• Proceedings of the Korea Air Pollution Research Association Conference
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• 2003.11a
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• pp.501-502
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• 2003

매년 우리나라를 찾아오는 황사는 주로 중국 북부의 황토 지대에서 바람에 의하여 하늘 높이 불어 올라간 무수의 모래 먼지가 서서히 강하하는 현상 또는 강하하는 모래 먼지를 말한다(최재천 등, 2001). 황사는 동아시아 지역에서 태평양을 가로질러 하와이까지 수송되면서 국제적으로 중요한 이슈가 되고 있으며, 아프리카 사하라 사막에서 발생한 사하라 먼지(Sahara dust)가 대서양을 가로질러 플로리다반도에서 관측됨으로서 세계적인 문제로 대두되고 있다. 최근에는 황사의 농도뿐만 아니라, 황사 중에 포함된 중금속의 농도에 관한 관심이 고조되고 있다(전병일, 2003).(중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2001.11a
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• pp.327-328
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• 2001

한반도 지역은 중국과 인접해 있는 관계로 매년 봄철이면 고비사막이나 중국의 황토고원에서 발생한 황사(yellow sand) 현상에 의해 많은 고통을 겪고 있다. 중국본토에서 발생된 황사에어로졸은 수 천 km를 장거리 이동하여 한국 및 일본등의 대기에어로졸의 질량 loading에 엄청난 변화를 초래할 뿐 만 아니라, 에어로졸을 구성하고 있는 화학적 조성에도 많은 변화를 가져온다. 특히, 에어로졸 중에서도 입자 크기가 2.5-10 $\mu\textrm{m}$사이에 있는 조대입자 ("coarse mode")의 광학적 및 화학적 특성에 많은 변화를 야기시키는 것으로 알려져 있다. (중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.04a
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• pp.87-88
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• 2002

동북아 지역은 중국과 인접해 있는 관계로 매년 봄철이면 고비사막이나 중국의 황토고원에서 발생한 황사(yellow sand) 현상에 의해 많은 고통을 겪고 있다. 중국본토에서 발생된 황사에어로졸은 수 천 km 장거리 이동하여 한국 및 일본 둥의 대기에어로졸의 질량 loading에 엄청난 변화를 초래할 뿐 만 아니라, 에어로졸을 구성하고 있는 화학적 조성에도 많은 변화를 가져온다. 일반적으로 분진은 입경에 따라 미세입자와 거대입자로 나눌 수 있다. (중략)

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2002.11a
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• pp.360-361
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• 2002

대기 중의 에어로졸은 지구의 복사평형에 직·간접적으로 영향을 끼친다. 직접적인 영향으로는 에어로졸이 가시광선과 자외선 영역의 에너지를 산란 또는 흡수함으로써 기후에 영향을 미치며, 간접적으로는 microphysical process에 의한 구름의 특성을 변화시키거나 불균일적인 화학반응을 통해서 복사특성을 지니는 가스들을 변화시킴으로써 기후에 영향을 미친다. 또한 동북아 지역 및 인접한 태평양 지역은 중국과 인접해 있는 관계로 매년 봄철이민 고비사막이나 중국의 황토고원에서 발생한 황사(Asian Dust) 현상에 의해 많은 고통을 겪고 있다. (중략)

• Journal of Korean Society of Environmental Engineers
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• v.35 no.6
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• pp.422-429
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• 2013

It is generally known that the increase of the Earth surface temperature due to the global warming together with the land desertification by rapid urban development has caused severe climate and weather change. In desert or desertification land, it is observed that there are always severe flooding phenomena, even if desert sand has the high porosity, which could be believed as the favorable condition of rain water infiltration into ground water. The high runoff feature causes possibly another heavy rain by quick evaporation with the depletion of underground water due to the lack of infiltration. The basic physics of desert flooding is reasonably assumed due to the thermal buoyancy of the higher temperature of the soil temperature than that of the rain drop. Considering the importance of this topic associated with water resource management and climate disaster prevention, no systematic investigation has, however, been reported in literature. In this study, therefore, a laboratory scale experiment together with the effort of numerical calculation have been performed to evaluate quantitatively the basic hypothesis of run-off mechanism caused by the increase of soil temperature. To this end, first, of all, a series of experiment has been made repeatedly with the change of soil temperature with well-sorted coarse sand having porosity of 35% and particle diameter, 2.0 mm. In specific, in case 1, the ground surface temperature was kept at $15^{\circ}C$, while in case 2 that was high enough at $70^{\circ}C$. The temperature of $70^{\circ}C$ was tested as this try since the informal measured surface temperature of black sand in California's Coachella Valley up to at 191 deg. $^{\circ}F$ ($88^{\circ}C$). Based on the experimental study, it is observed that the amount of runoff at $70^{\circ}C$ was higher more than 5% compared to that at $15^{\circ}C$. Further, the relative amount of infiltration by the decrease of the surface temperature from 70 to $15^{\circ}C$ is about more than 30%. The result of numerical calculation performed was well agreed with the experimental data, that is, the increase of runoff in calculation as 4.6%. Doing this successfully, a basic but important research could be made in the near future for the more complex and advanced topic for this topic.

