• 대한원격탐사학회지
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• 제40권3호
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• pp.307-316
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• 2024

2024년 1월 1일 일본 노토반도에서 모멘트 규모 7.5의 강진이 발생했다. 이 강진에 의해 노토반도에는 심각한 지표 변위가 발생하였다. 지표 변위 파악에는 global navigation satellite system (GNSS) 기지국에서 측정된 자료를 사용하나 기지국이 존재하지 않는 지역의 정보를 획득하기에는 한계점이 존재한다. 따라서 본 연구에서는 급격하게 발생한 변위를 탐지할 수 있는 offset tracking을 이용하여 노토반도 전역의 수평 지표 변위를 파악하고자 한다. Offset tracking 기법을 이용하여 노토반도를 분석한 결과 진앙이 위치한 노토반도의 북동쪽 지역보다 북서쪽 지역에서 더 많은 수평 방향 지표 변위가 발생하였으며 지표 변위 값이 최대 2.9 m에 달하는 것으로 나타났다. 본 연구의 결과는 지상 GNSS 기지국을 통해 지표 변위 자료를 획득하지 못하는 지역의 지표 변위 값을 산출하는 데 활용할 수 있을 것이다.

• Asian Journal of Atmospheric Environment
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• 제5권3호
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• pp.164-171
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• 2011

This work focuses on the analysis of bioaerosols in the atmosphere at higher altitudes over Noto Peninsula, Japan. We carried out direct sampling via aircraft, separated cultures, and identified present isolates. Atmospheric bioaerosols at higher altitudes were collected using a Cessna 404 aircraft for an hour at an altitude of 3,500 m over the Noto Peninsula. The aircraft-based direct sampling system was devised to improve upon the system of balloon-based sampling. In order to examine pre-existing microorganism contamination on the surface of the aircraft body, bioaerosol sampling was carried out just before takeoff using the same method as atmospheric sampling. Identification was carried out by a homology search for 16S or 18S rDNA isolate sequences in DNA databases (GenBank). Isolate sampling just before takeoff revealed Stretpomyces sp., Micrococcus sp., and Cladosporium sp. One additional strain, Bacillus sp., was isolated from the sample after bioaerosol collection at high altitude. As the microorganism contamination on the aircraft body before takeoff differed from that while in the air, the presence of additional, higher atmosphere-based microorganisms was confirmed. It was found that Bacillus sp. was floating at an altitude of 3,500 m over Noto Peninsula.

• Fisheries and Aquatic Sciences
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• 제3권2호
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• pp.97-110
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• 2000

To investigate characteristics of water masses and current structures around Noto Peninsula located in south-east coastal region of the East Sea, observation results of CREAMS (Circulations Research of the East Asian Marginal Seas) cruise and data report of oceanographic observation (Japan Meteorological Agency) in June, 1995 and 1996 were used. Water mass showing characteristics of Tsushima Warm Current (TWC) exists over the continental shelf. The depth is shallower than 200m and its width and thickness are 190km and 200m, respectively. Minimum level of dissolved oxygen occurred at the layers of maximum salinity. In the current structure, a noteworthy phenomenon is that the positions of the high-salinity water (more than 34.6 psu) match well with the distributions of the southwestward flow. In June of 1995 and June of 1996, a southwestward flow were separated into two parts along line C and line G. Current directions derived from the temperature and salinity match well with the distributions of the geostrophic currents in the vertical sections. The isothermal lines and the isohaline, which exist horizontally along the coastal area of the Japan, change abruptly at the frontal area of the Noto Peninsula, then turn toward the center of the East Sea. The dynamic depth anomalies centering around the region far northwest of the Noto Peninsula were relatively high, compared to those of other regions. The isopycnic surface (sigma-t, 25.8) existed near the surface in the central part of the East Sea, but, at the depth of 100m, the isopycnic surface was found in the coastal waters.

• 한국환경과학회지
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• 제12권9호
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• pp.943-948
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• 2003

Variation of the polar front in the East Sea is studied using temperature and dissolved oxygen data obtained from Japan Meteorological Agency from 1972 to 1999. Variation of the polar front in the East Sea has a close relation to the variation of the Tsushima Warm Current (TWC). When the TWC spreads widely in the East Sea, polar front moves northward. The spatial variation of the polar front is greater in the southwestern area of the East Sea and the northern area of Tsugaru Strait where the variation of the TWC's distribution area is greater than those in others of the East Sea. Hence, in the southeastern area of the East Sea, that is, between near Noto peninsula and Tsugaru Strait, the spatial variation of the polar front is not so wide as in the southwestern area because the flow of TWC is stable.

