An Open Knowledge System for Navigational Science: Zheng He’s Maritime Expeditions and Sino-Foreign Overseas Exchange

2019 ◽  
Vol 1 (1) ◽  
pp. 50-91
Author(s):  
Liu Yingsheng

The first section of this article begins by investigating the term “going down to the Western Oceans” (xia xiyang 下西洋), which was used as early as the time of Zheng He. It also discusses the origin of the concepts of the Eastern and Western Oceans. The second section discusses the influx of overseas geographical knowledge into China before the time of Zheng He, especially over two important periods: first, the coming of Indian geographical knowledge along with Buddhism to China from the Wei-Jin period (220–420 ce), and second, the advent of Islamic geographical knowledge during the Mongol-Yuan period (ca. 1206–1368). The third section discusses the contributions of foreign members in Zheng He’s fleet, especially fanhuozhang 番火長 (foreign pilot). Through an analysis of the records of three military encounters—the suppression of the pirate Chen Zuyi 陳祖義, the attack on Ceylon, and the battle with pirates on a return journey—we find that the term fanhuozhang appears in all three cases, showing that foreign experts were commonly present in all branches or segments of Zheng He’s fleet, and that it must have been their job to navigate in the Indian ocean portion of the journey. Based on these findings, the author suggests that even before the beginning of Ming, Chinese people had developed an understanding of navigation technology and absorbed expertise from other peoples, and that this knowledge formed the technological foundation of Zheng He’s long-distance voyages, evident of the fact that China’s ancient navigational technology was an open knowledge system.

2003 ◽  
Vol 46 (1) ◽  
pp. 46-87 ◽  
Author(s):  
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AbstractThe harbor town of Berenike functioned in the long-distance trade between the Mediterranean and the Indian Ocean Basin from the third century BC to the early sixth century AD. This contribution aims to view the Berenike material within its wider historical context through a preliminary analysis of the combined archaeological and textual evidence. By comparing the results of the work of different specialists, the potential of a multi-disciplinary approach becomes apparent. A number of caveats are given, which illustrate the interpretative problems arising from comparing the results of different disciplines. Lastly, this attempt at integration shows that the discrepancies between the different sources offer important insights. Le port maritime de Berenike fonctionnait dans le commerce de longue distance entre la Méditerranée et le bassin de la Mer des Indes depuis le troisième siècle avant JC jusqu'au début du sixième siècle après JC. Cette contribution examine le matériel de Berenike dans un contexte plus large par une analyse préliminaire croisant des données archéologiques et textuelles. En comparant les résultats proposés par plusieurs spécialistes, le potentiel du travail multidisciplinaire devient évident. Un nombre de caveats est présenté pour illustrer des problèmes d'interprétation, provenant des comparaisons de résultats de plusieurs disciplines. Enfin, cet essai d'intégration montre que les divergences entre plusieurs sources offre des aperçus importants.


Antiquity ◽  
1993 ◽  
Vol 67 (256) ◽  
pp. 609-612 ◽  
Author(s):  
Brian Hayden ◽  
D. E. Nelson ◽  
Jean Cataliotti-Valdina

A fragment of Cassis rufa shell, in modern times a species of the Indian Ocean, was reliably reported from the deep Mousterian deposits excavated at the beginning of the century from the Grotte du Prince, Monaco. Because its known habitat is so distant and exotic, there has always been question about the specimen's authenticity. A radiocarbon determination shows it to be recent, and no evidence for long-distance movement of shell in the European Middle Palaeolithic.


Antiquity ◽  
1941 ◽  
Vol 15 (59) ◽  
pp. 233-256 ◽  
Author(s):  
James Hornell

The few indications that have come down to us of ancient sea-traffic between the countries lying around the shores of the Red Sea, the Persian Gulf and the Indian Ocean are so fragmentary and obscure that it is extremely difficult to reconstruct any definite picture of their character and extent. In spite of this handicap study of the meagre evidence available compels the belief that movement by sea, although of a fluctuating character and confined for the most part to coastwise voyaging, was far more active and advanced in parts of this area in very early times than is generally realized. Had it been otherwise how could we interpret the signs graven on the rocks of the ravines of the Egyptian desert, and the transport by sea of great blocks of stone to Sumer in the time of Gudea of Lagash?The earliest evidence at present available comes from the Red Sea and the Persian Gulf, though it does not follow that either area is the cradle of sea-faring. It consists of :—(A) innumerable prehistoric and predynastic petroglyphs of ships engraved upon the rocks of the eastern desert of Egypt, particularly those in the Wadi Hammamat region;(B) the discovery on Sumerian sites of diorite statues, stated specifically to have been brought by sea from foreign lands early in the third millennium B.C.;(c) the presence in the ruins of Ur, Kish, and Lagash of artifacts cut from the shell of the sacred Indian chank (Xancus pyrum);(D) historical records of trading expeditions sent by sea from Egypt to Somaliland extending from the Vth to the XIIth Dynasties, and repeated in the XVIIIth Dynasty.


