• 대기
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• 제27권1호
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• pp.79-91
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• 2017

It is imperative to understand the characteristics of atmospheric circulation patterns under the climate system due to its impact on climatic factors. Thus this study focused on analyzing the impact of the atmospheric circulation on the relationship between precipitation and temperature regionally. Here we used monthly gridded observational data (i.e., CRU-TS3.2, NOAA-20CR V2c) and HadGEM2-AO climate model by RCP8.5, for the period of 1960~1999 and 2060~2099. The experiment results indicated that the negative relationship was presented over East Asia and Europe during summer. On the other hand, at around Korea (i.e. EA1: $31^{\circ}N{\sim}38^{\circ}N$, $126^{\circ}E{\sim}140^{\circ}E$) and Northwestern Europe (i.e. EU1: $48^{\circ}N{\sim}55^{\circ}N$, $0^{\circ}E{\sim}16^{\circ}E$) in winter, strong positive relationship dominate due to warm moist advection come from ocean related to intensity variation of the East Asian winter monsoon (EAWM) and North Atlantic Oscillation (NAO), respectively. It was found that values of positive relation in EA1 and EU1 at the end of the 21st century is regionally greater than at the end of 20th century during winter since magnitude of variation of the EAWM and NAO is projected to be greater in the future as result of simulation with RCP 8.5. Future summer, the negative correlations are weakened in EA1 region while strengthened in EU1 region. For better understanding of correlations with respect to RCP scenarios, a further study is required.

• 한국대기환경학회지
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• 제22권2호
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• pp.179-189
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• 2006

Ambient gas phase mercury concentrations including elemental mercury ($Hg^0$) were measured at the Potsdam, Stockton, and Sterling sites in NY from 2000 to 2003. Also, concentrations of ambient reactive gaseous mercury (RGM; $Hg^{2+}$) were measured at the Potsdam site during one year. The contribution of RGM($4.2{\pm}6.4pg/m^3$) was about $0.2{\sim}3%$ of the total gas phase mercury concentration measured (TGM: $1.84{\pm}1.24,\;1.83{\pm}0.32,\;3.02{\pm}2.14ng/m^3$ in Potsdam. Stockton, and Sterling, respectively) at the receptor sites. Potential Source Contribution Function (PSCF), a hybrid receptor modeling incorporating backward trajectories was performed to identify source areas of TGM. Using PSCF, southern New York, North Carolina, and eastern Massachusetts were identified as important source areas in the United States, while the copper smelters and waste incinerators located in eastern Quebec and Ontario were determined to be significant sources in Canada. The Atlantic Ocean was suggested to be a possible mercury source. PSCF incorporating back-dispersion and deposition was applied for RGM , as well as PSCF based on 2-days back-trajectories. Two different approaches yielded considerably different results, primarily due to the consideration of dispersion rather than deposition. Using back-trajectory based PSCF, eastern Ohio, southern New York, and southern Pennsylvania where large coal -fired power plants area located were identified as the large sources in US. Metallurgical industry located in eastern Quebec was resolved as well. From the result of back-dispersion and deposition based PSCF, Pennsylvania, mining facilities around Lake Superior, Toronto, Boston, MA, Quebec, and coal power plants in NY were identified to be the significant source areas for Potsdam site.

• 한국지역지리학회지
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• 제11권2호
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• pp.291-311
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• 2005

스페인의 전통 토지운영 체제의 하나였던 대농장은 1520년대 신대륙 개척기에 제국군대, 성직자, 상인은 물론 구대륙 생태계의 구성요소인 다양한 동식물과 함께 멕시코를 비롯한 현재의 중남미에 이식되었다. 중세기 스페인 남부의 대농체제인 라티푼디오의 전통과 신대륙의 자연환경이 접목된 아시엔다는 미국 남부의 플랜테이션에 비유되며 식민지시대가 막을 내리는 1821년에 이미 멕시코 농촌의 보편적인 경관으로 자리잡기에 이른다. 아시엔다는 식민지시대 멕시코를 일컫는 뉴-스페인 중부지방에 집중적으로 분포하였고, 입지결정에는 건조한 환경에서 필수적으로 요구되는 식수 및 농업용수가 깊이 관여하였으며, 수행하는 내부 경제출동의 종류에 따라 곡물아시엔다, 가축아시엔다, 광산아시엔다, 아네킨아시엔다 등 다양한 유형으로 분류된다. 대토지소유자, 농장관리자, 임노동 소작인을 주요 구성원으로 하는 아시엔다는 준 자급자족적 취락으로서 주거는 물론 종교, 농업, 문화전파 등 다양한 기능을 수행하였다. 식민지시대 멕시코의 아시엔다는 자본주의의 확산과 함께 전환기를 맞게되고 이를 계기로 내부적으로 대대적인 변형을 경험하는데, 축소된 형태이지만 오늘날 대농장과 영세농지를 특징으로 하는 멕시코 농촌경관의 일부로 잔존해 있다.

