Surface heat balance of the Gangjeong-Goryung Reservoir is analyzed for 12-17 August 2013. Each flux elements at the water surface is derived from the special field observations with application of an aerodynamical bulk method for the turbulent heat fluxes and empirical formulae for the radiation heat fluxes. The rate of heat storage in the reservoir is estimated by using estimated by surface heating rate and the vertical water temperature data. The flux divergence of heat transport is estimated as a residual. The features of the surface heat balance are almost decided by the latent heat flux and the solar radiation flux. On average for 12-17 August 2014 in the Gangjeong- Goryung Reservoir, if one defines the insolation at the water surface as 100 %, 94 % is absorbed in the reservoir; thereafter the reservoir loses about 30~50% by sensible heat, latent heat and net long-wave radiation. The residue of 50~80 % raises the water temperature in the reservoir or transported away by the river flow during the daytime.

This study analyzed the change in tropical cyclone (TC) activity according to the fluctuation in July-to-September average North Pacific Oscillation index (NPOI) and its underlying large-scale environment during the last 37 years from 1977 to 2013. For this purpose, seven years with highest index NPOI value (positive NPOI phase) and another seven years with lowest NPOI index value (negative NPOI phase) among the 37 years were selected as sample after excluding the ENSO years. During the positive NPOI phase, TCs were created in the east of tropical and subtropical western North Pacific and moved to the west from the Philippines toward the southern region in China or toward far eastern sea of Japan. Meanwhile, during the negative NPOI phase, TCs tended to proceed to the north toward Korea or Japan passing East China Sea from the eastern sea of the Philippines. As a result, also in the TC recurvature, TCs in positive NPOI phase showed a tendency of recurving toward more eastern direction compared to TCs in negative NPOI phase. Hence, TC intensity was stronger in negative NPOI phase which allowed more time for obtaining energy from the ocean.

Effect of seedling type and early transplanting of summer grown seedling on the growth and yield of tomato was investigated to minimize problems caused by legginess of seedling in summer. Grafted seedling, 20 days seedling (young seedling), 40 days seedling, and rooted cutting were raised from July 20 to Sept. 7 and young seedling was transplanted 20 days earlier than other seedling types. Young seedling growth was weaker than other seedling types and fresh weight was only 1/10 of 40 days seedling. Growth of young seedling at 20 days after transplanting was better than other seedling types and fresh weight was 3 times higher than 40 days seedling. Creased stem did not appear and trusses developed faster in young seedling. Total yield and commercial yield were highest in young seedling as 8,535 kg/10a, and 7,575 kg/10a. There is no significant difference among seedling types in fruit quality. This result shows that early transplanting of summer grown seedling is more effective to attain stable growth and yield in tomato.

In this study, we analyzed the characteristics of summer rainfall over South Korea during recent five(2009-2013) years using observation data. There was a significant contrast in interannual variability between July and August rainfall since 1998. Large increase of rainfall in July (2009 and 2011) and August (2010 and 2012) were found to be consistent over all 60 stations in South Korea. Enhanced precipitation over western tropical Paciÿc and anticyclonic anomaly to the east of Korean peninsula were the common features when there was rainfall increase both in July and August. Intraseasonal summer rainfall over South Korea evolves in time lag with intraseasonal Indian and Western North Pacific monsoon indices. The meridional tripole structure of intraseasonal convection from the Western North Pacific to East Asia and the baroclinic structure of intraseasonal circulation anomalies centered over Korean peninsula provided a favorable condition for the extreme rainfall(90 percentile) events to occur.

We analyzed diurnal variations in the surface air temperature using the high density urban climate observation network in Daegu metropolitan city, the representative basin-type city in Korea, in summer, 2013. We used a total of 28 air temperature observation points data(16 thermometers and 12 AWSs). From the distribution of monthly average air temperature, air temperature at the center of Daegu was higher than the suburbs. Also, the days of daily minimum air temperature more than or equal to 25℃ and daily maximum air temperature more than or equal to 35℃ at the schools near the center of Daegu was more than those at other schools. This tendency appeared more clearly on the days of daily minimum air temperature more than or equal to 25℃. Also, the air temperature near the center of the city was higher than that of the suburbs in the early morning. Thus it was indicated that the air temperature was hard to decrease as the bottom of the basin. From these results, the influence of urbanization to the formation of the daily minimum temperature in Daegu was indicated.