2005 ◽  
Vol 54 (1) ◽  
pp. 21-34 ◽  
Author(s):  
Yong-Ming Yuan ◽  
Sébastien Wohlhauser ◽  
Michael Möller ◽  
Jens Klackenberg ◽  
Martin W. Callmander ◽  
...  

2021 ◽  
Author(s):  
Justine Girardet ◽  
Francois Sarano ◽  
Gaëtan Richard ◽  
Paul Tixier ◽  
Christophe Guinet ◽  
...  

AbstractAdult male sperm whales (Physeter macrocephalus) are long distance runners of the marine realm, feeding in high latitudes and mating in tropical and subtropical waters where stable social groups of females and immatures live. Several areas of uncertainty still limit our understanding of their social and breeding behaviour, in particular concerning the potential existence of geographical and/or social fidelities.In this study, using underwater observation and sloughed-skin sampling, we looked for male social fidelity to a specific matrilineal sperm whale group near Mauritius. In addition, we captured a wider picture of kin relationships and genetic diversity of male sperm whales in the Indian Ocean thanks to biopsies of eight unique individuals taken in a feeding ground near the Kerguelen and Crozet Archipelagos (Southern Indian Ocean).Twenty-six adult male sperm whales, of which 13 were sampled, were identified when socializing with adult females and immatures off Mauritius. Long-term underwater observation recorded several noteworthy social interactions between adult males and adult females and/or immatures. We identified seven possible male recaptures over different years (three by direct observation, and four at the gametic level), which supports a certain level of male social fidelity. Several first- and second-degree kin relationships were highlighted between members of the social unit and adult males, confirming that some of the adult males observed in Mauritian waters are reproductive. Male social philopatry to their natal group can be excluded, as none of the males sampled shared the haplotype characteristic of the matrilineal social group. Mitochondrial DNA control region haplotype and nucleotide diversities calculated over the 21 total male sperm whales sampled were similar to values found by others in the Indian Ocean.Our study strongly supports the existence of some levels of male sperm whale social fidelity, not directed to their social group of birth, in the Indian Ocean. Males sampled in breeding and feeding grounds are linked by kin relationships. Our results support a model of male mediated gene flow occurring at the level of the whole Indian Ocean, likely interconnected with large-scale geographical fidelity to ocean basin, and a small-scale social fidelity to matrilineal social groups.


2010 ◽  
Vol 10 (22) ◽  
pp. 11017-11096 ◽  
Author(s):  
M. G. Lawrence ◽  
J. Lelieveld

Abstract. Southern Asia, extending from Pakistan and Afghanistan to Indonesia and Papua New Guinea, is one of the most heavily populated regions of the world. Biofuel and biomass burning play a disproportionately large role in the emissions of most key pollutant gases and aerosols there, in contrast to much of the rest of the Northern Hemisphere, where fossil fuel burning and industrial processes tend to dominate. This results in polluted air masses which are enriched in carbon-containing aerosols, carbon monoxide, and hydrocarbons. The outflow and long-distance transport of these polluted air masses is characterized by three distinct seasonal circulation patterns: the winter monsoon, the summer monsoon, and the monsoon transition periods. During winter, the near-surface flow is mostly northeasterly, and the regional pollution forms a thick haze layer in the lower troposphere which spreads out over millions of square km between southern Asia and the Intertropical Convergence Zone (ITCZ), located several degrees south of the equator over the Indian Ocean during this period. During summer, the heavy monsoon rains effectively remove soluble gases and aerosols. Less soluble species, on the other hand, are lifted to the upper troposphere in deep convective clouds, and are then transported away from the region by strong upper tropospheric winds, particularly towards northern Africa and the Mediterranean in the tropical easterly jet. Part of the pollution can reach the tropical tropopause layer, the gateway to the stratosphere. During the monsoon transition periods, the flow across the Indian Ocean is primarily zonal, and strong pollution plumes originating from both southeastern Asia and from Africa spread across the central Indian Ocean. This paper provides a review of the current state of knowledge based on the many observational and modeling studies over the last decades that have examined the southern Asian atmospheric pollutant outflow and its large scale effects. An outlook is provided as a guideline for future research, pointing out particularly critical issues such as: resolving discrepancies between top down and bottom up emissions estimates; assessing the processing and aging of the pollutant outflow; developing a better understanding of the observed elevated pollutant layers and their relationship to local sea breeze and large scale monsoon circulations; and determining the impacts of the pollutant outflow on the Asian monsoon meteorology and the regional hydrological cycle, in particular the mountain cryospheric reservoirs and the fresh water supply, which in turn directly impact the lives of over a billion inhabitants of southern Asia.


