We conclude if Jeju Peace Island for Koreas 2018 gets international awareness from participants in the spheres of Peace Island Education & Tourism Welfare Model at the Grass Roots Level, it will contribute to institutionalization of both peace island and welfare tourism. In addition, if Jeju government supports the financial budget for the establishment of a Jeju Peace University or a Jeju Environmental University, our efforts might include an impetus to create and operate a Jeju Peace University or a Jeju Environmental University based on collaborative Jeju Peace Studies in Korea and internationally in the nearer future. Of course, we believe that, through this kind of collaborative leadership, a vision of a Nonviolence Korea “Jeju Peace Island for two Koreas” might serve as a buffer zone potentially approved by the Six Nations in the Asia Pacific region in 2019.

Islanders have tried to find out real alternatives on how to keep sustainable Haenyeo communities through both developing traditional school system at community level (Hansupul Haenyeos School) and advanced school system at university level ( an educational certificate program for Interpreter of Haenyeos Culture and an advanced certificate program for Hanyeos Culture). In oder to share their wisdom of ordinary democratic life style around Bultuk, We created Global Peace Bultuk Assembly for younger generation to succeed in their tradition in July of 2010. It' s a time for us to find out Integrating Policy of the Sustainability of Jeju Haenyeo (Jamnyeo, Jamsu) Community facing their extinction into Jeju Village Conservation Model of Marine Resources Needed.

제주도 연안 정치망의 어획성능을 향상시키기 위한 어구구조개량과 조업방식의 생력화에 대한 기초자료를 제공할 목적으로 현재 제주도 연안 정치망 어장에 부설하여 조업을 행하고 있는 각망어구와 낙망어구의 어획성능을 비교하기 위해서 이들 실물어구를 1/30로 축소하고 제작한 모형어구를 이용하여 수조실험을 실시하고 고등어어군, 전갱이 어군, 독가시치 어군의 입·출망 행동을 관찰하고 해석하였는데, 그 결과는 다음과 같다. 1. 어군의 입망율은 경과시간 60초일 때 각망어구에서는 고등어 50%, 전갱이 18%, 독가시치 28%였고, 낙망 어구에서는 고등어 70%, 전갱이 60%, 독가시치 30%였다. 2. 어군의 출망율은 경과시간 60초일 때 각망어구에서는 고등어 70%, 전갱이 40%, 독가시치 24%였고, 낙망어구에서는 고등어, 전갱이가 각각 0%, 독가시치가 3%였다. 3. 어군의 잔존율은 경과시간 60초일 때 각망어구 에서는 고등어 30%, 전갱이 60%, 독가시치 76%였고, 낙망어구에서는 고등어, 전갱이가 각각 100%, 독가시치가 97%였다.

A model experiment of purse seine by the circulating water tank was carried out on the changes of net shape and the tension of purseline under operation in two layer current. In the circular tank, the two layer current was made by cutting off the current of upper layer and producing the bottom current by the equipment shown in Fig. 1. The model experiment of purse sein was made on a reduced scale 1 :400, and the experiment was carried out according to the Tauti's model law. When the bottom current of O. 5 knot flows to lower part of three-eighths of net, following results are derived. The depth of sinkerline reached only about 80% of that of no current set. The horizontal shift of sinker line caused by the bottom current is maximized in tight set. The enclosed area by the floatIine immediately after the completion of set net is 61. 5% in tight set, 50. 0 % in loose set and 54. 1 % in lateral set of those in the case of no current. In the first half period of pursing, the tension of the purseline is enhenced by the bottom current and the pattern of increasing is irregular in the tension curves.

In order to investigate the performance for the mackerel purse seine of one boat purse seiner using in the sea area of Cheju Island, a model net is made of the scale of 1/400 of its full scale, and model test on the shape of net and the tension of purse line is carried out in the stagnant water channel of the circulating water tank. Designing and testing for the model net are based on the Tauti's law. The obtained results are as follows; 1. The sinking rate of net is maximized the value of 6.40 m/min from 5 to 10 minutes after shooting net, and the mean value is 6.13 m/min. 2. The enclosed area formed with the float line after pursing operation is 76-84% of the area which is formed immediately after the shooting operation. At that time, purse seine is pulled inward the circle of surrounding net about 26.5% of the diameter. 3. In operating, when longitudinal section area of the central part of the net is maximized, the split area of both the wing-ends is 31-32% of the former. 4. When the time for the completing of pursing is 20 minutes, the maximum tension of the purse line is about 10.2 tons.

We used numerical models to reliably analyze the groundwater flow and hydraulic conductivity on Jeju Island. To increase reliability, improvements were made to model application factors such as hydraulic watershed classification, groundwater recharge calculation by precipitation, hydraulic conduction calculation using the pilot point method, and expansion of the observed groundwater level. Analysis of groundwater flow showed that the model-calculated water level was similar to the observed value. However, the Seogwi and West Jeju watersheds showed large differences in groundwater level. These areas need to be analyzed by segmenting the distribution of the hydraulic conductivity. Analyzing the groundwater flow in a sub watershed showed that groundwater flow was similar to values from equipotential lines; therefore, the reliability of the analysis results could be improved. Estimation of hydraulic conductivity distribution according to the results of the groundwater flow simulation for all areas of Jeju Island showed hydraulic conductivity > 100 m/d in the coastal area and 1 45 m/d in the upstream area. Notably, hydraulic conductivity was 500 m/d or above in the lowlands of the eastern area, and it was relatively high in some northern and southern areas. Such characteristics were found to be related to distribution of the equipotential lines and type of groundwater occurrence.

