• 제목/요약/키워드: extreme temperature days

검색결과 69건 처리시간 0.042초

Yield Response of Soybean [Glycine max (L.) Merrill] to High Temperature Condition in a Temperature Gradient Chamber

  • Baek, Jae-Kyeong;Sang, Wan-Gyu;Kim, Jun-Hwan;Shin, Pyong;Cho, Jung-Il;Seo, Myung-Chul
    • 한국작물학회지
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    • 제65권4호
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    • pp.339-345
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    • 2020
  • Recently, abnormal weather conditions, such as extreme high temperatures and droughts, have increased in frequency due to climate change, there has accordingly been growing concern regarding the detrimental effects on field crop, including soybean. Therefore, this study was conducted to examine the effects of increased temperatures on soybean growth and yield using a temperature gradient chamber (TGC). Two major types of soybean cultivar, a medium- seed cultivar such as Daepung-2 and a large-seed cultivar such as Daechan, were used and four temperature treatments, aT+1℃ (ambient temperature+1℃), aT+2℃ (ambient temperature+2℃), aT+3℃ (ambient temperature+3℃) and aT+4℃ (ambient temperature+4℃) were established to examine the growth response and seed yield of each cultivar. Seed yield showed a higher correlation with seed weight (r=0.713***) and an increase in temperature affected seed yield by reducing the single seed weight. In particular, the seed growth rate of the large-seed cultivar (Daechan) increased at high temperature, resulting in a reduction in the number of days for full maturity. Our results accordingly indicate that large-seed cultivar, such as Daechan, is potentially vulnerable to high temperature stress. The results of this study can be used as basic data in the development of cultivation technology to reduce the damage caused by elevated temperatures. Also, further research is required to evaluate the response of each process contributing to seed yield production under high temperatures.

Past and Future Regional Climate Change in Korea

  • Kwon, Won-Tae;Park, Youngeun;Min, Seung-Ki;Oh, Jai-Ho
    • 한국제4기학회지
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    • 제17권2호
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    • pp.161-161
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    • 2003
  • During the last century, most scientific questions related to climate change were focused on the evidence of anthropogenic global warming (IPCC, 2001). There are robust evidences of warming and also human-induced climate change. We now understand the global, mean change a little bit better; however, the uncertainties for regional climate change still remains large. The purpose of this study is to understand the past climate change over Korea based on the observational data and to project future regional climate change over East Asia using ECHAM4/HOPE model and MM5 for downscaling. There are significant evidences on regional climate change in Korea, from several variables. The mean annual temperature over Korea has increased about 1.5∼$1.7^{\circ}C$ during the 20th century, including urbanization effect in large cities which can account for 20-30% of warming in the second half of the 20th century. Cold extreme temperature events occurred less frequently especially in the late 20th century, while hot extreme temperature events were more common than earlier in the century. The seasonal and annual precipitation was analyzed to examine long-term trend on precipitation intensity and extreme events. The number of rainy days shows a significant negative trend, which is more evident in summer and fall. Annual precipitation amount tends to increase slightly during the same period. This suggests an increase of precipitation intensity in this area. These changes may influence on growing seasons, floods and droughts, diseases and insects, marketing of seasonal products, energy consumption, and socio-economic sectors. The Korean Peninsular is located at the eastern coast of the largest continent on the earth withmeso-scale mountainous complex topography and itspopulation density is very high. And most people want to hear what will happen in their back yards. It is necessary to produce climate change scenario to fit forhigh-resolution (in meteorological sense, but low-resolution in socio-economic sense) impact assessment. We produced one hundred-year, high-resolution (∼27 km), regional climate change scenario with MM5 and recognized some obstacles to be used in application. The boundary conditions were provided from the 240-year simulation using the ECHAM4/HOPE-G model with SRES A2 scenario. Both observation and simulation data will compose past and future regional climate change scenario over Korea.

