• 한국농림기상학회지
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• 제6권4호
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• pp.218-234
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• 2004

근래 지구온난화현상과 더불어 우리나라에 '춥지 않은 겨울' 날씨가 지속됨에 따라 가을보리 안전재배지역의 북상이 논의되고 있다. 본 연구는 '춥지 않은 겨울' 날씨를 보인 1987년부터 2000년까지 14년과 평년 (1971∼2000년)의 평균기온과 최저기온을 바탕으로 새로운 가을보리의 안전재배지대 설정을 시도하였던바 그 결과는 다음과 같다. 1. 평년(1971∼2000년)의 1월 평균기온의 산술평균값에 의한 겉보리의 안전재배지대는 강화-이천-충주-춘양-고성 지역을, 쌀보리는 천안-금산-문경-안동-속초 지역을, 맥주보리는 광주-장흥-산청-포항-울진 지역을 잇는 선으로 구분되었다. 반면에, '춥지 않은 겨울' 날씨를 보인 14년(1987∼2000년)동안의 기상조건을 기준으로 하였을 때는 가을보리 안전재배지대가 평년기준보다 북상하여, 겉보리는 포천-춘천-원주-양평-춘양 지역을, 쌀보리는 강화-이천-충주-의성-고성 지역을, 맥주보리는 군산-순천-진주-밀양-울진 지역을 잇는 선으로 구분 되었고, 내한성이 가장 강한 품종들(올보리 등)은 인제, 홍천, 태백, 제천지역 등 태백산맥의 인근지역까지도 안전재배가 가능한 것으로 나타났다. 2.평년(1971∼2000년)의 재현기간 10년에 해당하는 1월 평균기온에 의한 겉보리의 안전재배지대는 보령-남원-거창-구미-고성 지역을 잇는 선으로 구분되었고, 쌀보리는 서천-정읍-합천-영덕-속초 지역을 잇는 선으로 구분되었으며, 맥주보리는 부산, 통영, 여수 등 남부해안지역에서만 안전하고, 그 밖의 지역들은 10년에 한번이상 저온이 출현할 위험이 있는 것으로 판단되었다. 반면에 '춥지 않은 겨울' 날씨를 보인 14년 (1987∼2000년) 동안의 기상조건에서는 겉보리는 강화-이천-영주-고성 지역을, 쌀보리는 서산-남원-문경-안동-속초 지역을, 맥주보리는 광주-장흥-사천-울산-울진 지역을 잇는 선으로 구분되었고, 내한성이 가장 강한 품종들(올보리 등)은 강화-원주-충주-춘양-고성 지역을 잇는 선으로 구분되었다.

• 한국지역지리학회지
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• 제13권4호
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• pp.454-460
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• 2007

한국전쟁의 결과 한반도의 허리에 해당하는 DMZ 지역은 반세기 이상 인간의 관심에서 잊혀진 공간이었다. 그러나 최근 국 내외적으로 DMZ에 대한 관심이 고조되면서, 오늘날 DMZ를 대상으로 하는 연구는 점차 활발해 지고 있다. 그러나 정작 연구의 대상인 DMZ의 공간적 범위에 대한 연구는 매우 미약하다. 그마저도 선행연구를 분석한 결과 대부분의 연구에서 군사분계선과 DMZ, 한강하구 중립지역, 그리고 NLL에 대한 기술에 있어서 공간적인 오류를 범하고 있었다. 본 연구에서 조사한 결과, 동해안 고성의 명호리에서 서쪽의 임진강 하구에 이르는 군사분계선의 길이는 약 238km(148마일)이고, 군사분계선을 따라 설정되어 있는 DMZ의 면적은 약 $903.8km^2$로 측정되었다. 이는 현재 '155마일 휴전선' 등과 같이 남북을 양분하는 공간을 지칭하는 용어에 대한 재정립이 필요함을 의미하는 것이다.

