• Journal of Plant Biology
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• 제5권2호
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• pp.17-20
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• 1962

Altitudinal zones of Mt. Hanla were geoecologically investigated, and compared with climate index, according to Coniferae distribution. For climatic index, Warmth index was calculated on Mt. Hanla. With the resultsobtained, the altitudinal zones can be classified into the following three zones; Coniferous forest zone: below $43^{\circ}$ (month-degrees) (above 1, 450m) Deci(u)us broad-leaf forest zone: $84^{\circ}$-$43^{\circ}$ (600-1, 450m) Lucidophyllous forest zone: above $84^{\circ}$ (below 600m)

• 한국초지조사료학회지
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• 제40권4호
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• pp.265-273
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• 2020

We aimed to predict the Italian ryegrass (IRG) productivity change of introduced and domestic varieties based on climate factors and identify suitable areas for IRG cultivation using the RCP 8.5 scenario. The minimum mean air temperature in January showed the highest correlation with productivity. The ratio of possible and low productivity areas was high in Gangwondo, and the ratio of suitable and best suitable areas was relatively high in the central and southern regions in the past 30 years. The change in the IRG cultivation area was found to be 26.9% in the best suitable area between 1981-2010 but increased significantly to 88.9% between 2090s. In the IRG suitability comparison classes between domestic and introduced cultivars, the ratio of suitable and best suitable areas was relatively high in the domestic varieties during the past 30 years. However, there is almost no difference between the IRG domestic and introduced varieties in the IRG suitability classes after the 2050s. These results can predict changes in the IRG suitability classes between domestic and introduced cultivars according to the climate change scenario, but there are limitations in accurately predicting the productivity of IRG because the results may vary depending on other environmental factors.

• 농업생명과학연구
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• 제46권3호
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• pp.47-58
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• 2012

본 연구는 기후변화에 따른 난대상록수종인 황칠나무의 적지예측모델을 개발하기 위하여 수행하였다. 생장 및 입지환경 인자들간의 관계 구명을 통하여 양적 질적 자료 분석이 가능한 수량화 분석 방법에 의하여 황칠나무의 적지예측 평가기준을 도출하였다. 적지예측 프로그램은 ESRI, ArcView GIS 프로그램을 이용하여 개발하였다. 개발된 프로그램은 적지예측의 정확성 검토를 위하여 다양한 난대 상록활엽수가 분포하고 있는 전남 완도 지역에 적용하였다. 황칠나무의 적지예측 분석 결과, 최적지 표고 401~500m, 경사도 $15^{\circ}$ 이하, 국소지형은 산복 계곡부위, 퇴적양식 붕행토, 방위가 남쪽인 요철사면으로 나타났다. 완도지역의 황칠나무 최적지 등급별 맵핑 면적은 I 등급 1,487.2ha(25.4%), II 등급 1,020.3ha (17.4%), III 등급 2,231.8ha(38.2%), IV 등급 1,110.5ha(19.0%)로 나타났다.

• 한국수자원학회논문집
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• 제53권6호
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• pp.409-416
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• 2020

최근 증가하고 있는 이상기후현상으로 인한 사회·경제적 피해를 줄이기 위해 이상기후 감시가 필수적이다. 이 연구의 목적은 Noah 3.3 지면모형으로 추정한 토양수분자료를 활용하여 준실시간 주간 근역층 토양수분지수(Soil Moisture Index, SMI)를 산정하는데 있다. 동아시아영역(15-60°N, 70-150°E)에 대해 Noah 3.3 지면모형의 적용성을 평가하기 위해 양쯔강유역을 선정하였으며, 해당 유역에서 증발산과 현열을 FluxNet, FluxCom, Global Land Evaporation Amsterdam Model (GLEAM), ERA-5, Generalized Complementary Relationship (GCR)자료를 이용하여 비교·평가하였다. 양쯔강 유역에서 Noah 지면모형으로 추정한 증발산은 FluxNet, FluxCom, GLEAM, ERA-5, GCR에 의한 증발산과 0.96이상의 매우 높은 결정계수의 값을 보였으며, 현열의 경우에는 FluxNet 현열 자료와 0.71의 결정계수로 증발산 보다 다소 낮은 값을 보였다. 주간 근역층 SMI 시계열로부터 2019년 7월부터 10월까지 중국의 동부지역에서 극한가뭄(Extreme drought)이 확장되는 현상이 관측되었다. 월별 극한가뭄 발생일수의 트렌드 분석결과, 우리나라의 경우 봄철에는 극한가뭄이 지난 20년 동안 대체로 감소하는 경향이 나타났으나, 가을철에는 한반도 전역에 걸쳐 증가하는 경향이 나타났다. 이 연구가 가뭄의 시·공간적 지속성 및 확장성과 최근 가뭄발생의 경향성 등을 종합적으로 분석하고 판단하여, 가뭄으로 인한 사회·경제적 피해를 줄이기 위한 적절한 대책 마련에 활용성이 클 것으로 기대된다.

