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[표제지]=0,1,1

연구보고서=0,2,1

Contents=i,3,2

Contents Of Figure=iii,5,3

Contents Of Table[내용누락;p.vii]=vi,8,3

요약문=ix,11,1

Summary=x,12,1

1. 서론=1,13,1

2. 연구 자료=2,14,1

2.1. 레이더 고도각=2,14,1

2.2. 관측자료=2,14,2

3. 분석방법=3,15,1

3.1. 광덕산 레이더 고도각별 차폐=3,15,4

3.2. 광덕산 레이더 관측 고도각=6,18,3

4. 분석결과=8,20,1

4.1. 밝은 띠(Bright Band) 고도=8,20,1

4.1.1. 4월의 밝은 띠(Bright Band) 고도=9,21,8

4.1.2. 5월의 밝은 띠(Bright Band) 고도=17,29,7

4.1.3. 6월의 밝은 띠(Bright Band) 고도=24,36,6

4.1.4. 7월의 밝은 띠(Bright Band) 고도=30,42,7

4.1.5. 8월의 밝은 띠(Bright Band) 고도=37,49,8

4.2. 강우 유형별 분석=45,57,1

4.2.1. 층운형[내용누락;p.47]=45,57,5

4.2.2. 대류형=50,62,5

5. 요약 및 토의=55,67,2

참고문헌=57,69,3

Contents Of Table

Table2.1.1. Measurement Parameters=2,14,1

Table3.1.1. The Section Of Beam Blocking By PPI 0˚ Scan In Gwangdeoksan Radar Site=4,16,1

Table4.1.1. The Height Of Bright Band By Each Station=10,22,1

Table4.1.2. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=14,26,1

Table4.1.3. The Height Of Bright Band By Each Station=18,30,1

Table4.1.4. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=21,33,1

Table4.1.5. The Height Of Bright Band By Each Station=25,37,1

Table4.1.6. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=27,39,1

Table4.1.7. The Height Of Bright Band By Each Station=30,42,1

Table4.1.8. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=34,46,1

Table4.1.9. The Height Of Bright Band By Each Station=38,50,1

Table4.1.10. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=41,53,1

Table4.2.1. The Height Of Bright Band By Each Station=45,57,1

Table4.2.2. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=45,57,1

Table4.2.3. The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate=50,62,1

Contents Of Figure

Fig3.1.1. The Distribution Of Beam Blocking By PPI 0˚ Scan In Gwangdeoksan Radar Site=4,16,1

Fig3.1.2. The Distribution Of Beam Blocking By Each Elevation Angle In Gwangdeoksan Radar Site. The Elevation Angle Are (a) 0.0˚, (b) 0.69˚, (c) 1.39˚, (d) 2.19˚, (e) 3.19˚, (f) 4.59˚, (g) 6.5˚, And (h) 9.09˚=5,17,2

Fig3.2.1. Range-Height Diagram Of Gwangdeoksan Radar On 17 December 2004=7,19,1

Fig3.2.2. Same As Fig. 3.2.1 Expect For 9 April 2005=7,19,1

Fig3.2.3. Same As Fig. 3.2.1 Expect For 26 July 2005=8,20,1

Fig4.1.1. (a) The distribution Of Reflectivity Radar, (b) The Vertical Distribution Of Reflectivity From A to B, (c) AWS 15 Minute Accumulated Rainfall Amount Chart On 2230 KST 9 April 2005=9,21,1

Fig4.1.2. Range-Height Diagram Of Gwangdeoksan Radar On 9 April 2005=11,23,1

Fig4.1.3. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station=11,23,4

Fig4.1.4. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Seoseok.(AWS id : 535)=15,27,1

Fig4.1.5. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site On 2240 KST 9 April 2005=16,28,1

Fig4.1.6. (a) The Distribution Of Reflectivity Radar, (b) The Vertical Distribution Of Reflectivity From A to B, (c) AWS 15Minute Accumulated Rainfall Amount Chart On 0500 KST 18 May 2005=17,29,1

Fig4.1.7. Range-Height Diagram Of Gwangdeoksan Radar On 18 May 2005=18,30,1

Fig4.1.8. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station=19,31,2

Fig4.1.9. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Daema(AWS id : 651)=22,34,1

Fig4.1.10. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site On 0100 KST 18 May 2005=23,35,1

Fig4.1.11. (a) The Distribution Of Reflectivity Radar, (b) The Vertical Distribution Of Reflectivity From A to B, (c) AWS 15Minute Accumulated Rainfall Amount Chart On 0620 KST 27 June 2005=24,36,1

Fig4.1.12. Range-Height Diagram Of Gwangdeoksan Radar on 27 June 2005=25,37,1

Fig4.1.13. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station On From 1900 KST 26 to 0200 KST 27 June 2005=26,38,1

Fig4.1.14. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Inje(AWS id : 211)=28,40,1

Fig4.1.15. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site On 2300 KST 26 June 2005=29,41,1

Fig4.1.16. (a) AWS 15 Minute, (b) 1 Hour Accumulated Rainfall Amount Chart, (c, e) PPI Elevation Angle 0˚ Scan In GDK Radar, (d, f) The Vertical Distribution Of Reflectivity From A To B, On 0800 KST 11 July 2005=31,43,1

Fig4.1.17. Range-Height Diagram Of Gwangdeoksan Radar On 11 July 2005=32,44,1

Fig4.1.18. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station On 11 July 2005=32,44,3

Fig4.1.19. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Sinnam(AWS id : 585)=35,47,1

Fig4.1.20. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site on 0800 KST 11 July 2005=36,48,1

Fig4.1.21. (a) The Distribution Of Reflectivity Radar, (b) The Vertical Distribution Of Reflectivity From A to B, (c) AWS 15 Minute Accumulated Rainfall Amount Chart On 0700 KST 11 August 2005=37,49,1

Fig4.1.22. Range-Height Diagram Of Gwangdeoksan Radar on 11 August 2005=38,50,1

Fig4.1.23. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station On 11 August 2005=39,51,3

Fig4.1.24. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Jeongseon(AWS id : 527)=42,54,1

Fig4.1.25. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site On 0700 KST 11 August 2005=43,55,1

Fig4.1.26. Melting Layer Obtained Of Seasons By Gwangdeoksan Radar=44,56,1

Fig4.2.1. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station From 19 to 20 April 2005=46,58,1

Fig4.2.2. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Daema-ri. (AWS id : 651)=48,60,1

Fig4.2.3. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site On 2210 KST 19 April 2005=49,61,1

Fig4.2.4. Time Series Distributions Of Vertical Reflectivity And Precipitation Of AWS By Each Station From 30 June to 1 July 2005=51,63,2

Fig4.2.5. Distribution Of The Best Correlation Coefficient Between Radar Elevation Angle And Rainfall Rate In Seoseok(AWS id : 535)=53,65,1

Fig4.2.6. The Corrected Reflectivity By Each Of Elevation Angle In Gwangdeoksan Radar Site On 0150 KST 1 July 2005=54,66,1

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