The main activities of the Applied Meteorology Research Laboratory(AMRL) are to carry out the researches for biometeorology, urban climatology, Asian dust and air pollution meteorology with the close relationship to human for well-being life.
a
Micrometeorology and urban climatology
Air pollutants physiochemistry
Hwangsa (Asian dust) and air pollution meteorology
Industrial and traffic- aviation meteorology
Agriculture meteorology and public weather services
Human biometeorology
Meteorology impact assessment
Monitoring and analysis of meteorology and air pollutants at Gosan station in Jeju island
Development of the techniques on the Asian dust monitoring and prediction
Monitoring and prediction of urban climate meteorology
Research on human biometeorology
The source region of ¡°Hwangsa¡±
Hwangsa(Asian dust) that affects the Korean peninsula occur most frequently in the spring season, and originate in the arid and semi-arid regions of sand deserts, including Badainjaran, Tengger, Mu Us, Hunsandakue, and Keoeolchin, gobi regien and loess regions of the Asian continent. The origins of Hwangsa include most of Mongolia and northern China. The southeastward moving low-pressure systems accompained with the cold fronts and disseminate the dust into the atmosphere, often resulting in a visibility reduction of less than 1 km.



Dust storm monitoring towers at (a) Duolun, (b) Yulin, and (c) Zhangye in the source region

Simulation of Hwangsa phenomenon in Korea
The operational meteorological model of Regional Data Assimilation and Prediction System(RDAPS) and the operational aerosol model(S. U. Park, 2002) are used to forecast dust phenomena. The Model results are compared with the monitored PM10 concentration in China and Korea. .

Heat-related morbidity and mortality
Interest in the impact of weather on human health has increased dramatically in recent years, especially in light of future climate changes. In particular, it is evident that hot weather contributes to increased morbidity and mortality in large urban areas (e.g., Philadelphia in 1993, Shanghai in 1998, Paris in 2003, and so on). The heat watch/warning systems based on the digital output from numerical weather prediction (NWP) model of the Korea Meteorological Administration (KMA) have been constructed. The figure shows daily mortality at Seoul as a function of daily maximum temperature during the recent 14 years (1991 to 2004). In abnormal hot summer of 1994 and 2004, daily mortality exponentially increased with maximum temperature.



Construction of human well-being bioclimate map
In order to more fully understand the effects of atmospheric conditions on human health, well-being and performance, it is necessary to transform the primary meteorological information so that it becomes biologically and medically relevant. Perceived Temperature or PT compares the actually existing outside conditions with the temperature that would prevail in a standard environment in order to experience an identical feeling of warmth, comport or cold. The figure shows mean frequency of thermal (heat stress as red circles and cold stress as blue circles in the day number a year) stress for the major cities in South Korea from 1983 to 2004. Geographical distribution of thermally comfortable zone in South Korea will be finally constructed in the biometeorology project in KMA/METRI.

Monitoring of urban climate
The intensive observation in the urban area was performed to investigate the urban meteorological characteristics such as urban thermal environment, urban hydrology, urban wind road. Especially, long-term meteorological monitoring system in the Cheonggye stream area was used to evaluate quantitatively the land-use change effects of before and after Cheonggye stream restoration on the urban meteorology.



Monitoring of urban climate change in Cheonggye stream



Distribution of the net radiation and sensible heat in the Cheonggye stream in 2003 and 2005

Prediction of urban flow
dynamics (CFD) model coupled to a mesoscale model (MM5).



Three characteristics flow regimes (a) channeling flow, (b) double-eddy circulation, and (c) recirculation zone.