Author(s):  
Tom Hoogervorst

Southeast Asian history has seen remarkable levels of mobility and durable connections with the rest of the Indian Ocean. The archaeological record points to prehistoric circulations of material culture within the region. Through the power of monsoon sailing, these small-scale circuits coalesced into larger networks by the 5th century bce. Commercial relations with Chinese, Indian, and West Asian traders brought great prosperity to a number of Southeast Asian ports, which were described as places of immense wealth. Professional shipping, facilitated by local watercraft and crews, reveals the indigenous agency behind such long-distance maritime contacts. By the second half of the first millennium ce, ships from the Indo-Malayan world could be found as far west as coastal East Africa. Arabic and Persian merchants started to play a larger role in the Indian Ocean trade by the 8th century, importing spices and aromatic tree resins from sea-oriented polities such as Srivijaya and later Majapahit. From the 15th century, many coastal settlements in Southeast Asia embraced Islam, partly motivated by commercial interests. The arrival of Portuguese, Dutch, and British ships increased the scale of Indian Ocean commerce, including in the domains of capitalist production systems, conquest, slavery, indentured labor, and eventually free trade. During the colonial period, the Indian Ocean was incorporated into a truly global economy. While cultural and intellectual links between Southeast Asia and the wider Indian Ocean have persisted in the 21st century, commercial networks have declined in importance.


Author(s):  
Peter H. Reid

The action takes place along a triangle between three towns in Tanzania. Mwanza, the third-largest city in Tanzania, sits on the shores of Lake Victoria at an altitude that provides a pleasant, temperate climate. The trial eventually will be held in Mwanza. Maswa, adjacent to the famous Serengeti National Park, is the site of Peppy’s death and where various preliminary activities take place. It is a small, dusty town. Dar es Salaam, is the site of the U.S. embassy and the Peace Corps headquarters in Tanzania. Communications between Tanzania and Washington, D.C., flow out of Dar es Salaam, the capital of Tanzania at the time, which is on the coast facing Zanzibar and the Indian Ocean.


2017 ◽  
Vol 1 (1) ◽  
Author(s):  
Xingrong Chen ◽  
Yi Cai ◽  
Fangli Qiao

 The physical decomposition method suggested by Qian (2012) is used to examine the interannual variability of sea surface temperature (SST) and anomaly (SSTA) in the Indian Ocean (IO) for the period 1945.2003. The monthly mean SSTs taken from the global ocean reanalysis produced by the Simple Ocean Data Assimilation (SODA) are decomposed into four terms. The first term is the zonally averaged monthly climatological SST ([Tt(ϕ)]), which features relatively warm surface waters in the tropical IO and relatively colder surface waters over the southern IO. This term also has a relatively low SST pool between the Equator and 20°N. The SST at the center of the pool in summer is about 1-2°C lower than in spring and autumn. The second term is the spatially-varying monthly climatological SSTA (Tt*(λ,ϕ)), due mainly to the topographic effect and seasonal variation in wind forcing. The values of Tt*(λ,ϕ) are negative over the western coastal waters and positive over the eastern coastal and shelf waters in the tropical and northern IO. The third term is the zonally-averaged transient SSTA([T(ϕ,t)']Y). The largest values of [T(ϕ,t)']Y occur over the subtropical and mid-latitudes of the IO, which differs from the SSTA in the tropical waters of the Pacific Ocean. Time series of zonally and meridionally averaged T(ϕ,t)'Y in the tropical-subtropical IO is strongly correlated with the Indian Ocean basin-wide (IOBW) mode. The fourth term is the spatially-varying transient SSTA (T(λ,ϕ,t)*Y']. The REOF analysis of the fourth term demonstrates that the first REOF is correlated strongly with the South Indian Ocean Dipole (SIOD) mode. The second REOF is correlated strongly with the equatorial Indian Ocean dipole (IOD) mode. The third REOF is highly correlated with the tropical IOBW mode.


1900 ◽  
Vol 32 (4) ◽  
pp. 763-768
Author(s):  
T. K. Krishṇa Menon

Malayalam is the language of the south-west of the Madras Presidency. It is the third most important language of the Presidency, the first and the second being Tamil and Telugu respectively. It is spoken in Malabar, Cochin, and Travancore. Out of a total of 5,932,207 inhabitants of these parts, 5,409,350 persons are those who speak Malayalam. These countries, taken as a whole, are bounded on the north, by South Canara, on the east by the far-famed Malaya range of mountains, on the south by the Indian Ocean, and on the west by the Arabian Sea.


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