scholarly journals Evaluation of the Dimensions of the Tsunami Evacuation Path for the Community of Air Tawar Barat Village, North Padang District, Padang City, Based on Geographic Information System (GIS)

2021 ◽  
Vol 4 (4) ◽  
pp. 123-129
Author(s):  
Faisal Ashar ◽  
Iqbal Maulana Yusup ◽  
Fitra Rifwan ◽  
Laras Oktavia Adreas
Keyword(s):  
River Mouth ◽  
The West ◽  
Evacuation Time ◽  
Tsunami Disaster ◽  
The North ◽  
Network Analyst ◽  
Parking Lot ◽  
The Indian Ocean ◽  
The Government ◽  
Evacuation Route

Air Tawar Barat Village is located in North Padang District, Padang City which is directly adjacent to the Indian Ocean in the west, so there is a risk of a tsunami disaster. The current evacuation route, which is one of the efforts to overcome the tsunami disaster, seems to be still ineffective to use because the distance that must be covered is 3-5 km in less than 30 minutes. This study aims to determine the direction of an effective evacuation route and then make a comparison with the evacuation route that has been determined by the Government. The method used is Network Analyst. The results of this study obtained 3 alternatives to make evacuation more effective. The alternative is to make access roads around Jalan Gajah to go to P-TES in the UNP area. Alternative 2 is to make P-TES in the parking lot of the Air Tawar Health Center so that people around the river mouth can evacuate faster because they are closer. Alternative 3, the community around the North Padang Police Sector can evacuate by heading to P-TES on Jalan Polonia, Air Tawar Timur Village to stay away from the beach. The three alternatives make the evacuation time to 10 minutes by heading to 26 P-TES. In addition, the evacuation map as a result of the analysis is more effective because the route has a route that is more likely to be taken by the community compared to the government evacuation map.

scholarly journals XXXVII. Memoir on the Eastern Branch of the River Indus, giving an Account of the Alterations produced on it by an Earthquake, also a Theory of the formation of the Runn, and some Conjectures on the Route of Alexander the Great; drawn up in the years 1827–1828

1834 ◽  
Vol 3 (3) ◽  
pp. 550-588 ◽  
Author(s):  
Alex Burnes
Keyword(s):  
Alexander The Great ◽  
Sandy Desert ◽  
The West ◽  
The North ◽  
Inland Lake ◽  
Western Shore ◽  
The Indian Ocean ◽  
River Indus ◽  
The Government ◽  
North Western

In the north-western extremity of our Indian possessions, and under the tropic, is situated the small and sterile territory of Cutch, of importance to the government from its advanced position, but of more attraction to the student of history from its western shore being washed by the waters of the classic Indus and from its proximity to the scene of Alexander's glories. Divested, however, of these alluring enticements to enter on its history, Cutch is a country peculiarly situated. To the west it has the inconstant and ever varying Indus. To the north and east the tract called Runn, which is alternately a dry sandy desert and a muddy inland lake. To the south it has the Gulf of Cutch and the Indian Ocean, with waters receding yearly from its shores.

Art. VII.—Notes on Persian Belúchistán. From the Persian of Mirza Mehdy Khán. Published Teheran, July, 1875

1876 ◽  
Vol 9 (1) ◽  
pp. 147-154
Author(s):  
A. H. Schindler
Keyword(s):  
Indian Ocean ◽  
Temperate Climate ◽  
The South ◽  
The West ◽  
The North ◽  
The People ◽  
The Indian Ocean ◽  
The Hill ◽  
Cool Climate

The part of Belúchistán now under Persian rule is bounded upon the north by Seistán, upon the east by Panjgúr and Kej, upon the south by the Indian Ocean, and upon the west by Núrámshír, Rúdbár, and the Báshákerd mountains.This country enjoys a variety of climates; almost unbearable heat exists on the Mekrán coast, we find a temperate climate on the hill slopes and on the slightly raised plains as at Duzek and Bampúr, and a cool climate in the mountainous districts Serhad and Bazmán. The heat at Jálq is said to be so intense in summer that the gazelles lie down exhausted in the plains, and let themselves be taken by the people without any trouble.

