is it. Pier 80. Lashed to the far side of the sea of asphalt is a ship, of modest size by contemporary standards but its sheer bulk impressive nonetheless—a hulking mass of emerald green steel looming three stories above the tarmac, a pale yellow superstructure rising eight stories above that in the stern, and a wall of red and blue containers stacked six high above the forward decks. The ship looks awkward and ungainly. It looks like it may well challenge the principles of buoyancy and displacement. It looks like nothing that neither James nor I have ever trusted his life to before. Our hallucinatory float down the Copper River is ten days behind us. We’ve reentered civilization in Anchorage, visited friends in Seattle, finally met Gary Cook of Baikal Watch and our Russia-specialist travel agent Debbie, and made other last-minute arrangements here in San Francisco, and now we’re riding across the acres of asphalt in the back of a battered yellow van and our friend Eleanor, who drove us down here, is repeating, as if a mantra, Oh my god, I can’t believe you’re getting on this thing. . . . Oh my god, I can’t believe . . .
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Conference papers on the topic "South Red Sea"

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Mohriak, Webster. "Comparisons between Red Sea and South Atlantic." In 15th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 31 July-3 August 2017. Brazilian Geophysical Society, 2017. http://dx.doi.org/10.1190/sbgf2017-076.

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Hwang, Do-Hyun, Su-Ho Bak, Heung-Min Kim, Hong-Joo Yoon, Don-Hyug Kang, and Yong-Hyun Chung. "The Relation between the Red Tide Occurrence and the Sea Water Temperature in South Sea of Korea." In Next Generation Computer and Information Technology 2017. Science & Engineering Research Support soCiety, 2017. http://dx.doi.org/10.14257/astl.2017.145.26.

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Court, Kenneth E. "Extended Cruising The Second Time Around." In SNAME 7th Chesapeake Sailing Yacht Symposium. SNAME, 1985. http://dx.doi.org/10.5957/csys-1985-005.

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Some years ago, in 1975, I presented a paper and a slide show at an earlier sailing yacht symposium in Annapolis. The subject was a four-year, 28,000 mile cruise I had made in the years 1965 - 1968 most of the way around the world: Hawaii and the South Pacific, New Zealand, Australia's Barrier Reef, the Indian Ocean, the Red Sea, the Mediterranean, including the Greek Islands, an Atlantic crossing to Barbados from the Canary Islands, the Caribbean, and home to the Chesapeake. The paper I wrote then was entitled "Extended Cruising: An Overview" and contained sketches and data from my logs. It was same 55 pages long and talked about many facets of cruising from my vantage point, primarily as seen from the decks of Mamari, the 28 foot ketch I had bought in New Zealand. Lest Mamari 's size appear too small, which perhaps would make me seen heroic, recognize that in displacement and accomodations Mamari was the equivalent of a 33 foot boat. To dispel one other misconception, be advised that I normally sailed with a crew of two, sometimes more, and only sailed two legs single-handed, of about 500 miles each, one from Tonga to Fiji in the Pacific, the other in the Gulf of Suez and from Port Said to the Greek Islands. The 1975 paper reflected my background as a naval architect, combined with my experience as a sailor. I told of things I learned from others. I analyzed log data, presented photographs, drawings and tables, and wrote a series of "yarns" such as sailors spin about their travels. The paper is touched with a flavor of the sea, a flavor of talk over run or coffee in a snug anchorage or on a shared night watch. That 1975 paper makes good reading, and much of the information is still valid. It could be reprinted and if there is enough interest l will do so (contact me). This present paper is a brief look at my experiences on a series of sailing trips, but in particular a one year voyage in a 37 foot yawl from Turkey to the Chesapeake via the West Indies in 1980-81. The paper answers the question posed at the 1975 symposium, would I do the trip again? Then, I thought so, but could not be sure, now my reply is, "of course."
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Charlton, T. R. "Mid-crustal detachment beneath southern Timor-Leste: seismic evidence for Australian basement in the Timor collision complex (and implications for prospectivity)." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-98.

