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Detection of Submarine Groundwater Discharge (SGD) Signal by Stacking Landsat Thermal Infrared (TIR) Images in Jeju Island : Landsat 열적외선 영상의 중첩을 통한 제주도에서의 SGD 신호 탐지

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dc.contributor.advisor김덕진-
dc.contributor.author김윤지-
dc.date.accessioned2018-05-29T05:08:24Z-
dc.date.available2018-05-29T05:08:24Z-
dc.date.issued2018-02-
dc.identifier.other000000150932-
dc.identifier.urihttps://hdl.handle.net/10371/142458-
dc.description학위논문 (석사)-- 서울대학교 대학원 : 자연과학대학 지구환경과학부, 2018. 2. 김덕진.-
dc.description.abstractAlthough submarine groundwater discharge (SGD) has recently attracted, dispersive and weak SGD signals have not been satisfactorily identified. Since SGD varies spatially and temporally, the locations of SGD are generally hard to detect from a single satellite image. Due to such spatiotemporal characteristics, multi temporal data are required to detect SGD appeared in various patterns and weak amplitudes. Additionally, weak SGD signals may be missed on a single satellite image as they may fall below the noise threshold dictated by Landsats noise equivalent differential temperature (NEdT). Thus, this study proposes a practical method by applying stacking method to Landsat data for SGD detection.
The stacking method is comprised of two main processing steps: 1) mask out the land area and calculate sea surface temperature (SST) anomalies by subtracting the offshore SST, and 2) stack SST anomalies by summing multiple images. The optimal seasonal and tidal conditions for the detection of a weak SGD signal were determined, and then Landsat images satisfying the conditions of month and tide level were stacked in order to strengthen SGD signals and confirm the presence of SGD.
In this study, the method was applied to three sites on Jeju Island. The results show that this method is very successful at detecting SGD signal, even for weak signals.
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dc.description.tableofcontents1. Introduction 1
2. Methodology 4
2.1 Theoretical Basis of TIR Remote Sensing and Stacking 4
2.1.1 TIR Remote Sensing in SGD Detection 4
2.1.2 Atmospheric Correction 5
2.1.3 Conversion of DN to SST 6
2.1.4 SST Anomaly Estimation 10
2.1.5 Stacking Method 11
2.2. Study Area and Dataset 12
2.2.1 Study Area 12
2.2.2 Landsat Data 15
2.2.3 Airborne Data 18
2.2.4 Comparison between Airborne Data and Landsat Data 18
2.3 Data Processing 21
3. Stacking Condition Analysis 24
3.1 Spatial and Temporal Variability of SGD 24
3.2 Relationship between SST and SST Anomaly 28
3.3 Monthly Analysis of SST Anomaly 30
3.4 Tidal Analysis of SST Anomaly 33
3.5 Stacking Condition Analysis with NEdT 36
4. Stacking Landsat Data Satisfying the Optimum Condition 40
4.1 Stacking Under the Optimum Condition 40
4.2 Validation with Airborne Data 45
5. Conclusion 47
References 49
국문 요약 55
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dc.formatapplication/pdf-
dc.format.extent2642491 bytes-
dc.format.mediumapplication/pdf-
dc.language.isoen-
dc.publisher서울대학교 대학원-
dc.subjectThermal infrared(TIR) remote sensing-
dc.subjectLandsat-
dc.subjectSubmarine groundwater discharge (SGD)-
dc.subjectStacking-
dc.subjectNoise equivalent differential temperature (NEdT)-
dc.subject.ddc550-
dc.titleDetection of Submarine Groundwater Discharge (SGD) Signal by Stacking Landsat Thermal Infrared (TIR) Images in Jeju Island-
dc.title.alternativeLandsat 열적외선 영상의 중첩을 통한 제주도에서의 SGD 신호 탐지-
dc.typeThesis-
dc.description.degreeMaster-
dc.contributor.affiliation자연과학대학 지구환경과학부-
dc.date.awarded2018-02-
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