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Relevant bibliographies by topics / North-eastern Red Sea

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Academic literature on the topic 'North-eastern Red Sea'

Author: Grafiati

Published: 5 June 2025

Last updated: 2 August 2025

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Journal articles on the topic "North-eastern Red Sea"

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Garzon, Francesco, Collin T. Williams, Jesse E. M. Cochran, et al. "A multi-method characterization of Elasmobranch & Cheloniidae communities of the north-eastern Red Sea and Gulf of Aqaba." PLOS ONE 17, no. 9 (2022): e0275511. http://dx.doi.org/10.1371/journal.pone.0275511.

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The Red Sea is particularly biodiverse, hosting high levels of endemism and numerous populations whose extinction risk is heightened by their relative isolation. Elasmobranchs and sea turtles have likely suffered recent declines in this region, although data on their distribution and biology are severely lacking, especially on the eastern side of the basin in Saudi Arabian waters. Here, we present sightings of elasmobranchs and sea turtles across the north-eastern Red Sea and Gulf of Aqaba collected through a combination of survey methods. Over 455 survey hours, we recorded 407 sightings belon

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Taqi, Ahmed Mohammed, Abdullah Mohammed Al-Subhi, Mohammed Ali Alsaafani, and Cheriyeri Poyil Abdulla. "Estimation of geostrophic current in the Red Sea based on sea level anomalies derived from extended satellite altimetry data." Ocean Science 15, no. 3 (2019): 477–88. http://dx.doi.org/10.5194/os-15-477-2019.

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Abstract. Geostrophic current data near the coast of the Red Sea have large gaps. Hence, the sea level anomaly (SLA) data from Jason-2 have been reprocessed and extended towards the coast of the Red Sea and merged with AVISO data at the offshore region. This processing has been applied to build a gridded dataset to achieve the best results for the SLA and geostrophic current. The results obtained from the new extended data at the coast are more consistent with the observed data (conductivity–temperature–depth, CTD) and hence geostrophic current calculation. The patterns of SLA distribution and

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Ehrmann, Werner, Paul A. Wilson, Helge W. Arz, Hartmut Schulz, and Gerhard Schmiedl. "Monsoon-driven changes in aeolian and fluvial sediment input to the central Red Sea recorded throughout the last 200 000 years." Climate of the Past 20, no. 1 (2024): 37–52. http://dx.doi.org/10.5194/cp-20-37-2024.

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Abstract. Climatic and associated hydrological changes controlled the transport processes and composition of the sediments in the central Red Sea during the last ca. 200 kyr. Three different source areas for mineral dust are identified. The dominant source is located in the eastern Sahara (Sudan and southernmost Egypt). We identify its imprint on Red Sea sediments by high smectite and Ti contents, low 87Sr / 86Sr, and high εNd. The availability of deflatable sediments was controlled by the intensity of tropical rainfall and vegetation cover over North Africa linked to the African monsoon. Inte

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Abdulla, Cheriyeri P., and Abdullah M. Al-Subhi. "Sea Level Variability in the Red Sea: A Persistent East–West Pattern." Remote Sensing 12, no. 13 (2020): 2090. http://dx.doi.org/10.3390/rs12132090.

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Based on 26 years of satellite altimetry, this study reveals the presence of a persistent east–west pattern in the sea level of the Red Sea, which is visible throughout the years when considering the east–west difference in sea level. This eastern–western (EW) difference is positive during winter when a higher sea level is observed at the eastern coast of the Red Sea and the opposite occurs during summer. May and October are transition months that show a mixed pattern in the sea level difference. The EW difference in the southern Red Sea has a slightly higher range compared to that of the nort

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Serels, Steven. "Famines of War: The Red Sea Grain Market and Famine in Eastern Sudan, 1889–1891." Northeast African Studies 12, no. 1 (2012): 73–94. http://dx.doi.org/10.2307/41960559.

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Abstract During the first few months of 1890, thousands of destitute, starving Bija-speaking semi-pastoralists from Eastern Sudan made their way to Sawākin in search of food. Though the region was plagued by both drought and locust swarms during the 1889-1890 cultivaaon year, ecological hazards are insufficient to explain the famine that precipitated this refugee migration. In the second half of the nineteenth century, Eastern Sudanese semi-pastoraluts produced less than half of the grain that they consumed. These communities depended on trading pastoral products for grain imported from India

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Volodina, A. A. "On findings of the red alga Gaillona rosea (Roth) Athanasiadis (Rhodophyta) in the Russian part of the South-Eastern Baltic." Marine Biological Journal 4, no. 2 (2019): 111–14. http://dx.doi.org/10.21072/mbj.2019.04.2.12.

