30.—Weather Routing of Ships on the North Atlantic.

1972 ◽  
Vol 72 (1) ◽  
pp. 311-320
Author(s):  
R. F. Zobel

Modern ship routing is a matter for specialist forecasters using a mass of meteorological observations processed by large, high-speed electronic computers, as will appear below.Historically, some form of routing has been practised for centuries as the result of observations made by navigators and explorers as they gradually laid bare the geography of the earth's oceans and continents.It cannot be known whether the very early navigators followed routes based on weather considerations, but they may have done so in limited areas of the globe. There is some reason to suppose that the Atlantic islands and even perhaps the West Indies were known to the Phoenicians. Legends which suggest this are supported by the finding of a stock of fourth century b.c. Phoenician coins at Corvo in the Azores. It has been reasonably supposed in some quarters that these coins were from a Phoenician trader wrecked on the island whilst on passage westwards, but how far west we cannot be sure.It has never been seriously doubted that the north-east coast of America was discovered and temporarily colonised by Vikings from Greenland during the latter part of the first century A.D. Certain archaeological finds have been held by some to support this view. An account of some early pioneering voyages has been given by Villiers (1956).These early voyages can hardly have been consciously weather routed, though some knowledge of the prevailing wind conditions may well have been acquired. Perhaps it was as late as the end of the fifteenth century that the first known weather-routed voyage was made. Henry the Navigator (Prince Henry of Portugal) was intent on finding a way round the Cape into the Indian Ocean in order to oust the Venetians and Arabs from their lucrative trading in that area. He fitted out expedition after expedition, but they all turned back as they hugged the African coast and were caught in the doldrums. Eventually they learned to stand well out to sea and so get the benefit of the N.E. trades and in 1434 they reached the equator. However, it was another half-century before the Cape was reached and this could conceivably be regarded as the first weather-routed voyage.

2017 ◽  
Author(s):  
Olga Makarieva ◽  
Nataliia Nesterova ◽  
Lyudmila Lebedeva ◽  
Sergey Sushansky

Abstract. As of 2017, 70 years have passed since the beginning of work at the Kolyma water-balance station (KWBS), a unique scientific research hydrological and permafrost catchment. The volume and duration (50 continuous years) of hydrometeorological standard and experimental data, characterizing the natural conditions and processes occurring in mountainous permafrost conditions, significantly exceeds any counterparts elsewhere in the world. The data are representative of the vast territory of the North-East of Russia. In 1997, the station was terminated, thereby leaving Russia without operating research watersheds in the permafrost zone. This paper describes the dataset containing the series of daily runoff from 10 watersheds with area from 0.27 to 21.3 km2, precipitation, meteorological observations, evaporation from soil and snow, snow surveys, soil thaw and freeze depths, and soil temperature for the period 1948–1997. It also highlights the main historical stages of the station's existence, its work and scientific significance, and outlines the prospects for its future, where the Kolyma water-balance station could be restored to the status of a scientific research watershed and become a valuable international center for hydrological research in permafrost. The data is available at https://doi.pangaea.de/10.1594/PANGAEA.881731.


1988 ◽  
Vol 38 ◽  
pp. 175-184 ◽  
Author(s):  
R. M. Harrison

Amorium is in eastern Phrygia, 170 km. south-west of Ankara, 70 km. north-east of Afyon, 12 km. east of the town of Emirdaǧ, and near the source of the Sakarya (Sangarius) (Fig. 1). It lies on the north-facing lower slopes of the mountains of Emirdaǧ (the Turkish town, previously called Aziziye, has the same name), and the ancient site of Amorium lies within the relatively recent village of Hisarköy. The mountain of Emirdaǧ gives rise to various streams which flow into a tributary of the Sakarya, and at Amorium the view to the north extends over some 50 km., showing, in the middle distance, the tree-lined course of the river, and the mountains of Sivrihisar beyond. The ancient town (which includes a large prehistoric hüyük) was mentioned by Strabo, and indeed the name of Amorium appeared earlier on coins, in the second or first century B.C. The site was rediscovered by W. J. Hamilton in 1836.


1965 ◽  
Vol 23 ◽  
pp. 78-105 ◽  
Author(s):  
A. F. P. Hulsewé

In antiquity, China was far from being the China we know today, neither in extent, nor in political and social organisation. To the south it did not extend beyond the Yangtze River, to the north it stopped short of the Mongolian steppe, to the north-east, only a small part of the south Manchurian plain was included, whereas in the west it merely went up to the easternmost part of what is now Kansu Province; the Szechwan plain was only included at the end of the fourth century B.C. Politically, the King of Chou was theoretically the overlord of most of this area, but in actual practice, independent rulers reigned over a congeries of larger and smaller states. As a result of wars of conquest, seven large states had come to be formed by the middle of the fifth century B.C. and these were engaged in a ceaseless struggle for supremacy. The time between the middle of the fifth century and 221 B.C., when the western state of Ch'in finally conquered all its rivals, is known as the period of the Warring States.


