• Title/Summary/Keyword: <한반도>

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Generation and verification of the synthetic precipitation data (고해상도 종합 강우자료 복원 및 검증)

  • Kang, Hyung Jeon;Oh, Jai Ho
    • Proceedings of the Korea Water Resources Association Conference
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    • 2016.05a
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    • pp.142-146
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    • 2016
  • 최근 저해상도 기상자료를 바탕으로 한 단기간에 내린 폭우나 극심한 가뭄 등과 같은 국지적인 기상 예보는 한계가 있기 때문에 고해상도 기상자료에 대한 수요가 증대되고 있으며, 특히 지형이 복잡한 한반도의 경우 지형적인 영향을 고려한 고해상도 기상자료가 요구되고 있다. 하지만 현재 기상청에서 제공하는 남한 지역의 지상 관측 자료는 약 10km의 불규칙한 간격으로 분포하고 있으며 이는 복잡한 남한지역의 지형 특성을 고려하기에는 해상도가 낮아 상세한 기상 현상을 예측하기 힘들다. 또한, 북한의 경우 사용가능한 관측 자료가 부족하여 한반도 전체를 대상으로 한 기상 예보 및 기후 특성 분석에는 한계가 있다. 따라서 본 연구에서는 정량적 강수 예측 모형인 QPM(Quantitative Precipitation Model)을 이용하여 3시간 간격의 현재기후(2000-2014년)에 대한 한반도 지역의 1km 강우 자료를 복원하였다. 관측 자료가 부족한 북한의 경우 재분석 자료를 이용하여 1km 해상도의 강우 자료를 복원하였다. 이를 위해 몇 가지 특정한 강우 Case를 선별하였고, QPM 수행 시 필요한 강수, 상대습도, 지위고도, 연직 기온, 연직 바람장 등의 변수에 대하여 남한 지역에 해당하는 지점의 여러 재분석 자료와 실제 남한 지역의 지상/고층 관측 자료와의 비교 및 Correlation 분석을 통해 가장 적절하다고 판단되는 재분석 자료인 NASA에서 제공하는 MERRA Reanalysis data를 선정하였다. 또한, 소규모 지형효과를 고려하기 위한 상세 지형자료로 고해상도 지형 자료인 DEM(*Digital Elevation Model) 1km 자료를 사용하였다. 한반도의 강우를 복원하기 위하여 Barnes 기법을 이용하여 불규칙적으로 분포해 있는 강수량 데이터를 규칙적인 자료로 격자화 하였고, 격자화 한 10km 해상도의 자료를 QPM을 통해 복잡한 지형 특성을 고려한 1km 해상도의 강우 자료로 복원하였다. 또한, QPM의 모의 성능을 검증하기 위하여, 위에서 선별한 특정 강우 Case에 대하여 복원한 1km 강우자료와 200m 이내의 거리에서 겹치는 지상관측자료와의 비교를 통하여 모의 성능을 검증하였다. 본 연구를 통해 복원된 한반도 상세 강우 자료를 통해 통일을 대비한 기상, 농 수산업, 수자원 등 다양한 분야에서 활용 될 수 있으며, 국지적인 폭우 및 가뭄 등의 이상 기상 현상을 분석하는 데 참고 기초 자료로써 활용 될 수 있을 것으로 기대된다.

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A Review of Regional Climate Change in East-Asia and the Korean Peninsula Based on Global and Regional Climate Modeling Researches (전구 및 지역기후 모델 결과에 근거한 동아시아 및 한반도 지역기후 변화 전망 연구 소개 및 고찰)

  • Hong, Song You;Kwon, Won Tae;Chung, Il Ung;Baek, Hee Jeong;Byun, Young Hwa;Cha, Dong Hyun
    • Journal of Climate Change Research
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    • v.2 no.4
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    • pp.269-281
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    • 2011
  • In this review, numerical model results from global and regional climate models are introduced to regional detailed climate changes over East Asia and Korea. In particular, regional climate change scenarios in this region, which are created by several research groups in Korea based on Special Report on Emissions Scenarios (SRES) of IPCC 4th assessment report are introduced and characteristics of the scenarios are investigated. Despite slight differences in intensity, all scenarios reveal prominent warming over the Korean peninsula in future climate. Changes in precipitation amount vary with given scenarios and periods, but the frequency and intensity of heavy precipitation generally tend to increase in all scenarios. South Korea except for mountainous regions is expected to change into subtropical climate in future, which accompanies distinct changes in ecosystems and seasons.