본 연구에서는 강우의 변동특성 분석에 있어 기존의 접근법인 지속기간별 강우량의 변화 분석을 통하여 얻는 데 한계가 있는 강우의 구조적 변동특성을 분석하기 위하여 추계학적 강우모형을 이용하였다. Neyman-Scott 구형펄스 모형(Neyman-Scott Rectangular Pulse Model, NSRPM)은 점 과정을 이용한 추계학적 강우생성 모형으로 시간단위 강우를 생성함으로써 수문학 분야에서 널리 쓰이고 있으며 강우특성과 관련한 5개의 매개변수로 구성되어있다. 각 매개변수는 물리적인 의미를 가지고 있으므로 서울지점의 1973~2011년 여름철 시강우자료를 이용하여 NSRPM의 매개변수를 추정하고 추정된 매개변수의 변화를 분석하여 강우의 구조적인 변화를 분석하고 기존연구와 비교 분석하였다.

In this study, before and after sunset carbon dioxide concentration and air temperature were observed in two points of atmosphere (lower observation point of the GL + 0.1 m, the upper observation point of GL + 1.0 m) on the foreshore at located in Suncheon Bay and their variations were analyzed. Observation was performed on the foreshore on 2~4 August 2010. Instrument (VAISALA, GMP343) was set two hours before sunset and then observation was made continuously for six hours. In three days, observed carbon dioxide concentration was 375~419 ppm, and the air temperature was in the range of 28.7~32. 5℃. The average concentration of carbon dioxide was 388~399 ppm in the upper observation point and 386~396 ppm in the lower observation point. It was higher in the upper observation point and its fluctuations were similar in two observation points. Correlation coefficients between carbon dioxide concentration and air temperature in the upper observation point were in the range of –0.64~–0.88, and were calculated –0.65 to -0.90 in the lower observation point. For the carbon dioxide concentration, correlation coefficients between the upper part and the lower part were very high as 0.98 in three times. For the air temperature, correlation coefficients between the upper part and the lower part were very high as 0.97 and 0.99. In the same observation time, the slope of the linear regression function as carbon dioxide concentration in the lower observation point for the upper observation point was in the range of 0.97~1.01. Carbon dioxide concentration was slightly higher in the upper observation point. Because carbon dioxide in the lower observation point was closer on the surface of the foreshore and absorbed from atmosphere to the foreshore. In this study, it was showed that the vertical variation of carbon dioxide concentration was insignificant in the several meter scale of atmosphere on the surface of the foreshore.

본 연구는 저장 중 참외(Cucumis melo var. makuwa)의 품질 개선 효과를 보기 위하여 일반 골판지 박스로 포장한 무처리 대조구, 아이스 팩을 첨가하여 포장한 시험구, 및 아이스 팩과 알루미늄 코팅 보드로 처리된 박스로 포장한 시험구를 각각 사용하여 실험을 수행하였다. 참외의 품질 변화는 30oC의 저장 조건에서 21일 동안 저장 기간에 따른 참외의 호흡률, 중량감소율, 색도, 경도, 당도, 외관 품질 및 부패과 발생율로 관찰하였다. 저장 21일째 아이스 팩을 첨가한 포장 그리고 아이스 팩 및 알루미늄 코팅 보드를 적용한 포장으로 저장한 참외는 호흡률, 중량감소율, 및 색도, 및 경도 값의 지연으로 뛰어난 선도 유지 효과를 나타냈을 뿐만 아니라 특히 외관품질, 부패과 발생율을 감소시켜 상품성이 유지 효과를 보았다. 반면 참외의 가용성 고형분 함량 값은 각각 다른 형태로 적용한 포장에 의해 큰 영향을 받지 않았다. 아이스 팩과 알루미늄 코팅 보드를 적용한 박스로 포장한 참외는 아이스 팩으로 만 포장한 참외 보다 상대적으로 품질이 개선되는 것을 확인 할 수 있었다. 골판지 박스 내부에 아이스 팩의 적용은 참외 과실이 품고 있는 온도를 낮출 뿐만 아니라 알루미늄 코팅 보드는 외부 고온 환경으로 부터 온도 차단 효과로 포장 내부의 온도 상승에 따른 빠른 품질 변화를 막을 수 있는 역할을 한다고 판단된다.