• Proceedings of the KSRS Conference
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• 2007.03a
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• pp.49-54
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• 2007

고분해능복사계(AVHRR) 자료로부터 산출한 아시아지역 지면피복 분류자료들 (United States Geological Survey: USGS, International Geosphere Biosphere Programme: IGBP, University of Maryland: UMd)의 분류특성을 분석하였으며 이를 근거로 하여 이 지역에 대한 지면피복의 분류를 시도하였다. 서로 다른 지면피복 분류 자료들의 비교를 위하여 지도 투영법을 일치시켰으며 지면피복 정의가 유사한 유형들만 비교하였다. 세 지면피복 자료에서 분류가 모두 일치하는 비율은 33.57%이고 3 자료 중 두 자료에서 분류가 일치하는 비율은 49.69%로 나타났다. 전체적으로 나대지(사막)， 도시 및 혼합림과 같이 식생의 생물리적 특성이 뚜렷한 유형들에서는 분류의 일치율이 높게 나타났다. 반면에 농지， 낙엽활엽수림， 및 낙엽침엽수렴과 같이 식생의 생물리적 특성이 유사한 유형에서는 일치율이 낮게 나타났다. 분류에 사용된 기본 입력자료수， 지면피복 유형수，분류기법 및 입력 자료의 전처리 수준 등이 지면피복 분류 결과에 차이를 유발한 것으로 판단된다. 지면피복 자료들의 비교결과와 각 유형별 식생지수의 평균 계절변동 특성을 이용하여 이 지역에 대한 지면피복 분류자료를 보완하였다.

• Korean Journal of Remote Sensing
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• v.34 no.6_3
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• pp.1369-1382
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• 2018

As the number of multispectral satellites increases, it is expected that it will be possible to acquire and use images for periodically. However, there is a problem of data discrepancy due to different overpass time, period and spatial resolution. In particular, the difference in band bandwidths became different reflectance even for images taken at the same time and affect uncertainty in the analysis of vegetation activity such as vegetation index. The purpose of this study is to estimate the band adjustment factor according to the difference of bandwidth with other multispectral satellites for the application of KOMPSAT-3 satellite in agriculture field. The Spectral band adjustment factor (SBAF) were calculated using the hyperspectral satellite images acquired in the desert area. As a result of applying SBAF to the main crop area, the vegetation index showed a high agreement rate of relative percentage difference within 3% except for the Hapcheon area where the zenith angle was 25. For the estimation of SBAF, this study used only one set of images, which did not consider season and solar zenith angle of SBAF variation. Therefore, long-term analysis is necessary to solve SBAF uncertainty in the future.

• The Korean Journal of Ecology
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• v.17 no.3
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• pp.311-318
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• 1994

We examined spatial and temporal patterns of root decomposition for three and half years, from October 1986 to April 1990, in semi-arid Chihuahuan Desert. Decomposition of roots occurred in a two-phased pattern: an early period of rapid mass loss followed by a period of slower loss. The rate of root decomposition had a high negative correlation with the initial lignin concentration in roots (r=-0.84, p<0.05). Annual mass loss rate of Baileya multiradiata, a herbaceous annual, was the highest with the value of 0.60, while that of Panicum obtusum. a perennial grass which was restricted to playa, was the lowest with 0.13. The mass loss rate of roots in the playa was the lowest among the vegetation zones along the transect. After 42 months elapsed, fluffgrass roots in playa lost 40% of the initial mass, while in other sites it lost on average 55% of the initial mass. In all roots except for desert marigold, there was an initial release of nitrogen early in decomposition followed by net nitrogen immobilization. Nitrogen concentration of the desert marigold roots showed linear increase from the beginning. Lignin concentration of perennial grass roots were higher than those of herbaceous annual and woody perennial root.

• Journal of the Korean Society of Environmental Restoration Technology
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• v.15 no.6
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• pp.29-41
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• 2012

This study was conducted in Ningxia Hui autonomous region, located at southern part of Mu Us sand land in China. To investigate relationships between windbreak effect and installation cost of sand barriers, plastic net is utilized by using four kind of heights (0.2, 0.3, 0.4 and 0.5m) and four kind of porosities (20, 30, 50 and 70%). These heights and porosities are measured for estimating distances for effective windbreak. It is shown that porosity and the distance have a positive relationship at same heights and porosity on ground indicates a constant figure when height reaches a certain level, regardless of the porosity. This implies that there is a difference of level of windbreak with different porosities; however, distance of windbreak effect is same at the same height of sand barrier. As a result of comparison between porosity of sand barrier on the ground and installation cost in each sand barrier with various heights and porosities (16 combinations), 0.4m and 0.5m height sand barriers describe highest economical efficiency. Within two variables, we concluded that height has a higher impact on windbreak effect than porosity.

• The Journal of the Korea Contents Association
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• v.16 no.1
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• pp.578-584
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• 2016

The Purpose of this study is to suggest various kinds of applicability by analyse a case of application, Gaga movement Language of Ohad Naharin. There are experiences based on participation on Gaga Workshop in Tel Aviv, 2015, Gaga People Website that Gaga Movement Ltd. have for running programs, Dance Journals and Theses for materials. As a result, Gaga was applied to performing arts, education and Tourism. It evolved movement in dance works and narrowed the distances between dancers and audiences in performing arts. Gaga/Dancers was for dance education contents for professional dancers. Gaga/people was for Dance education contents for public. Last, Gaga was applicable to tourism as it combined with regional nature of desert, in Gaga in Desert. This achievement is originated by the way of Gaga Movement Ltd. business Most of all, it was the attitude of returning their achievement of dance in art. It is considered that various kinds of application on dance contents enriches culture in society.