• Title/Summary/Keyword: METRI

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Predictability of the Seasonal Simulation by the METRI 3-month Prediction System (기상연구소 3개월 예측시스템의 예측성 평가)

  • Byun, Young-Hwa;Song, Jee-Hye;Park, Suhee;Lim, Han-Chul
    • Atmosphere
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    • v.17 no.1
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    • pp.27-44
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    • 2007
  • The purpose of this study is to investigate predictability of the seasonal simulation by the METRI (Meteorological Research Institute) AGCM (Atmospheric General Circulation Model), which is a long-term prediction model for the METRI 3-month prediction system. We examine the performance skill of climate simulation and predictability by the analysis of variance of the METRI AGCM, focusing on the precipitation, 850 hPa temperature, and 500 hPa geopotential height. According to the result, the METRI AGCM shows systematic errors with seasonal march, and represents large errors over the equatorial region, compared to the observation. Also, the response of the METRI AGCM by the variation of the sea surface temperature is obvious for the wintertime and springtime. However, the METRI AGCM does not show the significant ENSO-related signal in autumn. In case of prediction over the east Asian region, errors between the prediction results and the observation are not quite large with the lead-time. However, in the predictability assessment using the analysis of variance method, longer lead-time makes the prediction better, and the predictability becomes better in the springtime.

Features on the Vertical Size Distribution of Aerosols using Ballon-borne Optical Particle Counter at Anmyeon (광학입자계수기를 이용한 안면도 연직 에어러솔 수농도 크기 분포 특성)

  • Choi, B.C.;Iwasaka, Y.;Lim, J.C.;Jeong, S.B.;Kim, Y.S.;Dmitri, T.;Nagatani, T.;Yamada, M.;Kim, S.B.;Hong, G.M.;Lee, Y.G.;Yoo, H.J.
    • Atmosphere
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    • v.15 no.3
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    • pp.149-153
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    • 2005
  • A balloon-borne Optical Particle Counter (hereafter "OPC Sonde"), which was developed by the atmospheric research group of Nagoya University, is used for getting the information of vertical profile of particle size and concentration in Anmyeon ($36^{\circ}32^{\prime}N$ $126^{\circ}19^{\prime}E$) on 18 March 2005. A range of five different particle sizes is shown in the vertical profile of aerosol number density estimated from the OPC Sonde. It was found that small size particles have vertically larger aerosol number density than relatively big ones. For all size ranges the vertical aerosol number density shows a decreased pattern as the altitude becomes higher. The aerosol number density of $0.3{\sim}0.5{\mu}m$, $0.5{\sim}0.8{\mu}m$, $0.8{\sim}1.2{\mu}m$ size ranges at the 10km height, which is the tropopause approximately, are $1,000,000ea/m^3$, $100,000ea/m^3$, $10,000ea/m^3$ respectively. The data of OPC Sonde are also compared with the data of PM10 $\beta$-ray) and Micro Pulse Lidar which are operating at Korea Global Atmosphere Watch Observatory in Anmyeon.

2007 Ambient noise levels study about new and moving seismic stations at KMA (2007년도 기상청 신설 및 이전 지진관측소의 배경잡음 특성 연구)

  • Jeon, Young-Soo;Nam, Sung-Tae;Sheen, Dong-Hoon;Cho, Beom-Jun
    • 한국지구물리탐사학회:학술대회논문집
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    • 2007.06a
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    • pp.163-166
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    • 2007
  • KMA established short period seismometer, accelerometer, and ocean bottom seismometer network to build the detail earthquake monitoring system and Tsunami monitoring system. KMA also replaced borehole seismometer and wave height meter monitoring system. The purposes of this study are to record the ambient seismic noise levels of short period seismometer and accelerometer installed in 2006 and 2007, and compare their characteristics to present the standard of site selection criteria.

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Characteristics on the Variations of the Total Ozone over Pohang (1994-2004) using the Brewer Spectrophotometer and TOMS

  • Hong Gi-Man;Choi Byoung-Cheol;Goo Tae-Young;Lim Jae-Chul;Lim Byung-Sook;Baek Moon-Hee
    • Proceedings of the KSRS Conference
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    • 2005.10a
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    • pp.388-391
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    • 2005
  • The characteristics of the total ozone variations measured by the ground-based Brewer Ozone Spectrophotometer and the Total Ozone Mapping Spectrometer (TOMS) over Pohang are statistically examined from January 1994 to December 2004. First of all, in the correlation analysis of the total ozone measured from the Brewer Ozone Spectrophotometer and the TOMS, the correlation coefficient was 0.88 and the used data were 2190. The annual mean value of the total ozone is 311 DU with the standard deviation of 13 DU. The maximum and the minimum value were found in March (343 DU) and in September (282 DU), respectively. It was also revealed that the longest seasonal variation is in Spring (341 DU) and the smallest is in Autumn (283 DU). The time series data of the total ozone indicates that the annual variation is significant and the variations for three months and six months are relatively weak. Finally, the annual mean total ozones in Pohang (Brewer), Seoul (Brewer) and Busan (TOMS) are 312 DU, 324 DU and 304 DU, respectively.

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Aerosol Optical and Spectral Characteristics in Yellow Sand Events on April, 1998 in Seoul. Part I: Observation (분광복사계와 일사계 관측에 의한 황사 및 에어러솔의 광학적 특성 연구)

  • Hye-Sook Park;Hyo-Sang Chung;Gyun-Myeong Bag;Hong-Ju Yoon
    • Korean Journal of Remote Sensing
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    • v.14 no.3
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    • pp.307-314
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    • 1998
  • To examine the detectability of the yellow sand and/or aerosol from China crossing over the Yellow Sea within the range of OSMI wavelengths(400-900 nm), we have investigated the optical characteristics of aerosols in yellow sand events observed on April, 1998 in Seoul. The spectral reflectance(%) and aerosol optical thickness in the range of Visible(VIS) and near Infrared (NIR) wavelengths were derived from the measurements of solar radiation using the GER-2600 spectroradiometer and sunphotometer during the April, 1798. The average spectral reflectance for the yellow sand events is over 40% and higher around 14:30 than 12:00 LST, but that for clear days is about 20% both at 12:00 and 14:30 LST in the range of 500-900 nm. The aerosol optical thickness at 501 nm varied from 0.25 on very clear day to 1.01 during a so-called "yellow-sand" episode and that for 673 nm varied from 0.14 to 0.92, respectively.