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2018년 전라남도 고흥 유자나무 동해 발생에 대한 기상학적 구명 (Agrometeorological Analysis on the Freeze Damage Occurrence of Yuzu Trees in Goheung, Jeonnam Province in 2018)

  • 김경희;고영진;김광형
    • 식물병연구
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    • 제25권2호
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    • pp.71-78
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    • 2019
  • 2018년 전남 고흥군에서 발생한 유자나무의 집단 고사가 발생했다. 이에 대한 원인 조사를 위해 고흥군 풍양면에 있는 18개 유자 과수원을 무작위로 선정하여 조사를 수행한 결과 과수원별 고사증상을 보인 나무의 비율은 평균 43.6%(7.5%~100% 피해율), 증상을 보인 나무 중 56.5%는 나무 전체가 완전 고사되는 피해를 입은 것으로 나타났다. 고사 증상을 보인 대부분의 유자나무에서는 동해의 전형적인 증상인 표피 안 형성층과 목부의 갈변, 잎눈과 꽃눈의 무 발아, 가지나 줄기에 쪼개짐 증상 등이 관찰되었다. 따라서 기상 조건과 유자나무의 고사 증상이 연관 되어있을 것이라는 가설을 바탕으로 고흥지역의 과거 기상 자료를 분석하였다. 2017년 1월과 2월 고흥지역의 일평균 기온은 $-10^{\circ}C$ 이상이었으나, 2018년의 동 기간에는 $-10^{\circ}C$ 아래로 떨어진 날이 7일이나 되었다. 특히 2018년에는 1월과 2월에 유자의 내한성을 훨씬 넘어선 극최저기온(각각 $-12.6^{\circ}C$$-11.5^{\circ}C$)이 관측되었다. 또한 그해 3월 중순과 4월 초에 일 최저기온이 $13^{\circ}C$로 상승한 이상고온 직후 급격히 기온이 $0^{\circ}C$로 떨어지는 현상이 발생하였다. 결론적으로, 2018년 겨울철에 기록적인 극최저기온과 이상고온에 이은 급격한 기온의 저하로 인한 동해가 고흥지역에 대발생한 고사증상의 주요 원인이 되었을 것으로 추정하였다.

GK2A AMI를 이용한 한반도 식생건강지수 산출 (Retrieval of Vegetation Health Index for the Korean Peninsula Using GK2A AMI)

  • 이수진;조재일;류재현;김나리;김광진;손은하;박기홍;장재철;이양원
    • 대한원격탐사학회지
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    • 제38권2호
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    • pp.179-188
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    • 2022
  • 지구온난화는 기후변화를 야기하며 전지구적으로 이상기상 현상을 유발하고 있다. 우리나라에서도 폭염, 가뭄과 같은 이상기상 현상이 증가하고 있는 상황이다. 이상기상 감시를 위하여 지표면온도(Land Surface Temperature, LST), 온도상태지수(Temperature Condition Index, TCI), 식생활력지수(Normalized Difference Vegetation Index, NDVI), 식생상태지수(Vegetation Condition Index, VCI), 식생건강지수(Vegetation Health Index, VHI) 등의 위성자료가 활용되고 있다. TCI와 VCI를 이용하여 계산되는 VHI는 온도, 강수와 같은 기상 요인에 의한 식생 스트레스를 나타내며, 기후변화 상황에서 가뭄 평가에 주로 활용되고 있다. TCI, VCI는 날짜 및 장소에 따른 LST, NDVI의 과거 평년치를 참조해서 산출되기 때문에, 아직 2년여의 자료밖에 없는 천리안위성 2A호(GK2A) AMI (Advanced Meteorological Imager) 자료로부터 TCI, VCI, VHI를 산출하는 것은 현재로서는 쉽지 않은 일이다. 본 연구에서는 대안적인 방법으로 VIIRS (Visible Infrared Imaging Radiometer Suite) 센서의 LST, NDVI를 이용하여 GK2A의 VHI 산출 가능성을 모색하였다. GK2A와 VIIRS의 LST, NDVI는 상당히 높은 상관성을 보이기 때문에, GK2A에 존재하지 않는 과거 평년치를 VIIRS 자료로 대체하는 방식을 택하였다. 8일 간격으로 GK2A 격자에 해당하는 LST, NDVI의 최소·최대값 조견표를 구축하여 TCI, VCI, VHI를 산출하였고, 최근 우리나라 이상기상 현상에 대한 해석을 수행하였다. GK2A VHI는 2020년 3월과 6월의 폭염, 4월과 7월의 저온, 8월의 폭우 등으로 인한 식생 스트레스의 변화를 잘 표현하는 것으로 나타났지만, 미국 해양대기청(National Oceanic and Atmospheric Administration, NOAA)의 VHI 산출물은 그렇지 않았다. 본 연구에서 제시한 GK2A VHI는 향후 LST, NDVI의 과거 평년치에 대한 통계적으로 엄밀한 보완을 거친다면 폭염, 가뭄으로 인한 식생 스트레스 감시에 활용될 수 있을 것으로 사료된다.

