• 제목/요약/키워드: warm period

검색결과 423건 처리시간 0.033초

Pacific Equatorial Sea Surface Temperature Variation During the 2015 El Niño Period Observed by Advanced Very-High-Resolution Radiometer of NOAA Satellites

  • Lee, Seongsuk;Yi, Yu
    • Journal of Astronomy and Space Sciences
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    • 제35권2호
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    • pp.105-109
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    • 2018
  • El $Ni{\tilde{n}}o$ is the largest fluctuation in the climate system, and it can lead to effects influencing humans all over the world. An El $Ni{\tilde{n}}o$ occurs when sea surface temperatures in the central and eastern tropical Pacific Ocean become substantially higher than average. We investigated the change in sea surface temperature in the Pacific Ocean during the El $Ni{\tilde{n}}o$ period of 2015 and 2016 using the advanced very-high-resolution radiometer (AVHRR) of NOAA Satellites. We calculated anomalies of the Pacific equatorial sea surface temperature for the normal period of 1981-2010 to identify the variation of the 2015 El $Ni{\tilde{n}}o$ and warm water area. Generally, the warm water in the western tropical Pacific Ocean shifts eastward along the equator toward the coast of South America during an El $Ni{\tilde{n}}o$ period. However, we identified an additional warm water region in the $Ni{\tilde{n}}o$ 1+2 and Peru coastal area. This indicates that there are other factors that increase the sea surface temperature. In the future, we will study the heat coming from the bottom of the sea to understand the origin of the heat transport of the Pacific Ocean.

농업용수의 수온 상승에 관한 연구

  • 황은;김철규;이상범
    • 물과 미래
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    • 제5권2호
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    • pp.17-29
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    • 1972
  • The persent study aims at finding out a means of prevention cool spell damages on the hilly areas. The irrigation plots of 24 hour stored water warm water way and warm water plots, cool water way are respectively established to find out water temperature and influnce on the growing rice plants. The results obtained are summed up as follows. 1. Warm water areas consisted of $5 m^2 Q=0.93 1{\ell}/sec$, V=31 cm/sec, S=1/1, 000, L=81.6m, B=5cm, h=6cm, t=4min 33sec, drops=9 areas, are constructed to help the water temperature of $14.5^{\circ}C$ rise to that of $21.6^{\circ}C$. This indicates lower temperature than $23^{\circ}C$ of critical water temperature in irrigation facilities by $1.45^{\circ}C$ and than $26.2^{\circ}C$ of balanced water temperature of Seoul arears by $4.6^{\circ}C$. But this does not give much influance on rice plant cultivation. 2. The rising of water temperature is influened according to the temperature, solar radiation but the water temperature changes according to the heat absorption of organized materials, weather and terraces. The difference of water temperature could be found in the first growing stage. 3. Through the warm water way of water rises to the temperature of $21.6^{\circ}C$ which also rises to the temperature of around $30^{\circ}C$ in the paddy field of submerged irrigation. The rice plants are comparatively free from prolonged cool damage, reproduction abstructive damage. 4. The water temperature in rice field in proportion to temperature influence of weather condition but the water temperature approaches to that of weather in the days of later growing stage and water temperature become lower than the air temperature in the fruit stage. 5. The water in the submreged field is $10^{\circ}C$ warmer than in the warm water way during the first growing stage period but the water temperature in the warm water way is warmer in the later growing stage period. The cool water of $14.5^{\circ}C$ is warmed to $30.1^{\circ}C$ and rice plants cultivation is free from other damages. 6. The 12% increased production or 570.98kg/10a is made cool water plot by rising the temperature of water from $14.5^{\circ}C$ to $21.6^{\circ}C$ making the water run through warm water way. 7. The damage inflicted by the cool water irrigation during the first growing stage period is the obstruction of peak tillering stage and the obstruction of heading the later growing stage period and the obstruction of fruiting and number of panides per fill.