Historic specimens collected from the Korean Peninsula in the early 20th century (II) (20세기초에 채집된 한반도 고표본 (II))

  • SUN, Eun-Mi;CHANG, Kae Sun;SON, Hyun-Duk;IM, Hyoung-Tak
    • Korean Journal of Plant Taxonomy
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    • v.49 no.3
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    • pp.240-252
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    • 2019
  • Many of the historic plant specimens collected on the Korean Peninsula in the early twentieth century were lost during the Korean War, though some of them were deposited in the herbarium of Tokyo University (TI) and thus remained unharmed. Data on historic Korean plant specimens at TI are very important given the lack of current data on North Korean plants. Moreover a number of unidentified Korean historic specimens are present at TI. We carried out an identification process and created a list of plants in a newly found collection held by Dr. Ikuma Yoichiro, a Japanese entomologist. He traveled from Cheongjin to Hyesanjin via Baekdu-san (Mt.) in August of 1913 and collected 240 species. We also secured one duplicate set.

Tectonic Movement in the Korean Peninsula (II): A Geomorphological Interpretation of the Spatial Distribution of Earthquakes (한반도의 지반운동 (II): 한반도 지진분포의 지형학적 해석)

  • Park, Soo-Jin
    • Journal of the Korean Geographical Society
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    • v.42 no.4
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    • pp.488-505
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    • 2007
  • The purposes of this research are twofold; 1) to verify spatial differences of tectonic movement using the spatial distribution of earthquakes, and 2) to infer mechanisms that generate spatial accumulation patterns of earthquakes in the Korean Peninsula. The first part of this sequential paper (Park, 2007) argues that the Korean Peninsula consists of four geostructural regions in which tectonic deformation and consequent geomorphological development patterns are different from each other Since this conclusion has been made by terrain analyses alone, it is necessary to verify this suggestion using other independent geophysical data. Because earthquakes are results of movement and deformation of land masses moving in different directions, the distribution of earthquake epicenters may be used to identify the direction and rates of land mass movement. This paper first analysed the spatial distribution of earthquakes using spatial statistics, and then results were compared with the spatial arrangement of geostructural regions. The spatial distribution of earthquakes in the Korean Peninsula can be summarized as the followings; firstly, the intensity of earthquakes shows only weak spatial dependency, and shows large difference even at adjacent regions. Secondly, the epicenter distribution has a clear spatial accumulation pattern, even though the intensity of earthquake shows a random pattern. Thirdly, the high density area of earthquakes shows a clear 'L' shape, passing through Pyeongannam-do, centered at Pyeongyang, and Hwanghae-do, Seosan and Pohang. The correlation coefficient between the density of earthquakes and distance from geostructral region boundaries is much higher than those between the density of fault lines and distance from tectonic division boundaries. Since fault lines and tectonic divisions in the Korean Peninsula are the results of long-term geological development, there is an apparent scale discrepancy to find significant correlations with earthquakes. This result verifies the research hypothesis that the Korean Peninsula is divided into four geostructral regions in which each has its own moving direction and spatial deformation characteristics. The existence of geostructural regions is also supported by the movement parrerns of land masses estimated from the GPS measurements. This conclusion is expected to provide a new perspective to understand the geomorphological developments and the earthquake occurrences in the Korean Peninsula.

Tectonic Movement in the Korean Peninsula (I): The Spatial Distribution of Tectonic Movement Identified by Terrain Analyses (한반도의 지반운동 ( I ): DEM 분석을 통한 지반운동의 공간적 분포 규명)