Art. VII.—Account of the Province of Rámnád, Southern Peninsula of India. Compiled from the “Mackenzie Collection,” and edited by the Secretary to the Royal Asiatic Society

1836 ◽  
Vol 3 (5) ◽  
pp. 165-188
Keyword(s):  
General Aspect ◽  
The South ◽  
The West ◽  
Asiatic Society ◽  
The North ◽  
Artificial Lakes ◽  
Ancient Times ◽  
The Government ◽  
Royal Asiatic Society ◽  
North Latitude

This province, the government of which is now administered by the British, formed in ancient times the greater part of the principality, or fiefship, of the Sétu-pattis, the chiefs or guardians of the passage leading from the continent of India to the island of Ráméswara, and thence to the opposite coast of Ceylon, called Ráma's Bridge, or Adam's Bridge. These chieftains, dating their authority from the period of the establishment of a place of pilgrimage on the island of Ráméswara, by the Great Ráma, claim an antiquity even higher than that of the Pándyans, or kings of Madura, but to whom, it would appear, that they were, in general, tributary, though now and then asserting and maintaining their independence. Of their history, however, we are not now to speak, but of the province as it was in the year 1814, when the data were taken from which chiefly the following account is compiled. It lies between the ninth and tenth degrees of north latitude, and the seventy-eighth and seventy-ninth of east longitude; is bounded on the north by the provinces of Tanjore and Pudukotta, on the south and east by the sea, and on the west by the districts of Tinnevelly, Madura, and Sivaganga; and comprehends an area of nearly two thousand five hundred square miles. Its general aspect is that of high and low lands, the latter having numerous artificial lakes, constructed for the purpose of promoting cultivation; the former exhibiting a variety of dry grain-fields, while the northern districts abound with extensive groves of Palmyra trees, with scarcely a vestige of jungle. The whole is divided into seventeen districts, comprising one thousand six hundred and sixtyeight towns and principal and subordinate villages, with a population, at the period to which we allude, of about one hundred and fifty-seven thousand.

scholarly journals III. Account of three unpublished Greek Coins, in Letters from the Rev. Stephen Weston, B.D. F.R.S. and F.A.S. to the Earl of Leicester, President

Archaeologia ◽  
1812 ◽  
Vol 16 ◽  
pp. 9-13
Author(s):  
Stephen Weston
Keyword(s):  
Free State ◽  
The West ◽  
The North ◽  
The Government ◽  
North And South

I have the honour to present to your Lordship and the Society, for their inspection, a curious, unpublished, autonomous, small brass coin of Sala in Phrygia, in fine preservation, of excellent workmanship, and undoubted antiquity. The type of this coin is a bearded, and laureated head, and on the reverse a bunch of grapes with the letters CAΛH very distinct: the NΩN, or termination of the word CAΛHNΩN, is now not visible, owing to the nun, omega, and nun, having been clipped, in order to reduce the size of, the coin, that it might be set as a gem. This we know has been sometimes the case with coins of superior workmanship. The position of Sala was upon the Mænder, between Pylaceum and Gazèna, to the north and south of it, making the boundary of Phrygia towards Lycia. Its longitude, in Mercator's map, is from Ptolemy 60–15, and latitude, which is reckoned, after its longitude, is 38–20. It lies on the river to the west of Mount Taurus, between the Lycus and the Mænder. This Sala, in Phrygia magna, is not mentioned by Stephanus Byzantinus, Strabo, or D'Anville; and, although passed over in silence by these great names in geography, richly deserves to be recorded, were it only for its excellence in the numismatic art, in its free state, and under the government of its own laws.

Validation of the replacement name Eusceliotes Stebbing, 1888 for the pelagic hyperiidean amphipod genus Euscelus Claus, 1879 (Crustacea: Amphipoda: Hyperiidea: Parascelidae), preoccupied by Euscelus Schoenherr, 1833 (Insecta: Coleoptera: Attelabidae)

Zootaxa ◽  
2017 ◽  
Vol 4254 (3) ◽  
pp. 377
Author(s):  
WOLFGANG ZEIDLER
Keyword(s):  
North Atlantic ◽  
West Indies ◽  
North Atlantic Ocean ◽  
Zoological Museum ◽  
Leaf Rolling ◽  
The West ◽  
The North ◽  
Large Genus ◽  
The Indian Ocean ◽  
The Caribbean

