준관성주기파(NIW)는 주로 바람에 의해 생성되며, 해양 연직혼합에 중요한 요소이다. 태풍의 빠른 풍속과 이동경로에 따른 풍향변화는 NIW 생성에 충분한 조건을 제공한다. 본 연구에서는 동...
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https://www.riss.kr/link?id=A107025083
송하진
(인하대학교 해양과학‧생물공학과)
;
전찬형
(Massachusetts Institute of Technology (MIT))
;
채정엽
(인하대학교)
;
이은주
(인하대학교)
;
이강녕
(인하대학교 해양과학‧생물공학과)
;
최영석
(지오시스템)
;
박재훈
(인하대학교)
;
SONG, HAJIN
;
JEON, CHANHYUNG
;
CHAE, JEONG-YEOB
;
LEE, EUN-JOO
;
LEE, KANG-NYEONG
;
TAKAYAMA, KATSUMI
;
CHOI, YOUNGSEOK
;
PARK, JAE-HUN
2020
Korean
KCI등재
학술저널
55-66(12쪽)
0
0
상세조회0
다운로드국문 초록 (Abstract)
준관성주기파(NIW)는 주로 바람에 의해 생성되며, 해양 연직혼합에 중요한 요소이다. 태풍의 빠른 풍속과 이동경로에 따른 풍향변화는 NIW 생성에 충분한 조건을 제공한다. 본 연구에서는 동...
준관성주기파(NIW)는 주로 바람에 의해 생성되며, 해양 연직혼합에 중요한 요소이다. 태풍의 빠른 풍속과 이동경로에 따른 풍향변화는 NIW 생성에 충분한 조건을 제공한다. 본 연구에서는 동해 실시간 해황예보모형 출력자료를 이용하여 태풍의 영향으로 인한 NIW의 생성과 분포 그리고 동해 중규모 소용돌이가 NIW의 심층 전파에 주는 영향에 대해 검토하였다. 이용한 출력자료 기간은 2013년부터 2017년까지 총 5개년이며, 이 기간 중 동해에 강한 NIW에너지를 만든 3개 태풍(할롱, 고니, 차바)에 초점을 맞추었다. 태풍에 의한 NIW 변동을 검토하기 위하여 강제력으로 작용하는 태풍의 바람에너지유입(${\bar{W}}_I$)과 함께 NIW 에너지의 지표인 혼합층 및 심층 수평운동에너지(${\bar{HKE}}_{MLD}$, ${\bar{HKE}}_{DEEP}$)를 계산하였다. ${\bar{HKE}}_{MLD}$는 ${\bar{W}}_I$와 밀접한 관련을 보였으며 태풍 경로의 오른편에서 강하게 나타났다. ${\bar{HKE}}_{DEEP}$는 주로 동해 남부에서 패치형태로 강하게 나타났으며, 음의 상대 소용돌이도를 가지는 난수성 소용돌이와의 상관성이 확인되었다. NIW에너지에 태풍이 주는 영향을 확인하기 위해, 태풍이 없는 여름철과 12월의 에너지와 상호 비교하였다. 그 결과, 태풍에 의한 ${\bar{HKE}}_{MLD}$는 태풍이 없는 여름에 비해 2.5~5.7배, NIW가 가장 큰 12월 평균대비 0.4~1.0배였고, 태풍에 의한 ${\bar{HKE}}_{DEEP}$는 태풍이 없는 여름대비 1.2~1.6배, 12월 평균대비 0.8~1.0배로 태풍에 의한 NIW가 혼합층과 심층의 해양 연직혼합 모두에 상당한 영향을 줄 수 있음을 확인하였다.
다국어 초록 (Multilingual Abstract)
Near-inertial waves (NIW) which are primarily generated by wind can contribute to vertical mixing in the ocean. The energetic NIW can be generated by typhoon due to its strong wind and preferable wind direction changes especially on the right-hand sid...