Long-term pattern changes of sea surface temperature during summer and winter due to climate change in the Korea Waters

  • In-Seong Han;Joon-Soo Lee;Hae-Kun Jung
    • Fisheries and Aquatic Sciences
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    • 제26권11호
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    • pp.639-648
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    • 2023
  • The sea surface temperature (SST) and ocean heat content in the Korea Waters are gradually increased. Especially the increasing trend of annual mean SST in the Korea Water is higher about 2.6 times than the global mean during past 55 years (1968-2022). Before 2010s, the increasing trend of SST was led by winter season in the Korea Waters. However, this pattern was clearly changed after 2010s. The increasing trend of SST during summer is higher about 3.9 times than during winter after 2010s. We examine the long-term variations of several ocean and climate factors to understand the reasons for the long-term pattern changes of SST between summer and winter in recent. Tsushima warm current was significantly strengthened in summer compare to winter during past 33 years (1986-2018). The long-term patterns of Siberian High and East Asian Winter Monsoon were definitely changed before and after early- or mid-2000s. The intensities of those two climate factors was changed to the increasing trend or weakened decreasing trend from the distinctive decreasing trend. In addition, the extreme weather condition like the heatwave days and cold spell days in the Korea significantly increased since mid- or late-2000s. From these results, we can consider that the occurrences of frequent and intensified marine heatwaves during summer and marine cold spells during winter in the Korea Waters might be related with the long-term pattern change of SST, which should be caused by the long-term change of climate factors and advection heat, in a few decade.

Influence of water saturation on fracture toughness in woven natural fiber reinforced composites

  • Kim, Hyo-Jin;Seo, Do-Won
    • Advanced Composite Materials
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    • 제16권2호
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    • pp.83-94
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    • 2007
  • Woven sisal textile fiber reinforced composites were used to evaluate fracture toughness, tensile and three-point bending. The water absorption testing of all specimens was repeated five times in this study. All specimens were immersed in pure water during 9 days at room temperature, and dried in 1 day at $50^{\circ}C$. Two kinds of polymer matrices such as epoxy and vinyl-ester were used. Fractured surfaces were taken to study the failure mechanism and fiber/matrix interfacial adhesion. It is shown that it can be enhanced to improve their mechanical performance to reveal the relationship between fracture toughness and water absorption fatigue according to different polymer matrices. Water uptake of the epoxy composites was found to increase with cycle times. Mechanical properties are dramatically affected by the water absorption cycles. Water-absorbed samples showed poor mechanical properties, such as lower values of maximum strength and extreme elongation. The $K_{IC}$ values demonstrated a decrease in inclination with increasing cyclic times of wetting and drying for the epoxy and vinyl-ester.

폭염 시 어린이공원의 온열환경 (Thermal Environments of Children's Parks during Heat Wave Period)

