CAUSES OF POWERFUL STORM SURGES OF THE 18TH CENTURY CONFIRMED FROM HISTORICAL RECORDS AND THOSE IN COASTAL SEDIMENTS ON THE WEST COAST OF THE KOREAN PENINSULA

2018 ◽  
Author(s):  
Dong-Yoon Yang ◽  
◽  
Min Han ◽  
Min Han ◽  
Jong Yeon Kim ◽  
...  
2016 ◽  
Vol 2016 ◽  
pp. 1-15 ◽  
Author(s):  
Jae-Won Choi ◽  
Yumi Cha ◽  
Hae-Dong Kim ◽  
Sung-Dae Kang

The present study analyzed the interdecadal variation by applying the statistical change-point analysis to the frequency of the tropical cyclone (TC) that landed in the Korean Peninsula (KP) for the recent 54 years (1951 to 2004) and performed cluster classification of the Korea-landfall TC tracks using a Fuzzy Clustering Method (FCM). First, in the interdecadal variation analysis, frequency of TC that landed in the KP was largely categorized into three periods: high frequency period from 1951 to 1965, low frequency period from 1966 to 1985, and high frequency period from 1986 to 2004. The cluster analysis result of the Korea-landfall TC tracks produced the optimum number of clusters as four. In more detail, Cluster A refers to a pattern of landing in the southern coast in the KP starting from East China Sea followed by heading north while Cluster B refers to a pattern of landing in the west coast of the Korean Peninsula, also starting from East China Sea followed by heading north. Cluster C refers to a pattern of landing in the southern region of the west coast in the KP moving from mainland China while Cluster D refers to a pattern of landing in the mid-north region of the west coast in the Korean Peninsula, also moving from mainland China.


2013 ◽  
Vol 65 ◽  
pp. 254-259 ◽  
Author(s):  
Sok Kuh Kang ◽  
Kyung Tae Jung ◽  
Eun Jin Kim ◽  
Jae Kwi So ◽  
Jong Jin Park

2019 ◽  
Vol 176 (10) ◽  
pp. 4623-4640 ◽  
Author(s):  
Chang Ki Kim ◽  
Seong Soo Yum ◽  
Hyun-Goo Kim ◽  
Yong-Heack Kang

2001 ◽  
pp. 167-180
Author(s):  
Lance van Sittert

Lance van Sittert explores the historical records concerning the exploitation of marine resources along the West Coast of Africa, using them to provide evidence of the commerical importance of the West Coast over the East or South. The date demonstrates a boom-bust cycle along the West Coast, pertaining to whales, snoek, guano, rock lobster, hake, and pilchard.


2019 ◽  
Vol 1 ◽  
pp. 1-2
Author(s):  
Jong-geun Kim

<p><strong>Abstract.</strong> Modern nautical charts, the result of scientific coastal research and survey, had been made from late 18th century, and at the end of 19th century almost of the world had been charted. Different to the neighbouring countries such as China and Japan, Korean peninsula had not been accurately charted until the end of 19th century. Moreover, during the 19th century, the shape of Korean peninsula had been changed several times in the Western nautical charts. However, in the academic circle of the history of cartography, this case was scantly examined. In this presentation, this author, firstly, analyse the changes in the shape of the Korean Peninsula on the British Charts in the 19th Century and, secondly, identifies factors that influence the changes. For this research, British nautical charts, which are the representative and finest charts during the 19th century in the world, are selected. Examined charts are ‘Map of the Islands of Japan Kurile &amp; C.’ (Year of 1811, 1818) of Aaron Arrowsmith (1750&amp;ndash;1823), the hydrographer to his majesty, ‘The Peninsula of Korea (No.1258)’ (year of 1840, 1849) and ‘(Preliminary Chart of) Japan, Nipon Kiusiu and Sikok and a part of the coast of Korea (No. 2347)’ (Year of 1855, 1862, 1873, 1876, 1892, 1898, 1902, 1914) of the British hydrographic office. According to the analysis, major shape changes of the Korean Peninsula were occurred in 1818, 1840, 1849, 1855, 1862, 1873, 1876, 1892, and the shape of the Peninsula became perfect in the chart of the year 1914.</p><p>Meanwhile, the factors of the shape changes of the Korean peninsula in these nautical charts were various voyages, expeditions, and military surveys to Korea. For example, the change in the map of 1818 was initiated by the voyage of the captain Basil Hall in 1816 to the west coast of Korea, and the change in the map of 1840 was made by the map of Korea of A.J. von Krusenstern (1770&amp;ndash;1846) and the voyage of H.H.Lindsay (1802&amp;ndash;1881) to the west coast of Korea in 1832. Moreover, the modification of 1849 was made by the outcome of E. Belcher’s scientific survey around Jeju Island and other southern islands of Korea. In 1852, French admiral G. de Roquemaurel (1804&amp;ndash;1878) surveyed eastern coast of Korea and drew nautical chart and this chart became the source of the British chart of the year 1855. A Russian admiral, Yevfimy Putyatin (1803&amp;ndash;1883), also surveyed east side of the peninsula and triggered the change of nautical chart of eastern part of Korea. During French campaign against Korea in 1866 and United States expedition to Korea in 1871, French and American navy surveyed west-middle part of the peninsula and added detailed coastline of it and British chart also reflected these changes. The Japan-Korea treaty of 1876 enabled coastal survey of the Korean peninsula by the Japanese navy by the article 7, which permitted any Japanese mariner to conduct surveys and mapping operations at will in the seas off the Korean Peninsula's coastline. By virtue of the treaty, Japan could directly surveyed coastline of Korea and could make updated nautical charts of Korea. These Japanese charts were circulated to the Western countries and British hydrographers made the best use of them. Thanks to this situation, the British admiralty could update the chart of Korean peninsula and the perfect one published in 1914.</p><p>This analysis contribute not only to understand how and why the shape of Korean peninsula changed in British nautical charts during the 19th century, but also to add the historical case of the map trade and geographical knowledge circulation in East Asia.</p>


2021 ◽  
Author(s):  
Woo Hun Ryang ◽  
Alexander R. Simms ◽  
Hyun Ho Yoon ◽  
Seung Soo Chun ◽  
Gee Soo Kong

Abstract. Like most of the world’s coastlines, the Korean Peninsula experienced higher-than-present sea levels during the Last Interglacial (LIG) otherwise known as Marine Isotope Stage (MIS) 5e. However, the expression of that highstand in sea levels differs across the eastern and western Korean Peninsula. The active east coast of the Korean Peninsula is characterized by broad uplifted marine terraces, while the stable west coast is characterized by tidal flats and rias. In this study, we used a standardized database template to review and extract the existing constraints on LIG sea levels along both the east and west coasts of the Korean Peninsula. A total of 62 LIG constraining data points were compiled including 34 sea-level indicators, 22 marine limiting records, and 6 terrestrial limiting records. The ages from these data points are based on 61 optically stimulated luminescence (OSL) measurements and 1 paleomagnetic-based age. Along the uplifted east coast, LIG sea-level indicators based on marine terraces are at elevations ranging from +9 to +32 m. The uplifted marine terraces are cut or otherwise deformed by faults developed under a compressional regime due to backarc closing of the East Sea since the early Pliocene. As a result, tectonic uplift likely contaminates the elevation of the east coast LIG shorelines. On the contrary, LIG sea-level constraints on the west coast of the Korean Peninsula are found at heights of between +2 and +5 m and include marine and terrestrial limiting records as well as true sea-level indicators. The LIG sea-level constraints along the west coast of the Korean Peninsula are likely uncontaminated by vertical movement or experienced minor subsidence during the Quaternary.


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