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    Characteristic large-scale circulation pattern of the persistent droughts of Northeast Asia from premonsoon season to monsoon season

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    ํ•™์œ„๋…ผ๋ฌธ (๋ฐ•์‚ฌ)-- ์„œ์šธ๋Œ€ํ•™๊ต ๋Œ€ํ•™์› : ์ง€๊ตฌํ™˜๊ฒฝ๊ณผํ•™๋ถ€, 2014. 2. ์ž„๊ทœํ˜ธ.Characteristic patterns of atmospheric circulation anomalies over the northeast Asian region in the dry and wet premonsoon seasons have been analyzed. The relationship between these patterns in the premonsoon season and the precipitation anomalies in the monsoon season has been also investigated. Since this study focuses on dry premonsoon season, features of anomalous large-scale atmospheric circulations during springtime droughts that occurred over the northeast Asia are revealed. The Palmer drought severity index is used in order to define drought years. In drought years, the anomalous circulation over the northeast Asia exhibits the weakened northward flow from the western North Pacific, and the position of the East Asian westerly Jet (EAWJ) maximum core at 300hPa is shifted southward. Thus, the rainfall band is moved southward, and the associated precipitation is suppressed over Korea, Japan, and southeastern China during spring droughts. The Sea Surface Temperature (SST) anomalies and outgoing longwave radiation anomalies, which show a northโ€“south dipole pattern between the Philippines and the northeast Asian region, support these dry conditions through the Hadley circulation. The anomalously warm SSTs in the western North Pacific seem to play an important role in the atmospheric circulation associated with persistent northeast Asian droughts The persistent features of extreme precipitation over the northeast Asia frompremonsoon season to monsoon season are found. In order to understand some characteristics of the circulation anomalies associated with persistent features of extreme precipitation, six dry cases and six wet cases in the premonsoon season are selected. Both of the extreme conditions are nearly persistent in each case. As mentioned in spring drought analysis, the weakened western North Pacific subtropical high (WNPSH) and the southward-shifted EAWJ are predominant