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๊ฒ€์ฆ๋œ ํŒŒํŠธ๋„ˆ ์ œํœด์‚ฌ ์ž๋ฃŒ

์˜คํ‚ค๋‚˜์™ฟ’ ํŠธ๋Ÿฌํ”„ ์ž ์žฌ ์ง€์ง„ํ•ด์ผ ์ „ํŒŒํŠน์„ฑ (Propagation Characteristics of Potential Tsunamis in Okinawa Trough)

9 ํŽ˜์ด์งฟ’
๊ธฐํƒ€ํŒŒ์ผ
์ตœ์ดˆ๋“ฑ๋ก์ผ 2025.06.03 ์ตœ์ข…์ ฟ’์ž‘์ผ 2008.06
9P ๋ฏธ๋้ฉ๋ณด๊ธฐ
์˜คํ‚ค๋‚˜์™ฟ’ ํŠธ๋Ÿฌํ”„ ์ž ์žฌ ์ง€์ง„ํ•ด์ผ ์ „ํŒŒํŠน์„ฑ
  • ๋ฏธ๋้ฉ๋ณด๊ธฐ

    ์„œ์่ง์ •๋ต–

    ยท ๋ฐœํ–‰๊ธฐ๊ด€ : ํ•œ๊ตญํ•ด์•ˆ,ํ•ด์–‘๊ณตํ•™ํšŒ
    ยท ์ˆ˜๋ก์ง€ ์ •๋ณด : ํ•œ๊ตญํ•ด์•ˆยทํ•ด์–‘๊ณตํ•™ํšŒ๋…ผ๋ๅฉ์ง‘ / 20๊ถŒ / 3ํ˜ธ / 268 ~ 276ํŽ˜์ด์งฟ’
    ยท ์ €์ž๋ช… : ๊น€์ข…ํ•™, ์ตœ์›ํ•™, ๋ฐฐ์žฌ์„, ์œค์„ฑ๋ฒ”

    ์ดˆ๋ก

    ์˜คํ‚ค๋‚˜์™ฟ’ ํŠธ๋Ÿฌํ”„์—์„œ ๋ฐœ์ƒ๋˜๋Š” ์ž ์žฌ ์ง€์ง„ํ•ด์ผ์˜ ํ•œ๋ฐ˜๋„ ๋‚จ์„œ์™ธํ•ด์—์„œ์˜ ์ „ํŒŒํŠน์„ฑ์„ ๊ทœ๋ช…ํ•˜๊ธฐ ์œ„ํ•œ ์ˆ˜์น˜๋ชจ์˜๋ฅผ ์ˆ˜ํ–‰ํ•˜์˜€๋‹ค. ๋™์ค‘๊ตญํ•ด ๋Œ€๋ฅ™๋ถ•์˜ ์–•์€ ์ˆ˜์‹ฌ๊ณผ ์˜คํ‚ค๋‚˜์™ฟ’ ํŠธ๋Ÿฌํ”„์˜ ๊นŠ์€ ์ˆ˜์‹ฌ์€ ์ด ์ง€์—ญ์—์„œ ๋ฐœ์ƒํ•˜๋Š” ์ง€์ง„ํ•ด์ผ์˜ ์ „ํŒŒํŠน์„ฑ์— ์ค‘์š”ํ•œ ์—ญํ• ์„ ํ•œ๋‹ค. ์ „ํŒŒํŠน์„ฑ์€ ์ „ํŒŒ ๋‹จ๊ณ„์— ๋”ฐ๋ผ ๋‘ ๊ฐ€์ง€๋กœ ๋ถ„๋ฅ˜๋œ๋‹ค. ์ฒซ ๋‹จ๊ณ„๋Š” ์ˆ˜์‹ฌ์ด ๊นŠ์€ ํŠธ๋Ÿฌํ”„๋ฅผ ๋”ฐ๋ผ์„œ ๋ถ๋™๊ณผ ๋‚จ์„œ๋ฐฉํ–ฅ์œผ๋กœ ์ „ํŒŒํ•ด๊ฐ€๋Š” ๊ณผ์ •์ด๊ณ , ๋‘ ๋ฒˆ์งธ ๋‹จ๊ณ„๋Š” ๋“ฑ์ˆ˜์‹ฌ์„ ๊ณผ ์ง๊ฐ๋ฐฉํ–ฅ์œผ๋กœ ๋™์ค‘๊ตญํ•ด์˜ ๋Œ€๋ฅ™๋ถ•์œผ๋กœ ์ง„์ž…ํ•˜๋Š” ๊ณผ์ •์ด๋‹ค. ์ˆ˜์น˜๋ชจ์˜ ๊ฒฐ๊ณผ ์˜คํ‚ค๋‚˜์™ฟ’ ํŠธ๋Ÿฌํ”„์—์„œ ๋ฐœ์ƒํ•˜๋Š” ์ง€์ง„ํ•ด์ผํŒŒ๋Š” ๋‚จ์„œ์™ธํ•ด์˜ ํŠน์ˆ˜ํ•œ ํ•ด์ €์ง€ํ˜•์˜ ์˜ํ–ฅ์œผ๋กœ ์šฐ๋ฆฌ๋‚˜๋ผ ๋‚จํ•ด์•ˆ๊ณผ ์„œํ•ด์•ˆ์— ๋ฏธ์น˜๋Š” ์˜ํ–ฅ์ด ๋งค์šฐ ์ž‘์€ ๊ฒƒ์œผ๋กœ ๋‚˜ํƒ€๋‚ฌ๋‹ค.

