• 제목/요약/키워드: KMA

검색결과 818건 처리시간 0.033초

PARK Formula Can Replace "Guide to Medical Certificate" Published by Korean Medical Association in Deciding the Treatment Duration

  • Park, Chan Yong;Yeo, Kwang Hee;Ahn, Sora
    • Journal of Trauma and Injury
    • /
    • 제31권2호
    • /
    • pp.58-65
    • /
    • 2018
  • Purpose: Many doctors have difficulty in deciding the treatment duration in trauma patients to write in the casualty medical certificate. We tried to find a solution for this problem by using abbreviated injury scale (AIS). Methods: A total of 39 patients treated in our regional trauma center who requested an author to write treatment duration on casualty medical certificate from January 2014 to April 2017 were included. And the treatment duration was decided based on the PARK Formula (AIS). PARK Formula $(AIS)=(AIS{\times}2){\sim}([AIS{\times}2]+2)$ Results: Among 39 patients included and 36 (92.3%) had treatment duration on casualty medical certificate within the range of treatment duration calculated by PARK Formula (AIS). Compared to the PARK Formula (AIS), the mean value was 0.13 week (0.90 day) smaller. Comparing the treatment duration between Korean Medical Association (KMA) guideline and PARK Formula (AIS), only 22 patients (56.4%) showed agreement. The mean value was 1.02 week (7.18 days) smaller in KMA guideline. Conclusions: For the decision of the treatment duration in trauma patients, utilizing worldwide used AIS scoring system is very efficient. Using PARK Formula (AIS), doctors can document the treatment duration in the casualty medical certificate with ease. KMA should provide more practical 'treatment duration of each diagnosis in writing casualty medial certificate' for the doctors. We recommend PARK Formula (AIS) as a good alternative for KMA guide.

AOGCM에 의해 모의된 동아시아지역의 강수 연변동성에 대한 불확실성 평가 (An Uncertainty Assessment for Annual Variability of Precipitation Simulated by AOGCMs Over East Asia)

  • 신진호;이효신;김민지;권원태
    • 대기
    • /
    • 제20권2호
    • /
    • pp.111-130
    • /
    • 2010
  • An uncertainty assessment for precipitation datasets simulated by Atmosphere-Ocean Coupled General Circulation Model (AOGCM) is conducted to provide reliable climate scenario over East Asia. Most of results overestimate precipitation compared to the observational data (wet bias) in spring-fall-winter, while they underestimate precipitation (dry bias) in summer in East Asia. Higher spatial resolution model shows better performances in simulation of precipitation. To assess the uncertainty of spatiotemporal precipitation in East Asia, the cyclostationary empirical orthogonal function (CSEOF) analysis is applied. An annual cycle of precipitation obtained from the CSEOF analysis accounts for the biggest variability in its total variability. A comparison between annual cycles of observed and modeled precipitation anomalies shows distinct differences: 1) positive precipitation anomalies of the multi-model ensemble (MME) for 20 models (thereafter MME20) in summer locate toward the north compared to the observational data so that it cannot explain summer monsoon rainfalls across Korea and Japan. 2) The onset of summer monsoon in MME20 in Korean peninsula starts earlier than observed one. These differences show the uncertainty of modeled precipitation. Also the comparison provides the criteria of annual cycle and correlation between modeled and observational data which helps to select best models and generate a new MME, which is better than the MME20. The spatiotemporal deviation of precipitation is significantly associated with lower-level circulations. In particular, lower-level moisture transports from the warm pool of the western Pacific and corresponding moisture convergence significantly are strongly associated with summer rainfalls. These lower-level circulations physically consistent with precipitation give insight into description of the reason in the monsoon of East Asia why behaviors of individually modeled precipitation differ from that of observation.