for dry cases. For wet cases, the strengthening of WNPSH, the northward-shifted EAWJ in spring, and southward-shifted EAWJ in summer are apparent. However, dry cases are associated with the warm SST anomalies of the western North pacific, whereas wet cases are related to the warm SST anomalies of the Indian Ocean and Bay of Bengal. The dependency of extreme precipitation on this SST anomaly pattern is supported through numerical experiments. Based on the observational analysis and model experiments, the main connection system between extreme precipitation such as drought and SST is the anomalous cyclonic circulation over the western North Pacific.Table of Contents Abstract ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท i Table of Contents ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท v List of Figures ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท vii List of Tables ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท xi 1. Introduction ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 1 2. Data and methods ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 5 2.1 Data ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 5 2.2 Methods ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 8 2.2.1 Definition of premonsoon season ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 8 2.2.2 Analysis domain and selection of dry and wet years ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 17 3. Prominent features of large-scale circulation during drought ยทยทยทยทยทยทยทยทยทยทยทยท 21 3.1 Mean fields of atmospheric circulation during boreal spring ยทยทยทยทยทยทยทยท 21 3.2 Definition and selection of drought years ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 25 3.3 Atmospheric circulation anomalies during drought years ยทยทยทยทยทยทยทยทยทยทยทยท 27 3.4 Teleconnection between drought and SSTs ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 36 3.4.1 SST and OLR anomalies ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 36 3.4.2 Definition of the EAJ index ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 39 3.4.3 The relationship among the EAJ index, SST, and precipitation ยทยทยท 42 4. Characteristics of anomalous large-scale circulations in the spring and summer ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 47 4.1 Selection of dry and wet cases ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 47 4.2 Precipitation anomalies ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 48 4.3 Geopotential height anomalies at 850 hpa ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 50 4.4 Zonal wind anomalies at 200 hpa ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 57 4.5 Moisture flux anomalies at 850 hpa ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 60 4.6 Linkage of the anomalous circulation and SST anomalies ยทยทยทยทยทยทยทยทยทยทยทยท 64 5. Results of model experiments ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 69 5.1 Model and experimental designยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 69 5.2 Circulations at 850 hPa in dry/wet force run ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 71 5.3 EAWJ at 200 hPa in dry/wet force run ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 74 6. Summary and conclusions ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 83 References ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 91 ๊ตญ๋ฌธ์ดˆ๋ก ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 98 ๊ฐ์‚ฌ์˜ ๊ธ€ ยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยทยท 102Docto

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    ํ”Œ๋กœํŒ… ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์€ ์ผ๋ฐ˜ ๊ฑด์ถ•๋ฌผ๊ณผ ํ˜•ํƒœ๋Š” ๊ฐ™์ง€๋งŒ ๊ธฐ์ดˆ๊ฐ€ ๋•…์ด ์•„๋‹Œ ํ•˜๋ถ€ ๋ถ€์ฒด์— ์ง€์ง€๋˜๋Š” ๊ตฌ์กฐ๋ฌผ๋กœ ํŒŒ๋ž‘ํ•˜์ค‘์— ์˜ํ•œ ์˜ํ–ฅ์„ ํฌ๊ฒŒ ๋ฐ›์œผ๋ฉฐ, ํŒŒ๋ž‘ํ•˜์ค‘์— ์˜ํ•œ ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ๋ณ€ํ˜•์ด ์ ‘ํ•ฉ๋ถ€์— ์˜ํ–ฅ์„ ๋ฏธ์ณ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ์ด์šฉ์ž์—๊ฒŒ ์‚ฌ์šฉ์„ฑ ๋ฐ ์•ˆ์ „์„ฑ์˜ ๋ฌธ์ œ๋ฅผ ๋ฐœ์ƒ์‹œํ‚ค๊ฒŒ ๋œ๋‹ค. ์ด์— ๋”ฐ๋ผ ๋ณธ ๋…ผ๋ฌธ์—์„œ๋Š” 3์ฐจ์› ํ”Œ๋กœํŒ… ๊ตฌ์กฐ๋ฌผ์˜ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ๊ณผ ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์„ ์ผ์ฒดํ™”ํ•œ ์ „ํ•ด์„์„ ํ†ตํ•˜์—ฌ ๊ฐ•์ ‘๊ณผ ๋ฐ˜๊ฐ•์ ‘(TSD)์ ‘ํ•ฉ์— ๋Œ€ํ•ด ํƒ„์„ฑ ํ•ด์„์„ ์‹ค์‹œํ•˜๊ณ , ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์„ ์ œ์™ธํ•œ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผํ•ด์„์„ ํ†ตํ•˜์—ฌ ์†Œ์„ฑํ•ด์„์„ ๋ถ„์„ํ•˜์˜€๋‹ค. ๊ตฌ์กฐ๋ฌผ์˜ ์ „ํ•ด์„๊ณผ ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์„ ์ œ์™ธํ•œ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผํ•ด์„์„ ๋น„๊ต ๋ถ„์„ ํ•˜์˜€์œผ๋ฉฐ ํƒ„์„ฑ ํ•ด์„์„ ํ†ตํ•ด ํŒŒ๋ž‘ํ•˜์ค‘์˜ CASE๋ฅผ ๋‚˜๋ˆ„์–ด ํŒŒ๋ž‘ํ•˜์ค‘์˜ ๋ณ€ํ™”์— ๋”ฐ๋ฅธ ๊ตฌ์กฐ๋ฌผ์˜ ๋ชจ๋ฉ˜ํŠธ ๋ฐ ๋ณ€์œ„๋ฅผ ์ ‘ํ•ฉ๋ถ€์— ๋”ฐ๋ผ ๋ถ„๋ฅ˜ํ•˜๊ณ  ์†Œ์„ฑํ•˜์„์„ ํ†ตํ•ด 3์ฐจ์› ํ”Œ๋กœํŒ… ๊ตฌ์กฐ๋ฌผ์˜ ๊ฑฐ๋™์„ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ ๋‹ค์Œ๊ณผ ๊ฐ™์€ ๊ฒฐ๋ก ์„ ๋„์ถœํ•˜์˜€๋‹ค. 1. ๊ตฌ์กฐ๋ฌผ์˜ ์ „ํ•ด์„๊ณผ ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์„ ์ œ์™ธํ•œ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผํ•ด์„์˜ ๋ชจ๋ฉ˜ํŠธ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ ์ „์ฒด์ ์ธ ๋ชจ๋ฉ˜ํŠธ ๊ฐ’์€ ๋น„์Šทํ•˜์ง€๋งŒ ์ „ํ•ด์„์˜ ๊ฒฝ์šฐ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผํ•ด์„ ๋ณด๋‹ค ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ์˜ํ–ฅ์œผ๋กœ ์ €์ธต ๋ณด ๋ถ€์žฌ์—์„œ ๋ชจ๋ฉ˜ํŠธ ๊ฐ’์ด ๋Œ€์ฒด์ ์œผ๋กœ ์ž‘์€ ๊ฒƒ์„ ์•Œ ์ˆ˜ ์žˆ์—ˆ๋‹ค. ์ด์— ๋”ฐ๋ผ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ๊ณผ ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ์ผ์ฒดํ™”ํ•˜์—ฌ ์ „ํ•ด์„์„ ํ•  ๊ฒฝ์šฐ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ๋งŒ ํ•ด์„ํ•œ ๊ธฐ์กด์˜ ์ž๋ฃŒ์— ๋น„ํ•ด ์ข€ ๋” ์ •ํ™•ํ•œ ํ•ด์„์ด ๊ฐ€๋Šฅํ•˜๋ฆฌ๋ผ ์‚ฌ๋ฃŒ๋œ๋‹ค. 2. ํŒŒ๋ž‘ํ•˜์ค‘์— ๋Œ€ํ•ด ํŒŒํ–ฅ์„ 0o์™€ 90o๋กœ ๋‚˜๋ˆ„์–ด ๋ชจ๋ฉ˜ํŠธ๋ฅผ ๋น„๊ตํ•œ ๊ฒฐ๊ณผ ํŒŒํ–ฅ 0o์—์„œ๋Š” ํŒŒํ–ฅ 90o์ผ๋•Œ์— ๋น„ํ•˜์—ฌ ๋ณด๋ถ€์žฌ์˜ ๋ชจ๋ฉ˜ํŠธ๊ฐ€ ๊ฑฐ์˜ ๋ฐœ์ƒํ•˜์ง€ ์•Š์•„ ํŒŒํ–ฅ 90o์ผ๋•Œ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์— ๋ฏธ์น˜๋Š” ์˜ํ–ฅ์ด ๋” ํฐ ๊ฒƒ์„ ์•Œ ์ˆ˜ ์žˆ์—ˆ๋‹ค. 3. ํŒŒํ–ฅ 90o์—์„œ๋Š” ํŒŒ๋ž‘ํ•˜์ค‘์„ ์ ์šฉ์‹œ์ผฐ์„ ๋•Œ์™€ ์กฐํ•ฉํ•˜์ค‘์„ ์ ์šฉ์‹œ์ผฐ์„ ๋•Œ ๋ชจ๋‘ CASE2์—์„œ ์ตœ๋Œ€ ๋ชจ๋ฉ˜ํŠธ๊ฐ€ ๋ฐœ์ƒํ•˜์˜€๊ณ  ์กฐํ•ฉํ•˜์ค‘์˜ ๊ฒฐ๊ณผ ๋ฐ˜๊ฐ•์ ‘์„ ์ ์šฉํ•˜์˜€์„ ๊ฒฝ์šฐ ์ตœ๋Œ€ ๋ชจ๋ฉ˜ํŠธ๋Š” ๋‹จ๋ถ€์—์„œ ๊ฐ์†Œํ•˜์˜€๋‹ค. ๋ฐ˜๊ฐ•์ ‘์„ ์ ์šฉํ•œ ๋ณด ์ค‘์•™๋ถ€์—์„œ๋Š” ๋ชจ๋ฉ˜ํŠธ๊ฐ€ ์ฆ๊ฐ€ํ•˜์˜€์ง€๋งŒ ๊ฒฐ๊ณผ์ ์œผ๋กœ๋Š” ๋ณด๋ถ€์žฌ์˜ ์ตœ๋Œ€ ๋ชจ๋ฉ˜ํŠธ๋Š” ๊ฐ์†Œํ•˜์˜€๋‹ค. ์ด์— ๋”ฐ๋ผ ํ”Œ๋กœํŒ… ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€ ์‚ฌ์šฉ ์‹œ ์ตœ๋Œ€ ๋ชจ๋ฉ˜ํŠธ๋ฅผ ์ค„์ผ ์ˆ˜ ์žˆ์–ด ๋ถ€์žฌ์˜ ๋‹จ๋ฉด์„ ์ค„์ผ ์ˆ˜ ์žˆ์„ ๊ฑฐ๋ผ ์‚ฌ๋ฃŒ๋œ๋‹ค. 4. ํ”Œ๋กœํŒ… ๊ตฌ์กฐ๋ฌผ์˜ ์ตœ๋Œ€ ๋ณ€์œ„๋Š” ํŒŒ๋ž‘ํ•˜์ค‘์— ์˜ํ•ด ์ง€๋ฐฐ์ ์œผ๋กœ ๋ฐœ์ƒํ•˜๋ฉฐ ํŒŒ๋ž‘ํ•˜์ค‘์— ์˜ํ•œ ๊ฐ•์ ‘๊ณผ ๋ฐ˜๊ฐ•์ ‘์˜ ๋ณ€์œ„์ฐจ์ด๋Š” ๊ฑฐ์˜ ๋ฐœ์ƒํ•˜์ง€ ์•Š๊ณ  ์ •์ ํ•˜์ค‘์— ์˜ํ•œ ๋ณ€์œ„ ์ฐจ๋Š” ๋ฐ˜๊ฐ•์ ‘ ์ผ๋•Œ ๊ฐ•์ ‘์— ๋น„ํ•ด ์ฆ๊ฐ€ํ•˜์˜€๋‹ค. ํŒŒ๋ž‘ํ•˜์ค‘์˜ ์œ„์น˜ ๋ณ€ํ™”์— ๋”ฐ๋ผ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์˜ -๋ณ€ํ˜•์„ ํ•˜๊ฒŒ ๋  ๊ฒฝ์šฐ ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€๋Š” ์ตœ๋Œ€ ๋ณ€์œ„๊ฐ€ ๊ฐ์†Œํ•˜๊ฒŒ ๋˜๋ฉฐ +๊ฑฐ๋™์„ ํ•˜๊ฒŒ ๋  ๊ฒฝ์šฐ ์ฆ๊ฐ€ํ•˜๊ฒŒ ๋œ๋‹ค. ํŒŒ๋ž‘ํ•˜์ค‘์˜ ์ง„ํญ์ด ์ปค์งˆ์ˆ˜๋ก ํŒŒ๋ž‘ํ•˜์ค‘์— ์˜ํ•œ ์‘๋‹ต์ด ์ง€๋ฐฐ์ ์ด๊ฒŒ ๋˜์–ด ๊ฐ•์ ‘๊ณผ ๋ฐ˜๊ฐ•์ ‘์˜ ์ตœ๋Œ€ ๋ณ€์œ„ ์ฐจ์ด๋Š” ์ค„์–ด๋“ค๊ฒŒ ๋œ๋‹ค. 5. ํŒŒ๋ž‘ํ•˜์ค‘์˜ ์ง„ํญ์ด ์ปค์ง€๊ฒŒ ๋จ์— ๋”ฐ๋ผ ํ”Œ๋กœํŒ… ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ์ตœ๋Œ€ ํ•˜์ค‘๊ณ„์ˆ˜๋Š” ๊ฐ์†Œํ•˜๊ณ  ์ตœ๋Œ€ ๋ณ€์œ„๋Š” ์ฆ๊ฐ€ํ•˜๊ฒŒ ๋˜์–ด ๊ตฌ์กฐ๋ฌผ์ด ์ตœ๋Œ€ ๋ฐ›์„ ์ˆ˜ ์žˆ๋Š” ํ•˜์ค‘์€ ๊ฐ์†Œํ•˜๊ฒŒ ๋œ๋‹ค. ์ ‘ํ•ฉ๋ถ€์— ๋ฐ˜๊ฐ•์ ‘์„ ์ ์šฉํ•˜๊ฒŒ ๋˜๋ฉด ์ ‘ํ•ฉ๋ถ€์˜ ์—ฐ์„ฑ์ด ์ฆ๊ฐ€ํ•˜์—ฌ ๊ฐ•์ ‘์ผ ๋•Œ์— ๋น„ํ•ด ์ตœ๋Œ€ ํ•˜์ค‘๊ณ„์ˆ˜๋Š” ๊ฐ์†Œํ•˜๊ฒŒ ๋˜๋ฉฐ ๋ณ€์œ„๋Š” ์ฆ๊ฐ€ ํ•˜๋Š” ๊ฑฐ๋™์„ ๋ณด์˜€๋‹ค.๋ชฉ ์ฐจ ๋ชฉ ์ฐจ ํ‘œ๋ชฉ์ฐจ ๊ทธ๋ฆผ๋ชฉ์ฐจ ABSTRACT 1. ์„œ ๋ก  1.1 ์—ฐ๊ตฌ์˜ ๋ฐฐ๊ฒฝ ๋ฐ ๋ชฉ์  1.2 ์—ฐ๊ตฌ๋™ํ–ฅ 1.3 ์—ฐ๊ตฌ๋ฒ”์œ„ ๋ฐ ๋ฐฉ๋ฒ• 2. ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€ ๋ถ„๋ฅ˜ ๋ฐ ํ•ด์„ ๋ชจ๋ธ 2.1 ๊ฐœ์š” 2.2 ๊ทœ์ค€์— ๋”ฐ๋ฅธ ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€์˜ ๋ถ„๋ฅ˜ 2.3 ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€์˜ ์ข…๋ฅ˜ 2.4 ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€์˜ ๋ชจ๋ธ๋ง 3. ํ”Œ๋กœํŒ… ๊ตฌ์กฐ๋ฌผ์˜ ๊ตฌ์กฐํ•ด์„ 3.1 ํ”Œ๋กœํŒ… ๊ตฌ์กฐ๋ฌผ์˜ ๊ณ„ํš ๋ฐ ํ•ด์„ 3.2 ํ”Œ๋กœํŒ… ๊ตฌ์กฐ๋ฌผ์˜ ํŒŒ๋ž‘ํ•˜์ค‘ ์‚ฐ์ • 3.3 ํ•˜๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ๋ณ€ํ˜• ๋ฐ ์‘๋ ฅ ๋ณ€ํ™” 4. ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€๋ฅผ ์ ์šฉํ•œ ์ ์šฉ์˜ˆ์ œ ๊ตฌ์กฐ๋ฌผ 4.1 ์ ์šฉ ์˜ˆ์ œ ๊ตฌ์กฐ๋ฌผ 4.2 TSD ๋ฐ˜๊ฐ•์ ‘ ์ ‘ํ•ฉ๋ถ€ ํŠน์„ฑ 4.3 ๋ถ€๋ ฅ ์‚ฐ์ • 4.4 ํ•˜์ค‘ ์‚ฐ์ • 4.5 ์ „ํ•ด์„๊ณผ ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผํ•ด์„์˜ ๋น„๊ต 4.6 ์ƒ๋ถ€๊ตฌ์กฐ๋ฌผ์˜ ์‘๋ ฅ ๊ฒ€ํ†  5. ํŒŒ๋ž‘ํ•˜์ค‘ ๋ณ€ํ™”์— ๋”ฐ๋ฅธ ๊ตฌ์กฐ๋ฌผ์˜ ์‘๋‹ต ํ•ด์„ 5.1 ํŒŒ๋ž‘ํ•˜์ค‘๋ณ„ ์ตœ๋Œ€ ๋ชจ๋ฉ˜ํŠธ ๋น„๊ต 5.2 ํŒŒ๋ž‘ํ•˜์ค‘๋ณ„ ์ตœ๋Œ€ ๋ณ€์œ„ ๋น„๊ต 5.3 ์†Œ์„ฑํ•ด์„์— ์˜ํ•œ ๊ฑฐ๋™๋ถ„์„ 6. ๊ฒฐ ๋ก  ์ฐธ๊ณ  ๋ฌธ

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    CNN-based ship resistance prediction using voxelization