  • 류남형;이춘석
    • 한국조경학회지
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    • 제44권6호
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    • pp.84-97
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    • 2016
  • 본 연구는 폭염 시 어린이공원 내 포장 및 차양의 유형에 따른 온열환경을 규명하고자 하였다. 이를 위해 진주기상대에서 측정한 일 최고기온이 $35.9{\sim}36.8^{\circ}C$를 나타낸 2016년 8월 11일부터 8월 13일까지 3일간 진주시내 어린이공원 2곳(칠암어린이공원: $N\;35^{\circ}11^{\prime}1.4{^{\prime}^{\prim}}$, $E\;128^{\circ}531.7{^{\prime}^{\prime}}$, 표고: 38m; 가호제12어린이공원: $N\;35^{\circ}09^{\prime}56.8{^{\prime}^{\prime}}$, $E\;128^{\circ}6^{\prime}41.1{^{\prime}^{\prime}}$, 표고: 24m)의 모래밭, 고무칩포장지, 쉘터, 녹음지를 대상으로 미기상을 측정하였다. 미기상환경으로서 지상 60cm 높이에서 기온, 흑구온도, 상대습도, 풍속, 6방향의 장파 및 단파 복사를 측정하였고, 이를 바탕으로 열스트레스 지수인 WBGT와 UTCI를 산정 및 분석하였다. 또한 열화상카메라로 포장면과 놀이시설의 표면온도를 측정하였으며, 이를 바탕으로 단시간 피부접촉시 화상의 위험을 평가하였다. 연구결과는 다음과 같다. 어린이공원의 3일 시간 평균 최고 기온은 $36.6{\sim}39.4^{\circ}C$였으며, 모래밭에 비해 녹음에서 $2.8^{\circ}C$, 쉘터에서 $1.0^{\circ}C$$2.3^{\circ}C$ 낮게 나타났다. 시간 평균 최저 습도는 44~50%였으며, 모래밭이나 고무칩포장지에 비해 녹음에서 6%, 쉘터에서 4% 및 6% 높게 나타났다. 열사병위험지수 WBGT 값에 근거하면 폭염 시 어린이공원의 주간의 열사병 위험도는 높은 또는 극심한 정도로 나타났다. 3일 30분 평균 최고 WBGT 값은 $31.2{\sim}33.6^{\circ}C$였으며, 모래밭에 비해 녹음에서 $2.8^{\circ}C$, 쉘터에서 $2.3^{\circ}C$$1.0^{\circ}C$ 낮게 나타났으나, 차양에 의해서도 열사병 위험을 피할 수는 없었다. 체감더위지수 UTCI 값에 근거하면 폭염 시 어린이공원의 주간의 온열 스트레스의 범주는 매우 강한 또는 극심한 정도로 나타났다. 3일 30분 평균 최고 UTCI 값은 $39.9{\sim}48.1^{\circ}C$였으며, 모래밭에 비해 녹음에서 $7.8^{\circ}C$, 쉘터에서 $8.2^{\circ}C$$4.1^{\circ}C$ 낮게 나타났으나, 차양에 의해서도 극심한 또는 매우 강한 온열 스트레스를 강한 또는 적정한 온열 스트레스로 낮출 수는 없었다. 단시간 피부접촉에 의한 화상 온도 기준에 따르면, 놀이시설 및 포장면의 최고 표면온도가 스텐레스 스틸($70.8^{\circ}C$)은 무도장 철재 3초 $60^{\circ}C$, 고무칩포장($76.5^{\circ}C$)은 플라스틱 5초 $74^{\circ}C$, 청색 플라스틱 미끄럼판($68.5^{\circ}C$)과 앉음판($71.0^{\circ}C$)은 플라스틱 1분 $60^{\circ}C$ 기준을 초과한 것으로 나타났다. 하지만 그늘이 진 놀이시설의 표면온도는 햇빛에 노출된 놀이시설의 표면온도에 비해 $20^{\circ}C$ 내외로 낮게 나타나, 차양에 의해 화상의 위험을 현저하게 개선할 수 있을 것으로 판단된다. 폭염 시에는 어린이공원의 온열환경은 어린이들에게 높거나 극심한 열사병 위험에 빠지게 하고, 매우 강한 또는 극심한 온열 스트레스를 주기 때문에 보호자나 관리자가 어린이들의 어린이공원 이용을 제한해야 한다. 그리고 폭염시에는 어린이공원의 포장면 또는 놀이시설에 의한 화상의 위험이 매우 높으므로 이용 시 주의를 해야 하며, 화상의 예방을 위해서는 차양시설을 적극적으로 도입해야 한다.

1994년 7월 부산지역의 폭염으로 인한 일 사망률 특성 연구 (Characteristics of daily mortality due to heat waves in Busan in July 1994)

  • 이대근;김지영;최병철
    • 대기
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    • 제17권4호
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    • pp.463-470
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    • 2007
  • This study aims to assess the impact of the hot summer weather on daily mortality in Busan. Daily total all-caused mortality in the entire population in Busan has been examined during 1991-2005. The daily deaths were standardized to account for the long-term trend in mortality and their seasonal and weekly cycles. We found the net increase (about 8.2%) of excess deaths during the extraordinary heat wave period in July of 1994. It corresponds to the excess deaths of 109.5 during the month. The abnormality of temperature extremes in July of 1994 and their impacts on human health were also investigated. Unusual heat wave appeared in the first ten days in July of 1994. The excess deaths are likely to be attributable to the record-breaking heat waves. The result suggests that unusual early heat waves would be dangerous, even for inhabitants who live in an acclimated region to the heat waves such as Busan.