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Information on the first findings of Gaillona rosea (Roth) Athanasiadis 2016:814 (Aglaothamnion roseum (Roth) Maggs & L’Hardy-Halos 1933:522) in the Russian part of the South-Eastern Baltic is given. Samples of algae in the Russian part of the South-Eastern Baltic along the coast of the Kaliningrad region at depths of 1–15 m were collected by diving method on the north coast of the Sambian Peninsula near Cape Taran and Cape Gvardeysky at the stations confined to hard ground. First samples of G. rosea collected from drifting mats of perennial algae Furcellaria lumbricalis and Polysiphonia f

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Rimbu, N., G. Lohmann, T. Felis, and J. Pätzold. "Shift in ENSO Teleconnections Recorded by a Northern Red Sea Coral." Journal of Climate 16, no. 9 (2003): 1414–22. http://dx.doi.org/10.1175/1520-0442-16.9.1414.

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Abstract El Niño–Southern Oscillation (ENSO) teleconnections over Europe and the Middle East are evaluated using an oxygen isotope coral time series from the northern Red Sea and various instrumental datasets. A shift in the correlation between the Niño-3 index and the Red Sea coral record in the 1970s is detected, and it is shown that this shift can be attributed to nonstationary circulation regimes and related ENSO teleconnections. It is found that positive anomalies of oxygen isotope in the Red Sea coral record from the middle 1930s to the late 1960s are associated with a strong Pacific–Nor

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Abou Auf, M. A. "Variation of benthic foraminiferal assemblages in different microenvironments along the shore zone north of the Rabigh Coast, eastern Red Sea, Saudi Arabia." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1996, no. 3 (1996): 129–39. http://dx.doi.org/10.1127/njgpm/1996/1996/129.

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Teferra, Damtew. "National Herbarium [Ethiopia]: From Where to Where?" African Research & Documentation 59 (1992): 1–8. http://dx.doi.org/10.1017/s0305862x00013194.

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Ethiopia is located in Eastern Africa and lies between 3° and 18° N and 33° and 48° E in what is usually called The Horn of Africa. It borders Sudan to the North, North West and West; Kenya to the South; Somalia to the South East and East and the Djibouti Republic and the Red Sea to the East and North East.The Country enjoys great geographical diversity ranging from high and rugged mountains, flat topped plateaus, deep gorges to river valleys and lowland plains. The vegetation is also as varied: ranging from desert, tropical forest, alpine shrub to grassland. Ethiopia has a greater diversity o

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Teferra, Damtew. "National Herbarium [Ethiopia]: From Where to Where?" African Research & Documentation 59 (1992): 1–8. http://dx.doi.org/10.1017/s0305862x00013194.

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Ethiopia is located in Eastern Africa and lies between 3° and 18° N and 33° and 48° E in what is usually called The Horn of Africa. It borders Sudan to the North, North West and West; Kenya to the South; Somalia to the South East and East and the Djibouti Republic and the Red Sea to the East and North East.The Country enjoys great geographical diversity ranging from high and rugged mountains, flat topped plateaus, deep gorges to river valleys and lowland plains. The vegetation is also as varied: ranging from desert, tropical forest, alpine shrub to grassland. Ethiopia has a greater diversity o

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Books on the topic "North-eastern Red Sea"

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Bačić, Jacques. Red Sea, Black Russia: Prolegomena to the history of North Central Eurasia in antiquity and the Middle Ages. East European Monograph, 1995.

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Bacic, Jacques. Red Sea-Black Russia: Prolegomena to the history of North Central Eurasia in antiquity and the Middle Ages. East European Monograph, distribubed by Columbia University Press, 1995.

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Kennedy, Hugh, and Fanny Bessard, eds. Land and Trade in Early Islam. Oxford University PressOxford, 2025. https://doi.org/10.1093/oso/9780198863083.001.0001.

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Abstract This collection of essays sheds new light on the economy of the Islamic Middle East in the three centuries from 750 to 1050 ce, a period when this area sustained the largest and most complex economic systems in Western Eurasia. It is also a period that has been largely neglected by modern scholarship, focusing as it has on the transition from Late Antiquity to Islam or the impact of the coming of the Franks to the Eastern Mediterranean from the eleventh century on. The essays in the volume investigate the causes of this development and the interactions of different factors. These chap

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Johansen, Bruce, and Adebowale Akande, eds. Nationalism: Past as Prologue. Nova Science Publishers, Inc., 2021. http://dx.doi.org/10.52305/aief3847.