  • Park, Soo-Jin
    • Journal of the Korean Geographical Society
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    • v.42 no.3 s.120
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    • pp.368-387
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    • 2007
  • In order to explain geomorphological characteristics of the Korean Peninsula, it is necessary to understand the spatial distribution of tectonic movements and its causes. Even though geomorphological elements which might have been formed by tectonic movements(e.g. tilted overall landform, erosion surface, river terrace, marine terraces, etc.) have long been considered as main geomorphological research topics in Korea, the knowledge on the spatial distribution of tectonic movement is still limited. This research aims to identify the spatial distributions of tectonic movement via sequential analyses of Digital Elevation Model(DEM). This paper first developed a set of terrain analysis techniques derived from theoretical interrelationships between tectonic uplifts and landsurface denudation processes. The terrain analyses used in this research assume that elevations along major drainage basin divides might preserve original landsurfaces(psuedo-landsuface) that were formed by tectonic movement with relatively little influence by denudation processes. Psuedo-landsurfaces derived from a DEM show clear spatial distribution patterns with distinct directional alignments. Lines connecting psuedo-landsufaces in a certain direction are defined as psuedo-landsurface axes, which are again categorized into two groups: the first is uplift psuedo-landsurface axes that indicate the axis of landmass uplift; and the second is denudational psuedo-landsurface axes that cross step-shaped pusedo-landsurfaces formed via surface denudation. In total, 13 axes of pusedo-landsurface are identified in the Korean Peninsula, which show distinct direction, length, and relative uplift rate. Judging from the distribution of psudo-landsurfaces and their axes, it is concluded that the Korean Peninsula ran be divided into four tectonic regions, which are named as the Northern Tectonic Region, Center Tectonic Region, Southern Tectonic Region, and East Sea Tectonic Region, respectively. The Northern Tectonic Region had experienced a regional uplift centered at the Kaema plateau, and the rate of uplift gradually decreased toward southern, western and eastern directions. The Center Tectonic Region shows an arch-shaped uplift. Its uplift rate is the highest along the East Sea and the rate decreases towards the Yellow sea. The Southern Tectonic Region shows an asymmetric uplift centered a line connecting Dukyu and Jiri Mountains in the middle of the region. The eastern side of the Southern Regions shows higher uplift rate than that of the western side. The East Sea Tectonic Region includes south-eastern coastal area of the peninsula and Gilju-Myeongchun Jigudae, which shows relatively recent tectonic movements in Korea. Since this research visualizes the spatial heterogeneity of long-term tenonic movement in the Korean peninsula, this would provide valuable basic information on long-term and regional differences of geomorphological evolutionary processes and regional geomorphological differences of the Korean Peninsula.

A Review of Recent Climate Trends and Causes over the Korean Peninsula (한반도 기후변화의 추세와 원인 고찰)

  • An, Soon-Il;Ha, Kyung-Ja;Seo, Kyong-Hwan;Yeh, Sang-Wook;Min, Seung-Ki;Ho, Chang-Hoi
    • Journal of Climate Change Research
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    • v.2 no.4
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    • pp.237-251
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    • 2011
  • This study presents a review on the recent climate change over the Korean peninsula, which has experienced a significant change due to the human-induced global warming more strongly than other regions. The recent measurement of carbon dioxide concentrations over the Korean peninsula shows a faster rise than the global average, and the increasing trend in surface temperature over this region is much larger than the global mean trend. Recent observational studies reporting the weakened cold extremes and intensified warm extremes over the region support consistently the increase of mean temperature. Surface vegetation greenness in spring has also progressed relatively more quickly. Summer precipitation over the Korean peninsula has increased by about 15% since 1990 compared to the previous period. This was mainly due to an increase in August. On the other hand, a slight decrease in the precipitation (about 5%) during Changma period (rainy season of the East Asian summer monsoon), was observed. The heavy rainfall amounts exhibit an increasing trend particularly since the late 1970s, and a consecutive dry-day has also increased primarily over the southern area. This indicates that the duration of precipitation events has shortened, while their intensity became stronger. During the past decades, there have been more stronger typhoons affecting the Korean peninsula with landing more preferentially over the southeastern area. Meanwhile, the urbanization effect is likely to contribute to the rapid warming, explaining about 28% of total temperature increase during the past 55 years. The impact of El Nino on seasonal climate over the Korean peninsula has been well established - winter [summer] temperatures was generally higher [lower] than normal, and summer rainfall tends to increase during El-Nino years. It is suggested that more frequent occurrence of the 'central-Pacific El-Nino' during recent decades may have induced warmer summer and fall over the Korean peninsula. In short, detection and attribution studies provided fundamental information that needed to construct more reliable projections of future climate changes, and therefore more comprehensive researches are required for better understanding of past climate variations.

One unrecorded species from Korea: Suaeda malacosperma Hara (나문재속 한반도 미기록식물 1종)

  • Shim, Hyun-Bo;Chung, Joo-Young;Choi, Byoung-Hee
    • Korean Journal of Plant Taxonomy
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    • v.31 no.4
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    • pp.383-387
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    • 2001
  • One unrecorded species of Suaeda is found from the western and southern coast of Korea. The morphological characteristics and habitat of the plant are described. The species is distinguished from the other Korean species in the genus by its thin and broad leaves and the stellate shape of fruits.