• 한국어병학회지
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• 제35권2호
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• pp.215-223
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• 2022

Disease including parasite, bacteria and virus cause serious mortality to salmonid fish in the aquaculture. In this study, we investigated the current disease status of the rainbow trout (Oncorhynchus mykiss) and coho salmon (Oncorhynchus kisutch) in Yanayang, Pyeongchang, Jeongseon and Yeongwol of Gangwon province in 2021 and performed molecular characterization of those pathogen. For parasites, Ichthyophthirius multifiliis was observed at 2 farms. For bacteria, we identified Aeromonas sobria from kidney of rainbow trout using phylogenetic analysis of gyrB gene. A. salmonicida were isolated from necrosis site of gill cover and fin in coho salmon and necrotic lesion of fin in rainbow trout. Phylogenetic analysis using vap gene indicated that A. salmonicida isolated in this study were clustered with previously reported A. salmonicida subsp. salmonicida isolates. For virus, JRt-Nagano type of infectious haematopoietic necrosis virus was detected in rainbow trout, but infectious pancreatic necrosis virus and Oncorhynchus masou virus were not detected. These results provide useful information for the prevention of disease spread and transmission when cultivating new species such as Atlantic salmon in Korea.

• 대기
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• 제33권2호
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• pp.125-154
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• 2023

Since the Korean Meteorological Society was organized in 1963, the climate dynamics fields have been made remarkable progress. Here, we documented the academic developments in the area of climate dynamics performed by members of Korean Meteorological Society, based on studies that have been published mainly in the Journal of Korean Meteorological Society, Atmosphere, and Asia-Pacific Journal of Atmospheric Sciences. In these journals, the fundamental principles of typical ocean-atmosphere climatic phenomena such as El Niño, Madden-Julian Oscillation, Pacific Decadal Oscillation, and Atlantic Multi-decadal Oscillation, their modeling, prediction, and its impact, are being conducted by members of Korean Meteorological Society. Recently, research has been expanded to almost all climatic factors including cryosphere and biosphere, as well as areas from a global perspective, not limited to one region. In addition, research using an artificial intelligence (AI), which can be called a cutting-edge field, has been actively conducted. In this paper, topics including intra-seasonal and Madden-Julian Oscillations, East Asian summer monsoon, El Niño-Southern Oscillation, mid-latitude and polar climate variations and some paleo climate and ecosystem studies, of which driving mechanism, modeling, prediction, and global impact, are particularly documented.

• 한국어류학회지
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• 제35권2호
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• pp.136-140
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• 2023

우리나라에서 붉평치는 2014년 11월 삼척에서 정치망으로 채집되어 Jeong et al.(2015)에 의해 Lampris guttatus로 처음 보고되었다. 이후, Underkoffler et al. (2018)에 의해 1종(L. lauta)의 학명 부활 및 3종(L. australensis, L. incognitus, L. megalopsis)이 새롭게 보고되어, 국내 붉평치의 학명 재검토가 필요한 실정이다. 국내 미기록종 표본은 현재 서대문자연사박물관에 박제 표본으로 보존되어 있으며, 박제 표본은 다음의 형태적 특징을 가진다: 안경이 가랑이체장의 5%보다 크다; 머리, 흉부, 새개부를 포함한 몸 전체에 둥근 반점이 산재한다; 둥근 반점의 크기는 불규칙적이다; 지느러미가 모두 붉다. 또한, L. guttatus는 북대서양에 분포하는 반면 L. megalopsis는 전 세계의 온대 및 열대 해역에 분포한다. 따라서, 본 연구 결과는 형태 및 분포 특징에 의거 한국산 붉평치의 학명이 L. guttatus에서 L. megalopsis로 변경되어야 함을 시사한다.