• 한국수자원학회논문집
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• 제53권4호
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• pp.285-291
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• 2020

이 연구에서는 Noah 3.3 지면모형을 이용하여 표층과 근역층(root-zone)의 토양함수비를 추정하고, 이를 위성기반 및 재분석 토양수분자료와 비교·검증하였다. 먼저, Noah 3.3 지면모형으로부터 추정한 4개 토양층 중 지면에 가까운 3개층(즉, 표층으로부터 1 m 깊이까지) 토양함수비를 이용하여 3개층의 깊이 가중평균값을 근역층 토양 함수비로 정의하였다. 이렇게 Noah 3.3 지면모형으로 추정한 토양함수비를 위성기반 표층 토양 함수비(European Space Agency Climate Change Initiatives Soil Moisture Product v04.4, ESA CCI SM v04.4)와 ERA-interim 재분석 표층 및 근역층 토양함수비와 비교·검증하였다. 또한, 전지구의 주요 5개 유역(Yangtze, Mekong, Mississippi, Murray-Darling, Amazon)에 대해 Gravity Recovery and Climate Experiment (GRACE) 관측 Total Water Storage Anomaly (TWSA) 와 TWS Change (TWSC)를 이용하여 비교·검증하였다. Noah 3.3 지면모형으로 산정한 토양수분 자료는 동아시아 지역과 남아시아 지역, 호주, 북미와 남미 등 대부분의 아시아·태평양지역에서 높은 아노말리 상관관계를 보였으며, 5개 유역에서 호주의 머레이-달링(Murray-Darling)유역에서 다소 낮은 상관관계를 보였으나, 나머지 4개 유역에서는 대체로 높은 상관성을 보였다. Noah 3.3 지면모형은 준실시간 토양수분 모의가 가능하기 때문에 이에 기반한 가뭄감시가 가능하며, 선제적 가뭄 대응 대책 마련에 활용성이 클 것으로 기대된다.

• Asian-Australasian Journal of Animal Sciences
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• 제28권7호
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• pp.943-950
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• 2015

Heat stress has adverse effects on fertility of dairy animals. Decline in fertility is linearly associated with an increase in combination of both temperature and humidity. The purpose of this study was to investigate the relationship between temperature humidity index (THI) and the pregnancy rate of Murrah buffaloes in a subtropical climate. The effects of genetic and non-genetic factors viz., sire, parity, period of calving and age group at first calving were found non-significant on pregnancy rate. The effect of THI was found significant (p<0.001) on pregnancy rate of Murrah buffaloes calved for first time and overall pregnancy rate. The threshold THI affecting the pregnancy rate was identified as THI 75. The months from October to March showed THI<75 and considered as non heat stress zone (NHSZ), while months from April to September were determined as heat stress zone (HSZ) with $THI{\geq}75$. The lowest overall pregnancy rate (0.25) was obtained in July with THI 80.9, while the highest overall pregnancy rate (0.59) was found in November with THI 66.1. May and June were identified as critical heat stress zone (CHSZ) within the HSZ with maximum decline (-7%) in pregnancy rate with per unit increase in THI. The highest overall pregnancy rate was estimated as 0.45 in NHSZ with THI value 56.7 to 73.2. The pregnancy rate was found to have declined to 0.28 in HSZ with THI 73.5 to 83.7. However, the lowest pregnancy rate was estimated as 0.27 in CHSZ with THI value 80.3 to 81.6.

• 한국지형학회지
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• 제24권3호
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• pp.1-11
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• 2017

The pollen analysis on the deposits of the lower marine terrace I of the estimated paleoshoreline height of 18m was performed in order to estimate the formation age of this terrace developed at the Sanha-dong coast, Ulsan, southeastern coast of the Korean peninsula. The pollen assemblage of the peat layer of SH-1 pollen zone (Quercus-Ulmus/Zelkova zone), lying directly on the marine rounded pebble layer of this terrace, shows that the climatic environment of the deposition period of SH-1 pollen zone was almost similar to that of the Postglacial climatic optimum period, but slightly cooler than that of the late warm stage of Last Interglacial(MIS 5a) in the eastern coast of Korea. This heightens the possibility that the deposition period of the marine rounded pebble layer which was covered by the above SH-1 peat layer is the MIS 5e which has been estimated by a previous study of the sedimentary facies of this terrace deposits (Choi, 2016). The pollen assemblage of SH-2 pollen zone (Pinus-Quercus zone) shows that the climate of this period was almost similar to that of the late Postglacial, but slightly cooler than that of the period of SH-1 pollen zone. This means that the climate around the Sanha-dong was still warmer in the deposition period of the peat layer of SH-2 pollen zone. Thus, the peat layer of SH-2 pollen zone was considered to have been deposited during the period from the early regression stage of the MIS 5d which is the estimated final stage in the deposition period of the above peat layer of SH-1 pollen zone to any stage in which the warmer environment of MIS 5 has still lasted. The humic silt layer of SH-3 pollen zone (Pinus-Ulmus/Zelkova-Abies zone) is assumed to have been deposited during the interstadial of the Last Glacial (MIS 3).