The estimation of groundwater usage in Jeju island is important to understand hydrologic cycle system and to plan management of water resource because large amounts of groundwater have been used for agricultural and domestic purpose. The model has been developed to estimate agricultural groundwater usage for garlic at uplands and citrus at orchards raising outdoors using the soil water balance model from FAO 56, respectively. The total amount of water supplied for the crop evapotranspiration and the multipurpose function such as sprout promotion can be simulated by the model. However, due to the discrepancy of water use in initial stage between calculated and observed, the model was calibrated and verified using actual groundwater usage monitoring data for 3.5 years (2011.6 to 2014.12) at three uplands for garlic and three orchards for citrus. Consequently, it would be concluded that the model simulated efficiently actual water usage in that root mean square (RMS) and normalized RMS of the validation stage were less than 8.99 mm and 2.43%, respectively, in two different conditions.

Groundwater level hydrographs from observation wells in Jeju island clearly illustrate distinctive features of recharge showing the time-delaying and dispersive process, mainly affected by the thickness and hydrogeologic properties of the unsaturated zone. Most groundwater flow models have limitations on delineating temporal variation of recharge, although it is a major component of the groundwater flow system. Recently, a convolution model was suggested as a mathematical technique to generate time series of recharge that incorporated the time-delaying and dispersive process. A groundwater flow model was developed to simulate transient groundwater level fluctuations in Pyoseon area of Jeju island. The model used the convolution technique to simulate temporal variations of groundwater levels. By making a series of trial-and-error adjustments, transient model calibration was conducted for various input parameters of both the groundwater flow model and the convolution model. The calibrated model could simulate water level fluctuations closely coinciding with measurements from 8 observation wells in the model area. Consequently, it is expected that, in transient groundwater flow models, the convolution technique can be effectively used to generate a time series of recharge.

본 연구에서는 잠재증발산량과 실제증발산량간의 보완관계 기반의 증발산량 산정 모형인 Brutsaert and Stricker (1979)의 AA 모형과 Morton (1983)의 CRAE 모형을 제주도내 두 개의 상시하천 유역에 처음으로 적용하고 이 지역에 적합한 모형의 매개변수를 제안하였다. AA 모형과 CRAE 모형의 매개변수 검정과 모형의 검증을 위한 대표유역으로 각각 북제주에 위치한 한천 유역과 남제주에 위치한 강정천 유역을 선정하였다. 한천 유역에 대해 AA 모형의 경험상수 α와 이류에너지항 M, CRAE 모형의 경험상수 B1과 b2를 바꾸어가면서 실제증발 산량을 산정하고 이를 유역수문모델링 결과와의 비교를 통해 매개변수 검정을 수행하였다. 그 결과 AA 모형은 α=1.00, M=30.0Wm-2, CRAE 모형은 b1=33.0Wm-2, b2=1.02이 최적의 값으로 산정되었다. 동일한 매개변수를 사용하여 AA 모형과 CRAE 모형의 검증 대상유역인 강정천 유역에 적용한 결과, 두 모형 모두 식생의 성장기 및 비성장기에 유역수문모델링 결과와 유사한 것으로 분석되었다.

Since Jeju island has depended a water resource on the underground water because of a poor development of the surface flow, Jeju island is in need of the surface resource development to prevent the future shortage of the underground water due to excessive development and use of it. The study shows that the SWAT model(continuous rainfall-runoff model) is applied to estimate the outflow in the drainage watershed area, where it has been urbanized through the change of the land, such as a tourism development, cultivation, housing, and impervious layer road development. Near Oaedo watershed area in Jeju island, weather and topographical SWAT input data were collected, and compared the outflow change of past and present.

The discharge within the basin in Jeju Island was calculated by using SWAT model, which a Semi-distributed rainfall-runoff model to the important rivers. The basin of Chunmi river of the eastern region of Jeju Island, as the result of correcting as utilizing direct runoff data of 2 surveys, appeared the similar value to the existing basin average runoff rate as 22% of average direct runoff rate for the applied period. The basin of Oaedo river of the northern region showed R2 of 0.93, RMSE of 14.92 and ME of 0.70 as the result of correcting as utilizing runoff data in the occurrence of 7 rainfalls. The basin of Ongpo river of the western region showed R2 of 0.86, RMSE of 0.62 and ME of 0.56 as the result of correcting as utilizing runoff data except for the period of flood in 2002~2003. Yeonoae river of the southern region showed R2 of 0.85, RMSE of 0.99 and ME of 0.83 as the result of correcting as utilizing runoff data of 2003. As the result of calculating runoff for the long term about 4 basins of Jeju Island from the above results, SWAT model wholly appears the excellent results about the long-term daily runoff simulation.

The SWAT model developed by the USDA-Agricultural Research service for the prediction of rainfall runoff, sediment, and chemical yields in a basin was applied to Jeju Island watershed to estimate the amount of runoff. The research outcomes revealed that the estimated amount of runoff for the long term on 2 watersheds showed fairly good performance by the long-term daily runoff simulation. The watershed of Chunmi river located the eastern region in Jeju Island, after calibrations of direct runoff data of 2 surveys, showed the similar values to the existing watershed average runoff rate as 22% of average direct runoff rate for the applied period. The watershed of Oaedo river located the northern region showed R2 of 0.93, RMSE of 14.92 and ME of 0.70 as the result of calibrations by runoff data in the occurrence of 7 rainfalls.