• 한국환경과학회지
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• 제18권10호
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• pp.1089-1101
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• 2009

In this paper, changes in the intensity (e.g., central pressure and maximum sustained wind speed) of Tropical Cyclone (TC) in summer in the regions located at $30^{\circ}N$ in East Asia from 1988 to 1991 were found. The intensity of TC from 1991 to 2007 was much higher than that of TC from 1965 to 1988. The reason for this was that the frequency of TCs passing China from 1991 to 2007 was much lower than that of TCs from 1965-1988 because a northeasterly wind caused by high-pressure circulation in East Asia got severer along the East Asian coast. Instead, TCs moved from the eastern region of the Tropical West Pacific to Korea and Japan mainly after passing the East China Sea due to the low-pressure circulation strengthened in the subtropical waters of East Asia. In addition, low Vertical Wind Shear (VWS) was created along the mid-latitude regions of East Asia and the main path of TCs from 1991 to 2007. Most of the regions in the Northwestern Pacific showed higher Sea Surface Temperature (SST) from 1991 to 2007, and had a good environment where TCs were able to maintain a higher intensity on the mid-latitude. In particular, a low sensible heat flux occurred due to high snow depth in East Asia in the spring of 1991 to 2007. Accordingly, the lower layer of East Asia showed high-pressure circulation, and the sea surrounding East Asia showed low-pressure circulation. Thus, the typical west-high, east-low pattern of winter atmospheric pressure was shown. The possibility of snowfall in East Asia in spring to be used as a factor for predicting the summer intensity of TC in the mid-latitude regions of East Asia was insinuated. The characteristics of TC in a low-latitude region were the same in Korea. The latest intensity of TCs got higher, and the landing location of TCs gradually changed from the west coast to the south coast.

• 천문학논총
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• 제32권1호
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• pp.157-161
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• 2017

The dusty torus of Active Galactic Nuclei (AGNs) is one of the important components for the unification theory of AGNs. The geometry and properties of the dusty torus are key factors in understanding the nature of AGNs as well as the formation and evolution of AGNs. However, they are still under discussion. Infrared observation is useful for understanding the dusty torus as thermal emission from hot dust with the dust sublimation temperature (~ 1500 K) has been observed in the infrared. We have analyzed infrared spectroscopic data of low-redshift and high-redshift quasars, which are luminous AGNs. For the low-redshift quasars, we constructed the spectral energy distributions (SEDs) with AKARI near-infrared and Spitzer mid-infrared spectra and decomposed the SEDs into a power-law component from the nuclei, silicate features, and blackbody components with different temperatures from the dusty torus. From the decomposition, the temperature of the innermost dusty torus shows the range between 900-2000 K. For the high-redshift quasars, AKARI traced rest-frame optical and near-infrared spectra of AGNs. Combining with WISE data, we have found that the temperature of the innermost dusty torus in high redshift quasars is lower than that in typical quasars. The hydrogen $H{\alpha}$ emission line from the braod emission line region in the quasars also shows narrow full width at half maximum of $3000-4000km\;s^{-1}$. These results indicate that the dusty torus and the broad emission line region are more extended than those of typical quasars.

• Structural Engineering and Mechanics
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• 제52권3호
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• pp.603-612
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• 2014

A series of experimental work is carried out with the aim to understand the flexural performance of laminated glass (LG) beams using polyvinyl butyral (PVB) and Ionoplast interlayers subjected to short term duration loads in the circumstance of elevated temperature. The study is based on a total of 42 laboratory tests conducted in ambient temperature ranging from $25^{\circ}C$ to $80^{\circ}C$. The load duration is kept within 20 seconds. Through the tests, load-stress and load-deflection curves of the LG are established; appropriate analytical models for the LG are indentified; the effective thicknesses as well as the shear transfer coefficients of the LG are semi-empirically determined. The test results show that within the studied temperature range the bending stresses and deflections at mid-span of the LG develop linearly with respect to the applied loads. From $25^{\circ}C$ to $80^{\circ}C$ the flexural behavior of the PVB LG is found constantly between that of monolithic glass and layered glass having the same nominal thickness; the flexural behavior of the Ionoplast LG is equivalent to monolithic glass of the same nominal thickness until the temperature elevates up to $50^{\circ}C$. The test results reveal that in calculating the effective thicknesses of the PVB and Ionoplast LG, neglecting the shear capacities of the interlayers is uneconomic even when the ambient temperature is as high as $80^{\circ}C$. In the particular case of this study, the shear transfer coefficient of the PVB interlayer is found in a range from 0.62 to 0.14 while that of the Ionoplast interlayer is found in a range from 1.00 to 0.56 when the ambient temperature varies from $25^{\circ}C$ to $80^{\circ}C$.