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Nationalism: Past as Prologue began as a single volume being compiled by Ad Akande, a scholar from South Africa, who proposed it to me as co-author about two years ago. The original idea was to examine how the damaging roots of nationalism have been corroding political systems around the world, and creating dangerous obstacles for necessary international cooperation. Since I (Bruce E. Johansen) has written profusely about climate change (global warming, a.k.a. infrared forcing), I suggested a concerted effort in that direction. This is a worldwide existential threat that affects every living t

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Book chapters on the topic "North-eastern Red Sea"

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Hancock, James F. "Golden age of Byzantium." In Spices, scents and silk: catalysts of world trade. CABI, 2021. http://dx.doi.org/10.1079/9781789249743.0010.

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Abstract This chapter discusses the reign of the Eastern Roman Empire as well as the state of the international trade during its golden era. It consists of thirteen subchapters which are about the Shift of Roman Power, the rule of Constantine, the drastic transition of world trade after the fall of the West Roman Empire, the exotic luxuries of Byzantium, the golden age of the Eastern Roman Empire under Justinian, Byzantine attitudes about trade. Trade in the Byzantine world was highly regulated by the state, the empire was essentially a huge trading organization. It continues with the subchapt

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Sørbø, G. M. "Systems of pastoral and agricultural production in eastern Sudan." In The Agriculture of The Sudan. Oxford University PressOxford, 1991. http://dx.doi.org/10.1093/oso/9780198592105.003.0014.

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Abstract Eastern Sudan is defined for the purposes of this chapter as the country lying to the east of the Blue Nile and to the north of the line of permanent villages and regular cultivation that runs approximately from Sennar through Gedaref to the valley of the Settit River. To the north it includes the whole of the Red Sea Hills area as far as the Egyptian frontier. In administrative terms, the whole of Red Sea Province and the major part of Kassala Province are included.

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Goudie, Andrew S. "The Libyan Desert." In Great Warm Deserts of the World. Oxford University PressOxford, 2002. http://dx.doi.org/10.1093/oso/9780199245154.003.0005.

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Abstract In Egypt there are two deserts. One of these occurs east of the Nile and abuts the Red Sea. It is called the Eastern Desert. An early description is provided by Hume (1907). More recently, its tectonic setting has been described by Steckler and Omar (1994) and its Quaternary history by Arvidson et al. (1994) and Moeyersons et al. (1999). It consists essentially of a backbone of rugged, high igneous mountains that run parallel to the Red Sea coast from the Ethiopian Plateau, northwards to the Gulf of Suez. These igneous peaks and masses are flanked to the north and west by intensively

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Trenhaile, A. S. "Coral Reefs." In Coastal Dynamics and Landforms. Oxford University PressOxford, 1997. http://dx.doi.org/10.1093/oso/9780198233534.003.0010.

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Abstract Coral reefs extend over about 2 x 106 km2 of the tropical oceans, making them the largest biologically constructed formations on Earth. Of the areas covered by coral reefs and associated communities living down to depths of 30 m, about 30 percent are between northern Australia, Indonesia, the Philippines, and continental Asia; 25 percent in the Pacific Ocean; 24 percent in the Indian Ocean; 6 percent in the Red Sea and Persian (Arabian) Gulf; 14 percent in the Caribbean Sea and the North Atlantic; and 1 percent in the South Atlantic. More than half the world’s coral reefs are therefor

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Schneider, Marius, and Vanessa Ferguson. "Sudan." In Enforcement of Intellectual Property Rights in Africa. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198837336.003.0051.

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Sudan is situated in north-eastern Africa bordered by the Red Sea, Egypt, Libya, Chad, Central Africa Republic, South Sudan, Ethiopia, and Eritrea. It has an area of 1,886 million square kilometres (km) and an estimated 2019 population of 42.81 million. South Sudan gained independence from Sudan on 9 July 2011, and as such the provisions only relate to Sudan (North), which is now formally known as the Republic of Sudan. The capital of Sudan is Khartoum. The working week in Sudan is from Saturday to Wednesday with business hours beginning at 0800 and ending at 1630, Thursday’s hours are from 08

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Essen, Hans Van, and Dick Mol. "Plio-Pleistocene proboscideans from the southern bight of the North Sea and the Eastern Scheidt, The Netherlands." In The Proboscidea. Oxford University PressOxford, 1996. http://dx.doi.org/10.1093/oso/9780198546528.003.0021.