Climate Change Impacts in Natural Resources and Livestock in Mongolia Climate

  • Batima, P.;Natsagdorj, L.;Bayarbaatar, L..;Bolortsetseg, B.;Natsagsuren, N.;Erdenetsetseg, B.
    • 한국제4기학회지
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    • 제18권2호통권23호
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    • pp.103-104
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    • 2004
  • This paper discuss some results of observed changes of meteorological elements as temperature, precipitation and some extreme indexes in Mongolia. Mongolia is one of the largest landlocked countries in the world. The climate is characterized by a long lasting cold winter, dry and hot summer, low precipitation, high temperature fluctuation and relatively high number of sunny days per year. During last 60 years the annual mean air temperature has risen $1.66^{\circ}C$. Intensive warming of > $2^{\circ}C$ was observed at higher altitudes of high mountains when warming of < $1^{\circ}C$ was observed the Domod steppe and the Gobi Desert. Heat Wave Duration have statistically significant risen trend with increaded number of days by 8-18 at significance level of 95-99.9% depending on geography and Cold Wave Duration have shortened by 13.3 days significance level of 95-99%. In general, by the amount of precipitation, Mongolia falls in semi-arid and arid region. It is 300-350 mm in the high mountain regions while it is only 50-150 mm in Gobi Desert regions. The changes of annual precipitation have very localized character i.e.decreasing at one site and increasing at a sit nearby. Annual precipitation decreased by 30-90 mm in the northern-central region and increased by 2-60 mm in the western and eastern region. The magnitude of alteration changes in precipitation regardless increasing or decreasing is 5-25%. A trends, significant at the level of 90%, found where changes are more than 40 mm or more than 15% of annual mean value. Moreover, the soil moisture resources was decreased in the last 40 years. Specially, moisture contents of the top soil have decreased 2 times(N. Natsagsuren, 2002). Months of June and July in Mongolia is the year that moisture is not inhibiting vegetation growth. Unfortunately, its also found that moisture in this time tends to decrease. Increased temperature, decreased precipitation and soil moisture are most likely resulted in occurences of more intense drought spells that have taken place during the recent years. Intimately, these changes have considerable impact on livestock in Mongolia.

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FOLLOW-UP PHOTOMETRY OF TWO NEW ECLIPSING PCEBs FROM THE SLOAN DIGITAL SKY SURVEY

  • WANGNOK, KITTIPONG;SANGUANSAK, NUANWAN;IRAWATI, PUJI;DHILLON, VIK;MARSH, TOM R.
    • 천문학논총
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    • 제30권2호
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    • pp.217-218
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    • 2015
  • In this work, we present the result of our follow-up observations of SDSS J092741.73+332959.1 and SDSS J130733.49+215636.7 using the 2.35 m Thai National Telescope and ULTRASPEC instrument. Both systems are listed among the recently found white dwarf main sequence binaries from the Sloan Digital Sky Survey. SDSS J092741.73+332959.1 is a new PCEB with a period of 2.3 days, the longest orbital period known to date for white dwarf binaries. SDSS J130733.49+215636.7 is confirmed to be an eclipsing system with a period of 0.21 days from the Catalina Survey's light curve, however the parameters for the white dwarf are still uncertain. Our goal is to determine precise parameters for both systems using the Binary Maker 3 software. The observation for SDSS J0927+3329 was done on 9 January 2014 in the SDSS r' filter while the data for SDSS J1307+2156 were taken in the z' filter on 27 April 2014. Our models show that the red dwarf companions in both systems are well constrained inside their Roche Lobes. We find that the binary M2/M1 ratio in SDSS J0927+3329 is close to 0.5, with white dwarf and M-dwarf temperatures of 12000 K and 3300 K, respectively. Our preliminary result for SDSS J1307+2156 show that this system has an extreme mass ratio of 0.3. The white dwarf in this system has a temperature of 7500 K and the companion star has an effective temperature of 3150 K.