• Journal of The Geomorphological Association of Korea
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• v.19 no.4
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• pp.97-108
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• 2012

There exist plenty of geomorphological resources in Haean Basin, Yonghwasan Mt., and Gandong Basin in Eastern DMZ area in Gangwon Province which can be used as geotourism resources. Meticulous strategies are necessary to improve the geotourism bases in such a mountainous region. Potential geosites including Yongneup and Simjeog wetlands are nearby, so it is necessary to include these geosites when planning geotourism courses. The values of these sites coinciding with the goal of geopark are as follows: this region shows contrasting landforms derived from distinctive rocks such as gneiss and biotite granite, and there are many landforms derived from differential weathering of granite too. They can be used to explain the developmental history of numerous basin structures in entire Korean peninsula.

• Journal of Wetlands Research
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• v.15 no.2
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• pp.179-189
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• 2013

The Haean basin is a unique geographical feature formed by differential erosion and it borders the military demarcation line. Recently the basin has become an interest of civilians due to security tour, highland vegetables and wetland. After the civil war, the population decreased but it has increased since 2007. The annual mean air temperature in the basin has increased with a rate of $+0.016^{\circ}C/yr$ and the annual precipitation also has increased with a rate of +10.41 mm/yr. The precipitation occurring in June~August (wet season) occupied most of the total precipitation increase. In addition, recently the number of groundwater wells and its use have gradually increased and most of them are for agriculture including cultivation of rice and highland vegetables. If the air temperature further increases in the future according to the climate change scenarios, the highland vegetables cultivation will be difficult. Furthermore, if the rainstorm in the summer will be enforced, the groundwater recharge and water management will be aggravated. Therefore, an evaluation for sustainable groundwater development in the basin and a reform of the current agriculture (change of cultivating crops) depending on much water are essentially required.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
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• 1996.10a
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• pp.151-155
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• 1996

지중해의 조석 현상은 그 크기가 수 cm 정도로서 큰 관심을 갖지 못했는데 근해의 위성 고도계에 의한 순환 연구가 활발해 짐에 따라 조석 모델링이 시작되고 있다(Tsimplis 등, 1995; Kantha, 1994). 지중해는 Sicily 해협을 중심으로 두 개의 분지로 나뉘어져 서측 분지는 지브랄타 해협을 통해 대서양과 연결되며 아드리아해와 에게해는 오트란드 해협과 크레테 해협을 동해 동측 분지와 연결되고 있다. (중략)

• Proceedings of the Korea Water Resources Association Conference
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• 2015.05a
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• pp.145-145
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• 2015

본 연구에서는 SWAT(Soil and Water Assessment Tool) 모형을 이용하여 고랭지 농업 지역인 해안분지유역($63km^2$)을 대상으로 RCP 기후변화 시나리오에 따른 미래 수문순환 전망을 평가하였다. 모형의 보정(2009년-2010년) 및 검증(2011년)은 3지점의 실측된 유출량을 활용하여 실시하였다. 모형의 보정 및 검증 결과 결정계수($R^2$)는 X.XX-X.XX이고, Nash-Sutcliffe 모형 효율(NSE)는 X.XX-X.XX으로 분석되어 신뢰성 있는 유출량 모의 결과를 나타내었다. 미래 기후변화 시나리오는 기상청에서 제공하는 HadGEM3-RA 모형의 RCP 4.5 및 8.5 자료를 수집하였다. 다음으로 과거 13년(1999년-2011년, Baseline period)의 기상자료를 기준으로 편이보정(Bias Correction)기법을 이용하여 오차보정 후, SWAT 모형에 적용하여 2040s(2020년-2059년) 및 2080s(2060년-2099년) 기간에 대해서 분석하였다. 그 후, 수문요소인 증발산, 토양수분, 지표유출, 중간유출, 회귀유출 및 하천유출량의 변화량을 분석하여 고랭지 농업 유역의 기후변화에 따른 미래 수문순환을 전망하였다.

