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Alopecia Mucinosa(점액성(粘液性) 탈모증(脫毛症))의 피부치료(皮膚治療)를 위한 황련해독탕(黃連解毒湯)의 사용
김해민 ( Hae-min Kim ),송원석 ( Won-seok Song ) 대한상한금궤의학회 2010 대한상한금궤의학회지 Vol.2 No.1
Objective : whether Alopecia mucinosa can be treated by Hwangryeonhaedok-tang(Huanglianjiedutang). Method : studying theses regarding Hwangryeonhaedok-tang(Huanglianjiedu-tang) and treatment of Mucinous alopecia. Results : 1. Hwangryeonhaedok-tang(Huanglianjiedu-tang) can be used as a drug for treatment on skin inflammation of Alopecia mucinosa. 2. Mucinous alopecia shows the characteristics of the Ban of red papules and Inflammatory Board. This is causing inflammation in oder to prevent skin regeneration. 3. Many studies showed that Hwangryeonhaedok-tang(Huanglianjiedu-tang) can be useful as in antiinflammatory agent for skin treatment. 4. Hwangryeonhaedok-tang(Huanglianjiedu-tang) is used to inhibit the production of inflammationrelated substances and helps regeneration of skin damage caused by inflammation. Conclusions : Hwangryeonhaedok-tang(Huanglianjiedu-tang) can be used for treatment on skin inflammation of Alopecia mucinosa.
김해민(Hae-Min Kim),정승필(Sueng-Pill Jung),인소라(So-Ra In),최병철(Byoung-Choel Choi) 한국기상학회 2018 대기 Vol.28 No.2
The heavy snowfall phenomenon with thunder and lightning occurred in Yeongdong coastal region on 20 January 2017. Amount of snow on that day was a maximum of 47 cm and was concentrated in a short time (2 hours) at the Yeongdong coastal area. The mechanism of thundersnow was investigated to describe in detail using observational data and numerical simulation (Weather Research and Forecast, WRF) applied lightning option. The results show that a convective cloud occurred at the Yeongdong coastal area. The east wind flow was generated and the pressure gradient force was maximized by the rapidly developed cyclone. The cold and dry air in the upper atmosphere has descended (so called tropopause folding) atmospheric lower layer at precipitation peak time (1200 LST). In addition, latent heat in the lower atmosphere layer and warm sea surface temperature caused thermal instability. The convective cloud caused by the strong thermal instability was developed up to 6 km at that time. And the backdoor cold front was determined by the change characteristics of meteorological elements and shear line in the east sea. Instability indexes such as Total totals Index (TT) and Lightning Potential Index (LPI) are also confirmed as one of good predictability indicates for the explosive precipitation of convective rainfall.
김해민 ( Kim Hae Min ) 한국중국어문학회 2021 中國文學 Vol.106 No.-
The Lian Ju Shi(聯句詩 or Joint Sentences Poem) that began with the Han Dynasty Bai Liang Ti was created in earnest at the Zhong Tang, and among them, the Lian Ju Shi(聯句詩 or Joint Sentences Poem) of the Han Meng School of poetry(韓孟詩派) are considered the highest peak of Lian Ju Shi(聯句詩 or Joint Sentences Poem). Lian Ju Shi(聯句詩 or Joint Sentences Poem) in which several people create one piece of work, not only has an entertaining function, but also competes for talents among participants, therefore creating a strong sense of competition for each other. The Lian Ju Shi(聯句詩 or Joint Sentences Poem) of the Han Meng School of poetry(韓孟詩派) used contents that were not covered in the previous Lian Ju Shi(聯句詩 or Joint Sentences Poem) while having the basic characteristics of the Lian Ju Shi(聯句詩 or Joint Sentences Poem), and various changes were made in the formal aspect of the Lian Ju Shi(聯句詩 or Joint Sentences Poem). This study examines the characteristics of the Lian Ju Shi(聯句詩 or Joint Sentences Poem) created by the Han Meng School of poetry(韓孟詩派), comparison with the Lian Ju Shi(聯句詩 or Joint Sentences Poem) created by Bai Ju Yi and Liu Yu Xi, who were active in the same period. I will examine the characteristics of the Lian Ju Shi(聯句詩 or Joint Sentences Poem) of the Han Meng School of poetry(韓孟詩派), and analyze the means of the Lian Ju Shi(聯句詩 or Joint Sentences Poem) used by the Han Meng School of poetry(韓孟詩派) through these features.
