• 한국데이터정보과학회:학술대회논문집
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• 한국데이터정보과학회 2002년도 춘계학술대회
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• pp.9-15
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• 2002

This paper presents the seasonal forecasting of the occurrence of tropical cyclone (TC) over Western North Pacific (WNP) using the generalized linear model (GLM) and dynamic linear model (DLM) based on 51-year-data (1951-2001) in TC season (June to November). The numbers of TC and TY are predictands and 16 indices (the E1 Nino/Southern Oscillation, the synoptic factors over East asia and WNP) are considered as potential predictors. With 30-year moving windowing, the estimation and prediction of TC and TY are performed using GLM. If GLM forecasts have some systematic error like a bias, DLM is applied to remove the systematic error in order to improve the accuracy of prediction.

• 한국해양학회지
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• 제8권1호
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• pp.4-8
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• 1973

Recent dynamic computations of zonal flow and analysis of oceanographic data of CSK in winter indicate year-to year variations in the location and dynmic structure of the Subtropic Countercurrent in the western North Pacific. In January 1966, the Subtropical Countercurrent migrated southward to 21$^{\circ}$- 22$^{\circ}$N Lat in association with the subsurface Subtropical Convergence. At the area of 25$^{\circ}$- 26$^{\circ}$N Lat, another surface thermal front was formed along which a stronger eastward flow of approximately 0.4kt is seen. On the section of 142$^{\circ}$E Long in January 1967, eastward flow appears at every interval of 2$^{\circ}$latitude in the northern waters of 20$^{\circ}$N Lat.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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• pp.7-11
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• 2002

This study introduces the first method that determines tropospheric ozone column directly from a space-based instrument. This method is based on the physical differences in the Total Ozone Mapping Spectrometer (TOMS) measurement as a function of its scan-angle geometry. Tropospheric ozone in September-October exhibits a broad enhancement over South America, the southern Atlantic Ocean, and western South Africa and a minimum over the central Pacific Ocean. Tropical tropospheric ozone south of the equator is higher than north of the equator in September-October, the southern burning season. Conversely, ozone north of the equator is higher in March, the northern burning season. Overall, the ozone over the southern tropics during September-October is significantly higher than over the northern tropics. Abnormally high tropospheric ozone occurs over the western Pacific Ocean during the El Nino season when the ozone amounts are as high as the ozone over the Africa.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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• pp.383-385
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• 2006

• 한국해안·해양공학회논문집
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• 제25권5호
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• pp.267-275
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• 2013

HadGEM2-AO 기후모델의 기후변화 시나리오 자료와 파랑 모델을 이용하여 기후변화에 따른 북서태평양에서의 미래 파랑 기후를 전망하였다. 21세기말 북서태평양에서 연 평균 풍속이 현재보다 낮아질 것으로 전망됨에 따라 연 평균 유의파고도 낮게 전망되었다. 현재 기후에 비해서 21세기 말 연평균 유의파고는 RCP4.5 시나리오의 경우 2~7% 감소하고, RCP8.5의 경우 4~11% 정도 감소하는 것으로 나타났다. 극한파랑의 경우도 유의파고 및 풍속이 현재에 비해서 감소할 것으로 전망되었다. 계절별로 분석한 결과 겨울철의 극한파랑은 연 극한 파랑과 비슷하게 감소하는 경향을 보인 반면, 여름철의 경우 북서태평양에서는 현재보다 증가할 것으로 나타나 미래에는 태풍의 강도가 강화 될 것으로 전망된다.

• 한국동물학회지
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• 제15권2호
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• pp.87-91
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• 1972

西部 北太平洋에 있어서의 本種에 대한 地理分布와 垂直分布 및 晝夜垂直移動에 관한 知見은 극히 限定된 海域과 深度에 있어서의 報告가 있을 뿐이다. 筆者는 北緯 20度에서 47度에 이르는 東經 50度 以西의 西部 北太平洋과 이의 附屬海에 걸친 광범위한 調査를 통하여 本種의 地理分布에 관한 새로운 知見을 얻었다. 그 結果로 東支那海의 表層을 제외한 68地點에서 本種이 出現함으로써 浮游性 端脚類中에서도 唯一하게 西部 北太平洋 全域에 걸쳐 一樣하게 分布하고 있으며 季節的인 消長이 없음이 究明되었다. 한편 垂直的으로는 0 $\\sim$ 1,500m 以上에 分布하고 있으며 最深採集記錄은 定點 229 $(34^\\circ 44.3'N, 140^\\circ 04.4'E)$에서의 1,650 $\\sim$ 2,220m層에서 얻어졌다. 晝夜垂直移動의 類型을 보면 本種은 晝間에는 深層部에 分布하며 夜間에 表層部로 현저한 晝夜移動을 하고 있음을 밝혔다. 이 移動의 範圍는 100 $\\sim$ 200m에 달한다. 또한 黑潮域에서는 新潮域에 비하여 垂直分布의 深度가 얕으며 서로 垂直分布의 深度와 移動의 範圍가 다르다. 즉 黑潮域에서는 晝間 0 $\\sim$ 200m層에 夜間 100 $\\sim$ 300m層에 個體群의 中心이 分布하며 100m의 範圍로 垂直移動을 하는데 反하여 新潮域에서는 晝間 400 $\\sim$ 700m, 夜間 100 $\\sim$ 500m로 200m의 範圍로 移動한다. 이는 兩海域에 있어서의 個體群의 組成이 서로 다른데 起因되는 결과로 사료된다.