Near-inertial waves (NIW) which are primarily generated by wind can contribute to vertical mixing in the ocean. The energetic NIW can be generated by typhoon due to its strong wind and preferable wind direction changes especially on the right-hand side of the typhoon. Here we investigate the generation and distribution of NIW using the output of a real-time ocean forecasting system. Five-year model outputs during 2013-2017 are analyzed with a focus on cases of energetic NIW generation by the passage of three typhoons (Halong, Goni, and Chaba) over the East Sea. Calculations of wind energy input (${\bar{W}}_I$), and horizontal kinetic energy in the mixed layer (${\bar{HKE}}_{MLD}$) reveal that the spatial distribution of ${\bar{HKE}}_{MLD}$, which is strengthened at the right-hand side of typhoon tracks, is closely related with ${\bar{W}}_I$. Horizontal kinetic energy in the deep layer (${\bar{HKE}}_{DEEP}$) shows patch-shaped distribution mainly located at the southern side of the East Sea. Spatial distribution of ${\bar{HKE}}_{DEEP}$ shows a close relationship with negative relative vorticity regions caused by warm eddies in the upper layer. Monthly-mean ${\bar{HKE}}_{MLD}$ and ${\bar{HKE}}_{DEEP}$ during a typhoon passing over the East Sea shows about 2.5-5.7 times and 1.2-1.6 times larger values than those during summer with no typhoons, respectively. In addition, their magnitudes are respectively about 0.4-1.0 and 0.8-1.0 times from those during winter, suggesting that the typhoon-induced NIW can provide a significant energy to enhance vertical mixing at both the mixed and deep layers during summer.
참고문헌 (Reference)
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3 Lee, D. -K., "The inertial chimney: The near‐inertial energy drainage from the ocean surface to the deep layer" 103 (103): 7579-7591, 1998
4 D’Asaro, E.A, "The energy flux from the wind to near‐inertial motions in the surface mixed layer" 15 (15): 1043-1059, 1985
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7 Noh, Y., "Simulations of temperature and turbulence structure of the oceanic boundary layer with the improved near‐surface process" 104 (104): 15621-15634, 1999
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학술지 이력
연월일 | 이력구분 | 이력상세 | 등재구분 |
---|---|---|---|
2027 | 평가예정 | 재인증평가 신청대상 (재인증) | |
2021-01-01 | 평가 | 등재학술지 유지 (재인증) | ![]() |
2018-01-01 | 평가 | 등재학술지 유지 (등재유지) | ![]() |
2015-01-01 | 평가 | 등재학술지 유지 (등재유지) | ![]() |
2011-01-01 | 평가 | 등재 1차 FAIL (등재유지) | ![]() |
2009-01-01 | 평가 | 등재학술지 유지 (등재유지) | ![]() |
2007-09-04 | 학술지명변경 | 외국어명 : 미등록 -> JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY | ![]() |
2006-01-01 | 평가 | 등재학술지 선정 (등재후보2차) | ![]() |
2005-05-30 | 학술지명변경 | 한글명 : 한국해양학회지 바다 -> 바다 | ![]() |
2005-01-01 | 평가 | 등재후보 1차 PASS (등재후보1차) | ![]() |
2004-01-01 | 평가 | 등재후보학술지 유지 (등재후보2차) | ![]() |
2003-01-01 | 평가 | 등재후보 1차 PASS (등재후보1차) | ![]() |
2002-01-01 | 평가 | 등재후보학술지 유지 (등재후보1차) | ![]() |
1999-07-01 | 평가 | 등재후보학술지 선정 (신규평가) | ![]() |
학술지 인용정보
기준연도 | WOS-KCI 통합IF(2년) | KCIF(2년) | KCIF(3년) |
---|---|---|---|
2016 | 0.6 | 0.6 | 0.56 |
KCIF(4년) | KCIF(5년) | 중심성지수(3년) | 즉시성지수 |
0.54 | 0.59 | 0.933 | 0.13 |