2020년 2월 8일 영동지역 강설 사례 시 관측과 수치모의 된 바람 분석
김해민(Hae-Min Kim),남형구(Hyoung-Gu Nam),김백조(Baek-Jo Kim),지준범(Joon-Bum Jee) 한국기상학회 2021 대기 Vol.31 No.4
The wind speed and wind direction in Yeongdong are one of the crucial meteorological factors for forecasting snowfall in this area. To improve the snowfall forecast in Yeongdong region, Yeongdong Extreme Snowfall-Windstorm Experiment, YES-WEX was designed. We examined the wind field variation simulated with Local Data Assimilation and Prediction System (LDAPS) using observed wind field during YES-WEX period. The simulated wind speed was overestimated over the East Sea and especially 2 to 4 times in the coastal line. The vertical wind in Yeongdong region, which is a crucial factor in the snowfall forecast, was not well simulated at the low level (850 hPa~1000 hPa) until 12 hours before the forecast. The snowfall distribution was also not accurately simulated. Three hours after the snowfall on the East Sea coast was observed, the snowfall was simulated. To improve the forecast accuracy of snowfall in Yeongdong region, it is important to understand the weather conditions using the observed and simulated data. In the future, data in the northern part of the East Sea and the mountain slope of Taebaek observed from the meteorological aircraft, ship, and drone would help in understanding the snowfall phenomenon and improving forecasts.
김현욱(Kim, Hyunuk),김백조(Kim, Baek-Jo),김해민(Kim, Hae-Min),이진화(Lee, Jin-Hwa),심재관(Shim, Jae-Kwan) 한국방재학회 2020 한국방재학회논문집 Vol.20 No.1
본 연구는 대설 피해가 빈번하게 발생하는 10개 관측지점을 대상으로 피해유발 임계값을 추정하였다. 또한, 추정된 임계값을기반으로 유사한 지역을 구분하고 그 특징을 조사하였다. 연구 자료는 기상청에서 제공하는 신적설 관측 자료와 행정안전부에서발행되는 재해연보의 피해 자료를 사용하였다. 연구방법은 로지스틱회귀분석, Critical Success Index, Probability of Detection 그리고 False-Alarm Ratio를 적용하였다. 연구 결과, 추정된 임계값은 지역별로 차이를 보였다. 이와 같은 결과는 분석방법, 지역별 방재대책, 지역주민의 대처, 구조물의 취약성 그리고 기상현상 등 많은 요인이 원인으로 판단된다. 또한, 추정된임계값을 활용하여 임계값이 민감한 지역, 임계값의 차이가 큰 지역과 작은 지역은 각각 해안지역, 강원지역, 내륙지역에대응되었다. 강원지역은 강설의 지속시간이 길고, 폭설이 관측된 경우가 많았으나, 내륙지역은 상대적으로 약한 강설과 짧은강설 지속시간을 보였다. In this study, the estimation of damage-causing thresholds and their application to regional classification were examined using logistic regression, critical success index, probability of detection, and a false-alarm ratio. For 10 stations where damage caused by heavy snow occurred frequently, the fresh snow depth data provided by the Korea Meteorological Administration and heavy snow-related damage data obtained by the Ministry of Interior and Safety were used. Results show that the estimated thresholds differed by region. These results are attributed to many factors such as analysis methods, regional disaster protection, the response of local residents, vulnerability of structures, and meteorological characteristics. Additionally, based on estimated thresholds, the area with the highest threshold-sensitivity and the areas with the most internal differences and similarities between calculated thresholds corresponded to the coastal region, the Gangwon region, and the inland region, respectively. Gangwon region, where heavy snow was often observed, had a long duration of snowfall, whereas inland regions faced snowfalls that were relatively weaker in intensity and shorter in duration.
2011년 2월 11~12일 부산 근해에서 발달한 극저기압에 대한 사례연구
이재규(Jae Gyoo Lee),김해민(Hae-Min Kim),김유진(Yu-Jin Kim) 한국기상학회 2016 대기 Vol.26 No.2
The evolutionary process of the polar low, which caused the heavy snowfall in the East Coast area on 11~12 February 2011, was investigated to describe in detail using synoptic weather charts, satellite imageries, and ERA (European Centre for Medium-Range Weather Forecasts Re-Analysis) -Interim reanalysis data. It was revealed that 1) the polar low was generated over the sea near Busan where a large cyclonic shear in the inverted trough branched from the parent low existed, 2) during the developing and mature stages, there was a convectively unstable region in the lower layer around the polar low and its south side, 3) the polar low was developed in the region where the static stability in the 500~850 hPa layer was the lowest, 4) the result from the budget analysis of the vorticity equation indicated that the increase in the vorticity at the lower atmosphere, where the polar low was located, was dominated mainly by the stretching term, 5) the warm core structure of the polar low was identified in the surface-700 hPa layer during the mature stage, 6) there was a close inverse relationship between a development of the polar low and the height of the dynamic tropopause over the polar low, and 7) for generation and development of the polar low, large-scale circulation systems, such as upper cold low and its combined short wave trough, major low (parent low), and polar air outbreak, should be presented, indicating that the polar low has the nature of the baroclinic disturbance.