• Title/Summary/Keyword: mesoscale

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Analysis of the Relation between Spatial Resolution of Initial Data and Satellite Data Assimilation for the Evaluation of Wind Resources in the Korean Peninsula (한반도 풍력자원 평가를 위한 초기 공간해상도와 위성자료 동화의 관계 분석)

  • Lee, Soon-Hwan;Lee, Hwa-Woon;Kim, Dong-Hyuk;Kim, Hyeon-Gu
    • Journal of Korean Society for Atmospheric Environment
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    • v.23 no.6
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    • pp.653-665
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    • 2007
  • Several numerical experiments were carried out to clarify the influence of satellite data assimilation with various spatial resolution on mesoscale meteorological wind and temperature field. Satellite data used in this study is QuikSCAT launched on ADEOS II. QuikSCAT data is reasonable and faithful sea wind data, which have been verified through many observational studies. And numerical model in the study is MM5 developed by NCAR. Difference of wind pattern with and without satellite data assimilation appeared clearly, especially wind speed dramatically reduced on East Sea, when satellite data assimilation worked. And sea breeze is stronger in numerical experiments with RDAPS and satellite data assimilation than that with CDAS and data assimilation. This caused the lower estimated surface temperature in CDAS used cases. Therefore the influence of satellite data assimilation acts differently according to initial data quality. And it is necessary to make attention careful to handle the initial data for numerical simulations.

Simulating Evapotranspiration and Yield Responses of Rice to Climate Change using FAO-AquaCrop (FAO-AquaCrop을 이용한 기후변화가 벼 증발산량 및 수확량에 미치는 영향 모의)

  • Chung, Sang-Ok
    • Journal of The Korean Society of Agricultural Engineers
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    • v.52 no.3
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    • pp.57-64
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    • 2010
  • The impacts of climate change on yield and evapotranspiration of rice have been modeled using AquaCrop model developed by Food and Agriculture Organization (FAO). Climate change scenario downscaled by Mesoscale Model 5 (MM5) regional model from ECHO-G General Circulation Model (GCM) outputs by Korea Meteorological Research Institute (METRI) was used in this study. Monthly average climate data for baseline (1971-2000) and three time periods (2020s, 2050s and 2080s) were used as inputs to the AquaCrop model. The results showed that the evapotranspiration after transplanting was projected to increase by 4 % (2020s), 8 % (2050s) and 14 % (2080s), respectively, from the baseline value of 464 mm. The potential rice yield was 6.4 t/ha and water productivity was 1.4 kg/$m^3$ for the baseline. The potential rice yield was projected to increase by 23 % (2020s), 55 % (2050s), and 98 % (2080s), respectively, by the increased photosynthesis along with the $CO_2$ concentration increases. The water productivity was projected to increase by 19 % (2020s), 44 % (2050s), and 75 % (2080s), respectively.

Study of evaluation wind resource detailed area with complex terrain using combined MM5/CALMET system (고해상도 바람지도 구축 시스템에 관한 연구)

  • Lee, Hwa-Woon;Kim, Dong-Hyeuk;Kim, Min-Jung;Lee, Soon-Hwan;Park, Soon-Young;Kim, Hyun-Goo
    • 한국신재생에너지학회:학술대회논문집
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    • 2008.10a
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    • pp.274-277
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    • 2008
  • To evaluate high-resolution wind resources for local and coastal area with complex terrain was attemped to combine the prognostic MM5 mesoscale model with CALMET diagnostic modeling this study. Firstly, MM5 was simulated for 1km resolution, nested fine domain, with FDDA using QuikSCAT seawinds data was employed to improve initial meteorological fields. Wind field and other meteorological variables from MM5 with all vertical levels used as initial guess field for CALMET. And 5 surface and 1 radio sonde observation data is performed objective analysis whole domain cells. Initial and boundary condition are given by 3 hourly RDAPS data of KMA in prognostic MM5 simulation. Geophysical data was used high-resolution terrain elevation and land cover(30 seconds) data from USGS with MM5 simulation. On the other hand SRTM 90m resolution and EGIS 30m landuse was adopted for CALMET diagnostic simulation. The simulation was performed on whole year for 2007. Vertical wind field a hour from CALMET and latest results of MM5 simulation was comparison with wind profiler(KEOP-2007 campaign) data at HAENAM site.