• 한국수산과학회지
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• 제40권6호
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• pp.394-410
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• 2007

Anchovy spawn from the end of May to mid-October, when the water temperature is $14.8-27.2\;^{\circ}C$ and the salinity is 26.0-33.6 psu. The main spawning season is between July to August, when the water temperature is $21.7-27.2\;^{\circ}C$ and the salinity is between 26.0-32.2 psu. The main spawning grounds of anchovy are coastal areas shallower than 50 m around the islands located in the Jeju Strait. Anchovy larvae are distributed near the fronts between Chuja-do, Jangsu-do, Yeoseo-do, and the open sea rather than in the spawning grounds. Anchovy eggs and larvae density increased in accordance with the high level of $Chlorophyll-{\alpha}$ during the summer season (July-August). In terms of the suspended sediment (SS) levels along the northern coast of the Jeju Strait, high densities of anchovy eggs (12.0-18.0 mg/L) were observed, mainly in the area affected by the coastal waters of the southern sea with high SS levels, while larvae (10.0-19.0 mg/L) tended to be distributed over a wide area with high SS levels, including the open sea. In terms of the dissolved oxygen (DO) content, eggs (5.4-6.8 mg/L) were observed in coastal areas with a high DO content, while larvae (4.2-6.4 mg/L) were distributed widely in areas with a relatively low DO content, from the southern coast to the open sea.

• 한국지구과학회지
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• 제24권4호
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• pp.303-314
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• 2003

2002년 7월 8일에서 10일까지 AWS와 CTD를 이용하여 서해 중부 연안역에서 해양기상관측을 실시하였다. 수심이 낮은 태안반도 연안역에서 17$^{\circ}C$ 이하의 냉수가 출현하였고, 36$^{\circ}$20'N와 36$^{\circ}$30'N 사이에 정선을 따라 조석전선이 형성되었다. 기온의 분포는 수온의 분포양상과 유사하게 나타났다. 덕적도 주변(Al)에서 24시간 연속관측결과, 조류와 같은 주기로 북동부로부터 고온저염수와 남서부로부터 저온고염수의 이동이 관측되었다. 관측기간 중에 7월 8일 23시에서 9일 1시 30분까지, 9일 3시에서 5시까지 해무가 발생하였다. 해무발생 시 북태평양 고기압이 약해지면서 기온은 18$^{\circ}C$까지 하강하였고, 바람은 2-4m/s의 북동풍이 불었다. 위성사진을 분석하였을 때, 이 안개는 표층수온이 높은 황해서부를 중심으로 발생하여 시간이 지나면서 관측해역으로 확장된 증기안개이다. 이 해무는 기온과 풍속이 상승하면서 소멸되었다.

• 한국버섯학회지
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• 제13권3호
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• pp.228-232
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• 2015

모본 ASI 3305mut와 L5(3265-238701-2)-16을 2011년에 교잡하여, 2012년부터 2013년까지 생산력 검정시험을 통해 PM-L5(농진고)를 출원하였다. 농진고의 균사배양 최적온도는 $30^{\circ}C$이며, 버섯 발생온도는 $15{\sim}23^{\circ}C$로 중고온성이다. 자실체의 갓은 평반구형이며 색깔은 황갈색이고, 인피는 갓의 둘레에 생긴다. 버섯의 배양은 1.5kg 배지에서 최소 90~100일이 소요되며, 갈변이 다소 늦은 편이다. 버섯 발생형은 집중형이나 산조701에 비하여 초기 발생이 다소 늦으면서 개체수가 10개 내외이고, 주기별 발생이 고른 편이다. 톱밥 봉지재배 품종으로 지면 재배, 균상재배에서 모두 적합하다.

• 한국초지조사료학회지
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• 제5권1호
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• pp.22-32
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• 1985