• 한국방재학회:학술대회논문집
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• 한국방재학회 2009년도 정기 학술발표대회
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• pp.26-35
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• 2009

Efficient recovery assistance for individual households is one of the inevitable issues in management after a disaster. Discussion on how the assistance should be provided to them, however, has been put aside whereas amount or contents of it have been disputed every time a disaster happens. Public support system in a time of disaster in Japan is very complicated because many laws are related to recovery support and each law covers just a part of total recovery needs of affected household. It is difficult to see whole picture of the system for affected households. Therefore, households must have many interactions with various sections in charge of particular assistance service to know the contents of each assistance and requirements to receive it to decide combination of supports they use. It is crucial for efficient recovery assistance operation to manage those customer relations since considerable part of troubles in individual recovery came from failure in each interactions caused by lack of common understanding on each recovery process between them. In this paper, I want to introduce how support system in Japan is fragmented, a case of Anamizu town which adopted a customer-oriented framework of information management system for their assistance operation after Mar. 2007 Noto peninsula earthquake and what was learned from the case.

• 지구물리와물리탐사
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• 제13권1호
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• pp.88-95
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• 2010

천부와 광역적인 지체 구조를 해석하기 위하여 일본 혼슈섬 중부에 위치한 노토 반도 연안을 따라 2008년 10월 헬리콥터를 이용한 항공 중력 탐사를 수행하였다. 항공탐사 측선은 총 700 km 정도이며, 세 개의 교차측선을 포함하여 2 km 간격으로 연안에서 20 km 이내에서 수행되었다. 항공탐사를 통해 해석된 부게 이상은 육상탐사와 선상탐사의 결과와 잘 부합하고 있으며, 해안으로 갈수록 중력값이 감소하는 패턴 및 선행연구 결과로 알려진 와지마만의 특성을 잘 보여주고 있어 타당성 있는 항공 탐사 결과임을 확인할 수 있었다. 이번 연구에서 제안하는 항공중력 시스템은 공간적으로 2km 정도의 해상도를 제공해 주고 있다. 항공탐사 결과를 기준변의 자료로 보정해 주기 위하여 항공, 선상, 육상 탐사 결과를 모두 이용하였으며, 이를 위하여 입체각을 이용한 수치 적분을 반복적으로 수행하였다. 최종적으로는 해발 300 m 높이의 중력 이상값으로 계산하였다. 그러나, 선상중력자료와의 자연스러운 자료 통합을 수행하기 위해서는 2-5 mGal 정도의 추가 보정이 필요하였으며, 이를 고려하면, 이번 항공 중력 측정 자료는 2-g mGal 의 오차 범위를 갖는 것으로 판단된다.

• 한국어업기술학회:학술대회논문집
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• 한국어업기술학회 2001년도 춘계 수산관련학회 공동학술대회발표요지집
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• pp.242-243
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• 2001

Tsushima Warm Current(WD entering into the East Sea through the Korean Strait flows northeastward and during this travel it shows complicated movement like meandering and eddy. It is considered that these variations of TWC are important causes making water masses unstable and also have influence on biological and chemical properties of water masses. Lee and Cho(2000) suggested that meandering of TWC in adjacent waters of Noto peninsula has much influence on fluctuation of current structure. (omitted)

• Asian Journal of Atmospheric Environment
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• 제5권3호
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• pp.146-151
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• 2011

1-Nitropyrene (1-NP), 2-NP and 2-nitrofluoranthene (2-NFR) are useful markers for studying the atmospheric behaviors of polycyclic aromatic hydrocarbons (PAHs) and nitropolycyclic aromatic hydrocarbons (NPAHs). However, present methods for measuring trace levels of these compounds are lesssensitive and laborious. Here we describe several improvements to a previously reported high-performance liquid chromatography-chemiluminescence detection system that allows it to determine trace levels of 1-, 2-NPs and 2-NFR. The proposed system was equipped with a reducer column packed with Pt/Rh instead of zinc whose life-time was limited. The combination of Cosmosil MS-II (monomeric ODS) and AR-II (polymeric ODS) columns was used instead of polymeric ODS columns as the separator column to improve the separation. An ethanol mixture with acetate buffer (pH 5.5) was used in place of an acetonitrile mixture with the same buffer to activate the reducer column. The same ethanol mixture was used as the mobile phase for the clean-up column. The switching time of the column switching valve was optimized to concentrate the amino-derivatives of above NPAHs quantitatively on the concentrator column. The concentrations of bis(2,4,6-trichlorophenly) oxalate and hydrogen peroxide in the chemiluminescence reagent solution were optimized to 0.4 mM and 30 mM, respectively, to increase the sensitivity. Under the above conditions, the detection limits (S/N=3) of 1-, 2-NPs and 2-NFR were 1 fmol (0.25 pg), 10 fmol (2.5 pg) and 4 fmol (1 pg), respectively. The proposed system was effectively used to determine trace levels of 1-, 2-NPs and 2-NFR in airborne particulates collected at Noto Peninsula. The atmospheric concentrations of 1-, 2-NPs and 2-NFR were not more than sub pg $m^{-3}$ levels. They were higher in winter (January) than in summer (July). In both seasons, the concentrations were in decreasing order, [2-NFR]>[1-NP]>[2-NP].