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Seismic data originally acquired over SW Timor-Leste in 1994 shows two consistent seismic reflectors mappable across the study area. The shallower ‘red’ reflector (0.4-1s twt) deepens southward, although with a block-faulted morphology. The normal faults cutting the red marker tend to merge downward into the deeper ‘blue’ marker horizon (0.5-2.8s twt), which also deepens southward. Drilling intersections in the Matai petroleum exploration wells demonstrate that the red marker horizon corresponds to the top of metamorphic basement (Lolotoi Complex), while the blue marker horizon has the geometry of a mid-crustal extensional detachment. We see no indications for thrusting on the seismic sections below the red marker horizon, consistent with studies of the Lolotoi Complex at outcrop. However, surficial geology over much of the seismic survey area comprises a thin-skinned fold and thrust belt, established in 8 wells to overlie the Lolotoi Complex. We interpret the fold and thrust belt as the primary expression of Neogene arc-continent collisional orogeny, while the Lolotoi Complex represents Australian continental basement underthrust beneath the collision complex. In the seismic data the basal décollement to the thrust belt dips southward beneath the synorogenic Suai Basin on the south coast of Timor, and presumably continues southward beneath the offshore fold and thrust belt, linking into the northward-dipping décollement that emerges at the Timor Trough deformation front. The same seismic dataset has been interpreted by Bucknill et al. (2019) in terms of emplacement of an Asian allochthon on top of an imbricated Australian passive margin succession. These authors further interpreted a subthrust anticlinal exploration prospect beneath the allochthon, which Timor Resources plan to drill in 2021. This well (Lafaek) will have enormous significance not only commercially, but potentially also in resolving the long-standing allochthon controversy in Timor: i.e., does the Lolotoi Complex represent ‘Australian’ or ‘Asian’ basement?
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Keuning, J. A., P. F. van Terwisga, and B. Nienhuis. "The Possible Application of an AXE Bow on a 5000 Ton Frigate." In SNAME 13th International Conference on Fast Sea Transportation. SNAME, 2015. http://dx.doi.org/10.5957/fast-2015-021.

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During some time now the application of the so called AXE Bow has proven very successful. Typical applications so far have been as Fast Crew Suppliers in the Offshore industry, as Patrol Boats with Coast Guards and SAR boats all in the range of 50 till 20 meter length overall and speeds ranging from 25 to 35 knots. Applying the AXE Bow Concept on smaller boats than 15 meter length overall is a challenge, because minimal stability requirements generally ask for a smaller L/B ratio and so beamier ships. On the other end application on frigate type hulls, which have generally a rather high L/B ratio and already fine bow could be considered less advantageous because high vertical accelerations, bow slamming and added resistance in head waves are already relatively small. In an earlier study commissioned by the Netherlands, Italian and Danish navies some 10 years ago (the THALES Project reported in Ref [1]) the application of the Enlarged Ship Concept and the AXE Bow Concept on a frigate type hull were already considered but only on a limited scale. Over the last decade a large amount of design information has been gathered from the experience gained from full scale measurements on board of real AXE Bow ships. This refers amongst others to increased directional stability particular in following waves by applying fixed skegs and so reduced rudder motions to be applied, the possibility to vary and increase the maneuverability at wish by making these skegs retractable (Ref [2]), a reduced added resistance in waves and considerably less shipping of green water when sailing in head waves. All these aspects led to the question raised when the replacement of the presently employed “M Frigate” of the Royal Netherlands Navy came in sight whether the application of the AXE Bow Concept on the new frigate would be a desirable and feasible option. The main question to be addressed by the present research was How does the Conventional Frigate hull type compare to the AXE Bow hull with respect to: the calm water resistance, taking on green water, the behavior in stern quartering waves, and the maneuverability. These research questions were formulated and the project commissioned by the DAMEN Shipyard at Gorinchem, Damen Schelde Naval Shipbuilding and the Defense Material Organization from the Ministry of Defense of the Netherlands to the Ship Hydromechanics Department of the Delft University of Technology. An extensive research plan including a large test program has been set up to investigate the behavior of both designs, both in the towing tank of the Delft University and from MARIN at Wageningen and also on open water on an estuary in the south with radio controlled models. Part of the measurements were conducted on open water to be able to carry out turning circles at various forward speeds and rudder angles. Also for the tests in following and stern quartering waves the addition of open water tests seemed essential to gather sufficient statistically reliable results on rarely occurring events such as broaching. The main results of this research project will be reported in this paper.
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Reports on the topic "South Red Sea"