• 수산해양기술연구
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• 제15권2호
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• pp.67-76
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• 1979

트로올선 No.85 Ptaro가 1975년 9월부터 1976년 8월까지 대서양 아프리카 연안 어장에서 조업한 어획상황을 분석한 결과 예망당 어획량의 일주기변동은 대략 다음과 같다. 1. 오징어는 일출후에 월등하게 많고 일몰후에 현저하게 적으며 주야간의 어획량비는 54:17로 획간에 많았다. 2. 갑오징어는 개체중량 300g이상의 대형어는 일출후에 다소 많고 일몰후에 적으며 주야간의 어획비는 45:28로서 획간에 많고, 개체중량 300g 미만의 소형어는 주야간의 어획량비가 40 : 32로서 큰 차이가 없다. 3. 문어는 개체중량 700g 이상의 대형어는 일출후에 적고 일몰후에 적으며, 오전보다 오후에 많은 경향이 있고, 주야간의 어획량비는 43 : 31로서 획간이 많으나, 개체중량 700g 미만의 소형어는 일출후에 적고 일몰후에 많은 경향이 있고, 주야간의 어획량비는 32 : 44로서 야간에 많았다. 4. 서대류는 일출후에 현저하게 적고 일몰후에 월등하게 많으며, 주야간의 어획량비는 16 : 41로서 획간에 많았다. 5. 돔류, 기타 A, B 잡어는 일출후에 월등하게 많고 일몰후에 현저하게 적으며, 주야간의 어획량비는 돔류 51 : 19, A 잡어류 50 : 19, B잡어류 42 : 25로서 획간에 많았다.

• Ocean and Polar Research
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• 제28권1호
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• pp.1-12
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• 2006

Analyses of sedimentological and geochemical parameters from two radiocarbon-dated sediment cores (JM98-845-PC and JM98-818-PC) retrieved from the central part of Isfjorden, Svalbard, in the Arctic Sea, reveal detailed paleoclimatic and paleoceanographic histories over the last 15,000 radiocarbon years. The overconsolidated diamicton at the base of core JM98-845-PC is supposed to be a basal till deposited beneath pounding glacier that had advanced during the LGM (Last Glacial Maximum). Deglaciation of the fjord commenced after the glacial maximum, marked by the deposition of interlaminated sand and mud in the ice-proximal zone by subglacial meltwater discharge, and prevailed between 13,700 and 10,800 yr B.P. with enriched-terrigenous organic materials. A return to colder conditions occurred at around 10,800 yr B.P. with a drop in TOC content, which is probably coincident with the Younger Dryas event in the North Atlantic region. At this time, an abrupt decrease of TOC content as well as an increase in C/N ratio suggests enhanced terrigenous input due to the glacial readvance. A climatic optimum is recognized between 8,395 and 2,442 yr B.P., coinciding with 'a mid-Holocene climatic optimum' in Northern Hemisphere sites (e.g., the Laurentide Ice sheet). During this time, as the sea ice receded from the fjord, enhanced primary productivity occurred in open marine conditions, resulting in the deposition of organic-enriched pebbly mud with evidence of TOC maxima and C/N ratio minima in sediments. Fast ice also disappeared from the coast, providing the maximum of IRD (ice-rafted debris) input. Around 2,442 yr B.p. (the onset of Neoglacial), pebbly mud, characterized by a decrease in TOC content, reflects the formation of more extensive sea ice and fast ice, which might cause decreased primary productivity in the surface water, as evidenced by a decrease in TOC content. Our results provide evidence of climatic change on the Svalbard fjords that helps to refine the existence and timing of late Pleistocene and Holocene millennial-scale climatic events in the Northern Hemisphere.