• 한국방재학회지
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• 제2권4호
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• pp.40-47
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• 2002

Since it is important to understand the bio-climatic change in Seoul for ecological city planning in the future, this paper gives an overview on bio-climate analysis of urban environments at Seoul. We analyzed its characteristics in recent years using the observations of 24 of Automatic Weather Station (AWS) by Korea Meteorological Administration (KMA). In urbanization, Seoul metropolitan area is densely populated and is concentrated with high buildings. This urban activity changes land covering, which modifies the local circulation of radiation, heat and moisture, precipitation and creating a specific climate. Urban climate is evidently manifested in the phenomena of the increase of the air temperature, called urban heat Island and in addition urban sqall line of heavy rain. Since a city has its different land cover and street structure, these form their own climate character such as climate comfort zone. The thermal fold in urban area such as the heat island is produced by the change of land use and the air pollution that provide the bio-climate change of urban eco-system. The urban wind flow is the most important climate element on dispersion of air pollution, thermal effects and heavy shower. Numerical modeling indicates that the bio-climatic transition of wind wake in urban area and the dispersion of the air pollution by the simulations of the wind variation depend on the urban land cover change. The winds are separately simulated on small and micro-scale at Seoul with two kinds of kinetic model, Witrak and MUKLIMO.

• 한국자원식물학회:학술대회논문집
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• 한국자원식물학회 2018년도 추계학술대회
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• pp.32-32
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• 2018

Flora investigations in Korea have been conducted by many researchers for diverse purposes. Accumulated flora investigation data has not been utilized efficiently because there is no accessible database for comparison. To overcome this shortcoming, we constructed web-based database of flora investigation, named as the Integrated Korean Flora Database (IKFD; http://www.floradb.net/intro.php). Until now, 284 flora references (263 papers, 14 reports and books, and 7 unpublished papers written in between 1962 and 2017) were digitalized into the database. From 134,711 records, 4,301 species belonging to 228 families and 1,079 genera were identified via mapping with two major Korean plant species lists. Polygon areas originated from references were used for distribution of plant species, identifying precise distribution area. It will be a better index to show plant ecological characteristics. Collected micro-climate data provided by Korea Meteorology Administration were also integrated in IFKD for understanding correlation between distribution of plants and micro-climate. Cold hardiness zone which has been utilized for classifying climate zones. 12 out of 26 zones identified based on micro-climate data in Korea were mapped with distribution of plants. More than half species were appeared in zone 6a, 6b, 7a, and 7b. Taken together with these results, IKFD will be a fundamental platform for understanding plants in Korea flora investigation as well as a new standard for classifying distribution of plants. Moreover, Biodiversity Observation Database (BODB; http://www.biodiversitydb.info/intro.php) which integrates plant distribution data was also integrated for further studies.

• 한국환경과학회지
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• 제13권12호
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• pp.1023-1032
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• 2004

Rapid progress in urbanization has resulted in a change of the micro climate, especially in the urban area. In order to investigate the phenomenon of the heat island in the residential micro climate, a field survey was carried out by 4 sets of the residential type in Jeonju under typical winter synoptic condition. As analytic methode, it is used the comparison on the relation of the Land-to-Coverage Rate to Heat Island and Oxygen Concentration. And as a key question it is asked how stable characteristics of the micro climate will result from the survey of the Heat Island and the Oxygen Concentration, used as indicator. To ensure the trustworthy result of research, it is calculated the critical influence of the wind velocity and the Land-to-Covearage Rate. As a result of comparative analysis, it could be confirmed that the local temperatures in all sets of the residential type were higher than the average temperature in Jeonju. But the housing type A 'exclusive use for housing zone' has relativly the most stable and best living condition. On the contrary the residential type B and D has the worst toward the oxygen concentration in the time zone 9-12 a.m., which didn't reach the minimum of the oxygen concentration $20.5{\%}.$ It means that the higer the development and population density is, the worse is the situation of the Quality of Life in the residential types in accordance with the heat island and oxygon con­centration.