본(本) 연구(硏究)는 고온기(高溫期) 초지(草地)의 예취관리(刈取管理)에 관(關)한 연구(硏究)로서 여름철 고온기간중(高溫期間中) 예취시기(刈取時期)와 예취(刈取)높이가 tall fescu 우점초지(優占草地)의 목초고사(牧草枯死), 잡초발생(雜草發生), 재생(再生)과 저장탄수화물함량(貯藏炭水化物含量) 및 수량(收量)에 미치는 영향을 구명(究明)하여 고온기(高溫期)의 적절한 예취방법(刈取方法) 모색하기 위해 실시(實施)되었다. 본(本) 시험(試驗)은 3차(次) 예취시기(刈取時期)(7월(月) 12일(日), 8월(月) 4일(日))를 주구(主區)로 하고 3차(次) 예취시(刈取時) 예취(刈取)높이(3, 6, 9cm)를 세구(細區)로 하여 4 반복 분할구 배치법으로 설계(設計)하였으며, 1984년도(年度) 수원(水原) 축산시험장(畜産試驗場) 초지시험포(草地試驗圃)에서 수행(遂行)된 결과(結果)의 요약(要約)은 다음과 같다. 1. 시험기간중(試驗期間中) 기상(氣象)을 요약(要約)하면 기온(氣溫)은 평년(平年)에 비해 $1{\sim}2^{\circ}C$높았으며 특(特)히 8월(月) 상(上) 중순(中旬)의 기온(氣溫)이 높았다. 강수량(降水量)은 7월(月) 상순(上旬), 8월(月) 하순(下旬) 및 9월(月) 상순(上旬)을 제외하고는 평년(平年)에 비해 적었다. 2. 고온기시(高溫期時) 지표(地表) 및 지중(地中)(10cm)온도(溫度)는 3차(次) 예취시(刈取時) 예취(刈取)높이가 낮을수록 높아지는 경향이었다(지표온도(地表溫度) : $2{\sim}4^{\circ}C$, 지중온도(地中溫度) : $1{\sim}2^{\circ}C$) 3. 3차(次) 예취후(刈取后) 예취(刈取)높이별(別) 재생초장(再生草長)과 재생엽면적(再生葉面積)은 예취(刈取)높이가 높을수록 빠른 생장(生長)을 보였다. 4. 3차(次) 예취후(刈取后) 그루터기내(內) 저장탄수화물(貯藏炭水化物)(TNC) 함량(含量)은 7월(月) 12일구(日區)가 8월(月) 4일구(日區)에 비해 회복이 빨랐으며 그 중 9cm 예취(刈取)높이구(區)에서 가장 빠른 회복을 보였고, 3cm구(區)가 가장 늦었다. 8월(月) 4일구(日區)에서는 고온(高溫)과 강우(降雨)로 인해 TNC의 회복이 더딘 것으로 생각되며 3cm높이구(區)에서 회복이 가장 늦은 경향을 보였다. 5. 고온기간(高溫期間)인 3차(次) 예취후(刈取后) 목초고사율(牧草枯死率)은 예취(刈取)높이가 낮아질수록 증가하였다(P<0.05). 6. 3차(次) 예취시(刈取時)에는 전체 시험포장에서 잡초발생(雜草發生)이 거의 없었으나 4차(次) 예취(刈取) 시(時)에는(7월(月) 12일구(日區)) 3cm구(區)에서는 60%의 잡초율(雜草率)을 보여 주었으며 6, 9cm로 예취(刈取)높이가 높아짐에 따라 잡초율(雜草率)은 21, 7%로 각각 감소하였다(P<0.05). 이는 5차(次) 예취시(刈取時)에도 비슷한 경향을 보였으며 주요발생잡초(主要發生雜草)로는 피>바램이>소리쟁이, 방동산이 등의 순으로 나타났다. 그러나 8월(月) 4일구(日區)에서는 예취(刈取)높이별(別) 잡초발생차이(雜草發生差異)는 크지 않았다. 7. 고온기시(高溫期時) 건물수량(乾物收量)(3차(次))은 8월(月) 4일구(日區)가 7월(月)12일구(日區)에 비해 많았으며, 예취(刈取)높이가 낮을수록 증가하였다(P<0.05). 그러나 4차(次)와 5차(次) 예취시(刈取時) 수량(收量)은 刈예취시기별(刈取時期別) 차이(差異)는 없었으나, 3차(次) 예취시(刈取時) 예취(刈取)높이가 높을수록 증가하였다(P<0.05). 8. 재생수량(再生收量)(4 + 5차(次))은 예취시기(刈取時期)에 관계없이 3차(次) 예취시(刈取時) 예취(刈取)높이가 높을수록 증가하였으며(P<0.05). 3, 4, 5차(次) 총건물수량(總乾物收量)을 볼 때 7월(月) 12일구(日區)에서는 예취(刈取)높이별(別) 차이(差異)가 인정되었으나(P<0.05), 8월(月) 4일구(日區)에서는 차이가 없었다. 9. 본(本) 시험(試驗)의 결과(結果)를 종합(綜合)하여 볼 때 여름철 고온기시(高溫期時) 목초(牧草)의 양호(良好)한 재생(再生)과 잡초발생억제(雜草發生抑制)를 위해서는 예취시기(刈取時期)에 관계없이 9cm의 높은 예취(刈取)높이가 바람직한 것으로 생각된다.

