• Title/Summary/Keyword: 대기과학

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Research and Policy Directions against Ambient Fine Particles (초미세먼지 문제 해결을 위한 연구 및 정책 방향)

  • Kim, Yong Pyo
    • Journal of Korean Society for Atmospheric Environment
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    • v.33 no.3
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    • pp.191-204
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    • 2017
  • Concerns on the air pollution problem caused by ambient fine particles have become a big social issue in Korea. Important factors that should be addressed to develop effective and efficient air quality management policy, especially, against fine particles are discussed and research and policy directions to address these factors are suggested. It is suggested that two factors are in high priority; one is scientific understanding of the major formation mechanisms of fine particles and the other is the process of policy decision and implementation. For the scientific understanding, smog chamber measurement, intensive field study, and chemical transport model development that can simulate the characteristics of Northeast Asia are considered to be important. For the policy directions, priority setting of the proposed policies and development and implement of effective communication sytem are considered to be important.

Characteristics of Long-term (2000~2020) Downslope Windstorm in the Yeongdong Region (영동지역 장기간(2000~2020년) 활강 강풍 특성)

  • Ji-Hoon Jeong;Byung-Gon Kim;Yu-jin Chae;Young-Gil Choi;Ji-Yoon Kim;Byung-Hwan Lim
    • Atmosphere
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    • v.33 no.1
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    • pp.21-32
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    • 2023
  • Characteristics of downslope windstorm (DW) has been examined mainly based on 1-min average wind and the other meteorological conditions in the Yeongdong region for 2000~2020. First, a classification procedure for the downslope windstorm is proposed using surface wind speed (greater than 99 percentile), 1-hour longevity of strong wind (SW), westerly wind direction, low humidity (less than 20 percentile), and leeside warming. The number of DW days satisfying the proposed criteria is 221 (2.9% of total days and 47.5% of SW days) while the number of SW days is 465 (6.1% of total days) for 2000~2020. The occurrences of both SW and DW shows distinctive annual variation with its peak in April. In addition, mean wind speed of DW days is 8.2 m s-1 with its duration of 2 hr 30 min and relative humidity of 28% at Gangneung. An episode (7 May 2021) was selected by applying the proposed criteria to SW days of 2021. The sounding shows that the layer of wind speed greater than 25 m s-1 was lowered down to 925 hPa at Gangneung (leeside) relative to 850 hPa at Hoengseong (Wonju), in the afternoon along with significant warming and drying. Froude numbers of Wonju and Gangneung for the DW events were increased 4 and 5 times greater than those of normal days, respectively. This kind of DW long-term statistics in the leeside of the mountains is thought to build a foundation of further understanding DW mechanism.

Understanding Physical Mechanism of 2022 European Heat Wave (2022년 발생한 기록적인 유럽 폭염 발생의 역학적 원인 규명 연구)

  • Ju Heon Kim;Gun-Hwan Yang;Hyun-Joon Sung;Jung Hyun Park;Eunkyo Seo
    • Atmosphere
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    • v.33 no.3
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    • pp.307-317
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    • 2023
  • This study investigates the physical mechanisms that contributed to the 2022 European record-breaking heatwave throughout May-August (MJJA). The European climate has experienced surface warming and drying in the recent decade (1979~2022) which influences the development of the 2022 European heatwave. Since its spatial pattern resembles the 2003 European heatwave which is a well-known case developed by the strong coupling of near-surface conditions to land surface processes, the 2022 heatwave is compared with the 2003 case. Understanding heatwave development is carried out by the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis version 5 (ERA5) and daily maximum surface temperature released by NCEP (National Centers for Environmental Prediction) CPC (Climate Prediction Center). The results suggest that the persistent high pressure along with clear sky tends to increase the downward shortwave radiation which leads to enhanced sensible heat flux with the land surface dryness. Terrestrial Coupling Index (TCI), a process-based multivariate metric, is employed to quantitatively measure segmented feedback processes, separately for the land, atmosphere, and two-legged couplings, which appears to the development of the 2022 heatwave, can be viewed as an expression of the recent trends, amplified by internal land-atmosphere interactions.

Calculations of the Single-Scattering Properties of Non-Spherical Ice Crystals: Toward Physically Consistent Cloud Microphysics and Radiation (비구형 빙정의 단일산란 특성 계산: 물리적으로 일관된 구름 미세물리와 복사를 향하여)

  • Um, Junshik;Jang, Seonghyeon;Kim, Jeonggyu;Park, Sungmin;Jung, Heejung;Han, Suji;Lee, Yunseo
    • Atmosphere
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    • v.31 no.1
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    • pp.113-141
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    • 2021
  • The impacts of ice clouds on the energy budget of the Earth and their representation in climate models have been identified as important and unsolved problems. Ice clouds consist almost exclusively of non-spherical ice crystals with various shapes and sizes. To determine the influences of ice clouds on solar and infrared radiation as required for remote sensing retrievals and numerical models, knowledge of scattering and microphysical properties of ice crystals is required. A conventional method for representing the radiative properties of ice clouds in satellite retrieval algorithms and numerical models is to combine measured microphysical properties of ice crystals from field campaigns and pre-calculated single-scattering libraries of different shapes and sizes of ice crystals, which depend heavily on microphysical and scattering properties of ice crystals. However, large discrepancies between theoretical calculations and observations of the radiative properties of ice clouds have been reported. Electron microscopy images of ice crystals grown in laboratories and captured by balloons show varying degrees of complex morphologies in sub-micron (e.g., surface roughness) and super-micron (e.g., inhomogeneous internal and external structures) scales that may cause these discrepancies. In this study, the current idealized models representing morphologies of ice crystals and the corresponding numerical methods (e.g., geometric optics, discrete dipole approximation, T-matrix, etc.) to calculate the single-scattering properties of ice crystals are reviewed. Current problems and difficulties in the calculations of the single-scattering properties of atmospheric ice crystals are addressed in terms of cloud microphysics. Future directions to develop physically consistent ice-crystal models are also discussed.