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    The resistance of a ship can be analyzed using computational fluid dynamics (CFD) or model tests. To explore a number of design candidates, for instance in the early design stages, it is too expensive to use the CFD and model tests because of their relatively long analysis time. Ship designers tend to often use statistical methods that are simple and need a short analysis time. The statistical methods provide such advantages, but are often relatively inaccurate due to their simplicity. To deal with the problem, we present a method for predicting ship resistance that is based on convolutional neural networks (CNNs). This converts input hulls into 3D voxels, which are the suitable data structure to use the CNNs. The CNNs extract only important features from the input hulls and this often allows for better convergence in the training of artificial neural networks (ANNs). In a case study, the proposed method was applied to developing ANNs for ship resistance prediction. It was compared with a parametric method which is also an ANNs, but the input of the ANNs used hull parameters such as the length overall, block coefficient, etc. The results of the case study show that the voxelized input improves the resistance prediction accuracy compared with the parametric input in developing ANNs for ship resistance prediction.The resistance of a ship can be analyzed using computational fluid dynamics (CFD) or model tests. To explore a number of design candidates, for instance in the early design stages, it is too expensive to use the CFD and model tests because of their relatively long analysis time. Ship designers tend to often use statistical methods that are simple and need a short analysis time. The statistical methods provide such advantages, but are often relatively inaccurate due to their simplicity. To deal with the problem, we present a method for predicting ship resistance that is based on convolutional neural networks (CNNs). This converts input hulls into 3D voxels, which are the suitable data structure to use the CNNs. The CNNs extract only important features from the input hulls and this often allows for better convergence in the training of artificial neural networks (ANNs). In a case