• 한국농림기상학회지
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• 제3권4호
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• pp.220-237
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• 2001

Over the 20th century global temperature increase has been 0.6$^{\circ}C$. The globally averaged surface temperature is projected to increase by 1.4 to 5.8$^{\circ}C$ over the period 1990 to 2100. Nearly all land areas will have higher maximum temperature and minimum temperature, and fewer cold days and frost days. More intense precipitation events will take plate over many areas. Over most mid-latitude continental interiors will have increased summer continental drying and associated risk of drought. By 2100, if the annual surface temperature increase is 3.5$^{\circ}C$, we will have 15.9$^{\circ}C$ from 12.4$^{\circ}C$ at present. Also the annual precipitation will range 1,118-2,447 mm from 972-1,841 mm at present in Korea. Consequently the average crop periods for summer crops will be 250 days that prolonged 32 days than at present. In the case of gradual increase of global warming, an annual crop can be adapted to the changing climate through the selection of filial generations in breeding process. The perennial crops such as an apple should be shifted the chief producing place to northern or high latitude areas where below 13.5$^{\circ}C$ of the annual surface temperature. If global warming happens suddenly over the threshold atmospheric greenhouse gases, then all ecosystems will have tremendous disturbance. Agricultural land-use plan, which state that farmers decide what to plant, based on their climate-based advantages. Therefore, farmers will mitigate possible negative imparts associated with the climate change. The farmers will have application to use agricultural meteorological information system, and agricultural long-range weather forecast system for their agroecosystems management. The ideal types of crops under $CO_2$ increase and climate change conditions are considered that ecological characteristics need indispensable to accomplish the sustainable agriculture as the diversification of genetic resources from yield-oriented to biomass-oriented characteristics with higher potential of $CO_2$ absorption and primary production. In addition, a heat-and-cold tolerance, a pest resistance, an environmental adaptability, and production stability should be also incorporated collectively into integrated agroecosystem.

• 한국양봉학회지
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• 제33권4호
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• pp.239-250
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• 2018

We investigated the pollination activity of honeybees (Apis mellifera L.) in terms of different climatic conditions in the greenhouse cultivation of watermelons (Citrullus lanatus L.) during winter. The aim of the study was to search a climatic condition which effectively can be use honeybees as pollinators during the flowering season of watermelons in winter or early spring. The average climatic conditions inside the greenhouse during the bee activity time (BAT)-between 10:00 and 16:00 in mid-Februarywere a temperature of $30.4^{\circ}C$, relative humidity of 53.7%, illuminance level of 22,728.4lx, and UV level of $0.233mW/cm^2$. Bee traffic and foraging activity were at their greatest at 10:00 and tended to decrease with time. Male watermelon flowers typically dehisced between 10:00 and 12:00. Climatic conditions were significantly correlated with bee activities, including bee traffic and foraging activity. Bee activities were positively correlated with temperature, illuminance level, and UV level but negatively correlated with relative humidity. Temperature had the greatest effect on honeybee behavior. Among the foraging honeybees, the number of high-flying bees that did not pollinate flowers showed a strong positive correlation with temperature, and the number of bees landing on the flowers showed a positive correlation with the UV level. The temperature range inside greenhouses at which the pollination activities of honeybees can be maintained efficiently during winter watermelon pollination was found to be $21{\sim}25^{\circ}C$.

• 한국작물학회지
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• 제42권4호
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• pp.473-482
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• 1997

Temperature, humidity and wetness duration were monitored for fully developed paddy rice canopies with 3 different structures induced by the seeding method(puddled-soil drill seeding, DS ; hand broadcasting, HB ; machine broadcasting, MB). Within-canopy air temperature averaged over "clear sky" hours during the study period(maximum tillering through heading) was lower than the screen temperature at a nearby standard weather station, especially in the night. The same trend was true for "overcast sky" hours except the diurnal distinction. Vapor pressure within the canopy was high during the daytime and low in the night, making the daytime deviation from outside the canopy more significant on clear days. Under the overcast sky, the canopy maintained a steady 5 to 10％ higher vapor pressure than the outside regardless of day or night. Daily maximum temperature was observed to be higher within the canopies with more leaf mass, making MB the highest, HB the lowest, and DS in between. Relative humidity was over 90％ in the night and dropped to 70％ in the mid-afternoon, but vapor pressure within the canopy was highest at around 13:00 LST. Dew point depression was lowest and, combined with the temperature, the relative humidity was highest in HB. Mean period of wetting duration was in the order of DS＞HB＞MB, while the dew point depression was greatest in DS.