본 연구에서는 전형적인 엘니뇨와 새로운 형태의 엘니뇨 Modoki에 따른 한강유역의 여름철(6～9월) 강우량의 특성 변화를 분석하였다. 전형적인 엘니뇨 시기에는 대체로 여름철 강우량이 감소하였으며, 강우의 변동성도 비교적 크게 나타났다(CV=0.40). 반면에 엘니뇨 Modoki 시기에는 한강 대부분 유역에서 평년보다 강우가 증가하는 경향을 보였으며, 여름철 강우의 변동성은 작은 것으로 분석되었다(CV=0.23). 엘니뇨 Modoki 시기에는 한강 남부의 11개 중권역에서 통계적으로 유의한 강우의 증가를 보였고, 30 mm/day와 50 mm/day를 초과하는 중호우의 강우발생일은 각각 9.9일과 5.4일로 나타났으며, 전형적인 엘니뇨 시기보다 백분위 편차가 각각 17.74%, 50.94% 큰 것으로 분석되었다. 본 연구에서는 새로운 형태의 엘니뇨 Modoki가 전형적인 패턴의 엘니뇨 보다 한강유역의 여름철 수자원 변동에 민감하게 영향을 주고 있음을 확인하였으며, 향후 수자원의 계절적 변동과 불확실성이 큰 지역에서 안정적인 수자원 확보를 위한 기초자료로 활용이 가능하리라 사료된다.

본 연구에서는 지상의 관측 자료와 광역의 정보를 제공하는 수치 예보 모형 자료 및 인공위성 자료를 이용하고 자료와 강수예측치의 물리적 상관 특성을 나타내기 위하여 자료 사이의 비선형 거동을 잘 나타내는 신경망 모형에 적용시켜 단시간 강수 예측을 수행하였다. 이를 위하여 서울지점에 대하여 현재로부터 3시간, 6시간, 9시간, 12시간의 선행시간을 가지는 인공위성 자료(MTSAT-1R) 및 수치 예보 모형 자료(RDAPS, Regional Data Assimilation and Prediction System)와 실시간 전송되는 자동 기상 관측 시스템(AWS, Automatic Weather System)의 관측치를 신경망 모형의 입력 자료로 하여 3시간, 6시간, 9시간, 12시간의 선행시간을 가지는 자료로 강수를 예측 할 수 있는 강수 예측 모형을 개발하였다. 장마와 태풍과 같이 전선형강수와 선풍형강수 등 강수 양상의 차이를 고려하기 위하여 6월, 7월과 8월, 9월 자료를 구분하여 신경망을 구축하였으며, 자료가용성에 기초하여 2006년에서 2008년 기간 동안에 대하여 모형을 학습하고 2009년에 대하여 모형의 적용성을 검증한 결과, 단시간 강수예측에 대한 모형의 적용 가능성을 보여주었으나 다양한 광역 자료와 인공신경망을 사용함에도 불구하고 단시간 강수예측의 정량적 정도향상을 위한 여지가 많음을 보여준다.

