지진해일 또는 조석과 같은 파의 거동을 수치모의할 때 해안선의 위치는 파랑의 움직임에 따라 끊임없이 이동하게 된다. 따라서, 이를 수치모형에 효과적으로 반영하기 위해서는 수치모형의 경계선을 파랑의 움직임에 따라 이동시켜야 한다. 본 연구에서는 경사지형을 계단지형으로 단순화한 이동경계조건에 대해 해안선의 이동을 보다 정확히 모의하기 위하여 천수방정식의 비선형항을 2차 정확도의 풍상차분기법으로 차분화하여 해석하였다. 개발된 수치모형을 검증하기 위하여 바닥마

유한요소기법을 이용하여 유동해석의 수치모델을 행하였다 공간을 이산화 할 때에는 Galerkin법을 적용하였으며, 시간의 함수를 이산화 할 때에는 많은 수의 요소와 비정상상태의 문제를 다루는데 있어 장점을 가진 2단계 양해법을 이용하였다. 이동경계조건을 고려한 2차원유통모델을 개발하였고, 직사자형 수조에서 개발된 유동모델을 적용하여 검증하였고, 유용성을 확인하였다. 제주항에 개발된 이동경계기법을 적용하여 계산한 결과, 본 이동경계기법의 좋은 적용성을 보여주었다. 본 연구로부터 이동경계처리 방법이 실해역에서의 유동해석에 있어 유용하고 효율적인 방법이라고 결론지을 수 있다.

The Rondonia Boundary Layer Experiment (RBLE-Ⅱ) was conceived to collect data the atmospheric boundary layer over two representative surfaces in the Amazon region of Brazil; tropical forest and a deforested, pasture area. The present study deals with the observations of atmospheric boundary layer growth and decay. Although the atmospheric boundary layer measurements made in RBLE-Ⅱ were not made simultaneously over the two different surface types, some insights can be gained from analysing and comparing with their structure. The greater depth of the nocturnal boundary layer at the forest site may be due to the influence of mechanical turbulence. The pasture site is aerodynamically smoother and so the downward turbulent diffusion will be much less, resulting in a lower surface temperature. The strength of thermal inversion is, consequently, higher over the pasture than over the forest. The development of the convective boundary layer is stronger over the pasture than over the forest. The influence of the sensible heat flux is important but may be not enough to explain the difference completely. It seems that energy advection may occur from the wet and colder (forest) to the dry and warmer area (pasture), rapidly breaking up the nocturnal inversion. Such advection can explain the abrupt growth of the convective boundary layer at the pasture site during the early morning.

Characgcteristics of nocturnal boundary layer (NBL) were analyzed by the upper-air observations data using with the airsonde and pilot balloons from 1994 to 1999 in Kyungpook province. The automatic weather system was also installed to obtain data in the surface layer. The atmospheric boundary layer can become stably stratified when the surface is cooler than the air. Stable nocturnal boundary layer heights were estimated from the top of surface stable layer where the vertical gradient of temperature and mixing ratio tend to zero or negative. The depth of the stable nocturnal boundary layer depended largely on the thermal effect rather than the wind effect at nighttime. The NBL was more developed on the land than on the coastal region. The stability index (bulk Richardson number) showed that the NBL was stable when the wind was weak and the vertical gradient of the temperature was strong. The heat budget in the NBL was studied by considering the effect of the radiative and the turbulent cooling rates in the cases with cloud and without cloud. The NBL under clear sky was cooled by both the longwave radiative flux and the divergence of the heat flux, while NBL under the cloudy sky the longwave radiative flux played a role of the warming. It was noted that the heat was not conserved in both cases. To complete the heat budget in the NBL the warming/cooling by advection and subsidence must be considered.