The generic name Euscelus was originally proposed by Schoenherr (1833: 205) for a genus of Leaf Rolling weevils (Insecta: Coleoptera: Attelabidae). It is a valid name, in current use, for a relatively large genus of weevils, widespread in northern South America and central America, including the West Indies and the Caribbean (e.g. Hamilton 2007; Legalov 2007). Euscelus Claus, 1879 was established as a monotypic genus of pelagic amphipod (Crustacea: Amphipoda: Hyperiidea: Parascelidae). It is a very rare genus, still monotypic, with the only species, E. robustus Claus, 1879, having been recorded only twice in the literature prior to my review of the families and genera of the superfamily Platysceloidea (Zeidler 2016); initially by Claus (1879), from the Indian Ocean (off Zanzibar), and secondly by Spandl (1927), from the North Atlantic Ocean (off the Azores). Both authors only recorded males. While examining the collections of the Zoological Museum, University of Copenhagen (Zeidler 2016) more specimens of this rare species were located amongst the collections of the Dana expeditions of 1928–1930 (Jespersen & Tåning 1934), thus enabling a more complete description of the species including that of females. It was recently brought to my attention that, according to the data base Interim Register of Marine and Nonmarine Genera (Rees 2016), Euscelus Claus, 1879 is a junior homonym of Euscelus Schoenherr, 1833. While researching this problem I discovered that Stebbing (1888) had also become aware of this homonymy and had suggested the replacement name Eusceliotes. Unfortunately, Stebbing (1888) only refers to the name in his index (pp. 1672, 1699) and hence subsequent authors were unaware of the above homonymy and Stebbing’s replacement name, although it is listed by Neave (1939: 370). The purpose of this communication is to resolve the above homonymy by validating Stebbing’s (1888) replacement name. This action is preferred to proposing yet another new name for Euscelus Claus, 1879, in order to avoid further confusion, because Stebbing’s name, Eusceliotes, already exists in the literature (Stebbing 1888, Neave 1939). 

Predictability of Indian Ocean Dipole (IOD)

2016 ◽  
Author(s):  
Jing-Jia Luo
Keyword(s):  
Indian Ocean ◽  
El Niño ◽  
El Nino ◽  
Tropical Indian Ocean ◽  
The West ◽  
The North ◽  
The Pacific ◽  
Westerly Winds ◽  
Ocean Atmosphere ◽  
The Indian Ocean

This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Climate Science. Please check back later for the full article. The tropical Indian Ocean is unique in several aspects. Unlike the Pacific and the Atlantic Oceans, the Indian Ocean is bounded to the north by a large landmass, the Eurasian continent. The large thermal heat contrast between the ocean in the south and the land in the north induces the world’s strongest monsoon systems in South and East Asia, in response to the seasonal migration of solar radiation. The strong and seasonally reversing surface winds generate large seasonal variations in ocean currents and basin-wide meridional heat transport across the equator. In contrast to the tropical Pacific and the Atlantic, where easterly trade winds prevail throughout the year, westerly winds (albeit with a relatively weak magnitude) blow along the equatorial Indian Ocean, particularly during the boreal spring and autumn seasons, generating the semi-annual Yoshida-Wyrtki eastward equatorial ocean currents. As a consequence of the lack of equatorial upwelling, the tropical Indian Ocean occupies the largest portion of the warm water pool (with Sea Surface Temperature [SST] being greater than 28 °C) on Earth. The massive warm water provides a huge potential energy available for deep convections that significantly affect the weather-climate over the globe. It is therefore of vital importance to discover and understand climate variabilities in the Indian Ocean and to further develop a capability to correctly predict the seasonal departures of the warm waters and their global teleconnections. The Indian Ocean Dipole (IOD) is the one of the recently discovered climate variables in the tropical Indian Ocean. During the development of the super El Niño in 1997, the climatological zonal SST gradient along the equator was much reduced (with strong cold SST anomalies in the east and warm anomalies in the west). The surface westerly winds switched to easterlies, and the ocean thermocline became shallow in the east and deep in the west. These features are reminiscent of what are observed during El Niño years in the Pacific, representing a typical coupled process between the ocean and the atmosphere. The IOD event in 1997 contributed significantly to floods in eastern Africa and severe droughts and bushfires in Indonesia and southeastern Australia. Since the discovery of the 1997 IOD event, extensive efforts have been made to lead the rapid progress in understanding the air-sea coupled climate variabilities in the Indian Ocean; and many approaches, including simple statistical models and comprehensive ocean-atmosphere coupled models, have been developed to simulate and predict the Indian Ocean climate. Essential to the discussion are the ocean-atmosphere dynamics underpinning the seasonal predictability of the IOD, critical factors that limit the IOD predictability (inter-comparison with El Niño-Southern Oscillation [ENSO]), observations and initialization approaches that provide realistic initial conditions for IOD predictions, models and approaches that have been developed to simulate and predict the IOD, the influence of global warming on the IOD predictability, impacts of IOD-ENSO interactions on the IOD predictability, and the current status and perspectives of the IOD prediction at seasonal to multi-annual timescales.

