지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
이 논문의 연구 히스토리 (6)
2015
2014
- 이 논문의 후속연구가 궁금하신가요?
- 연관 학술논문 또는 학술발표를 통해 보다 발전된 연구결과를 확인하실 수 있습니다.
- 이 논문의 연구 히스토리 확인하기
초록· 키워드
오류제보하기
Thermodynamic conditions related with localized torrential rainfall in the middle west region of Korean peninsula are examined using radar rain rate and radiosonde observational data. Localized torrential rainfall events in this study are defined by three criteria base on 1) any one of Automated Synoptic Observing System (ASOS) hourly rainfall exceeds 30 mmhr<SUP>?1</SUP> around Osan, 2) the rain (> 1 mmhr<SUP>?1</SUP>) area estimated from radar reflectivity is less than 20,000 ㎢, and 3) the rain (> 10 mmhr<SUP>?1</SUP>) cell is detected clearly and duration is short than 24 hr. As a result, 13 cases were selected during the summer season of 10 years (2004-13). It was found that the duration, the maximum rain area, and the maximum volumetric rain rate of convective cells (> 30 mmhr?1) are less than 9hr, smaller than 1,000 ㎢, and 15,000~ 60,000 m3s<SUP>?1</SUP> in these cases. And a majority of cases shows the following thermodynamic characteristics: 1) Convective Available Potential Energy (CAPE) > 800 Jkg<SUP>?1</SUP>, 2) Convective Inhibition (CIN) < 40 Jkg<SUP>?1</SUP>, 3) Total Precipitable Water (TPW) ? 55 mm, and 4) Storm Relative Helicity (SRH) < 120 ㎡s<SUP>?2</SUP>. These cases mostly occurred in the afternoon. These thermodynamic conditions indicated that these cases were caused by strong atmospheric instability, lifting to overcome CIN, and sufficient moisture. The localized torrential rainfall occurred with deep moisture convection result from the instability caused by convective heating.
목차
Abstract
1. 서론
2. 사례선정 및 연구방법
3. 국지성 집중호우사례의 강우특징
4. 국지성 집중호우와 열역학적 특성의 관계성
5. 요약 및 토의
REFERENCES
참고문헌 (25)
참고문헌 신청
1. [학술대회논문] - Atlas, D. / 1957 / Physical-synoptic variations of drop size parameter / Proc. 6th. Wea. Radar Conf. : 21 ~ 29
2. [학술지(정기간행물)] - Beebe, R. G. / 1955 / Types of air masses in which tornadoes occur / Bull. Amer. Meteor. Soc. 36 : 349 ~ 350
3. [단행본] - Byers, H. R. / 1949 / The thunderstorm / U.S. Government Printing Office : 287 ~
4. [단행본] - Djuric, D. / 1994 / Weather Analysis / Prentice-Hall, Inc. : 304 ~
5. [보고서] - Eblen, L. H. / 1990 / Severe thunderstorm forecasting : 42 ~
2. [학술지(정기간행물)] - Beebe, R. G. / 1955 / Types of air masses in which tornadoes occur / Bull. Amer. Meteor. Soc. 36 : 349 ~ 350
3. [단행본] - Byers, H. R. / 1949 / The thunderstorm / U.S. Government Printing Office : 287 ~
4. [단행본] - Djuric, D. / 1994 / Weather Analysis / Prentice-Hall, Inc. : 304 ~
5. [보고서] - Eblen, L. H. / 1990 / Severe thunderstorm forecasting : 42 ~
이 논문의 저자 정보
이 논문과 함께 이용한 논문
최근 본 자료
댓글(0)
0
UCI(KEPA) : I410-ECN-0101-2016-453-001001874