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Jung, Paul H., Jean-Claude Thill, and Luis Armando Galvis-Aponte. State Failure, Violence, and Trade: Dangerous Trade Routes in Colombia. Banco de la República, December 2021. http://dx.doi.org/10.32468/dtseru.303.

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We investigate the effect of domestic armed violence brought about by political instability on the geography of distance frictions in freight mobility and the resulting differential access of regions to global markets. The Colombian transportation system has been found to be impeded by deficiencies in landside transport infrastructure and institutions, and by fragmented political environments. The micro-level analysis of U.S.-bounded export shipping records corroborates that export freight shipping from inland regions is re-routed to avoid exposures to domestic armed violence despite greatly extended landside and maritime shipping distances. We exploit the trajectories of freight shipping from Colombian regions and spatial patterns of violent armed conflicts to see how unstable geopolitical environments are detrimental to freight shipping mobility and market openness. The discrete choice model shows that the shipping flow is greatly curbed by the extended re-routing due to domestic armed violence and that inland regions have restricted access to the global market. The perception of risk and re-routing behavior is found heterogeneous across shipments and conditional to shipment characteristics, such as commodity type, freight value and shipper sizes. The results highlight that political stability must be accommodated for improved freight mobility and export-oriented economic development in the global South.
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Matte, S., M. Constantin, and R. Stevenson. Mineralogical and geochemical characterisation of the Kipawa syenite complex, Quebec: implications for rare-earth element deposits. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329212.

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The Kipawa rare-earth element (REE) deposit is located in the Parautochton zone of the Grenville Province 55 km south of the boundary with the Superior Province. The deposit is part of the Kipawa syenite complex of peralkaline syenites, gneisses, and amphibolites that are intercalated with calc-silicate rocks and marbles overlain by a peralkaline gneissic granite. The REE deposit is principally composed of eudialyte, mosandrite and britholite, and less abundant minerals such as xenotime, monazite or euxenite. The Kipawa Complex outcrops as a series of thin, folded sheet imbricates located between regional metasediments, suggesting a regional tectonic control. Several hypotheses for the origin of the complex have been suggested: crustal contamination of mantle-derived magmas, crustal melting, fluid alteration, metamorphism, and hydrothermal activity. Our objective is to characterize the mineralogical, geochemical, and isotopic composition of the Kipawa complex in order to improve our understanding of the formation and the post-formation processes, and the age of the complex. The complex has been deformed and metamorphosed with evidence of melting-recrystallization textures among REE and Zr rich magmatic and post magmatic minerals. Major and trace element geochemistry obtained by ICP-MS suggest that syenites, granites and monzonite of the complex have within-plate A2 type anorogenic signatures, and our analyses indicate a strong crustal signature based on TIMS whole rock Nd isotopes. We have analyzed zircon grains by SEM, EPMA, ICP-MS and MC-ICP-MS coupled with laser ablation (Lu-Hf). Initial isotopic results also support a strong crustal signature. Taken together, these results suggest that alkaline magmas of the Kipawa complex/deposit could have formed by partial melting of the mantle followed by strong crustal contamination or by melting of metasomatized continental crust. These processes and origins strongly differ compare to most alkaline complexes in the world. Additional TIMS and LA-MC-ICP-MS analyses are planned to investigate whether all lithologies share the same strong crustal signature.
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