• Journal of the Korean association of regional geographers
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• v.16 no.4
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• pp.339-354
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• 2010

In this study, diurnal and intra-seasonal variations of summertime temperature lapse rate (TLR) by synoptic weather conditions in a mountainous basin are examined based on hourly temperature data observed in 2009 summer at an Automatic Weather Station (AWS) network deployed in Haean basin (called Punch Bowl), Yanggu in the Republic of Korea. Summertime average TLR between the top and bottom of the basin is $-0.53^{\circ}C$/100m. Due to its diurnal variations, TLR shows the lowest by $-0.25^{\circ}C$/100m at 6AM, while it maximizes up to $-0.85^{\circ}C$/100m between 4PM~5PM. Comparisons of daily average TLRs by synoptic weather patterns reveal that the magnitude of TLRs is greatest in the order of rainy days ($-0.63^{\circ}C$/100m), heavy rainfall days ($-0.53^{\circ}C$/100m), partly cloudy days ($-0.47^{\circ}C$/100m), and sunny days ($-0.39^{\circ}C$/100m). At dawn on sunny days in summer, strong cooling pools accompanying temperature inversion layers are formed within the basin, while on heavy rainfall days, warming pools are observed due to relatively low TLRs associated with the reduction of surface radiation cooling by clouds.

• Journal of The Geomorphological Association of Korea
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• v.19 no.3
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• pp.135-142
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• 2012

The map drawn on a scale of 1 to 50,000, modern Korea map drawn on a scale of 1 to 50,000 made by Japanese colonial era in 1910s, is the first topographical map using modern technical method. The map has been mainly used in human activities and geographic viewpoint, recently it is available on various field with recognizing high accuracy. It is especially expected that the map will provide us with lots of information on long-term change of topography in field of coastal area which is built on coastal structure. This study presents a method for analyzing before and after geographic change of coastal structure in independent drift sand system. The reference point to analyze long-term coastal geographic change was selected the map of 1910s.

• Journal of Korean Society of Coastal and Ocean Engineers
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• v.22 no.3
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• pp.143-148
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• 2010

Changes in coastline length and land area as well as coastline attribute distribution in Anmyondo were quantified by comparing topographic map produced in 1910's with coastline survey database compiled in 2003. Numerous reclamation has simplified complicated coastline, which resulted in reducing coastline length by 58% but increasing land area by 36%. In 2003, gravel coastline was mostly dominated. Coastline of tidal barrier also reached up to 33% of overall coastline. Gravel coastline occurred dominantly at the eastern side of Anmyondo, whereas sand coastline at the western side. An application of coastline attribute to coastal erosion zone required accurate coastline data, but it was conceived that the topographic map produced in 1910's was not useful for this purpose.

• Journal of The Geomorphological Association of Korea
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• v.19 no.4
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• pp.39-57
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• 2012

The volcanic edifice of Ulleungdo is largely divided into a shield volcano underwater and a tholoide above seawater. The geological features of the volcano above seawater are basically alkali volcanic rocks that are further divided into five geological strata: agglomerates and tuffs trachyte and phonolite trachytic pumice trachyandesite, and sedimentary layer. The topography of Ulleungdo consists of volcanic landform on the whole, and such volcanic landform is weathered and eroded into various weathering landform, stream landform, coastal landform, structural landform, etc. Major volcanic topography includes caldera basin, central cone, and columnar joint, whereas weathering topography features, tafoni, gnamma, tor, weathered cave, talus, etc. In major coastal topography are sea cliff, wave-cut platform, sea stack, sea arch, sea cave, shingle beach, coastal terrace, etc. For stream topography, its development is minimal except for waterfalls.