한반도 지진의 지속규모식에 관한 연구 (Duration Magnitude and Local-Duration Magnitude Relations for Earth-quakes of 1979-1998 Recorded at KMA Network)

  • 박삼근
    • 한국지진공학회:학술대회논문집
    • /
    • 한국지진공학회 1998년도 추계 학술발표회 논문집 Proceedings of EESK Conference-Spring 1998
    • /
    • pp.421-435
    • /
    • 1998
  • An empirical formula for estimating duration magnitude(MD)is determined by analyzing 619 epicentral distance-duration data set, obtained from earthquakes of 1989-1998 recorded at the KMA network. Based on two assumptions: 1) observed signal duration decreases with increasing epicentral distance, and 2) seismographs of KMA are set at low-gain and therefore inclusion of sensitivity correction term in the equation is not necessary, scaling predicted duration at epicenter to Tsuboi's local magnitude yielded the duration magnitude equation: MD =2.0292$\times$log$\tau$+0.00123Δ-1.4017 for 1/0$\leq$ML$\leq$5.0, where $\tau$is total signal duration(sec)and Δis epicentral distance(km). Event by event comparison of ML values against MD estimates for t152 events shows that for events having a same ML the difference in MD estimates reaches as high as 1.1 magnitude units. So, to test the usefulness of the duration magnitude equation, we have calculated ML-MD relations by which duration magnitude estimates are converted to local magnitudes ("predicted" ML, say) which are then compared with the directly determined local magnitude values. Except for events with stations where duration is anomalously reestimates(predicted ML) which are in an agreement within a 0.2 magnitude units with the corresponding ML values. Although this study could gain some insights into magnitudes of the past events, we still need to re-examine all the observables in order to obtain more reliable and precise information about magnitude and hypocenter location. So we will pursue a new local-magnitude scaling, as well as refinement of the duration magnitude equation, starting soon with re-reading the amplitudes-arrival time records of (and hence relocating) 250+earthquakes of 1979-present recorded at the KMA network. Thus, with more reliable and precise earthquake parameters determined we would better understand the recent seismicity and related tectonic process within and adjacent region to the Korean peninsula.peninsula.

  • PDF

파형 변환.합성을 이용해서 한반도 주변 해역 지진 분석을 위한 신속 정확한 분석 기술 (Fast and Accurate Analyzing Technology for Earthquakes in the Seas around the Korean Peninsula Using Waveform Format Conversion and Composition)

  • 김소구;박상표
    • 지질공학
    • /
    • 제16권2호
    • /
    • pp.171-178
    • /
    • 2006
  • 현재 한국의 지진 관측은 1905년도에 시작된 이후로 계속적인 지진 관측망 확충과 새로운 장비의 도입으로 선진국 못지않은 장비를 보유하고 있지만, 지진의 관측과 분석에 있어서는 그 수준이 미흡한 것이 실이다. 특히, 동해안 지진원인자 분석에 있어서 시간이 많이 소요되기 때문에 지진 정보나 지진 해일 경보를 발령하는데 어려움이 있다. 이번 연구에서는 일본에서 사용하는 지진 관측망(JMA), 한국 지진 관측망(KMA), 그리고 국제 관측망(IRIS) 지진 관측소의 파형 포맷을 하나의 공통 파형 포맷으로 변환 합성하고 공유 분석 프로그램인 FESNET(극동 지진 관측망 분석 체계)를 구축하여 2004년 5월 29일과 6월 1일에 발생한 울진 지진과, 2005년 3월 20일에 발생한 일본 후쿠오카 지진의 분석에 응용하였다. 분석결과 어느 한쪽 관측망(KMA, JMA)을 사용하는 것보다 이들 모든 관측망을 활용하는 FESNET을 이용할 때 더 좋은 결과를 얻을 수 있다는 것을 말 수 있다.

적설 관측자료 비교를 통한 정량적 SWE 산출에 관한 연구 (A Study of Quantitative Snow Water Equivalent (SWE) Estimation by Comparing the Snow Measurement Data)

  • 노용훈;장기호;차주완;정건희;최지원;하종철
    • 대기
    • /
    • 제29권3호
    • /
    • pp.269-282
    • /
    • 2019
  • While it is important to obtain the accurate information on snowfall data due to the increase in damage caused by the heavy snowfall in the winter season, it is not easy to observe the snowfall quantitatively. Recently, snow measurements using a weighing precipitation gauge have been carried out, but there is a problem that high snowfall intensity results in low accuracy. Also, the observed snowfall data are sensitive depending on wind speed, temperature, and humidity. In this study, a new process of quality control for snow water equivalent (SWE) data of the weighing precipitation gauge were proposed to cover the low accuracy of snow data and maximize the data utilization. Snowfall data (SWE) observed by Pluvio, Parsivel, snow-depth meter using laser or ultrasonic, and rainfall gauge in Cloud Physics Observation Site (CPOS) were compared and analyzed. Applying the QC algorithm including the use of number of hydrometeor particles as reference, the increased SWE per the unit time was determined and the data noise was removed and marked by flag. The SWE data converted by the number concentration of hydrometeor particles are tested as a method to restore the QC-removed data, and show good agreement with those of the weighing precipitation gauge, though requiring more case studies. The three events data for heavy snowfall disaster in Pyeongchang area was analyzed. The SWE data with improved quality was showed a good correlation with the eye-measured data ($R^2$ > 0.73).