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Latitude and seasons influence the prevalence of Theileria orientalis and affect the hematology of non-grazed dairy cows in Korea

  • Hector Espiritu;Hee-Woon Lee;Md Shohel Al Faruk;Su-Jeong Jin;Sang-Suk Lee;Yong-Il Cho
    • Parasites, Hosts and Diseases
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    • 제62권1호
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    • pp.64-74
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    • 2024
  • This pilot study aimed to investigate the effects of regional and seasonal variations on the prevalence of Theileria orientalis and the hematological profile of non-grazed dairy cows in Korea. A total of 365 clinically healthy lactating Holstein Friesian cows from 26 dairy farms in 7 provinces that were categorized into northern, central, and southern regions were sampled during the warm period from July to August and the cold period from October to December. The detection of T. orientalis major piroplasm surface protein gene and the hematology non-grazed dairy cows were analyzed using peripheral blood samples. The T. orientalis prevalence was 20.0% (73/365). The prevalence in the southern region was 35.9%, which was significantly higher than that in the central (21.6%) and northern (12.9%) regions (P<0.05). The prevalence during warm period was higher (43.0%) than that during the cold season (13.5%). The infected cows showed significantly lower erythrocyte counts in the southern region (5.8±0.6 M/㎕) and during the warm period (5.8±0.7 M/㎕) compared with those in the central and northern regions and during the cold season, which affected the extended RBC parameters, including hematocrit and hemoglobin concentrations. Our findings revealed the prevalence of T. orientalis in Korea, highlighting its high occurrence during warm periods and in certain geographical regions. Climatic factors could contribute to the health and productivity of cattle, as evidenced by the prevalence of T. orientalis and its negative impact on animals.

소복축어탕가감방과 온침요법으로 호전된 월경통 환자 8례에 대한 보고 (Clinical Study for Eight Cases of Dysmenorrhea Treated by Sobokchukeo-tang-gagambang and Warm Needle Therapy)

  • 안뜰에봄;김동철
    • 대한한방부인과학회지
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    • 제29권3호
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    • pp.57-67
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    • 2016
  • Objectives: This paper was aim to report the effects of Sobokchukeo-tang-gagambang and warm needle therapy on the dysmenorrhea patients.Methods: The patients having treated with Sobokchukeo-tang-gagambang and warm needle therapy, from January 1st in 2014 until May 31st in 2016, was enrolled in this study. We collected and analyzed their age, accessory complaint except dysmenorrhea, treatment period, dosage of herbal medicine, diagnosed gynecological disease, remedies’ effectiveness, etc.Results: All of the patients treated with Sobokchukeo-tang-gagambang and warm needle therapy in this study were recovered. Also, correlation between the characteristic and recovery status of patients was not confirmed.Conclusions: Sobokchukeo-tang-gagambang and warm needle therapy is effective on patients having variable gynecological diseases. But the cases are very deficient, so we need to study about availability of Sobokchukeo-tang and warm needle therapy on dysmenorrhea more systematically.

난지형 잔디와 한지형 잔디의 혼식에 관한 생태학적 연구 (Ecological Studies on the Warm-Season Turfgrass and Cool-Season Turfgrass Mixtures)

  • 박봉주
    • 한국환경복원기술학회지
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    • 제6권5호
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    • pp.21-27
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    • 2003
  • 본 연구는 난지형 잔디와 한지형 잔디의 혼식구의 5년간에 걸친 초종 구성비율의 경년변화를 조사하여 안정성이 높은 초종 품종의 조합을 밝히고 시비법이 난지형 잔디와 한지형 잔디 초종의 구성비율에 미치는 영향을 검토하였다. 한지형 잔디를 혼식하여 5년째인 시점에서 난지형 잔디와 한지형 잔디 혼식구의 초종 구성비율은 센티페드그래스와 버팔로그래스와의 혼식구를 제외하고는 들잔디, 세인트어거스틴그래스, 버뮤다그래스는 대체적으로 반반 정도의 비교적 안정된 혼식비율을 유지하고 있었다. 이들 초종들은 난지형 잔디와 한지형 잔디의 혼식을 위한 이용적성이 높은 것으로 사료된다. 그러나, 센티페드그래스와의 혼식구에서는 센티페드그래스가 버팔로그래스와의 혼식구에서는 한지형 잔디가 우점하여 이들 난지형 잔디는 한지형 잔디와의 혼식에 적합하지 않은 것으로 나타났다. 난지형 잔디와 한지형 잔디 혼식구의 시비는 난지형 잔디가 휴면중인 시기에 실시하면 한지형 잔디가 우점하게 되는 경향을 보여 난지형 잔디의 생육기인 4~8월 사이에 실시하는 것이 바람직한 것으로 나타났다. 이들 난지형 잔디와 한지형 잔디 혼식구는 장기간에 걸쳐 안정적으로 일정한 초종 구성비율이 유지되는 것이 중요하기 때문에 앞으로도 계속적인 조사가 이루어져야 할 것으로 사료된다.