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Abstract The Netherlands and the adjacent part of the North Sea are well known for their abundant remains of late Pleistocene mammals. On the other hand, fossils of Pliocene and early Pleistocene age are comparatively rare in this area. This chapter deals with dredged remains of proboscideans from the Plio-Pleistocene in the North Sea area. Dredging operations in the floodplains of the rivers Rhine, Waal, IJssel and Meuse (Fig. 20.1) still yield many mammalian fossils. In most cases they are typical of the late Pleistocene (Weichselian, 100 000-12 000 years BP) and characterized by the woolly

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Alaily, F. "Soil development and climatic changes during Quaternary in the north eastern part of the Red Sea Hills (Sudan)." In Geoscientific Research in Northeast Africa. CRC Press, 2017. http://dx.doi.org/10.1201/9780203753392-103.

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Searle, Mike. "Extruding Indochina: Burma, Vietnam, Yunnan, Thailand." In Colliding Continents. Oxford University Press, 2013. http://dx.doi.org/10.1093/oso/9780199653003.003.0017.

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Geographically, Indochina consists of the South East Asian countries Thailand, Laos, Cambodia, and Vietnam. Geologically, Indochina includes all the land bounded by two very large-scale strike-slip faults—the Sagaing fault, which runs down the length of Burma, and the Red River fault, which extends more than 1,100 kilometres from the south-eastern corner of Tibet south-east through Yunnan and North Vietnam to Hanoi and the Gulf of Tonkin. Both faults are active, and show that Indochina is moving south-east relative to both the Burma micro-plate to the west and the South China block north of th

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Bunson, Matthew. "N." In A Dictionary Of the Roman Empire. Oxford University PressNew York, NY, 1995. http://dx.doi.org/10.1093/oso/9780195102338.003.0014.

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Abstract NABATAEANS An ancient Arabian people who occupied an extensive part of Palestine, stretching through 1orthem ARABIA into areas on both sides of the Red Sea md north to eastern IDUMAEA and the Dead Sea. The capital of the Nabataeans (or Nabataei) was the stone city of ‘ETRA. Founded in the 4th century B.C., Petra eventually ·served as a major trade center. Caravans from the Mediverranean ports moved through the city to the Far East, and the Nabataeans based their wealth on trade in Arabian incense and myrrh, Indian spices, and silk and other textiles from China. In tum, their kings sta

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Schneider, Marius, and Vanessa Ferguson. "Egypt." In Enforcement of Intellectual Property Rights in Africa. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198837336.003.0018.

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Found in the north-eastern corner of Africa and south-western Asia, Egypt shares borders with the Gaza Strip, Israel, Libya, and Sudan. With a population of more than 95.6 million in 2016, it is one of the most populous countries in Africa and the Middle East. The population is expected to grow at an annual rate of nearly 2 per cent and will surpass 100 million by 2025. More than 97 per cent of the population lives on both sides of the Nile River and the Delta, with smaller numbers along the Mediterranean and Red Sea coasts. This is due to the geography of Egypt, where 95 per cent of the land

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Conference papers on the topic "North-eastern Red Sea"

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Binsiddiq, F. O., V. V. Cabanting, and J. H. Haberman. "Corrosion of Infrastructure within Madinat Yanbu Al-Sinaiyah, Saudi Arabia." In CORROSION 2000. NACE International, 2000. https://doi.org/10.5006/c2000-00825.

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Abstract Construction of sister cities of Madinat Al-Jubail Al-Sinaiyah in eastern Saudi Arabia and Madinat Yanbu Al-Sinaiyah (MYAS) in western Saudi Arabia began in the mid-1970's to promote industrial development and diversification of the Kingdom of Saudi Arabia. MYAS resides on the Red Sea approximately 350 km north of Jeddah. The environmental conditions in the Middle East are considered the most aggressive in the world. During summer months, temperatures in MYAS frequently exceed 40°C, with temperature variations of as much as 20°C per day. Relative humidity variations of 40 to 100% over

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Brown, John Paul, and Rajarajan Narayanasamy Naidu. "Lateral Extension in Response to Late Stage Transpression, An Example from the Zhdanov Field, Caspian Sea - An Alternative to Flower Structures." In Gas & Oil Technology Showcase and Conference. SPE, 2023. http://dx.doi.org/10.2118/214213-ms.