• Journal of the Korean association of regional geographers
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• v.2 no.1
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• pp.151-164
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• 1996

The regional division by the characteristics of the drainage patterns is important to understand its physical environment comprehensively, because the drainage network develops in reflecting characteristics of geological, geographical and climatical features in the drainage basin keenly. This study is the attempt to divide physical region in China whose drainage pattern is diverse. Chinese drainage basin is mainly divided into the interior drainage basin and the peripheral drainage basin. The interior drainage basin is divided into (1)the deranged pattern and (2)the centripetal pattern. The peripheral drainage basin is divided into (1)the dendritic pattern, (2)the parallel pattern, (3)the radial pattern and (4)the anastomatic pattern. Drainage patterns of the interior drainage basin are formed by affecting geographical features and climatic conditions mainly. In the peripheral drainage basin, drainage patterns are formed by other factors: the parallel pattern is connected with geological structure lineament by tectonic movement, the radial pattern with changes of the river channel resulted from the Yellow River's overflow, the anastomotic pattern with human's activities. The distributional features of the physical region in China are as follows: The deranged pattern appears in Zangbai Plateau, the centripetal pattern does in arid basin of the northwest China. the parallel pattern does in Hengduan mountains affected strongly by tectonic movement between Yangtze paraplatform and Indian Plate, does in the upper stream of Yangtze River and Ganges River in the south of Qinghai-Xizang Plateau, the radial pattern in Huaihe Haihe River drainage basin appearing in the alluvial fan region of Yellow River's downstream and the anastomotic pattern does in the delta of Yangtze River, in the northern coastal plain of the Jiangsu-Province and in the delta of Zhujiang River. Except these areas in the peripheral drainage basin, the dendritic pattern is usually found in the other areas.

• Proceedings of the Korea Water Resources Association Conference
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• 2016.05a
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• pp.173-173
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• 2016

토양유실은 수생태계에 악영향을 미칠 뿐만 아니라 상수원과 수계를 오염시키는 대표적인 오염원으로 간주되고 있다. 이러한 토양유실에 대한 문제를 해결하기 위해서는 무엇보다 토양유실 발생 현황을 파악하는 것이 중요하다. 토양유실 발생 현황을 파악하기 위하여 SWAT, SATEEC, APEX 등 다양한 수문모형 모델들이 개발되어 왔다. 그러나 각각의 수문모형 모델에서 어떠한 토양유실 산정 공식을 사용하였는지에 따라 모의 결과에서 다소 차이를 보이게 된다. 이에 본 연구에서는 우리나라의 필지나 유역을 대상으로 토양유실량을 산정함에 있어 어떠한 공식이 토양유실에 미치는 영향인자를 가장 잘 모의하는지 분석하여 적용하고자 하였다. 본 연구에서는 분지 특성의 유역으로, 유역 내 경작지가 집약적으로 모여 있어 토양유실 문제가 심각한 양구군 해안면 유역을 대상으로 시범 적용하였다. 토양유실량을 모의하기 위한 모델은 USLE, AOF, RUSLE, MUSLE, MUST, MUSS, MUSI의 공식 중에서 사용자가 지정한 공식에 따라 모의가 가능한 APEX 모델로 선정하였다. 본 연구에서는 양구군 해안면의 실측 유량자료를 기반으로 각 공식에 따른 토양유실량에 대하여 검정 작업을 진행하였으며, 이를 양구군 해안면의 토양유실 실측값과 비교 분석하여 해안면 유역에서 토양유실에 미치는 영향인자를 가장 잘 반영할 수 있는 공식이 무엇인지 확인하였다. 본 연구결과를 통해 양구군 해안면 유역에서 발생하는 토양유실량을 예측할 수 있는 최적의 공식을 확인함으로써 토양유실 관련 연구에 기여할 수 있을 것으로 기대된다. 그러나 본 연구에서는 양구군 해안면 유역을 대상으로 최적의 토양유실 산정공식을 찾았지만, 타 유역의 토양유실량을 평가하기에는 한계가 있다. 따라서 APEX를 이용한 전국단위 토양유실량 평가를 통해 범용화 할 수 있는 공식을 찾는 추가적인 연구를 진행한다면 보다 정밀한 토양유실량 산정이 가능하게 되어 향후 우리나라 토양유실 관련 연구에 큰 기여를 할 것으로 기대된다.