원발성 온난자가면역용혈빈혈의 치료에 대한 후향적 분석 (Retrospective Clinical Analysis of Treatment for Primary Warm Autoimmune Hemolytic Anemia)

  • 문홍섭;박치영
    • 한국임상약학회지
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    • 제25권3호
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    • pp.166-170
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    • 2015
  • Background: Primary warm autoimmune hemolytic anemia (AIHA) is a relatively rare hematologic disorder resulting from autoantibody production against red blood cells. There has been very few studies about primary warm AIHA in South Korea because of its low incidence. We retrospectively analyzed the treatment outcome of primary warm AIHA. Method: We reviewed retrospectively the medical records of 9 primary warm AIHA patients from December 2002 to January 2015. We analyzed the causes and clinical characteristics of primary warm AIHA patients. We retrospectively analyzed the clinical data in electronic medical records for 9 Korean patients with AIHA patients who were diagnosed during the period from December 2002 to January 2015 at the Regional University Hospital in Korea. The study protocol was approved by the Institutional Review Board (IRB #2015-08-007, Chosun University Hospital IRB). Results: The mean age was 52 years (range 27~78), the mean hemoglobin level was 5.0 g/dL (range 2.5~6.4 g/dL). All patients received steroids at therapeutic dosages (corticosteroid 1 mg/Kg) as first line treatment. Eight of them showed complete response (5/8, 62.5%) and partial response (3/8, 37.5%), one patient required second-line treatment with rituximab. Two patients who responded first line treatment were relapsed at 86 weeks and 24 weeks after response, respectively. Only one patient of them was retreated with corticosteroid because of anemic symptoms. Conclusion: This study indicates that oral corticosteroid is an effective therapy for primary warm AIHA.

운전자의 심리·생리 반응을 고려한 승용차 쾌적 난방 모드에 관한 연구 (Research on the Thermal Comfort Heating Mode Considering Psychological and Physiological Response of Automobile Drivers)

  • 김민수;금종수;박종일;김동규
    • 설비공학논문집
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    • 제30권3호
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    • pp.149-157
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    • 2018
  • In this research, the psychological and physiological reactions of the driver were measured during winter to evaluate thermal comfort. The experiment was conducted using 3 different cases which are hot air heating, warm-wire seat heating and hot air & warm-wire seat heater operating simultaneously. With regard to psychological reaction, the warm-wire heating mode was the most preferred. The reason is that it is dry in other cases. With regard to EEG response, thermal comfort increased by 37% in warm air mode heating. In addition, when the warm-wire heating mode and the hot air & warm-wire heating mode were simultaneously operated, the thermal comfort continuously increased by between 17% and 20% for 20 minutes after boarding. Under the change of the autonomic nervous system, the thermal stress level increased by 23% after 15 minutes on board in the hot air heating mode and decreased continuously by 13% during the warm-wire seat heating mode. We recommended the hot air heating mode is only used for a short time to raise the inside temperature during the early boarding period and that warm-wire seat heating mode be actively utilized.