• Journal of Astronomy and Space Sciences
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• 제34권4호
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• pp.257-270
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• 2017

Solar activity is known to be linked to changes in the Earth's weather and climate. Nonetheless, for other types of extreme weather, such as tropical cyclones (TCs), the available evidence is less conclusive. In this study the modulation of TC genesis over the western North Pacific by the solar activity is investigated, in comparison with a large-scale environmental parameter, i.e., El-$Ni{\tilde{n}}o$-Southern Oscillation (ENSO). For this purpose, we have obtained the best track data for TCs in the western North Pacific from 1977 to 2016, spanning from the solar cycle 21 to the solar cycle 24. We have confirmed that in the El-$Ni{\tilde{n}}o$ periods TCs tend to form in the southeast, reach its maximum strength in the southeast, and end its life as TSs in the northeast, compared with the La-$Ni{\tilde{n}}o$ periods. TCs occurring in the El-$Ni{\tilde{n}}o$ periods are found to last longer compared with the La-$Ni{\tilde{n}}o$ periods. Furthermore, TCs occurring in the El-$Ni{\tilde{n}}o$ periods have a lower central pressure at their maximum strength than those occurring in the La-$Ni{\tilde{n}}o$ periods. We have found that TCs occurring in the solar maximum periods resemble those in the El-$Ni{\tilde{n}}o$ periods in their properties. We have also found that TCs occurring in the solar descending periods somehow resemble those in the El-$Ni{\tilde{n}}o$ periods in their properties. To make sure that it is not due to the ENSO effect, we have excluded TCs both in the El-$Ni{\tilde{n}}o$ periods and in the La-$Ni{\tilde{n}}o$ periods from the data set and repeated the analysis. In addition to this test, we have also reiterated our analysis twice with TCs whose maximum sustained winds speed exceeds 17 m/s, instead of 33 m/s, as well as TCs designated as a typhoon, which ends up with the same conclusions.

• Journal of Astronomy and Space Sciences
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• 제35권3호
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• pp.151-161
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• 2018

Understanding solar influences on extreme weather is important. Insight into the causes of extreme weather events, including the solar-terrestrial connection, would allow better preparation for these events and help minimize the damage caused by disasters that threaten the human population. In this study, we examined category three, four, and five tropical cyclones that occurred in the western North Pacific Ocean from 1977 to 2016. We compared long-term trends in the positions of tropical cyclone occurrence and development with variations of the observed sunspot area, the solar North-South asymmetry, and the southern oscillation index (SOI). We found that tropical cyclones formed, had their maximum intensity, and terminated more northward in latitude and more westward in longitude over the period analyzed; they also became stronger during that period. It was found that tropical cyclones cannot be correlated or anti-correlated with the solar cycle. No evidence showing that properties (including positions of occurrence/development and other characteristics) of tropical cyclones are modulated by solar activity was found, at least not in terms of a spectral analysis using the wavelet transform method.

• Journal of the Korean Wood Science and Technology
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• 제37권5호
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• pp.451-458
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• 2009

Anatomical comparison of 8 North American species of Abies was executed to provide taxonomic information. The species of eastern (balsam and Fraser fir) and western (Pacific silver, white, grand, subalpine, California red, and noble fir) were found to be separated on the basis of crystals and color of contents in ray parenchyma cells and ray height. In eastern species, crystals in ray parenchyma cells were absent and ray parenchyma cell contents were colorless to very light. These two eastern species were further characterized by the absence of uniseriate rays exceeding 25 cells in height. In western species, only subalpine fir had colorless to very light contents but the remaining five species have dark contents in ray parenchyma cells. Crystals were absent to extremely sparse in Pacific silver fir, somewhat frequent in noble fir, frequent in grand and California red fir, and very frequent in white fir. Uniseriate rays exceeding 25 cells in height were regularly found in grand and California red fir but absent in white and noble fir.

• 대기
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• 제30권1호
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• pp.1-15
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• 2020

This study analyzed and compared development mechanisms leading to heat waves of 2016 and 2018 in Korea. The European Centre for Medium-Range Weather Forecasts Reanalysis Interim (ERA Interim) dataset and Automated Surface Observing System data are used for synoptic scale analysis. The synoptic conditions are investigated using geopotential height, temperature, equivalent potential temperature, thickness, potential vorticity, omega, outgoing longwave radiation, and blocking index, etc. Heat waves in South Korea occur in relation to Western North Pacific Subtropical High (WNPSH) pressure system which moves northwestward to East Asia during summer season. Especially in 2018, WNPSH intensified due to strong large-scale circulation associated with convective activities in the Philippine Sea, and moved farther north to Korea when compared to 2016. In addition, the Tibetan high near the tropopause settled over Northern China on top of WNPSH creating a very strong anticyclonic structure in the upper-level over the Korean Peninsula. Unlike 2018, WNPSH was weaker and centered over the East China Sea in 2016. Analysis of blocking indices show wide blocking phenomena over the North Pacific and the Eurasian continent during heat wave event in both years. The strong upper-level ridge which was positioned zonally near 60°N, made the WNPSH over the South Korea stagnant in both years. Analysis of heat wave intensity (HWI) and duration (HWD) show that HWI and HWD in 2018 was both strong leading to extreme high temperatures. In 2016 however, HWI was relatively weak compared to HWD. The longevity of HWD is attributed to atmosphere blocking in the surrounding Eurasian continent.