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Abstract The Zhdanov Field is located on the eastern margin of the Caspian Sea and is geologically a part of the Apsheron-PreBalkan Fault Zone which crosses the Caspian Sea from Azerbaijan to Turkmenistan. Structurally, the field is part of an east-west orientated plunging anticline (hereafter referred to as the Cheleken Nose) that plunges westwards from the Cheleken Dome for over 25 km into the Caspian Sea. The structure of the Zhdanov Field formed in response to Pleistocene to Recent (post Apsheron) transpressive reactivation of a pre-existing fault at the Miocene and deeper levels (hereafte

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Alsinan, Ali, Khalilur Rehman, and Ahmad Bakodah. "Towards Sustainable Excellence & Biodiversity Protection in Upstream O & G Facility." In Middle East Oil, Gas and Geosciences Show. SPE, 2023. http://dx.doi.org/10.2118/213248-ms.

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Objective The objective is to showcase the Abu Ali facility's commitment to protecting and preserving the Abu Ali biodiversity ecosystem. The project demonstrates a modern sustainable, circular, innovative and systemic approach to target the biodiversity threats in multi-dimensional aspects and transform these threats into opportunities to improve the island's ecosystem. The island is important to Aramco's upstream operations because it houses an oil and gas production facility. The organization has determined its environmental goals from the corporate policies and vision to be as follows. Con

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Голофаст, Л. А. "PHANAGORIA IN THE 4th – 7th CENTURIES (WRITTEN SOURCES AND ARCHAEOLOGICAL DATA)." In Hypanis. Труды отдела классической археологии ИА РАН. Crossref, 2023. http://dx.doi.org/10.25681/iaras.2021.978-5-94375-350-3.42-57.

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В статье прослеживается история Фанагории с середины 3 в., когда жизнь Боспорского царства, в состав которого входила Фанагория, была нарушена вторжением племенных союзов готов, до конца 7 столетия, когда Боспор захватили хазары, и в истории Фанагории начался новый период. Сопоставляются сведения, содержащиеся в письмен - ных источниках и эпиграфических памятниках, данные археологии и нумизматики. История Фанагории рассматривается на фоне политической и экономической ситуации в Северном Причерноморье. Уточнение хронологии ключевых групп материала и ряд новых находок позволили пересмотреть даты

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Reports on the topic "North-eastern Red Sea"

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Boyle, Maxwell, and Elizabeth Rico. Terrestrial vegetation monitoring at Cape Hatteras National Seashore: 2019 data summary. National Park Service, 2022. http://dx.doi.org/10.36967/nrr-2290019.

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The Southeast Coast Network (SECN) conducts long-term terrestrial vegetation monitoring as part of the nationwide Inventory and Monitoring Program of the National Park Service (NPS). The vegetation community vital sign is one of the primary-tier resources identified by SECN park managers, and monitoring is currently conducted at 15 network parks (DeVivo et al. 2008). Monitoring plants and their associated communities over time allows for targeted understanding of ecosystems within the SECN geography, which provides managers information about the degree of change within their parks’ natural veg

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Blais-Stevens, A., A. Castagner, A. Grenier, and K D Brewer. Preliminary results from a subbottom profiling survey of Seton Lake, British Columbia. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332277.

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Seton Lake is a freshwater fiord located in southwestern British Columbia, roughly 4 km west of Lillooet and 250 km north-northeast of Vancouver. Located in the Coast Mountains, it is an alpine lake about 22-km long and roughly 1-1.5 km wide. It is separated from nearby Anderson Lake, located to the west, by a large pre-historic rock avalanche deposit at Seton Portage. The lake stands at about 243 m above sea level and is up to about 150 m deep (BC gov., 1953). Water level is controlled by a hydroelectric dam (i.e., Seton dam) located at the eastern end of the lake. Here, the lake drains east

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Struthers, Kim. Natural resource conditions at Fort Pulaski National Monument: Findings and management considerations for selected resources. National Park Service, 2023. http://dx.doi.org/10.36967/2300064.

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The National Park Service (NPS) Water Resources Division’s Natural Resource Condition Assessment (NRCA) Program initiated an NRCA project with Fort Pulaski National Monument (FOPU) in 2022. The purpose of an NRCA is to synthesize information related to the primary drivers and stressors affecting natural resource conditions at a park and to report conditions for natural resource topics selected by park managers. Resource conditions are evaluated as either a condition assessment or a gap analysis, depending on data availability. For FOPU’s NRCA, managers selected salt marsh, shorebirds, Eastern

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