조선 후기 석제 앙부일구 분석 (ANALYSIS OF ANGBU-ILGU, A STONE MATERIAL IN THE LATE JOSEON DYNASTY)

  • 김상혁;민병희;김재영
    • 천문학논총
    • /
    • 제37권3호
    • /
    • pp.35-47
    • /
    • 2022
  • This study investigated the stone Angbu-ilgu (scaphe sundial) of the Korea Meteorological Administration (KMA) and the Seoul Museum of History (SMH). Since the first Angbu-ilgu was produced in Korea in 1434 (the year of the reign of King Sejong), Angbu-ilgu has been reproduced with various materials. The upper surface of these two stone Angbu-ilgus symbolizes the horizon. On the hemisphere concave at the center of the horizon, the South Pole, the time line, and the season line are engraved. On the horizon of both the KMA and SMH Angbu-ilgus, the schematic, typeface, and composition of the inscription completely coincide with each other. In this study, it was estimated that the appearance of the KMA Angbu-ilgu, which was damaged at some point previously at least once, was similar to that of the SMH Angbu-ilgu, and this means that it is superficially similar with Treasure No 840, the stone horizontal sundial. In the concave hemisphere of both the stone Angbu-ilgus of the KMA and SMH, there are hour lines and 24 solar-term lines (13 line), and there is an intersection point where these lines meet the horizon, respectively. It can be verified that these intersections of these two Angbu-ilgus can be calculated as having a latitude of +37°39'15". The hour lines of the two stone Angbu-ilgus show that they were made after about 1900.

국립기상과학원 Argo 사업의 현황 및 추진 방향 (Current Status and Future Direction of the NIMS/KMA Argo Program)

  • 김백조;조형준;강기룡;이철규
    • 대기
    • /
    • 제33권5호
    • /
    • pp.561-570
    • /
    • 2023
  • In order to improve the predictability of marine high-impacts weather such as typhoon and high waves, the marine observation network is an essential because it could be rapidly changed by strong air-sea interaction. In this regard, the National Institute of Meteorological Sciences, Korea Meteorological Administration (NIMS/KMA) has promoted the Argo float observation program since 2001 to participate in the International Argo program. In this study, current status and future direction of the NIMS/KMA Argo program are presented through the internal meeting and external expert forum. To date, a total of 264 Argo floats have been deployed into the offshore around the Korean Peninsula and the Northwestern Pacific Ocean. The real-time and delayed modes quality control (QC) system of Argo data was developed, and an official regional data assembling center (call-sign 'KM') was run. In 2002, the Argo homepage was established for the systematic management and dissemination of Argo data for domestic and international users. The future goal of the NIMS/KMA Argo program is to improve response to the marine high-impacts weather through a marine environment monitoring and observing system. The promotion strategy for this is divided into four areas: strengthening policy communication, developing observation strategies, promoting utilization research, and activating international cooperation.

2010년 여름철 수도권 집중관측기간에 나타난 호우 시스템의 대기연직구조 (Atmospheric Vertical Structure of Heavy Rainfall System during the 2010 Summer Intensive Observation Period over Seoul Metropolitan Area)