The purpose of this study was to identify the irrigation intervals and the amount of suitable growing substrate needed to achieve the desired shallow-extensive green roof system during a dry summer in Korea. In terms of treatment, three types (SL, P6P2L2, P4P4L2) with varying soil mixture ratios and two types (15 cm, 25 cm) with varying soil depths were created. The results have been analyzed after measuring growth and soil water contents. The difference of growth by treatment was significant in terms of green coverage, height, leaf width and photosynthesis. In measurement of chlorophyll content, no difference was detected when measured against soil depth. According to the growth measurement of Zoysia japonica with respect to differing soil mixture ratios in the 15 cm-deep treatment, a statistical difference was detected at the 0.05 significance level in photosynthesis. In case of green coverage, height, chlorophyll content and leaf width, no statistical significance was observed. In case of the 25 cm-deep treatment, a statistical significance was observed in height and photosynthesis. In terms of green coverage, chlorophyll content and leaf width, no statistical significance was detected. In comparisons of soil moisture tension and soil water contents, the irrigation interval and amount were 8 days and 14.9 L in the SL (15 cm) treatment, respectively. The irrigation interval showed for 10 days a 1.3-fold increase, and the irrigation amount was 27.4 L 1.8-fold more than SL (25 cm), respectively. For P6P2L2 (15 cm) treatment, the irrigation interval and amount were 12 days and 20.7 L, respectively. However, an irrigation interval under P6P2L2 (25 cm) was for 15 days 1.3 times longer than P6P2L2 (15 cm), and an irrigation amount of 40 L was 1.9 times more than that under P6P2L2 (15 cm). In P4P4L2 (15 cm) treatment, it was indicated that the irrigation interval was 15 days, and the irrigation amount was 19.2 L. It was not needed to irrigate for 16 days under P4P4L2 (25 cm) treatment during the dry summer and the longest no-rain periods. The irrigation interval and amount under P4P4L2 were 1.8-fold and 1.3-fold, respectively, more than SL treatment as affected by soil mixture ratio. Comparatively P4P4L2 had more 1.3-fold and 0.9-fold in irrigation interval and amount more than P6P2L2. Therefore, it can be noted that different soil depth and soil mixture ratios had a significant effect on the irrigation interval and amount.

The relative contributions of physical and chemical processes to the production of ozone (O3) were evaluated based on an integrated process rate (IPR) analysis using the MM5/CMAQ in a downtown (i.e., Yangsan_U) and suburban area (i.e., Ungsang) on high ozone days during spring and summer in 2006 (28 April and 8 August 2006). The IPR includes a horizontal advection (HADV) and diffusion (HDIF), a vertical advection (ZADV) and diffusion (VDIF), a dry deposition (DDEP), and a chemistry (CHEM). The VDIF in Yangsan_U was found to be the most dominant contributor (29.5% in spring and 32.1% in summer) to high O3 concentrations, followed by the HADV and ZADV. In contrast, the contributions of the HADV (40.3% in spring and 32.3% in summer) in Ungsang were significantly higher than those of VDIF and ZADV. Moreover, O3 production due to the chemical effect in the two areas (especially in Ungsang) during summer was found to be moderately higher than that during spring.

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 oN 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.

본 연구에서는 슈퍼요트의 쾌적한 실내환경조성을 목적으로 기초자료를 수집하였으며, 요트가 주로 운항되는 여름철 실내공간에 형성되는 실내환경성능에 대해 실측을 통해 분석함으로써 다음과 같은 결과를 얻었다. 1) 외부와 연결된 살롱의 문을 닫을 경우 선박배기가스의 실내유입은 거의 없으나 문을 여는 경우에는 급속히 실내공기가 오염되므로 쾌적한 실내공기환경을 유지하기 위해 실내환기방법 및 환기량에 대한 대책이 필요하다. 2) 운항 시에는 모든 실이 선원보호 소음규제치인 60dB을 넘고 있어 실내의 소음대책이 시급하다. 3) State cabin과 Guest cabin은 에어컨가동에 의해 과냉됨으로써 실내 환경이 쾌적범위를 벗어나고 있어 이에 대한 대책이 필요하다.

The observed relationships between the Asian summer monsoon and the sea surface temperature (SST) anomalies in the northwestern Pacific (NW Pacific) are verified using the intermediate complexity global climate model (GCM) (Planet Simulator: PLASIM). The climate responses over Asia for the monsoon season to forcing from NW Pacific SST anomalies are simulated in the GCM with the enhanced SST anomalies in the NW Pacific for the pre-monsoon season compared to climatological SST. During the pre-monsoon season, the enhanced SST anomalies result in an increase in lower-level convection and precipitation in the NW Pacific. A significantly weakened Indian summer monsoon is simulated for the enhanced SST experiment in the NW Pacific for the pre-monsoon season (p-value＜0.05). PLASIM dose a good job at representing the observed patterns of zonally averaged surface temperature, precipitation, and 850 hPa u-wind, although with some regional differences from observations (p-values of zonal correlation coefficients＜0.01).