우리나라 벼 수량의 기상반응을 종합적으로 검토하여 벼 수량예측모델을 구축하고자 1985년부터 1999년까지 15년간 수행한 20개 지역의 벼 지역적응시험 자료를 이용하여 기상에 대한 수량반응의 최대경계선(boundary line)분석을 하였으며, 이에 근거하여 수량예측모형을 설정하였다. 1. 벼의 생육기간을 영양생장기, 생식생장기, 등숙기로 구분하고 각 발육단계를 15-20일 간으로 구분하여 각 시기의 기상요소에 대한 수량반응의 최대경계선은 평균기온( Ta )과 일조시수( Sh)에 대해서는 지수함수 f( Ta )=β0(1-exp(-β1 / Ta ), f( Sh)=β0(1-exp(-β1 Th)로 나타났으며 일교차(Tr)는 2차함수 f( Tr)=β0(1-( Tr-β1 )2 )로, 이 식에서 상수항 β0를 제거하여 수량에 대한 각 기상요소의 영향도를 0-1로 나타내는 기상지수로 나타내었다. 2. 각 생육시기의 평균기온, 일조시간 및 일교차에 대한 수량반응의 최대경계선이외에 불임에 의한 등숙률 저하와 그에 따른 수량감소를 고려하기 위하여 Uchijima(1976)가 제안한 냉각도일수(cooling degree day)를 출수전 30일간의 생식생장기에 계산하여 이에 대한 수량과 등숙률 반응의 최대경계선을 계산하였는데 냉각도일수가 증가하면 수량이 감소하는 지수함수로 잘 표현되어 기존의 연구들과 같은 결과였다. 3. 기상지수는 벼의 생육기간을 영양생장기, 생식생장기 및 등숙기로 구별하고 각 시기별로 수량 기상지수를 각 기상요소 기상지수를 기하평균하여 산출하였는데 각 시기별 수량기상지수의 수량변이 설명도는 각각 0.383-0.430, 0.460-0.534, 0.4603-0.587로 결정계수는 영양생장기＜생식생장기＜등숙기의 순으로 컸다. 4. 최대경계선 분석방법을 통하여 얻어진 각 생육시기별 수량기상지수를 기하평균하여 구한 종합수량기상지수와 수량과의 직선회귀식을 구하여 수량예측모형(Model I, II, III)을 작성하였다. Model I, II, III)은 각각 결정계수가 0.6512, 0.6703, 0.6129로 모든 생육단계에 걸쳐서 기간을 15-20일 단위로 세분하여 모든 기간의 수량에 대한 기상지수를 고려하여 전 생육기간의 종합수량기상지수를 산출한 Model II가 기상변화에 따른 수량변이의 설명도가 가장 높았다.

본 연구에서는 경계요소법을 이용하여 수심이 변하는 지형을 통과할 때 발생하는 파랑의 회절을 수치해석하였다. 먼저, 트렌치지형을 통과하는 파랑의 반사율과 통과율을 계산하였으며 고유함수전개법에 의한 결과와 비교하여 본 모형을 검증하였다. 아울러, 경계요소법을 정현파형 지형에 적용하여 반사율 및 Bragg 반사를 연구하였다. 수치해석에 의한 반사율은 수리모형실험에 의한 관측결과 및 고유함수전개법에 의한 결과와 비교하였다. 전체적으로 본 연구의 결과는 기존의

강화인자 검출법을 이용 X염색체에 P[1ArB]이 형질전환되어 극세포 및 경게세포에서 표시유전자 lacZ를 발현하는 노랑초파리 (EDL 149)를 이용하여 난자형성과정 동안의 경계새포의 분화 및 이동을 조사하였다. 경계세포는 9기 난포의 선단에 위치한 난포 세포로부터 분화하여 9기와 10기에 이동하는 것을 확인하였다. 난소내 \beta -galactosidase의 활성은 우화 후 처음 4일간 급격히 증가하는 것을 확인하였으며 이 시기는 난포 내에서 경계

An one dimensional atmosphere-canopy-soil interaction model is developed to estimate of the heat budget parameter in the atmospheric boundary layer. The canopy model is composed of the three balance equations of energy, temperature, moisture at ground surface and canopy layer with three independent variables of T_f(foliage temperature), T_g(ground temperature), and q_g(ground specific humidity). The model was verified by comparative study with OSUID(Oregon State University One Dimensional Model) proved in HAPEX-MOBILHY experiment. Also we applied this model in two dimensional land-sea breeze circulation. According to the results of this study, surface characteristics considering canopy acted importantly upon the simulation of meso-scale circulation. The factors which used in the numerical experiment are as follows ; the change for a sort of soll(sand and peat), the change for shielding factor, and the change for a kind of vegetation.