  • 김도우;김연희;김기훈;신승숙;김동균;황윤정;박종임;최다영;이용희
    • 한국지구과학회지
    • /
    • 제33권2호
    • /
    • pp.148-161
    • /
    • 2012
  • 2010년 8월 13일부터 9월 3일까지 수도권지역에서 집중관측(Predictability and Observation Experiment of Korea-2010, ProbeX-2010)이 수행되었으며, 그 일환으로 동두천, 인천공항, 양평에서 6시간 간격으로 라디오존데 관측이 실행되었다. 관측기간 동안 우리나라의 전형적인 호우 패턴인 스콜선형, 정체전선형, 태풍 전면 수렴형, 열대저압부형, 태풍 직접형 호우가 연속적으로 발생하였다. 8월 15일 03 KST 경에는 스콜선형 구름대가 수도권 지역에서 발달하였다. 따뜻하고 습한 하층 공기 위로 건조한 중층 공기가 유입되어 강한 대류 불안정이 형성되었으며 이로 인해 호우가 발생하였다. 8월 23일부터 26일, 8월 27일부터 29일은 각각 정체전선과 태풍 전면 수렴대의 영향을 받아 강우가 발생하였다. 정체전선형 강우 초기에는 열적 불안정이 우세하게 나타났으나 강우 후기에는 역학적 불안정이 강화되었다. 이 기간 중 특히 강한 강수는 서해상에서 남풍류 하층 제트가 발달한 8월 25일에 발생하였다. 태풍 전면 수렴형 강우기간에는 열적 불안정과 역학적 불안정이 모두 유지되는 특징을 보였다. 이 기간 중 특히 강한 강수는 높은 상당온위(>345 K)를 가진 열대 공기가 대기 중하층에 거쳐 유입되었을 때 발생하였다. 8월 27일과 9월 2일에는 각각 열대저압부와 태풍 곤파스의 영향에 의해 강우가 발생하였다. 이 사례들 동안에는 역학적 불안정이 매우 강하게 발달하였다.

국내 인프라사운드 전파특성 연구 (Infrasound Wave Propagation Characteristics in Korea)

  • 제일영
    • 한국지진공학회:학술대회논문집
    • /
    • 한국지진공학회 2000년도 춘계 학술발표회 논문집 Proceedings of EESK Conference-Spring
    • /
    • pp.63-69
    • /
    • 2000
  • Korea Institute of Geology Mining and Materials(KIGAM) cooperating with Southern Methodist University(SMU) has been operating seismo-acoustic array in Chul-Won area to discriminate man-made explosions from natural earthquakes since at the end of July 1999. In order to characterize propagation parameters of detected seismo-acoustic signal and to associate these signals as a blast event accompanying seismic and acoustic signals simultaneously it is necessary to understand infrasound wave propagation in the atmosphere. Two comparable Effective Sound Velocity Structures(ESVS) in atmosphere were constructed by using empirical model (MSISE90 and HWM93) and by aerological observation data of Korea Meteorological Administration (KMA) at O-San area. Infrasound propagation path computed by empirical model resulted in rare arival of refracted waves on ground less than 200km from source region. On the other hand Propagation paths by KMA more realistic data had various arrivals at near source region and well agreement with analyzed seismo-acoustic signals from Chul-Won data. And infrasound propagation in specific direction was very influenced by horizontal wind component in that direction. Linear travel time curve drawn up by 9 days data of the KMA in autumn season showed 335.6m/s apparent sound velocity in near source region. The propagation characteristics will be used to associate seismo-acoustic signals and to calculate propagation parameters of infrasound wave front.

  • PDF

이동격자태풍모델을 이용한 2006년 태풍의 진로 및 강도 예측성능 평가 (Performance of MTM in 2006 Typhoon Forecast)

  • 김주혜;추교명;김백조;원성희;권혁조
    • 대기
    • /
    • 제17권2호
    • /
    • pp.207-216
    • /
    • 2007
  • The Moving-nest Typhoon Model (MTM) was installed on the Korea Meteorological Administration (KMA)'s CRAY X1E in 2006 and started its test operation in August 2006 to provide track and intensity forecasts of tropical cyclones. In this study, feasibility of the MTM forecast is compared with the Global Data Assimilation and Prediction System (GDAPS) of the KMA and the operational typhoon forecast models in the Japan Meteorological Agency (JMA), from the sixth tropical cyclone to the twentieth in 2006. Forecast skills in terms of the storm position error of the two KMA models were comparable, but MTM showed a slightly better ability. While both GDAPS and MTM produced larger errors than JMA models in track forecast, the predicted intensity was much improved by MTM, making it comparable to the JMA's typhoon forecast model. It is believed that the Geophysical Fluid Dynamics Laboratory (GFDL) bogus initialization method in MTM improves the ability to forecast typhoon intensity.