• Title/Summary/Keyword: snow falling phenomenon

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Snow Falling Phenomenon of the Korean Peninsular Based on the Records of Old Literatures (역사서 검색으로 관찰한 한반도 강설현상)

  • 김기원;신만용
    • Korean Journal of Agricultural and Forest Meteorology
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    • v.4 no.4
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    • pp.248-253
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    • 2002
  • This study was to provide information about snow falling phenomenon in Korea for 1934 years from BC 6 to 1928 based on the records of old literatures, which are the true record of the Chosun dynasty, records of king Kojong and Soonjong, and some data including history of the Koryo in internet home page of Korea meteorological administration. Key words used in search procedure were totally 20 words such as snow, heavy snow, big snow, snow pellets, snowstorm, avalanche, etc. The searching contents consisted of the time of the first and the last snow, the amount of snow falling, snow damage, the thought about heavy snow phenomenon, and unusual weather conditions related to snow. The earliest record for the first snow was July of the rural calendar in 733 and the latest record for the last snow was June 11 of the lunar calendar. From these records, it could be estimated that there were some snow falling even in summer season. The amount of almost heavy snow ranged from 1.2 m to 1.5 m, but sometimes there were some records about the amount of snow falling higher than 3 meters. It was also found that there were three records about big heavy snow damages. In 1524 and 1525, approximately 100 and 140 peoples in Kyungsung, Hamgyung Province were dead due to heavy snowstorm. It was also recorded that 91 people in Jeiu island were dead in 1670 because of snow damage. Some singular records about snow were also found in old literatures. There was a congratulatory ceremony of new snow when the first snow was falling in the year. There was also a ritual praying for snow when there was no snow in the year. It was also found that there was snow falling with worms and red snow falling.

Characteristics of Snow Falling Phenomenon in Korea Based on the Records of Old Literatures (고문헌 기록에 나타난 우리나라 강설현상의 특징)

  • 김기원;신만용
    • Proceedings of The Korean Society of Agricultural and Forest Meteorology Conference
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    • 2002.11a
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    • pp.89-92
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    • 2002
  • 동일 주제를 대상으로 현시대의 것과 지난 수 백년 전 과거의 것을 서로 비교하는 연구는 차이점을 발견할 수 있으리라는 기대감 하나 때문만이라도 흥미를 갖게 한다. 본 논문은 $\boxDr$국역 조선왕조실록$\boxUl$$\boxDr$국역 고종순종실록$\boxUl$ (서울 시스템간) 및 인터넷을 검색하여 과거 1934년 간의 우리나라 강설현상을 추적하여 그 특징을 정리하여 본 것이다.(중략)

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Projection of Future Snowfall by Using Climate Change Scenarios (기후변화 시나리오를 이용한 미래의 강설량 예측)

  • Joh, Hyung-Kyung;Kim, Saet-Byul;Cheong, Hyuk;Shin, Hyung-Jin;Kim, Seong-Joon
    • Journal of the Korean Association of Geographic Information Studies
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    • v.14 no.3
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    • pp.188-202
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    • 2011
  • Due to emissions of greenhouse gases caused by increased use of fossil fuels, the climate change has been detected and this phenomenon would affect even larger changes in temperature and precipitation of South Korea. Especially, the increase of temperature by climate change can affect the amount and pattern of snowfall. Accordingly, we tried to predict future snowfall and the snowfall pattern changes by using the downscaled GCM (general circulation model) scenarios. Causes of snow varies greatly, but the information provided by GCM are maximum / minimum temperature, rainfall, solar radiation. In this study, the possibility of snow was focused on correlation between minimum temperatures and future precipitation. First, we collected the newest fresh snow depth offered by KMA (Korea meteorological administration), then we estimate the temperature of snow falling conditions. These estimated temperature conditions were distributed spatially and regionally by IDW (Inverse Distance Weight) interpolation. Finally, the distributed temperature conditions (or boundaries) were applied to GCM, and the future snowfall was predicted. The results showed a wide range of variation for each scenario. Our models predict that snowfall will decrease in the study region. This may be caused by global warming. Temperature rise caused by global warming highlights the effectiveness of these mechanisms that concerned with the temporal and spatial changes in snow, and would affect the spring water resources.

The Yellow-Sand Phenomenon and Yellow Fog Recorded in the "Koryosa" (고려사에 기록된 황사와 황무 현상)

  • 전영신;오성남;권완태
    • The Korean Journal of Quaternary Research
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    • v.14 no.1
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    • pp.49-55
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    • 2000
  • The Yellow-Sand phenomena occurred during the period from l0C to 14C in Korea have been investigated using the historical record of the Koryosa. It is written as the "dust rain"or "mud" which means the falling down of dust from the sky. The authors have extracted 50 historical writings of dust rain from the Koryosa. The results show that the observation records concerning Yellow-Sand phenomenon for the period of Korea Dynasty (918~1392) are described with the scientific accuracy for the Yellow-Sand phenomena as the pure dust phenomena, the mixture of Yellow Sand with snow or rain, and the Yellow-Sand associated with fog or hail, etc. It is also found that the occurrence of Yellow-Sand phenomena was the incomprehensible natural phenomena such as Yellow-Sand were interpreted as a warning from the Heaven to the king and people of their fail in moral principles.in moral principles.

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A Case Study on Meteorological Analysis of Freezing Rain and Black Ice Formation on the Load at Winter (겨울철 노면에 발생하는 어는 비와 블랙아이스의 기상학적 분석에 관한 사례 연구)

  • Park, Geun-Yeong;Lee, Soon-Hwan;Kim, Eun-Ji;Yun, Byeong Yeong
    • Journal of Environmental Science International
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    • v.26 no.7
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    • pp.827-836
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    • 2017
  • Freezing rain is a phenomenon when precipitation falls as a liquid rain drop, but freezes when it comes into contact with surfaces or objects. In this study, we investigated the predictability of freezing rain and its characteristics, which are strongly related with the occurrence of black ice using synoptic scale meteorological observation data. Two different cases occurred at 2012 were analyzed and in the presented cases, freezing rain often occurs in the low-level low pressure with the warm front. The warm front due to the lower cyclone make suitable environment in which snow falling from the upper layer can change into supercooled water. The $0^{\circ}C$ temperature line to generate supercooling water is located at an altitude of 850 hPa in the vertical temperature distribution. And the ground temperature remained below zero, as is commonly known as a condition for black ice formation. It is confirmed that the formation rate of freezing rain is higher when the thickness after 1000-850 hPa is 1290-1310 m and the thickness of 850-700 hPa layer is larger than 1540 m in both cases. It can also be used to predict and estimate the generation of freezing rain by detecting and analyzing bright bands in radar observation.