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First Record of Odontobutid fish, Odontobutis obscura (Pisces, Gobioidei) from Korea (한국산 동사리과 어류의 1 미기록종, Odontobutis obscura (Pisces, Gobioidei))

  • Chae, Byung-Soo
    • Korean Journal of Ichthyology
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    • v.11 no.1
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    • pp.12-16
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    • 1999
  • Four specimens of the odontobutid fish, Odontobutis obscura (Temminck et Schlegel) of the family Odontobutidae were collected for the first time from Koje Island, Kyongsangnam-do, Korea. Odontobutis obscura was easily discriminated from congeners in that this species have no sensory canals at preoperculomandibular and supraorbital pit lines on head and the first band on lateral side of body is extending from the middle of the first dorsal fin. This species distributes in western Japan mainly and Koje island which situates southernmostly in Korean Peninsula. So a new Korean name "Nambangdongsari" is proposed.

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전(電)력질주_2 - 한반도 통일, 철저히 준비해야 '대박'

  • 대한전기협회
    • JOURNAL OF ELECTRICAL WORLD
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    • s.454
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    • pp.68-69
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    • 2014
  • 올 해 우리나라에서 가장 많이 회자된 단어 중 하나가 '통일대박'이 아닐까 싶다. 그런데 과연 한반도의 통일이 우리에게 대박을 가져다줄까. 이 질문에 대해 다른 분야에서는 모르겠지만, 전력산업 분야에 있어서 만큼은 '대박'을 충분히 기대할 수 있다는 것이 중론이다. 하지만 이 '대박'은 준비된 자만이 누릴 수 있는 혜택이라는 점 역시 분명한 사실이다. 그동안 전력분야에서 200만kW 대북송전 등 다양한 분야에서 논의가 있어 왔지만 북한의 전압체계가 어떻게 되는지, 전력망이 어떻게 연계돼 있는지 등 실상을 정확히 아는 이가 없는 것이 현 실태다. 이런 가운데 지난달 15일 국회 신성장산업포럼(대표 노영민 국회의원)이 주최하고 전기산업진흥회 전기연구원이 주관한 '남북 전력기자재 통일포럼'은 그 준비의 필요성을 알렸다는 점에서 의의를 찾을 수 있을 것이다. 포럼에서 나온 내용을 결론적으로 분석하면, 이제부터 철저히 준비하지 않으면 한반도가 통일이 되더라도 우리가 '대박'을 칠 수 없다는 점이다. 따라서 지금부터라도 정부를 중심으로 한전 등 전력그룹사, 전기계 협 단체, 관련 기업 등 범 전기계가 나서 통일대박을 위한 준비에 철저를 기해 나가야 할 것이다.

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한반도 남서지역 여름철 강수량의 시.공간 특성

  • Lee, Yeong-Seop;Kim, Hye-Jung;Yeom, Jun-Geun;Jo, Cheon-Ho;Jeong, Hyo-Sang
    • 한국데이터정보과학회:학술대회논문집
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    • 2003.10a
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    • pp.115-121
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    • 2003
  • 최근 빈번한 여름철 집중호우로 인하여 인명과 재산에 큰 피해를 보고 있다. 이러한 여름철 집중호우에 대한 시, 공간적 변동 특성 분석의 필요성이 증가되고 있다. 이에 최근에 빈번히 집중호우가 발생하는 한반도 남서 지역에 18개 관측 지점에 대해 1981년부터 2000년까지 시간별, 연도별 집중호우의 빈도수를 조사하였다. 분석결과, 최근에 집중 호우의 빈도는 증가하였으며 1일 집중호우 빈도는 해안지방이 많았으며, 시간당 집중호우 빈도는 해안지역 뿐만 아니라 산악 또는 내륙 지역에서도 증가하였다. 또한 시간별 집중호우는 해안지역의 경우에는 새벽에 많았으나 산악 또는 내륙 지역은 오후에 빈도수가 많았다. 월별 집중호우는 8월, 7월, 9월, 6월 순으로 많았다. 8월이 가장 많은 이유는 장마 종료 후 태풍의 영향이 컸음을 알 수 있다. 이러한 분석 결과를 기초로 하여 향후 한반도 남서 지역 집중 호우 발생에 대한 시..공간적 변동의 기후학적 특성에 대한 이해력 향상에 도움이 될 것이다.

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