최근 대중매체를 통해 합천의 여름철 고온화에 대한 보도가 잇따르고 있다. 합천의 여름철 기온 특성을 파악하기 위해 1973~2007년 여름철(6~8월)의 기온자료를 사용하였고, 합천과 인접한 우리나라 대표적 혹서지 중 하나인 대구를 비교대상으로 선정하였다. 두 지점의 일최고기온 일최저기온, 일최고기온 극값, 열대일, 열대야를 비교하였다. 상대적으로 합천은 일최고기온, 대구는 일최저기온이 높게 나타났다. 열대일 시작일, 열대일 일최고기온, 열대일 수는 2002년을 기점으로 다른 양상이 나타났다. 일최고기온의 순별 분포에서 합천의 최고값은 8월로 7월인 대구보다 늦게 나타났고, 열대일 수는 비슷한 경향이었다. 열대야는 열대일과 다른 경향이 나타나서 열대야 수와 순별 열대야 분포 모두 합천이 상대적으로 적게 나타났다. 하지만 지난 2년간 합천의 열대야가 상당히 증가하는 것은 특징적이다. 최근 5년간 합천의 최고기온이 대구에 비해 상대적으로 크게 증가하는 것으로 나타났다.

본 연구에서는 여름철 고온현상의 지속기간이 길고 극심했던 1994년과 고온현상 발생일수가 가장 작았던 1993년을 비교하여 서울시의 여름철 고온현상이 사망자 증가에 미치는 영향을 파악하고자 하였다. 여름철 고온현상이 극심했던 1994년 7월의 경우 일별 최고기온과 일별 사망자수 간의 변화 경향이 유사하게 나타났다. 최고기온의 최대값이 나타난 다음날 사망자수의 최대값이 나타났다. 여름철 고온현상이 극심했던 1994년의 경우 일 최고기온과 일별 사망자수 간에 r=0.548의 유의한 상관관계를 나타내었으나 고온현상 발생일수가 작았던 1993년의 경우 유의한 상관관계를 보이지 않았다. 고온현상이 지속되는 동안 사망자의 사망원인을 분석한 결과 내분비ㆍ영양 및 대사 질환으로 인한 사망자수가 43.0%, 순환기계통의 질환으로 인한 사망자수가 30.5%, 호흡기계통 질환으로 인한 사망자수가 43.8% 증가하였다. 여름철 고온현상이 극심했던 1994년은 그 전해에 비하여 65세 이상의 노년층이 다른 연령층에 비하여, 또한 여성이 남성에 비하여 고온에 취약한 것으로 나타났다.

본 실험은 강원도 영서지역에서 맥류 수확 후 가을채소 파종까지 휴경을 하게 될 경우의 여름 휴경지 관리방안으로 가을채소용 두과녹비작물의 도입에 필요한 기초 자료를 얻기 위하여 수행되었으며, 그 결과는 다음과 같았다. 1. 여름철 휴경을 할 경우 주요 잡초는 바랭이, 방동사니, 쇠비름 그리고 털비름 등 비두과 식물로, 자연적인 두과식물의 출현은 없었다. 2. 두과식물을 6월 중순 로타리 경운 후 파종할 경우 동부와 예팥은 출현율이 높았으나, 돌콩과 헤어리벳치는 출현율이 낮았으며, 동계일년생 두과녹비작물인 헤어리벳치는 하계잡초와의 경합에서 도태되는 경향이었다. 3. 만성형식물인 동부는 잡초의 생육을 가장 크게 억제하였으며, 만성 예팥이나 돌콩, 그리고 헤어리벳치보다 생육량이 많았다. 따라서 우리나라 기상조건에서 여름철 휴경을 할 경우 두과식물의 인위적인 파종이 필요하며, 동부는 여름철 휴경지의 녹비작물로서의 이용 가치가 높은 것으로 판단되었다.