• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.147-149
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• 2003

The wetness, a function of precipitation and temperature etc, and the warmth, a function of temperature, are the dominant factor for global vegetation distribution. This paper employs the normalized difference vegetation index (NDVI), warmth index (WAI), and wetness index (WEI), and focuses on an essential climate-vegetation relationship at global scale. The NDVI was acquired from ‘Twenty-year global 4-minute AVHRR NDVI dataset.’ The WEI is defined as the fraction of the precipitation to the potential evaporation. The WAI was calculated by accumulating the monthly mean temperature of the portion exceeded 5$^{\circ}C$ throughout the year. Meteorological data for the WEI and WAI calculation were obtained from the ISLSCP CD-ROM. All analyses were conducted for 1 ${\times}$ 1 degree grid box on the terrestrial area of the Earth, and on annual value basis averaged in 1987 and 1988. The result of analyses demonstrated that there are two regimes in their relations, that is, a regime in which NDVIs vary depending on the WEI, and a regime in which NDVIs vary depending on the WAI. These two regimes appeared to correspond to the wetness dominant and warmth dominant vegetation, respectively. The geographical distributions of two regimes were mapped. Most of the world vegetation is categorized into wetness dominant, while warmth dominant vegetation is seen in the high-latitude area mainly to the north of 60$^{\circ}$N in the Northern Hemisphere and high-altitude areas.

• Transactions on Electrical and Electronic Materials
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• 제17권4호
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• pp.189-195
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• 2016

Micro Hotplate (MHP) is the key component in micro-sensors, particularly gas sensors. Indeed, in metal oxide gas sensors MOX, micro-heater is used as a hotplate in order to control the temperature of the sensing layer which should be in the requisite temperature range over the heater area, so as to detect the resistive changes as a function of varying concentration of different gases. Hence, their design is a very important aspect. In this paper, we have presented the design and simulation results of a meander micro heater based on three different materials - platinum, titanium and tungsten. The dielectric membrane size is 1.4 mm × 1.6 mm with a thickness of 1.4 μm. Above the membrane, a meander heating film was deposed with a thickness of 100 nm. In order to optimize the geometry, a comparative study by simulating two different heater thicknesses, then two inter track widths has also been presented. Power consumption and temperature distribution were determined in the micro heater´s structure over a supply voltage of 5, 6, and 7 V.

• 대한원격탐사학회지
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• 제33권5_2호
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• pp.751-762
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• 2017

작황 정보 시스템은 작물 분포, 작황 정보 및 생산량에 대한 모니터링, 예측, 추정 또는 분석과 같은 다양한 형태를 통해 정보를 제공하며 본 논문은 한국, 미국 및 중국 데이터를 기반으로 구축한 웹기반 작황 정보 시스템을 제안한다. 온도, 강수량 및 일사량의 기후 데이터는 작물 성장에 미치는 영향을 분석하는데 사용되었으며, NDVI 데이터와 작물구분도 데이터는 각각 작물 모니터링과 작물 분포 관리를 목적으로 사용되었다. 본 시스템은 3가지의 주요 장점을 갖고 있으며 이는 다음과 같다: 1) 높은 시간 해상도의 데이터를 통한 정보 제공, 2) 보유 데이터 분석을 통한 보고서 작성의 자동화, 3) 사용자의 편리성을 위한 기능 제공.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2004년도 Proceedings of ISRS 2004
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• pp.553-556
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• 2004

Spatial and temporal aspects of toxic dinoflagellate Cochlodinium.p blooms and consequences of physical features in complex coastal ecosystems, off the southern Korean coast, have been investigated using data obtained from SeaWiFS and AVHRR as well as in-situ observations. Hydrographic parameters measured using CTD sensors were used to elucidate physical factors affecting the spatial distribution and abundance of Cochlodinium.p blooms. The results show spatial and temporal variations of chlorophyll-a (Chl-a) and sea surface temperature (SST) and reveal significant information about Cochlodinium.p blooms and process underlying their evolution. Satellitederived Chl-a estimates appear to be potential in explicating the evolution, movement and distribution of Cochlodinium.p blooms in the enclosed bays of the South Sea. The existence of thromohaline waters offshore provide favorable conditions for the rapid growth and subsequent southward initiation of Cochlodinium.p blooms that are influenced to flow on the offshore branch (OB) during September. It was observed that there was a significant variation in the sun-induced chlorophyll-a fluorescence signal in the remote sensing fluorescence spectra and its high-intensity was recognized during the period of exponential growth and physical transport. Satellite-derived Chl-a concentration during September 1999 ranged between $3­60mg/m^3$ inside the Jin-hae and adjacent Bays and $1-6mg/m^3$ in offshore waters, with varying Cochlodinium.p abundances 1500 to 26000 cells $ml^{-1}.$ The closely spaced CTD surveys and satellite-derived SST give a complete overview on the initiation of Cochlodinium.p blooms in hydrodynamically active regions of the offshore southern East Sea by the influence of Tsushima Warm Current (TWC).

