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Estimation of Water Availability in the Korean Peninsula Considering Climate Change : 기후변화를 고려한 한반도의 가용 수자원 추정

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dc.contributor.advisor이동근-
dc.contributor.author유소현-
dc.date.accessioned2017-07-14T06:19:59Z-
dc.date.available2017-07-14T06:19:59Z-
dc.date.issued2016-02-
dc.identifier.other000000133759-
dc.identifier.urihttps://hdl.handle.net/10371/125487-
dc.description학위논문 (석사)-- 서울대학교 대학원 : 생태조경·지역시스템공학부, 2016. 2. 이동근.-
dc.description.abstractClimate change is projected to have a direct impact on the water resources. In case of the Korean Peninsula, more than a half of the total rainfall amount is concentrated in summer. It has been always important issues that spatio-temporal variability of an available water resources in the Korean Peninsula. The water availability is projected to be influenced by climate change and it is expected to more intensify. Variations in water availability is related with the land use which is directly affected by water resources, such as agricultural area, urban area, and forests. Therefore, the changes in spatial variability along with the temporal changes of water availability should be investigated to establish an effective management plan and draw an implication for future spatial planning.
Available water resources can be defined in various ways, such as a storage of reservoir, and river discharge which can be used in a basin. This study defined water availability as a river discharge based on literature reviews. This study estimates water availability based on river discharge in the Korean Peninsula including North Korea, as the study area. In order to estimate water availability and draw a spatial implication considering climate change, HadGEM2-AO and RCP 8.5 scenario is applied as a future climate scenario, and grid-based hydrological model H08 is used. H08 was originally developed as a global hydrological model for the simulation of water availability in a spatial resolution of 1° 1°. However, it is also applicable for a regional hydrological simulation in a spatial resolution of 5ˊ 5ˊ. Input meteorological data of GSWP2 is used for historical simulation, and RCP 8.5 scenario from HadGEM2-AO was used for future climate change simulation. A bias in air temperature and precipitation of GCM was validated by comparing with observed meteorological data in Korea. Parameters of H08 was calibrated and validated for historical simulation of 10 years from 1986 to 1995, then climate change simulation is carried out for the estimation of hydrological changes using validated H08.
In order to investigate hydrological characteristics and water availability in the Korean Peninsula, representative gauging stations was presented for Amnok, Duman, Chongchon, Taedong River basin in North Korea, and Han, Nakdong, Geum, Yeongsan River basin in South Korea. Quantitative hydrological characteristics were presented for the representative 8 stations in the Korean Peninsula along with the meteorological aspects. Spatio-temporal variability was investigated for the hydrological attributes, such as evapotranspiration, runoff, as well as air temperature and precipitation. Estimated water availability based on RCP 8.5 scenario was spatially presented for the objective periods in order to derive spatial implication for the planning. However, there is uncertainties for future projection in the process of selecting future climate scenarios and hydrological model. This study assumed naturalized discharge which is not considering regulated flow due to the reservoir operation and artificial water supply capacity. This study estimated water availability on a grid basis using regionalized global hydrological model. The results of this study can be used as preliminary information for establishing spatial planning under climatic changes across the Korean Peninsula considering water availability.
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dc.description.tableofcontentsⅠ. Introduction 1

Ⅱ. Literature review 3
1. Climate change and water availability 3
1.1. Climate scenarios 3
1.2. Concept of water availability 5
2. Hydrological model studies in the Korean Peninsula considering climate change scenarios 9
3. Regional application of H08 in previous studies 13

Ⅲ. Methodology 16
1. Scope of the study 16
2. Materials and method 18
2.1. Study flow 18
2.2. Introduction to hydrological model H08 19
2.3. Meteorological data 24
2.4. Geographical data 27
2.5. Hydrological data 29

Ⅳ. Results and discussion 32
1. Validation of meteorological data 32
1.1. Validation and bias correction of GSWP2 data 32
1.2. Validation and bias correction of GCM data 38
2. Calibration and validation of H08 44
2.1. Parameter sensitivity analysis 44
2.2. Calibration of parameters 48
2.3. Validation of simulated discharge 53
3. Hydro-meteorological simulation 58
3.1. Meteorological characteristics and changes 58
3.2. Hydrological characteristics and changes 66
3.3. Estimation of water availability 78
4. Implication for spatial planning 85

Ⅴ. Conclusion 89

Ⅵ. References 91

국문초록 102
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dc.formatapplication/pdf-
dc.format.extent5169877 bytes-
dc.format.mediumapplication/pdf-
dc.language.isoen-
dc.publisher서울대학교 대학원-
dc.subjectWater availability-
dc.subjectClimate change-
dc.subjectRCP scenario-
dc.subjectGCM-
dc.subjectHydrological model-
dc.subjectH08-
dc.subject.ddc712-
dc.titleEstimation of Water Availability in the Korean Peninsula Considering Climate Change-
dc.title.alternative기후변화를 고려한 한반도의 가용 수자원 추정-
dc.typeThesis-
dc.description.degreeMaster-
dc.citation.pages104-
dc.contributor.affiliation농업생명과학대학 생태조경·지역시스템공학부-
dc.date.awarded2016-02-
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