한반도 호우유형의 중규모 특성 및 예보 가이던스 (Mesoscale Features and Forecasting Guidance of Heavy Rain Types over the Korean Peninsula)

  • 김선영;송환진;이혜숙
    • 대기
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    • 제29권4호
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    • pp.463-480
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    • 2019
  • This study classified heavy rain types from K-means clustering for the hourly relationship between rainfall intensity and cloud top height over the Korean peninsula, and then examined their statistical characteristics for the period of June~August 2013~2018. Total rainfall amount of warm-type events was 2.65 times larger than that of the cold-type, whereas the lightning frequency divided by total rainfall for the warm-type was only 46% of the cold-type. Typical cold-type cases exhibited high cloud top height around 16 km, large reflectivity in the upper layer, and frequent lightning flashes under convectively unstable condition. Phenomenally, the cold-type cases corresponded to cloud cluster or multi-cell thunderstorms. However, two warm-type cases related to Changma and typhoon were characterized by heavy rainfall due to long duration, relatively low cloud top height and upper-level reflectivity, and the absence of lightning under the convectively neutral and extremely humid conditions. This study further confirmed that the forecast skill of rainfall could be improved by applying correction factor with the overestimation for cold-type and underestimation for warm-type cases in the Local Data Assimilation and Prediction System (LDAPS) operational model (e.g., BIAS score was improved by 5%).

Climatic Changes During the Past 400,000 Years

  • Yi, HI-Il;Shin, Im-Chul
    • 한국제4기학회지
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    • 제18권2호통권23호
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    • pp.23-31
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    • 2004
  • Temperature variations, and carbon dioxide and methane concentrations are summarized during the past 400,000 years. Atmospheric temperature varied approximately within $10^{\circ}C$ during the past 400,000 years. Most of the time during the past 400,000 years, temperature was lower than today except 410000, 320000, 250000, and 125000 years ago. Temperature was slightly higher or at least similar to today during the time period of 410000. 320000, 250000, and 125000 years ago. The carbon dioxide concentration varied between 180 and 300 ppm, and the methane concentration varied between 40 and 700ppb. The present atmospheric concentration of carbon dioxide is 375 ppm and methane is 1750 ppb. Temperature was 5-$7^{\circ}C$ lower than today during the Last Glacial Maximum(18,000 years ago) and the Younger Dryas(10,000 years ago). Temprature was varied within $1^{\circ}C$ during the past 10,000 years. Especially Middle Holocene Climatic Optimum(6,000 years ago), Medieval Warm Period (500-1,000 years ago), and Little Ice Age(100-500 year ago) were global climatic events. In general, mechanism for the Middle Holocene Climatic Optimum, Medical Warm Period, and Little Ice Age can be explained by the solar insulation, however their exact mechnism is not well known. Carbon dioxide concentration during the past 400,000 years never reached the current value of 375 ppm. Furthermore, the current methane concentration never reached during the past 20Ma. However, current temperature value has happened several times during the past 400,000 years. The implication of this is unsolved question so far. This should be challenged in the near future.

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화성 연안의 중세온난기 이후 해수면 변동에 연동된 침식·퇴적 흔적 연구 (A Study on the Erosion and Sedimentation Traces According to the Sea Level Changes Since the Medieval Warm Period in the Hwaseong Coast)

  • 양동윤;한민;김진철;박수정;임재수
    • 한국지형학회지
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    • 제26권2호
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    • pp.39-54
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    • 2019
  • In this paper, based on evidence of coastal sediment, we show that erosion and sedimentation environments are very sensitive to sea level changes during the Medieval Warm Period (MWP) and the Little Ice Age (LIA). We identified four sedimentary units(4.57-3.07m), which formed in the Dark Age Cool Period (DACP), MWP and LIA were classified based on the lithostratigraphy, grain size distribution, magnetic susceptibility and geochemistry of a drilling core taken from the west coast of Hwaseong City. The unconformity surfaces as boundaries of the units were also identified by the lithostratigraphy shown on the drilling core. We propoese that sedimentation was dominant in the area during the periods of sea level rise, whereas erosion prevailed during the periods of sea level fall. Particularly, extreme events, such as floods and typhoons are believed to have accelerated these processes, and we found the associated evidence in sediments of two units. This study provides an example of estimating the relative sea level variation using coastal sediments and may be useful for studying past sea level changes around the Korean Peninsula.