• E2M - 전기 전자와 첨단 소재
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• 제9권6호
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• pp.605-615
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• 1996

In this paper, the effect of alkaline oxide addition such as Li$_{2}$O and Na$_{2}$O on the microstructure and humidity sensitivity of V$_{2}$O$_{5}$(2 mol%)-doped TiO$_{2}$(98 mol%) was investigated as a function of amount (0, 1, 2, 5, 10 mol%) of Li$_{2}$O and Na$_{2}$O additives. The pores in the alkaline free sample were distributed mostly in the range between 0.16 and 1.0.mu.m in diameter and its porosity was 23.29%. Li$_{2}$O caused grain overgrowth and reduced the porosity with a narrow distribution of the pore size, leading to poor humidity sensitivity. Na$_{2}$O helped to enlarge the distribution of the pore size through the formation of small soluble phases. The pore sizes of the sample containing Na$_{2}$O 2mol% were distributed mostly in the range between 1.0 and 2.5.mu.m in diameter and its porosity and intrusion volume of mercury were 31.13 % and 0.1155 mL/g respectively, which consequently improved the humidity sensing characteristics such as the sensitivity and temperature-stability. Especially, the addition of 2mol% of Na$_{2}$O improved the humidity-sensing characteristics such as sensitivity and linearity in the whole range between 30 and 90 %RH (Percentage Relative Humidity)y)

• 한국지리정보학회지
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• 제7권3호
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• pp.79-89
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• 2004

원격탐사 기법은 식생 및 토지이용과 같은 지형조건과 관련된 증발산량을 산정하기 위한 하나의 수단으로 효과적으로 이용될 수 있다. 지표면에서 발생되는 증발산량을 지배하는 인자는 기온, 습도, 바람, 일사량 및 토양조건 둥 매우 복잡하게 구성된다. 식생은 그 지점의 증발산량에 영향을 주고 있으며, 증발산량을 지배하는 복잡한 인자는 식생의 성장조건에 직접적으로 영향을 미친다. 결국 증발산량과 식생조건 사이에는 강한 상관관계가 성립될 수 있음을 예상할 수 있다. 비교적 넓은 지점에 대한 식생상태를 파악을 위해서는 NOAA/AVHRR 자료가 효과적으로 이용될 수 있으며, 이로부터 얻어지는 식생지수(NDVI)를 이용함으로서 증발산량과 NDVI 사이의 강한 상관관계를 생각할 수 있다. 본 연구에서는 이러한 점을 근거로 하여 NDVI와 기상자료를 조합하는 간편한 방법에 의한 실제증발산량 산정방법을 제안한다.

• 대한원격탐사학회지
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• 제34권2_1호
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• pp.167-178
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• 2018

도심녹지는 도심 주변의 높은 기온을 낮춰 주는 중요한 역할을 한다. 도심녹지의 냉각효과는 녹지내부 뿐만 아니라 주변 도로와 빌딩 지역에도 영향을 준다. 도심녹지가 주변에 미치는 영향을 분석하기 위해 2013년부터 2015년까지 관측된 Landsat 8 위성자료를 이용하여 서울 선정릉 주변의 지표면온도를 산출하였다. 선정릉 주변의 지표면온도 분포를 분석한 결과, 도심녹지의 냉각효과는 녹지를 중심으로 여러 방향에서 나타나는 것을 확인하였다. 도심녹지의 냉각효과에 미치는 토지피복의 영향을 살펴보기 위하여 주거지역과 상업지역에 대해 냉각효과를 분석한 결과 주거지역의 냉각효과 범위가 100~250 m로 나타났고, 평균 $2.3^{\circ}C$의 냉각효과를 보였다. 반면, 상업지역의 냉각효과 범위는 0~200 m 였고, 평균 약 $0.3^{\circ}C$의 냉각효과를 보였다. 이러한 분석 결과를 통해 도심녹지의 냉각효과는 상업지역보다 주거지역에서 강도와 범위가 큼을 알 수 있었다.