Uncertainty Evaluation of NOx Measurement in Ambient Air (환경대기 중 NOx 측정의 불확도 평가)

  • 임종명;이진홍;우진춘
    • Proceedings of the Korea Air Pollution Research Association Conference
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    • 2002.04a
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    • pp.141-142
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    • 2002
  • 대기환경 기준물질(criteria pollutants)은 NOx를 비롯하여 $O_3$, CO, SOx, PM 10, Pb 인데, 이러한 물질은 환경부에서 법적으로 규정한 대기오염공정 시험법에 따라서 분석된다. 대기오염공정 시험법이 충분한 과학적 근거를 갖는 분석법이 되기 위해서는 분석방법, 분석기기, 분석자 등에 의해 발생되는 불확실성을 최소화시키는 체계적인 관리가 필요하고, 분석기술의 발달수준, 측정분석의 요구수준, 새로운 국제 규격 통에 맞게 지속적으로 보완되어야 한다. (중략)

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Changes of approachs for the Safety Engineering (안전공학을 위한 접근방법론 -안전기술에서 안전공학까지-)

  • 강종권
    • Journal of the Korean Society of Safety
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    • v.1 no.1
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    • pp.65-70
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    • 1986
  • 첨단과학기술이란 말을 우리 주변에서도 흔히 듣게되며 하이테크시대란 용어도 심심치 않게 들을 수 있는 사회가 되었다. 그러나 그 첨단과학기술시스템을 안전하게 확보해 나가는 인간과 기계와 환경을 포함하는 안전공학의 시스템을 말하는 사람은 거의 없다. 안전을 대기에 비유하는 이도 있다. 마치 사람이 대기 속에서 아무 부자류를 느끼지 못하고 지낼 때는대기(산소)의 고마움을 자칫 잊어 버릴 수도 있는 것과 같이 안전이 잘 유지되고 있을 때는 그 가치를 자칫 과소평가할 수도 있기 때문이다.

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Analysis of Differences of Explanation on Gas Pressure and Atmospheric Pressure in Science Textbooks (과학 교과서에서 기압과 대기압에 대한 설명 방식의 차이점 분석)

  • Paik, Seoung-Hey;Song, Ju-Hyun
    • Journal of The Korean Association For Science Education
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    • v.22 no.2
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    • pp.240-251
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    • 2002
  • In this study, we analyzed differences of explanation on gas pressure and atmospheric pressure in elementary and secondary school science textbooks and general chemistry and general earth science textbooks based on three types of explanation criteria: first, explanation of mass; second, explanation of air pressure on unit area; third. explanation of molecular motion. The results were as follows. Elementary science textbook belonged to the first type. All of the secondary school chemistry textbooks belonged to the third type. But most of the general chemistry textbooks belonged to the first and second type. Most of the earth science textbooks for secondary school and most of the general earth science textbooks belonged to the first type. Therefore, the differences of explanation could disturb students' understanding on gas pressure and atmospheric pressure.

The Estimation of Arctic Air Temperature in Summer Based on Machine Learning Approaches Using IABP Buoy and AMSR2 Satellite Data (기계학습 기반의 IABP 부이 자료와 AMSR2 위성영상을 이용한 여름철 북극 대기 온도 추정)

  • Han, Daehyeon;Kim, Young Jun;Im, Jungho;Lee, Sanggyun;Lee, Yeonsu;Kim, Hyun-cheol
    • Korean Journal of Remote Sensing
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    • v.34 no.6_2
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    • pp.1261-1272
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    • 2018
  • It is important to measure the Arctic surface air temperature because it plays a key-role in the exchange of energy between the ocean, sea ice, and the atmosphere. Although in-situ observations provide accurate measurements of air temperature, they are spatially limited to show the distribution of Arctic surface air temperature. In this study, we proposed machine learning-based models to estimate the Arctic surface air temperature in summer based on buoy data and Advanced Microwave Scanning Radiometer 2 (AMSR2)satellite data. Two machine learning approaches-random forest (RF) and support vector machine (SVM)-were used to estimate the air temperature twice a day according to AMSR2 observation time. Both RF and SVM showed $R^2$ of 0.84-0.88 and RMSE of $1.31-1.53^{\circ}C$. The results were compared to the surface air temperature and spatial distribution of the ERA-Interim reanalysis data from the European Center for Medium-Range Weather Forecasts (ECMWF). They tended to underestimate the Barents Sea, the Kara Sea, and the Baffin Bay region where no IABP buoy observations exist. This study showed both possibility and limitations of the empirical estimation of Arctic surface temperature using AMSR2 data.