• Ocean and Polar Research
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• 제25권2호
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• pp.213-226
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• 2003

Kongsfjorden near Korean Arctic Station, Dasan, is a glacial fjord in the Svalbard archipelago, Arctic that is influenced by both Atlantic and Arctic water masses. During the Arctic field season August 2002, surface temperature, salinity, density, and phytoplankton biomass (chi a) was measured in Kongsfjorden. A total of 15 surface samples were collected for the phytoplankton related measurements. Chl a values ranged from 0.08 to 1.4mg chi a $m^{-3}$ (mean of 0.53mg chl a $m^{-3}$) in the overall surface stations. The highest values of the chi a concentrations (> 1.0mg chi a $m^{-3}$) were found near glacier in the northeastern part of Kongsfjorden. Nanoplanktonic (< $20{\mu}m$) phytoflagellates were important contributors for the increase of the chi a. The nano-sized phytoflagellates accounted for more than 90% of the total chi a biomass in the study area. Surface temperatures and salinities ranged from 2.5 to $7.18^{\circ}C$ (mean of $4.65^{\circ}C$) and from 22.55 to 32.97 psu (mean of 30.16 psu), respectively. The physical factors were not highly correlated with phytoplankton distribution. The character of surface water due to down-fjord wind was highly similar to phytoplankton distribution. Drifting ice, freshwater, and semdiment inputs from large tidal glaciers located in the inner part of Konsfjorden create steep physico- and biogeochemical environmental gradients along the length of this ford. The glacial inputs cause reduced biodiversity biomass and productivity in the pelagic community in the inner fjord. Primary production of benthic and pelagic microalgae is reduced due to the limited light levels in the turbid and mixed inner waters. The magnitude of glacial effects diminishes towards the outer fjord. Kongsfjorden is an important feeding ground fer marine mammals and seabirds. Especially, seabirds play the largest energy intake and also export nutrients for primary production of the marine microalgae. Kongsfjorden has received a lot of research attention as a site for exploring the impacts of climate changes. Dasan Station in Kongsfjorden will be an important Arctic site for monitoring and detecting future environmental changes.

• 한국해양학회지
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• 제29권3호
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• pp.228-238
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• 1994

제4기 동안에 일어난 해수면 변화는 지역적 그리고 나아가 전 지구 기후변화에 좋 은 지시자가 되고 있다. 세계 해수면은 제 4기 동안 매우 불규칙하게 변해왔는데 여기 에 대한 정밀한 수학적 접근은 어려운 실정이었다. 이 연구에서 처음으로 세계 해수면 변동자료에 확율 프랙탈을 적용하여 제4기 해수면 변동을 재구성 하였다. 미국 대서양 연안에 위치한 허드슨만과 델라웨어 해안의 홀로세 해수면 변화에 대한 프랙탈 차원을 상자 계산 방법으로 측정한 결과, 허드슨만 해수면 분노는 프랙탈 차원이 1,358이고 델라웨어 해수면 변화는 1,346이다. 프랙탈 내삽함수의 역산 방법 (IFIF)의 유효성이 허드슨만과 델라웨어 해수면의 내삽에 의해서 검증되었고, IFIF에 의해서 두지역에서 의 합리적인 해수면들이 복원되었다. 델라웨어 해수면 자료는 허드슨 해수면 자료보다 IFIF의 내삽에 대해 통계적 오차가 적게 나타나는데, 이는 델라웨어 해수면 자료가 허 드슨 자료보다 더 신빙성이 높다는 것을 의미한다. IFIF는 한국 해안의 해수면을 추정 하는 데도 이용되었는데, 한국 해안의 해수면 자료는 허드슨만이나 델라웨어 지역보다 자료가 충분치 못하다. 따라서 IFIF 의 적용 통계 오차가 적은 텔라웨어 해수면 자료 에서 구한 프랙탈 차원을 사용하여 한국 해안에 대한 IFIF의 수직 비율 인자를 계산하 였다.함수(FIF)를 한국 해안과 미국 대서양 연안의 고해수면의 재구성에 적용한 결과,한국의 고해수면은 미국의 고해수면과 다른 변화를 보였다.8000년 전부터 현재까지 두지역의 해수면은 비교해 보면 한국 해수면이 미국 해수면 보다 훨씬 높았다.