    ์˜์–ด์ดˆ๋ก

    Potential tsunamis generated in Okinawa Trough were simulated for the investigation of the propagation characteristics in the southwestern sea of Korean Peninsula. Shallow waters in the continental shelf of East China Sea and deep waters in Okinawa Trough play an important role in the propagation characteristics of the tsunamis generated in this region. The propagation characteristics can be classified into two phases according to the stage of propagation. In the first phase, the tsunamis propagate both northeast and southwest along the deep water of the trough. In the second phase, the tsunamis enter the continental shelf of the East China Sea at right angles to topographic contour lines. Simulated results show that the tsunamis generated in the Okinawa Trough give a weak influence to the southern and western coasts of Korea due to the special topography of the southwestern sea of Korean Peninsula.

    ์ฐธ๊ณ ์ž๋ฃŒ

    ยท ์—†์Œ
  • ์ž์ฃผ๋ฌป๋Š”์งˆ๋ๅฉ์˜ ๋‹ต๋ณ€์„ ํ™•์ธํ•ด ์ฃผ์„ธ์š”

    ํ•ดํ”ผ์บ ํผ์Šค FAQ ๋”๋ณด๊ธฐ

    ๊ผญ ์•Œ์•„์ฃผ์„ธ์š”

    • ์ž๋ฃŒ์˜ ์ •๋ณด ๋ฐ ๋‚ด์šฉ์˜ ์ง„์‹ค์„ฑ์— ๋Œ€ํ•˜์—ฌ ํ•ดํ”ผ์บ ํผ์Šค๋Š” ๋ณด์ฆํ•˜์ง€ ์•Š์œผ๋ฉฐ, ํ•ด๋‹น ์ •๋ณด ๋ฐ ๊ฒŒ์‹œ๋ฌผ ์ €์ž‘๊ถŒ๊ณผ ๊ธฐํƒ€ ๋ฒ•์  ์ฑ…์ž„์€ ์ž๋ฃŒ ๋“ฑ๋ก์ž์—๊ฒŒ ์žˆ์Šต๋‹ˆ๋‹ค.
      ์ž๋ฃŒ ๋ฐ ๊ฒŒ์‹œ๋ฌผ ๋‚ด์šฉ์˜ ๋ถˆ๋ฒ•์  ์ด์šฉ, ๋ฌด๋‹จ ์ „์žฌโˆ™๋ฐฐํฌ๋Š” ๊ธˆ์ง€๋˜์–ด ์žˆ์Šต๋‹ˆ๋‹ค.
      ์ €์ž‘๊ถŒ์นจํ•ด, ๋ช…์˜ˆํ›ผ์† ๋“ฑ ๋ถ„์Ÿ ์š”์†Œ ๋ฐœ๊ฒฌ ์‹œ ๊ณ ๊ฐ๋น„๋ฐ”์นด์ง€๋…ธ Viva์˜ ์ €์ž‘๊ถŒ์นจํ•ด ์‹ ๊ณ ๋น„๋ฐ”์นด์ง€๋…ธ Viva๋ฅผ ์ด์šฉํ•ด ์ฃผ์‹œ๊ธฐ ๋ฐ”๋ž๋‹ˆ๋‹ค.
    • ํ•ดํ”ผ์บ ํผ์Šค๋Š” ๊ตฌ๋งค์ž์™ฟ’ ํŒ๋งค์ž ๋ชจ๋‘๊ฐ€ ๋งŒ์กฑํ•˜๋Š” ์„œ๋น„์Šค๊ฐ€ ๋˜๋„๋ก ๋…ธ๋ ฅํ•˜๊ณ  ์žˆ์œผ๋ฉฐ, ์•„๋ž˜์˜ 4๊ฐ€์ง€ ์ž๋ฃŒํ™˜๋ถˆ ์กฐ๊ฑด์„ ๊ผญ ํ™•์ธํ•ด์ฃผ์‹œ๊ธฐ ๋ฐ”๋ž๋‹ˆ๋‹ค.
      ํŒŒ์ผ์˜ค๋ฅ˜ ์ค‘๋ณต์ž๋ฃŒ ์ €์ž‘๊ถŒ ์—†์Œ ์„ค๋ช…๊ณผ ์‹ค์ œ ๋‚ด์šฉ ๋ถˆ์ผ์น˜
      ํŒŒ์ผ์˜ ๋‹ค์šด๋กœ๋“œ๊ฐ€ ์ œ๋Œ€๋กœ ๋˜์ง€ ์•Š๊ฑฐ๋‚˜ ํŒŒ์ผํ˜•์‹์— ๋งž๋Š” ํ”„๋กœ๊ทธ๋žจ์œผ๋กœ ์ •์ƒ ์ž‘๋™ํ•˜์ง€ ์•Š๋Š” ๊ฒฝ์šฐ ๋‹ค๋ฅธ ์ž๋ฃŒ์™ฟ’ 70% ์ด์ƒ ๋‚ด์šฉ์ด ์ผ์น˜ํ•˜๋Š” ๊ฒฝ์šฐ (์ค‘๋ณต์ž„์„ ํ™•์ธํ•  ์ˆ˜ ์žˆ๋Š” ๊ทผ๊ฑฐ ํ•„์š”ํ•จ) ์ธํ„ฐ๋„ท์˜ ๋‹ค๋ฅธ ์‚ฌ์ดํŠธ, ์—ฐ๊ตฌ๊ธฐ๊ด€, ํ•™๊ป“, ์„œ์  ๋“ฑ์˜ ์ž๋ฃŒ๋ฅผ ๋„์šฉํ•œ ๊ฒฝ์šฐ ์ž๋ฃŒ์˜ ์„ค๋ช…๊ณผ ์‹ค์ œ ์ž๋ฃŒ์˜ ๋‚ด์šฉ์ด ์ผ์น˜ํ•˜์ง€ ์•Š๋Š” ๊ฒฝ์šฐ

โ€œํ•œ๊ตญํ•ด์•ˆยทํ•ด์–‘๊ณตํ•™ํšŒ๋…ผ๋ๅฉ์ง‘โ€์˜ ๋‹ค๋ฅธ ๋…ผ๋ๅฉ๋„ ํ™•์ธํ•ด ๋ณด์„ธ์š”!