• 한국지리정보학회지
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• 제2권3호
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• pp.71-80
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• 1999

본 연구의 목적은 Landsat TM 자료를 이용하여 시화호로부터 황해로 방류되는 오염된 시화호물의 방류범위를 해석하는 것이다. 본 연구지역은 Case 2 water에 속하는 지역이기 때문에 엽록소와 부유사의 정량적인 해석을 위한 알고리듬을 적용하는데는 한계가 있다. 본 연구의 초점은 다중시기의 Landsat TM 자료를 이용하는데 있다. 즉, 시화호로부터 방류되는 방류수의 공간적인 확산범위를 관측하기 위해 주성분분석을 적용하였다. 주성분분석의 결과는 엽록소, 부유사, 투명도, 표층수온, SeaWiFS 채널의 수중광학 측정결과인 반사치와 비교하였다. 그리고, PRR-600에 의해 얻어진 수중 광학 반사치는 Landsat TM 자료에서 얻어진 주성분분석 결과와 함께 분석되었다. 이러한 현장관측자료를 바탕으로 비록 다른 현장관측 측정변수가 낮은 상관관계를 나타냈음에도 불구하고 투명도(Secchi Disk Depth)와 주성분분석의 제 1 성분이 $R^2$=0.7631의 좋은 상관관계를 나타내었다. 또한 본 연구에서는 다중시기의 원격탐사자료를 사용하여 주성분분석을 할 때 나타나는 여러 문제를 토의하였다.

• 대한원격탐사학회지
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• 제35권1호
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• pp.57-81
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• 2019

Satellite images can be integrated into a crop model to strengthen the advantages of each technique for crop monitoring and to compensate for weaknesses of each other, which can be systematically applied for monitoring inaccessible croplands. The objective of this study was to outline the productivity of paddy rice based on simulation of the yield of all paddy fields in North Korea, using a grid crop model combined with optical satellite imagery. The grid GRAMI-rice model was used to simulate paddy rice yields for inaccessible North Korea based on the bidirectional reflectance distribution function-adjusted vegetation indices (VIs) and the solar insolation. VIs and solar insolation for the model simulation were obtained from the Geostationary Ocean Color Imager (GOCI) and the Meteorological Imager (MI) sensors of the Communication Ocean and Meteorological Satellite (COMS). Reanalysis data of air temperature were achieved from the Korea Local Analysis and Prediction System (KLAPS). Study results showed that the yields of paddy rice were reproduced with a statistically significant range of accuracy. The regional characteristics of crops for all of the sites in North Korea were successfully defined into four clusters through a spatial analysis using the K-means clustering approach. The current study has demonstrated the potential effectiveness of characterization of crop productivity based on incorporation of a crop model with satellite images, which is a proven consistent technique for monitoring of crop productivity in inaccessible regions.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2002년도 Proceedings of International Symposium on Remote Sensing
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• pp.615-620
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• 2002

Probability distribution of the sea surface slope is estimated using sun glitter images derived from visible radiometer on Geostationary Meteorological Satellite (GMS) and surface vector winds observed by spaceborne scatterometers. The brightness of the visible images is converted to the probability of wave surfaces which reflect the sunlight toward GMS in grids of 0.25 deg $\times$ 0.25 deg. Slope and azimuth angle required for the reflection of the sun's ray toward GMS are calculated for each grid from the geometry of GMS observation and location of the sun. The GMS images are then collocated with surface wind data observed by three scatterometers. Using the collocated data set of about 30 million points obtained in a period of 4 years from 1995 to 1999, probability distribution function of the surface slope is estimated as a function of wind speed and azimuth angle relative to the wind direction. Results are compared with those of Cox and Munk (1954a, b). Surface slope estimated by the present method shows narrower distribution and much less directivity relative to the wind direction than that reported by Cox and Munk. It is expected that their data were obtained under conditions of growing wind waves. In general, wind waves are not always developing, and slope distribution might differ from the results of Cox and Munk. Most of our data are obtained in the subtropical seas under clear-sky conditions. This difference of the conditions may be the reason for the difference of slope distribution.