• 한국응용곤충학회지
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• 제52권4호
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• pp.321-326
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• 2013

백령도와 연평도의 곤충상 조사결과, 통나방과 (나비목: 뿔나방상과)의 11종이 서해안지역에서는 처음으로 기록되었다. 그 중 Coleophora adjunctella Hodgkinson, C. chenopodii Oku, 그리고 C. kurokoi Oku는 한반도에서 처음으로 기록되는 종으로 이들 종 동정에 필요한 성충과 암컷 생식기 사진을 함께 기재한다.

• The Korean Journal of Ecology
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• 제8권2호
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• pp.89-98
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• 1985

Correlations between horizontal distributions of bamboos (Bambusaceae) in the Korean peninsula and environmental factors were studied using taxanomic and geographical literatures, both old and current. The vertical distributions of bamboos on Mt. Chiri were also studied, and environmental factors limiting horizontal and vertical distributions were compared. There are 18 species of bamboos (belonging to 5 genera) distributed in the Korean peninsula. The distributional range of each genus were distinct, although overlapped. Northern limit of bamboos of any species was marked by the line connecting Paikryung Island (124。40'E, 38。00'N), Mt. Changsoo, Mt. Myungji, Mt. Myohyung and Myungchum (129。40'E, 41。10'N). The optimum range of bamboos was concluded to be restricted to several southern province, with annual precipitation over 1,200 mm. The limiting factors on the distribution were inferred to be low temperature and duration of it. Mean daily minimum temperature of January and the number of days with daily mean temperatures below zero during January showed close associations with the distributional range, and an environmental factors favouring the distributrion of bamboos appeared to be vicinity of warm sea current, deep and extended snow acculation and southern exposure. The vertical distribution of bamboos on Mt. Chiri was limited by low temperature, unfavorable topographic and edaphic conditions caused by steep slope. Difference in the vertical limits between SE and NW slopes are caused by the differences in temperature and precipitation between the slopes. Bamboos were more abundant in valleys than on the ridge, apparently because the deeper snow in the valleys protected the plants from low temperature, heavy winter winds and desiccation.

• 한국환경과학회지
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• 제17권12호
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• pp.1331-1341
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• 2008

For providing basic data on estuary conservation and pattern of vegetation succession of sand bar, the flora of delta was investigated from March 2004 to August 2006 in the Nakdong River estuary of Korea. The flora in the eight surveyed areas was composed of total 159 taxa that belonged to 46 families, 123 genera, 133 species, 1 subspecies, 20 varieties, and 5 forms. Among them, naturalized plants and evergreen broad trees were 31 taxa and 5 taxa, respectively. The communities of main species at delta of estuary were composed of 16 species such as Rosa rugusa community, Scirpus triqueter community, Phragmites communis community, Carex kobomugi community, Digitaria ciliaris community. Especially, Rosa rugusa community which are important to establish the southern limit line of distribution as the northern factor was distributed through Jinwoodo. The succession of main vegetation community in the new delta (Doyodeung) was in order of Carex scabrifolia, Scirpus triqueter, Phragmites communis, Imperata cylindrica var. koenigii and Miscanthus sinensis var. purpurascens. Therefore, the succession order of the surveyed area seems to predict the pattern of the vegetation succession of another deltas in Nakdong River estuary.

• 해양환경안전학회:학술대회논문집
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• 해양환경안전학회 2007년도 추계학술발표회
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• pp.57-60
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• 2007