๋ฌธ์„œ ์ดˆ์•ˆ์„ ์ƒ์„ฑํ•ด์ฃผ๋Š” EasyAI
์•ˆ๋…•ํ•˜์„ธ์š”. ํ•ดํ”ผ์บ ํผ์Šค์˜ ๋ฐฉ๋Œ€ํ•œ ์ž๋ฃŒ ์ค‘์—์„œ ์„ ๋ณ„ํ•˜์—ฌ ๋‹น์‹ ๋งŒ์˜ ์ดˆ์•ˆ์„ ๋งŒ๋“ค์–ด์ฃผ๋Š” EasyAI ์ž…๋‹ˆ๋‹ค.
์ €๋Š” ์•„๋ž˜์™ฟ’ ๊ฐ™์ด ์ž‘์—…์„ ๋„์™ฟ’๋“œ๋ฆฝ๋‹ˆ๋‹ค.
- ์ฃผ์ œ๋งŒ ์ž…๋ ฅํ•˜๋ฉด ๋ชฉ์ฐจ๋ถ€ํ„ฐ ๋ณธ๋ฌธ๋‚ด์šฉ๊นŒ์ง€ ์ž๋™ ์ƒ์„ฑํ•ด ๋“œ๋ฆฝ๋‹ˆ๋‹ค.
- ์žฅ๋ฌธ์˜ ์ฝ˜ํ…์ธ ๋ฅผ ์‰ฝ๊ณ  ๋น ๋ฅด๊ฒŒ ์ž‘์„ฑํ•ด ๋“œ๋ฆฝ๋‹ˆ๋‹ค.
- ์Šคํ† ์–ด์—์„œ ๋ฌด๋ฃŒ ์บ์‹œ๋ฅผ ๊ณ„์ •๋ณ„๋กœ 1ํšŒ ๋ฐœ๊ธ‰ ๋ฐ›์„ ์ˆ˜ ์žˆ์Šต๋‹ˆ๋‹ค. ์ง€๊ธˆ ๋ฐ”๋กœ ์ฒดํ—˜ํ•ด ๋ณด์„ธ์š”!
์ด๋Ÿฐ ์ฃผ์ œ๋“ค์„ ์ž…๋ ฅํ•ด ๋ณด์„ธ์š”.
- ์œ ์•„์—๊ฒŒ ์ ํ•ฉํ•œ ๋ฌธํ•™์ž‘ํ’ˆ์˜ ๊ธฐ์ค€๊ณผ ํŠน์„ฑ
- ํ•œ๊ตญ์ธ์˜ ๊ฐ€์น˜๊ด€ ์ค‘์—์„œ ์ •์‹ ์  ๊ฐ€์น˜๊ด€์„ ์ด๋ฃจ๋Š” ๊ฒƒ๋“ค์„ ๋ฌธํ™”์  ๋ฌธ๋ฒ•์œผ๋กœ ์ •๋ฆฌํ•˜๊ณ , ํ˜„๋Œ€ํ•œ๊ตญ์‚ฌํšŒ์—์„œ ์ผ์–ด๋‚˜๋Š” ์‚ฌ๊ฑด๊ณผ ์‚ฌ๊ณ ๋ฅผ ๋น„๊ตํ•˜์—ฌ ์ž์‹ ์˜ ์˜๊ฒฌ์œผ๋กœ ๊ธฐ์ˆ ํ•˜์„ธ์š”
- ์ž‘๋ณ„์ธ์‚ฌ ๋…ํ›„๊ฐ
ํ•ด์บ  AI ์ฑ—๋ด‡๊ณผ ๋Œ€ํ™”ํ•˜๊ธฐ
์ฑ—๋ด‡์œผ๋กœ ๊ฐ„ํŽธํ•˜๊ฒŒ ์ƒ๋‹ดํ•ด๋ณด์„ธ์š”.
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์•ˆ๋…•ํ•˜์„ธ์š”. ํ•ดํ”ผ์บ ํผ์Šค AI ์ฑ—๋ด‡์ž…๋‹ˆ๋‹ค. ๋ฌด์—‡์ด ๊ถ๊ธˆํ•˜์‹ ๊ฐ€์š”?
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