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Thermohaline Structure of the Shelf Front in the Korea Strait in Early Winter (초겨울 大韓海峽에서 形成되는 淺海前線의 構造)

  • Lee, Jae Chul;Na, Jung Yul;Chang, Sun-Duck
    • 한국해양학회지
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    • v.19 no.1
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    • pp.56-67
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    • 1984
  • Mesoscale thermohaline structures of the meandering front in the Korea Strait during November 1976, 1980 and 1982 are studied by means of closely spaced oceanographic observations and the satellite infrared images. Strong thermal and salinity fronts coincide each other and show a wavelike meander motion with wavelengths of 40-60km and amplitudes of, 15-20km. Salinity minimum band of less than 33.0 is found along the onshore edge of the front. Width of the frontal zone corresponds approximately to the internal radius of deformation (R=5-10km) and the slope of density interface is confined to about 2R. A series of satellite infrared images with the interval of 4-5 days show a noticeable growth of frontal meander over the flat shelf west of the Korea Strait. Possible mechanisms of frontal meander and its growth are discussed.

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Analysis of Precision for Mean Sea Level Pressure simulated by high resolution Weather Model for Typhoon Manyi and Usagi in 2007 (2007년 태풍 Manyi와 Usagi 사례에 대한 고해상도 대기모델 해면기압 정확도 비교 분석)

  • You, Sung-Hyup;Kwon, Ji-Hye
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.13 no.3
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    • pp.127-134
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    • 2010
  • This study investigated the accuracy of mean sea level pressure(MSLP) predicted by weather models around Korean Peninsula during typhoon Manyi and Usagi period in 2007. The mesoscale regional model, RDAPS, KWRF with 30 and 10 km horizontal resolution and developed high-resolution WRF models with 9 and 3 km horizontal resolutions are used to predict the features of MSLP. The predicted MSLP aspects were verified using observed results from total 35 coastal stations including AWS and ocean buoy. Although 4 models showed the reasonable MLSP results during typhoon periods, the highest resolution, 3km WRF model show the most accurate MSLP results with maximum 69% and 60% improvement with comparisons of RDAPS and KWRF, respectively.

A Numerical Simulation for Thermal Environments by the Modification of Land-use in Busan (부산지역 토지이용(land-use) 변화에 의한 열환경 수치모의)

  • 김유근;문윤섭;오인보;임윤규
    • Journal of Korean Society for Atmospheric Environment
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    • v.18 no.6
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    • pp.453-463
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    • 2002
  • Prognostic meteorological model, MM5V3 (Mesoscale Model 5 Version 3) was used to assess the effects of the land-use modifications on spatial variations of temperature and wind fields in Busan during the selected period of summer season in 2000. We first examined sensitivity analysis for temperature between MM5V3 predictions and meteorological data observed at 4 AWS (Automatic Weather System) stations in Busan, which exhibited low structural and accurate errors (Mean Bias Error, MBE: 0.73, Root Mean Square Error, RMSE: 1.18 on maximum). The second part of this paper, MMSV3 simulations for the modification of land-use was performed with 1 km resolution in target domain, 46$\times$46 $\textrm{km}^2$ area around city of Busan. It was found that modification result from change of surface land-use in central urban area altered spatial distributions of temperature and wind. In particular, heat island core moved slightly to the seaward at 1300 LST. This results may imply that modification of surface land-use leads to change the thermal environments; in addition, it has a significant effect on local wind circulations and dispersions of air pollutants.

A Numerical Study on the Size and Depositions of Yellow Sand Events (황사의 크기 및 침착량에 대한 수치 모의)

  • 정관영;박순웅
    • Journal of Korean Society for Atmospheric Environment
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    • v.14 no.3
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    • pp.191-208
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    • 1998
  • Estimations of dry and wet depositions in Korea and the size distributions of yellow sand above Korea have been carried out using the Eulerian aerosol model with the simulated meteorological data from the SNU mesoscale meteorological model. The estimated particle size distribution in Korea shows a bimodal distribution with peak values at 0.6 pm and 7 pm and a minimum at 2 pm in the lower layer However, as higher up, the bimodal distribution becomes an unimodal distribution with a peak value at 4∼5mm. Among the total amount of yellow sand deflated in the source regions , the dry and wet deposition fluxes were about 92%, and about 1.3∼0.5%, repectively, and the rest(5∼6%) is suspended in the air, Most of dust lifted in the air during the clear weather is deposited in the vicinity of the source regions by dry deposition and the rest undergoes the long -range transport with a gradual removal by the wet deposition processes. Over Korean peninsula, the total amount of yellow sand suspended in the air was about 6∼8% of the emissions in the source region and the dry and wet deposition fluxes were about 0.005∼0.7% and 0.003∼0.051% of the total emitted amount, repectively. It is estimated that 2.7∼8.9 mesa-tons of yellow sand is transported annually over the Korean peninsula with the annual mean dry deposition of 2.1∼490 kilo-tons and the annual mean wet deposition of 1.5∼65 kilo-tons.

