[논문]한반도에서 위험기상 발생 시 나타나는 해수면온도 변동의 특성

정은실

doi:10.5467/jkess.2019.40.3.240

한반도에서 위험기상 발생 시 나타나는 해수면온도 변동의 특성
Characteristics of Sea Surface Temperature Variation during the High Impact Weather over the Korean Peninsula 원문보기

한국지구과학회지 = Journal of the Korean Earth Science Society, v.40 no.3, 2019년, pp.240 - 258

초록
AI-Helper

태풍, 집중호우, 대설은 매년 우리나라에서 치명적인 손실을 초래한다. 따라서 정기적인 관측을 통하여 이러한 현상의 발생 가능성을 미리 알 수 있다면, 사회적으로 큰 유익을 제공할 수 있을 것이다. 우리나라는 삼면이 바다로 둘러싸여 있고, 해수면온도가 태풍, 집중호우, 대설 발달에 직 간접적으로 영향을 미치므로, 이 논문에서는 위험기상과 관련하여 나타나는 해수면온도 변동성의 특성을 조사하였다. 우리나라에서 발생하는 집중호우는 서울경기 부근 및 서해안을 중심으로, 그리고 남해안을 중심으로 분포하였다. 대설은 주로 동해안지역(이하 영동 대설)과 남서부 지역(호남형 대설)에서 발생하였다. 위험기상 종류 및 주요 발생지역에 따라 해수면온도 변동성이 조금씩 다르게 나타났으며, 집중호우 발생 시에 진도-제주도-이어도-중국 상하이 방향으로 이어지는 해역에서 해수면온도 변동성이 크게 나타났다. 대설 발생 시, 대설형태와 상관없이, 제주도 남쪽 해상에서 해수면온도 변동성이 작은 영역이 관측되었으며, $130^{\circ}E$, $39^{\circ}N$ 부근 동해상에서 강한 해수면온도 변동성이 나타났다. 해수면온도 변동성이 큰 지역은, 대기-해양 상호작용 메커니즘을 연구하는 기초자료로 사용될 수 있을 뿐만 아니라, 배경대기 에어로졸 관측영역 결정에도 활용될 것이다.

Abstract ▼ AI-Helper

Typhoons, torrential rainfall, and heavy snowfall cause catastrophic losses each year in the Republic of Korea. Therefore, if we can know the possibility of this phenomenon in advance through regular observations, it will be greatly beneficial to Korean society. Korea is surrounded by sea on its three sides, and the sea surface temperature (SST) directly or indirectly affects the development of typhoons, heavy rainfall, and heavy snowfall. Therefore, the characteristics of SST variability related to the high impact weather are investigated in this paper. The heavy rainfall in Korea was distributed around Seoul, Gyeonggi, and west and southern coast. The heavy snowfall occurred mainly in the eastern coastal (hereafter Youngdong Heavy Snow) and the southwestern region (hereafter Honam-type heavy snow). The SST variability was slightly different depending on the type and major occurrence regions of the high impact weather. When the torrential rain occurred, the SST variability was significantly increased in the regions extending to Jindo-Jeju island-Ieodo-Shanghai in China. When the heavy snow occurred, the SST variability has reduced in the southern sea of Jeju island, regardless of the type of heavy snowfall, whereas the SST variability has increased in the East Sea near $130^{\circ}E$ and $39^{\circ}N$. Areas with high SST variability are anticipated to be used as a basis for studying the atmospheric-oceanic interaction mechanism as well as for determining the background atmospheric aerosol observation area.

주제어

질의응답

핵심어	질문	논문에서 추출한 답변
	집중호우는 어떤 것들과 밀접한 관련이 있는 것으로 알려져 있는가?	, 2016). 집중호우는 종관패턴 및 하층제트와 밀접한 관련이 있는 것으로 알려져 있으며 일반적으로 강수발생 전후에 하층제트가 나타난다(Baek et al., 2005).
	대규모 대기환경변수와 위험기상 발생 연관성에 대한 연구에는 어떤 예가 있는가?	, 2015; Jung and Kirtman, 2016b). 예를 들어, 이른 봄 미국에서 발생하는 토네이도는 엘니뇨-남방진동(El Nino-southern oscillation, ENSO) 과 밀접한 관계가 있지만(Allen et al., 2015), 늦은 봄에서 초 여름사이(5월에서 7월) 발생하는 대류성 폭풍과는 관련성이 적으며, 이 시기의 미국 내 토네이도 발생 가능성은 맥시코만 수온정보를 이용하여 예측할 수 있다(Jung and Kirtman, 2016b).
	태풍이란 무엇인가?	태풍은 북서태평양에서 발생하는 열대저기압으로 매년 약 3개 정도 한반도에 영향을 미치며, 주로 6월에서 10월 사이에 발생하여 한반도 강수량의 많은 부분을 차지한다(국가태풍센터). 우리나라에서 집중호우는 6월에서 9월 사이에, 대설은 11월에서 3월 사이에 주로 나타난다.

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용어 설명: PCR은 세균 특이성이 있는 primer를 이용하여 적은 수의 세균이 있을지라도 쉽게 검출할 수 있는 유용한 방법이며, 이를 이용하여 구강 내 치면세균막이나 타액에서 직접 세균을 검출할 수 있게 되었다[8].

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