study, the proposed method was applied to developing ANNs for ship resistance prediction. It was compared with a parametric method which is also an ANNs, but the input of the ANNs used hull parameters such as the length overall, block coefficient, etc. The results of the case study show that the voxelized input improves the resistance prediction accuracy compared with the parametric input in developing ANNs for ship resistance prediction.1. ์„œ๋ก  1 1.1 ์—ฐ๊ตฌ ๋ฐฐ๊ฒฝ 1 1.2 ์„ ํ–‰ ์—ฐ๊ตฌ 1 1.3 ์—ฐ๊ตฌ ๋ชฉํ‘œ ๋ฐ ๊ฐœ์š” 3 2. ๋”ฅ๋Ÿฌ๋‹ ๋ชจ๋ธ 5 2.1 ๋”ฅ๋Ÿฌ๋‹ ๊ฐœ์š” 5 2.2 ํ•ฉ์„ฑ๊ณฑ ์‹ ๊ฒฝ๋ง 8 2.2 ์ž„๋ฒ ๋”ฉ 10 2.3 ์™„์ „์—ฐ๊ฒฐ์ธต 12 3. ๋ฐ์ดํ„ฐ ๊ตฌ์„ฑ 13 3.1 ๋ฐ์ดํ„ฐ ๊ฐœ์š” 13 3.2 ์„ ํ˜• ๋ฐ์ดํ„ฐ์˜ ๋ณต์…€ํ™” 13 3.3 ๋ถ€๊ฐ€ ์ •๋ณด ๋ฐ์ดํ„ฐ 16 3.4 ์ €ํ•ญ ๋ฐ์ดํ„ฐ 17 4. ๋น„๊ต ์‹œํ—˜ 20 4.1 ์ž…ยท์ถœ๋ ฅ ๋ฐ์ดํ„ฐ ์ˆ˜์ง‘ ๋ฐ ๊ฒฐ์ • 21 4.1.1 ๋ฐ์ดํ„ฐ ์ˆ˜์ง‘ 21 4.1.2 ๋”ฅ๋Ÿฌ๋‹ ๋ชจ๋ธ์„ ์œ„ํ•œ ๋ฐ์ดํ„ฐ ๊ฒฐ์ • 25 4.2 ๋”ฅ๋Ÿฌ๋‹ ๋ชจ๋ธ ๊ฒฐ์ • 30 4.3 ๋ฐฉ๋ฒ•๋ก  ๋น„๊ต 34 5. ๊ฒฐ๋ก  38 5.1 ์š”์•ฝ 38 5.2 ํ–ฅํ›„ ๊ณผ์ œ 39Maste

    ์ €์ถœ์‚ฐ ๊ฐœ์„ ๋ฐฉ์•ˆ ์›Œํฌ์ˆ(CNI์„ธ๋ฏธ๋‚˜2017-028) (๋ฐ•์ข…์„œ, ๊น€์šฉํ˜„)

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    โ—‹๋ชฉ์  : ์ €์ถœ์‚ฐ์ด ์‹ฌ๊ฐํ•œ ์‚ฌํšŒ๋ฌธ์ œ๋กœ ๋– ์˜ค๋ฆ„์— ๋”ฐ๋ผ ๊ตญ์ฑ…์—ฐ๊ตฌ๊ธฐ๊ด€๊ณผ ๋”๋ถˆ์–ด ์ถฉ๋‚จ์—ฐ๊ตฌ์›์ด ์ค‘์•™์ •๋ถ€์™€ ์ง€๋ฐฉ์ •๋ถ€์˜ ๋Œ€์‘๋ฐฉ์•ˆ์„ ๋…ผ์˜ํ•˜๊ธฐ ์œ„ํ•œ ์›Œํฌ์ˆ ๊ฐœ์ตœ โ—‹๊ฐœ์š” - ์ฃผ์ œ : ์ €์ถœ์‚ฐ ๊ฐœ์„ ๋ฐฉ์•ˆ์— ๋Œ€ํ•œ ๋…ผ์˜ - ์ผ์‹œ : 2017๋…„ 4์›” 17์ผ(์›”) 15:00 - ์žฅ์†Œ : ์ถฉ๋‚จ์—ฐ๊ตฌ์› ๋Œ€ํšŒ์˜์‹ค โ—‹๋‚ด์šฉ - ์ฃผ์ œ๋ฐœํ‘œ 1 : ์ถœ์‚ฐ์˜ ์›์ธ๊ณผ ์ถœ์‚ฐ์œจ ํšŒ๋ณต์„ ์œ„ํ•œ ์ •์ฑ…๋ฐฉํ–ฅ์„ฑ(ํ•œ๊ตญ๋ณด๊ฑด์‚ฌํšŒ์—ฐ๊ตฌ์›, ๋ฐ•์ข…์„œ ๋ฐ•์‚ฌ) - ์ฃผ์ œ๋ฐœํ‘œ 2 : ์ถฉ๋‚จ๋„ ๋ฐ ์‹œ๊ตฐ ์ €์ถœ์‚ฐ ์ •์ฑ… ์‚ฌ๋ก€์—ฐ๊ตฌ(์ถฉ๋‚จ์—ฐ๊ตฌ์›, ๊น€์šฉํ˜„ ๋ฐ•์‚ฌ) - ์ง€์ •ํ† ๋ก  ย  ยท์ขŒ์žฅ : ๊ฐ•ํ˜„์ˆ˜(์ถฉ๋‚จ์—ฐ๊ตฌ์›์žฅ) ย  ยทํ† ๋ก  : ์ตœ์ƒ์ง„ ๊ณผ์žฅ(์ถฉ์ฒญ๋‚จ๋„ ์ €์ถœ์‚ฐ๊ณ ๋ นํ™”๋Œ€์ฑ…๊ณผ) ย ย ย ย ย ย ย ย ย ย  ๊ถŒ๊ฒฝ์ฃผ ์ด์‚ฌ(์„ธ๊ณ„๋„๋•์žฌ๋ฌด์žฅ ํ•œ๊ตญ๋ณธ๋ถ€) ย ย ย ย ย ย ย ย ย ย  ์ตœ์€ํฌ ๋ฐ•์‚ฌ(์ถฉ๋‚จ์—ฌ์„ฑ์ •์ฑ…๊ฐœ๋ฐœ์›)- ์ฃผ์ œ๋ฐœํ‘œ 1 : ์ถœ์‚ฐ์˜ ์›์ธ๊ณผ ์ถœ์‚ฐ์œจ ํšŒ๋ณต์„ ์œ„ํ•œ ์ •์ฑ…๋ฐฉํ–ฅ์„ฑ(ํ•œ๊ตญ๋ณด๊ฑด์‚ฌํšŒ์—ฐ๊ตฌ์›, ๋ฐ•์ข…์„œ ๋ฐ•์‚ฌ) - ์ฃผ์ œ๋ฐœํ‘œ 2 : ์ถฉ๋‚จ๋„ ๋ฐ ์‹œ๊ตฐ ์ €์ถœ์‚ฐ ์ •์ฑ… ์‚ฌ๋ก€์—ฐ๊ตฌ(์ถฉ๋‚จ์—ฐ๊ตฌ์›, ๊น€์šฉํ˜„ ๋ฐ•์‚ฌ) - ์ง€์ •ํ† 
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