북방한계선 주변의 한강하구는 지난 60년 동안 개발 및 이용이 금지되었기 때문에, 자연하천의 모습을 간직하고 있다. 그러나 최근 들어 경인수로를 비롯한 민간 이용을 위한 논의가 이루어지고 있으나, 한강하구의 기본적인 특성에 관한 정보가 부족한 실정이다. 본 연구에서는, 인공위성 합성개구레이더(SAR)를 이용한 하구역 퇴적상의 변동 조사를 실시하고, 퇴적상을 기반으로 한강하구 뱃길을 제안하고자 한다. 2000년부터 2005년까지의 Radarsat-1 영상을 이용하여 시계열해석한 결과에 따르면, 1) 한강 하구역은 집중호우등 에 의해 부유사가 많이 발생하며, 2) 식생역(vegetated area)은 거의 안정화단계에 있으며, 3) 퇴적상(bar)의 월 변동성은 크지 않으나, 매년 발생하는 호우 등에 의해 퇴적상의 위치 변화는 상당히 컸다. 여기서 얻어진 퇴적상의 변동 특성을 기반으로, 북방한계선 이남의 한강 수역에 대한 뱃길의 설계 방향을 제시하였다. 향후, 장기간에 대한 위성 및 현장 조가를 바탕으로 자연하천의 특성을 훼손하지 않는 범위에서의 개발이 이루어져야 한다.

• 한국환경과학회지
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• 제9권3호
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• pp.215-221
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• 2000

The relationship between the distribution of sea surface temperature(SST) and dinoflagellate(Cochlodinium polykrikoides) bloom areas were studied. The SST data were derived from the infrared channels of AVHRR(Advanced Very High Resolution Radiometer) sensor on NOAA(National Oceanic and Atmospheric Administration) 12 and 14 satellites during 1995-1998. The initial water temperature at C. polykrikoides bloom was about 21${\circ}C$ at the coastal areas of the South Sea and along the shore of the East Sea of Korea during the summer season of 1995. The northern limit of red tides was coincident with that of 21${\circ}C$ isothermal line in the East Sea. The red tides that initially bloomed at the coast of Pohang on September 21, 1995 moved to the coast of Uljin on September 26, 1995. The skipped appearance of the red tides in the areas between Pohang and Uljin was due to the East Korean Warm Current, which was moving offshore from Pohang to approach to Uljin. The cold water which was formed by tidal front in the western coast of the South Sea and by upwelling water from deep layer in the southeastern coast of the Korean peninsula played a role in blocking the spreading of red tides during summer season in 1997 and 1998. In conclusion, the distribution of red tides appeared to be dependent on the initial water temperature at red tides bloom. The SST at the red tides varied from 21${\circ}C$ to 25${\circ}C$; 21${\circ}C$, 23${\circ}C$, 24 and 24-25${\circ}C$ in 1995, 1996, 1997 and 1998, respectively.

• 한국철도학회논문집
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• 제20권5호
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• pp.612-624
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• 2017

기존 수도권 광역철도는 운행시간이 많이 걸리는 완행 위주의 운행을 하기 때문에 통행시간 측면에서 타 교통수단과의 경쟁력이 저하되고 있는 실정이고, 도로교통을 철도로 유인하는데 한계가 있기 때문에 급행열차 운행을 확대 운영해야 한다는 사회적 요구가 지속되고 있다. 특히 수도권 북부와 수도권 남서부 방면은 대도시 생활권 확대로 광역교통수요 증대에 따른 교통 혼잡 가중 및 통행시간 증가 등 사회적 비용이 과다 발생되고 있어 서울도심을 연결하는 급행 기능의 대중교통망체계가 필요하다. 국내에서 가장 효율적으로 급행화를 운행하는 노선은 서울지하철 9호선이며, 김포공항에서 고속터미널까지 27분 소요됨으로써 완행 44분 대비 약 40% 시간 단축 효과가 있고 혼잡도가 최대 240%에 달할 만큼 이용객의 선호도가 상당히 높다. 본 연구의 기술적 결과들은 광역철도의 급행화 방안의 수행을 위해 기여할 수 있을 것이라 기대한다.