2020 ◽  
Vol 2 (1) ◽  
pp. 46
Author(s):  
Nurtati Soewarno

Abstact – Indonesia is an archipelago that is located between two continents, Asia and Australia, also between two oceans, the Pasific and the Indian ocean. This prospers in the commercial activity. Because of the location, costal cities are more easy to reach, foreigner that drop in have significant impact to these cities, for example Cirebon, a costal city that lies in the north east part of West Jawa. Various foreigners that drop in and also stay in Cirebon could be seen by the heritage, one of them is the Vihara Dewi Welas Asih. The temple as a house of worship for Konghucu religion is easy to be known by the colour and Chinese specific architectural style. The city development pushes to changes, as to the Vihara Dewi Welas Asih, renovation and additional buildings is inevitable. This paper is to study the architectural style applied to the additional buildings surrounding the temple. By observation the architectural style of the new building is recognised, also how the context of the new building compare to the temple. It is expected that the new architectural style will be in harmony with the Vihara Dewi Welas Asih architectural style. It is also expected that intervention by the Local Government in organizing the alteration so the Cultural Heritage area is well maintained, become a tourist destination site giving a positive impact to the continuity of the Cultural Heritage building in Cirebon city. Keywords – architectural style addaptation, Vihara Dewi Welas Asih, Cultural Heritage Building


Author(s):  
Mike Searle

At 00.58 GMT (7.58 local time) on Sunday, 26 December 2004 a massive earthquake occurred off the north-west coast of Sumatra. The earthquake measured between magnitude 9.0 and 9.3 on the Richter scale with its epicentre at 3.32oN, 95.85oE, and occurred at a depth of approximately 30 kilometres. It was the second largest earthquake recorded since instrumental records began and was the deadliest natural disaster in recorded history. The earthquake and the resulting tsunami are estimated to have killed at least 228,000 people across fifteen countries bordering the Indian Ocean. The worst affected countries were Indonesia, Sri Lanka, India, Thailand, Burma, the Maldives, and Somalia. The earthquake occurred on the subduction zone interface between the down-going Indian Ocean plate and the overriding Burma–Andaman–Sumatra plate. It ruptured approximately 1600 kilometres’ length of the plate boundary from Sumatra all the way north to the Burmese coast, travelling at 2–3 kilometres per second. Aftershocks continued unrelentingly for over four months after the earthquake, several reaching magnitude 7.5 as far north as the northern Andaman Islands. The seismic waves indicated a thrust fault earthquake that tilted the surface up to the south-west and down to the north-east. The ground surface was elevated as much as 11 metres at the epicentre, with the tilted surface sinking up to one metre further to the north-east, offshore Sumatra. During the rupture, the Burma plate slipped as much as 15 metres horizontally as the Indian Ocean plate slipped beneath. The force of the quake perceptibly shifted the Earth’s axis, raised sea level globally and speeded Earth’s rotation. It has been suggested that the earthquake shortened the length of the day by 2.68 microseconds, because of the decrease in oblateness of the Earth. The earthquake caused the Earth to wobble on its axis by up to 2.5 cm in the direction of 145o east longitude. The natural ‘Chandler wobble’, a small motion in the Earth’s axis of rotation (the motion that occurs when the spinning object is not a perfect sphere) can be up to 9 metres over 433 days, so this eventually offsets the comparatively minor wobble produced by the earthquake.


2009 ◽  
Vol 23 (4) ◽  
pp. 633-647 ◽  
Author(s):  
V. Geethalakshmi ◽  
Akiyo Yatagai ◽  
K. Palanisamy ◽  
Chieko Umetsu

2012 ◽  
Vol 31 (2) ◽  
pp. 219-238
Author(s):  
Mary Pryor

The lives and work of eighteenth-century Scottish artists John and Cosmo Alexander, father and son, were dedicated to the Jacobite cause. They were men of a culture that was distinct to their own region, that of the north-east of Scotland, which from the late fifteenth century had been centred on the university circles of Aberdeen. In microcosm, the experiences of those in these circles reflected the oscillating tests of faith and fealty of that era. Assumed to be Catholics, and from a family which numbered at least one priest among its number, between them the Alexanders survived the turbulent times of the eighteenth-century Jacobite Risings. Both were wanted men after the 1746 Battle of Culloden. Drawing on local evidence, this paper explores the religious, political and social landscape surrounding the works with an Aberdeen connection produced by both John and Cosmo Alexander. All can be seen to demonstrate that the enduring bonds of faith and fealty, which, perforce, may not always have been openly displayed, could be reinforced through the subtle deployment of the painted image.


Britannia ◽  
1972 ◽  
Vol 3 ◽  
pp. 298-351 ◽  
Author(s):  
D. R. Wilson

Cae Metta (SH 536650), 1.5 km south-west of Llandeiniolen: preliminary examination of the polygonal enclosed hut-group suggested occupation from the mid third into the fourth century.Caernarvon fort (Segontium, SH 485624) :3 excavation outside the north-east gate (porta decumana) showed that the original Flavian causeway and inner ditch remained in use unaltered until shortly after 330. The causeway was then dug through and the ditch re-cut from a W-profile to the normal V-section, while a new outer ditch was constructed some 10 m out from the gate. Access to the gate was now over wooden bridges, for which structural evidence was found at the inner ditch. Fresh details were also obtained of the Flavian timber gate.


2009 ◽  
Vol 89 (8) ◽  
pp. 1679-1687
Author(s):  
Toufiek Samaai ◽  
Ruwen Pillay ◽  
Michelle Kelly

Cymbastela sodwaniensis sp. nov. (order Halichondrida: family Axinellidae) is described from the subtropical waters of Sodwana Bay on the north-east coast of South Africa. The genus was previously unknown from southern Africa or the western and eastern parts of the Indian Ocean. This record represents the westernmost extent of this predominantly Indo-Pacific to Australasian genus. This new species record brings the number of Cymbastela species described to a total of nine.


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