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Estimation of Nitrogen and Sulfur Dry Deposition over the Watershed of Lake Paldang (팔당호 유역에 대한 질소와 황의 건식 침적량 추정)

  • Kim J.Y;Ghim Y. S;Won J.-G;Yoon S.-C;Woo J.-H;Cho K.-T
    • Journal of Korean Society for Atmospheric Environment
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    • v.21 no.1
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    • pp.49-62
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    • 2005
  • Lake Paldang is a main resource of drinking water for 20 million people in the greater Seoul area. Dry deposition amounts of nitrogen and sulfur were estimated for three typical days in each season over the watershed of Lake Paldang. Models- 3/CMAQ (Community Multiscale Air Quality) and MM5 (Mesoscale Model) were used to predict air quality and meteorology, respectively. Aerosols as well as gaseous pollutants were considered. Nitrogen was mainly deposited in the form of HNO, while most of sulfur was deposited in the form of SO$_2$. Contribution of secondary pollutants was the largest in fall since they were transported from the greater Seoul area. However, contribution of secondarily-formed particulate pollutants to the nitrogen deposition was the largest in winter because semi-volatile ammonium nitrate favors lower temperature. Annual deposition amounts of nitrogen and sulfur were 37% and 26% of their emission amounts, respectively, over the watershed of Lake Paldang. Higher value of the nitrogen deposition showed a more influence of pollutants emitted in the greater Seoul area.

A Study on the Gust with Thunderstorm in Honam Area (호남지역에서 뇌우에 의한 돌풍사례 분석)

  • Cho, Eun-Hee
    • Journal of Integrative Natural Science
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    • v.2 no.2
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    • pp.101-130
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    • 2009
  • In recent years, South Korea has often witnessed damages by gusts caused by thunderstorms in summer. The Korea Meteorological Administration defines that a gust happens when the maximum instantaneous wind velocity is 10m/s or more and draws up hourly observation reports. When a cumulonimbus develops due to an ascending current and reaches the height of 12~16 km, the temperature of the cloud top drops and a lightening happens, which causes a gust accompanied by a thunderstorm and further regional meteorological damage. It's difficult to predict a regional gust with the mesoscale prediction model at the administration. Thus this study set out to analyze the damage cases by a gust accompanied by a thunderstorm and to make a contribution to the prediction and understanding of a gust by a thunderstorm. A gust by a thunderstorm happens where potential equivalent temperature converges or is higher than the surrounding areas. The convergence area of potential equivalent temperature matches the track of thunderstorm cells. The Kimje gust took place where high potential equivalent temperature converged, and the Jangsu gust did as the area of high potential equivalent temperature approached. There should be a good amount of vapor supply with the moisture flux converging at the bottom layer in order to bring instability. In addition, it should collide into a dry and cold atmosphere at 700 hPa. The moving track at the center of the low dew point spread corresponds to that of a gust.

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Study on Temporal and Spatial Variation of the Mesoscale Cold Core Eddy in the East China Sea Using IR and Ocean Color Remote Sensing (적외선 및 해색위성자료를 이용한 동중국해 중규모 와동류 변동 양상 연구)

  • 서영상;장이현;이나경;오현주;김상우;윤홍주;안유환
    • Proceedings of the Korean Association of Geographic Inforamtion Studies Conference
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    • 2004.03a
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    • pp.507-510
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    • 2004
  • 동중국해 북부에서 쿠로시오의 경계역으로 확장된 중국대륙 연안수가 주변의 북상 난류역에 의해 포획된 후 고립되는 현상이 1999년 및 2003년 NOAA 위성영상에 포착되었다. 1999년의 경우 cold core eddy는 약 2개월간 존재(5월초~6월 하순)하였고, cold core의 중심 수온은 15~20℃로 주변해역의 17~23℃보다 2~3℃ 낮게 나타났다. 1999년 5월 7일 획득된 SeaWiFS 위성자료로부터 추정된 클로로필 α 분포는 1999년 5월 6일부터 획득된 NOAA 위성수온 영상에 나타난 cold core eddy의 주변 가장자리 해역에서 비교적 높게 나타났다. 2003년 경우 2월 중순에 cold core의 수온은 9~10℃c였으며 직경 150km 정도였다. cold core의 수평규모는 50m 등수심 분포와 유사하게 나타났다. 이어도를 중심으로 동계 및 춘계에 나타나는 cold core eddy의 형성 메카니즘은 중국대륙 연안수와 쿠로시오 난류가 만나는 경계역에서의 힘의 균형과 계절풍 조건, 해저 지형 분포와 밀접한 관계성이 있는 것으로 사료된다.

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