Building Domestic Support for West Germany's Integration into NATO, 1953–1955

2020 ◽  
Vol 22 (2) ◽  
pp. 133-162
Author(s):  
Jan Uelzmann
Keyword(s):  
Public Relations ◽  
Large Scale ◽  
Federal Republic Of Germany ◽  
Lower Saxony ◽  
The West ◽  
The North ◽  
Public Sentiment ◽  
Competing Events ◽  
The Government ◽  
Domestic Support

Konrad Adenauer's government in the Federal Republic of Germany (FRG) engaged in a large-scale media campaign to create political consent for the FRG's integration into the West, a policy that rested to a large extent on rearmament and entry into the North Atlantic Treaty Organization. To counter public criticism of rearmament, the West German authorities used Mobilwerbung, a company that maintained a fleet of mobile film screening vans. Clandestinely financed by the government, Mobilwerbung brought government-commissioned films and political speakers into the FRG's remotest areas. Based on archival records on deployments in Lower Saxony and North Rhine-Westphalia, this article traces Mobilwerbung's role as a government unit that reacted dynamically to competing events. Through highly detailed reporting on audience reactions, Mobilwerbung served both as a public relations vehicle to foster consent and as an analytical tool that allowed the mapping of public sentiment regarding rearmament.

North Atlantic Treaty Organization

1957 ◽  
Vol 11 (1) ◽  
pp. 195-199
Keyword(s):  
Federal Republic ◽  
North Atlantic ◽  
Military Service ◽  
North Atlantic Treaty Organization ◽  
German Federal Republic ◽  
The West ◽  
The North ◽  
Compulsory Military Service ◽  
The Government ◽  
German Parliament

On September 28, 1956, Lord Ismay, Secretary General, called a special meeting of the Council of the North Atlantic Treaty Organization (NATO) to consider the implications of the decision by the government of the German Federal Republic to request the west German parliament to establish the term of national compulsory military service at 12 in lieu of 18 months. The Council feared that this decision would very probably prevent the German Federal Republic from meeting its commitments to NATO. The west German representative stated that his government would meet its previously negotiated commitments both as to quality and quantity; west German regular forces would be raised from 230,000 to 300,000 to compensate for the reduction of availability of conscripts. The Council requested the west German representative to inform his government of the concern of the Council.

scholarly journals Art. XXVII.—Notes on Malayalam Literature

1900 ◽  
Vol 32 (4) ◽  
pp. 763-768
Author(s):  
T. K. Krishṇa Menon
Keyword(s):  
Indian Ocean ◽  
Arabian Sea ◽  
The South ◽  
The West ◽  
The Third ◽  
The North ◽  
South West ◽  
The Indian Ocean

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.

Romania since the Revolution

1990 ◽  
Vol 25 (4) ◽  
pp. 484-496 ◽  
Author(s):  
Mark Almond
Keyword(s):  
The Political ◽  
Political Debate ◽  
The West ◽  
Coup D'etat ◽  
The North ◽  
Communist Revolution ◽  
Party Members ◽  
National Salvation ◽  
The Government ◽  
The Revolution

THE VIOLENCE WHICH MARKED THE OVERTHROW OF Nicolae Ceaugescu's regime at Christmas 1989, and the recurrent disorders, especially in Bucharest, which have punctuated developments over the last nine months, have made Romania's experience of anti-Communist revolution strikingly different from that of its neighbours to the north and to the west. Whatever the political and social tensions emerging in Hungary, Czechoslovakia and Poland (and whatever may be the GDR's legacy to a reunified Germany), it is unlikely that the charge of neo-communism will be central to their political debate. It is precisely that charge levelled against the government party (National Salvation Front/FSN) and against the person of Ion Ilescu by various opposition groups, and former prominent dissidents under Ceaugescu, which remains the most emotive issue in Romanian politics. The question of whether the revolution which overthrew Nicolae Ceauyescu and led to the dissolution of the Romanian Communist Party (RCP) was the result of a popular uprising or a coup d'état planned by Party members has haunted Romanian politics through the first nine months of the post-Ceauqescu period.

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