Kim, Sook Young. 1996. Interface between root compounds and synthetic compounds. Studies in Modern Grammatical Theories 9: 205-228. The aim of this study is to reach the interface between root compounds and synthetic compounds using the theories of Roeper/Siegel(1978),Selkirk(1982) and Fabb(1984). A compound is a lexical unit consisting of more than one base word and functioning both grammatically and semantically as a single word. It can be divided into two classes: root compounds(or primary compounds)and synthetic compounds(or verbal compounds). Root compounds are those compounds whose second elements are not derivatives from verbs. On the other hand, synthetic compounds refer to those words which contain deverbal second constituents. Roeper/Siegel generally assume that both sentences and synthetic compounds are formed from subcategorization frames associated with verbs. They propose the First Sister Principle, which applies to the formation of synthetic compounds. Selkirk`s theory consists of two claims: (i) synthetic compoundings and root compoundings are generated by the same rewriting roles, (ii) the interpretation of a synthetic compounds is due to the optional rule for assigning grammatical functions to the nonhead element. Fabb regards -ing and -er case-markers, and specifies that they may be attached in syntax. The differences of the theories were found in the different explanations of phrases and non-heads with complements, etc. They show the interface between root compounds and synthetic compounds. In conclusion a distinctive syntactic explanation on the deverbal words, the second constituents of the compounds, may thus be the key to the understanding of the interface between root compounds and synthetic compounds.

In genneral, Businger expression is used for determining a turbulance diffusion coefficient. In this study, it is applied to the surface elements of cities such as Asphalt, Ground, Grass, Pond. We set up 5 m-height bar and measured the dry temperature and wet temperature at the height of 0.13, 0.27, 0.5, 1.0, 3.0, 5.0 m. In addition we measured the wind gradient and wind velocity at the height 3 m, solar radiation continuously for 48 hours on the surface. Compared the measured data to Businger expression, the result showed that Businger expression can be well applied to the complex surface of the city.

Transport rate of windblown dusts such as soil, sand, snow is proportionate to U_*^3 and U_*, friction velocity, approximately to flow velocity of wind. Therefore, through measurement and the flow velocity of wind, it turned out that,considering different velocity distributions caused by downstream distance and porosity percent,windbreaks with appropriate porosity rate to the protection area should be chosen for the optimal fence effect. In the economic respect, better are fences with gap of 20%∼30%. Among the windbreaks to have the optimal fence effect.

For traffic proceeding in random directions on a plane surface the frequency of collision, if no avoiding action in taken ,is approximately proportional to the square of the traffic density and directly proportional to the size and speed of the ship, Avoiding is normally taken and the rte of collisions is therefore also governed by additional factors such as the visibility, the effectiveness of the collisionavoidance rules, the competence of personnel or watchkeeping attitude, the maneuverability of the ship and the efficiency of radar and other equipments. From the viewpoint of watchkeeper who is responsible for maneuvering, watchkeeping attitude such as lookout and action to avoid collision is the most controllable factor among those mentioned above. In practice, according to the investigation of the institution of marine courts, about 50% co collisions occurred is caused by disorbedience to steering and sailing rules of international regulations for preventing collision at sea including lookout. So we classify the process of collisions with first sight of another ship , assessment of risk of collisions and action to avoid collisions and make a factural survey about lookout and action to avoid collisions from the point on "time" and " distance", namely relationship among ship's size, speed, first sight time of another ship, action to avoid collisions ,and distance from sight of another ship to collision occurred. According to the results of the actual survey , we come to conclude that most of collisions occurred are due to improper lookout and ineffective action to avoid collision which means time lag from first sight of another ship to time of action taken to avoid collision is relatively long. is relatively long.