• 한국환경복원기술학회지
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• 제23권1호
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• pp.1-14
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• 2020

In this study, we 1) identified the damaged areas along the south limit line (SLL) of the demilitarized zone (DMZ) by the military's 'DMZ barren land campaign', and 2) categorized the identified damaged areas into a few ecological types. Using high-resolution satellite images, we delineated the total damaged areas to be 1,183.2 ha, which accounted for 50.1% of the 100-m northern buffer regions from the SLL. Of the total damaged areas, 16% were severely damaged, i.e., they had been damaged until recently and so remained barren without vegetation cover. In other areas, the levels of damage were either moderate (59.9%) or slight (24.1%), due to natural succession that turned those areas to grassland or forest. Using satellite image-derived land cover maps and climatic and topographic data, we categorized the damaged areas into seven types: lowland grassland (19.8%), western lowland forest (21.4%), low-altitude forest (25.5%), mid-altitude forest (18.4%), high-altitude forest (6.8%), vicinity in east coast (7.9%), and waterbody (0.2%). These types can be used to identify proper measures to restore ecosystems in the DMZ for now and after Korean reunification.

• Strategy21
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• 통권31호
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• pp.27-56
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• 2013

The United Nations Command (UNC) and the communist North failed to reach an agreement on where the maritime demarcation line should be drawn in the process of signing a truce after the Korean War because of the starkly different positions on the boundary of their territorial waters. As a result, the Armistice Treaty was signed on July 1953 without clarification about the maritime border. In the following month, Commander of the UNC unilaterally declared the Northern Limit Line (NLL) as a complementing measure to the Armistice. Referring to this, North Korea and its followers in South Korea wrongfully argue that the NLL is a "ghost line" that was established not based on the international law. However, one should note that the waters south of the NLL has always been under South Korea's jurisdiction since Korea's independence from Japan on August 15, 1945. There is no need to ask North Korea's approval for declaring the territorial waters that had already been under our sovereign jurisdiction. We do not need North Korea's approval just as we do not need Japan's approval with regard to our sovereign right over Dokdo. The legal status of the NLL may be explained with the following three characteristics. First, the NLL is a de facto maritime borderline that defines the territorial waters under the respective jurisdiction of the two divided countries. Second, the NLL in the West Sea also serves as a de facto military demarcation line at sea that can be likened to the border on the ground. Third, as a contacting line where the sea areas controlled by the two Koreas meet, the NLL is a maritime non-aggression line that was established on the legal basis of the 'acquiescence' element stipulated by the Inter-Korea Basic Agreement (article 11) and the Supplement on the Non-aggression principle (article 10). Particularly from the perspective of the domestic law, the NLL should be understood as a boundary defining areas controlled by temporarily divided states (not two different states) because the problem exists between a legitimate central government (South Korea) and an anti-government group (North Korea). In this sense, the NLL problem should be viewed not in terms of territorial preservation or expansion. Rather, it should be understood as a matter of national identity related to territorial sovereignty and national pride. North Korea's continuous efforts to problematize the NLL may be part of its strategy to nullify the Armistice Treaty. In other words, North Korea tries to take away the basis of the NLL by abrogating the Armistice Treaty and creating a condition in which the United Nations Command can be dissolved. By doing so, North Korea may be able to start the process for the peace treaty with the United States and reestablish a maritime line of its interest. So, North Korea's rationale behind making the NLL a disputed line is to deny the effectiveness of the NLL and ask for the establishment of a new legal boundary. Such an effort should be understood as part of a strategy to make the NLL question a political and military dispute (the similar motivation can be found in Japan's effort to make Dokdo a disputed Island). Therefore, the South Korean government should not accommodate such hidden intentions and strategy of North Korea. The NLL has been the de facto maritime border (that defines our territorial waters) and military demarcation line at sea that we have defended with a lot of sacrifice for the last sixty years. This is the line that our government and the military must defend in the future as we have done so far. Our commitment to the defense of the NLL is not only a matter of national policy protecting territorial sovereignty and jurisdiction; it is also our responsibility for those who were fallen while defending the North-Western Islands and the NLL.