하절기 도시의 지역별 장·단파복사 특성 분석과 해석
Analysis of Radiative Characteristics at Urban Area by Observation in Summer Season
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참고문헌
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초록
Theobjectiveofthisstudyistoanalyzethecharacteristicofradiationenvironmentintheurbanandrural throughthefieldobservationinthesummer.Theradiationbalancewascomparedthroughthemeasurementof theshortwaveradiationandlong-waveradiationintheurban,sub-urban,andrural.Thefollowingconclusion couldbeobtainedfrom thisresearch.(1)Intheresultsofobservationincludingtherain-day,itwasfoundthat theshortwaveradianceintheurbanislowerabout10% thantherural.(2)Theupperpartofatmospherelayers intheurbanareaabsorbmuchshortwaveradiationenergiescomparedwiththeruralrelatively.Itcanincrease thetemperatureoftheupperpartofatmospherelayersandtheemittanceoflongwaveradiation.(3)Theratio ofthedownwardshortwaveradiationtothedownwardlongwaveradiationwas1.24fortheurban,1.28for sub-urbanand1.35forrural.Itcanbeestimatedthattheatmosphereconditionoftheruralisbetterthanthat ofotherareas.(4)Thenetradiationoftheruralwaslowerthatoftheurban.Itwasfoundthattheenergyin andoutflow oftheruraliseasierthanthatoftheurban.(5)Thetemperaturevariationforthelong-waveradiation changeoftheruralshowedmoresensitivethanthatoftheurban.Itwascamefrom theradiationcharacteristics ofthesurrounding environmentandcanbeusedastheimportantindex toevaluatethethermalenvironment characteristicofurban.
Abstract
Theobjectiveofthisstudyistoanalyzethecharacteristicofradiationenvironmentintheurbanandrural throughthefieldobservationinthesummer.Theradiationbalancewascomparedthroughthemeasurementof theshortwaveradiationandlong-waveradiationintheurban,sub-urban,andrural.Thefollowingconclusion couldbeobtainedfrom thisresearch.(1)Intheresultsofobservationincludingtherain-day,itwasfoundthat theshortwaveradianceintheurbanislowerabout10% thantherural.(2)Theupperpartofatmospherelayers intheurbanareaabsorbmuchshortwaveradiationenergiescomparedwiththeruralrelatively.Itcanincrease thetemperatureoftheupperpartofatmospherelayersandtheemittanceoflongwaveradiation.(3)Theratio ofthedownwardshortwaveradiationtothedownwardlongwaveradiationwas1.24fortheurban,1.28for sub-urbanand1.35forrural.Itcanbeestimatedthattheatmosphereconditionoftheruralisbetterthanthat ofotherareas.(4)Thenetradiationoftheruralwaslowerthatoftheurban.Itwasfoundthattheenergyin andoutflow oftheruraliseasierthanthatoftheurban.(5)Thetemperaturevariationforthelong-waveradiation changeoftheruralshowedmoresensitivethanthatoftheurban.Itwascamefrom theradiationcharacteristics ofthesurrounding environmentandcanbeusedastheimportantindex toevaluatethethermalenvironment characteristicofurban.
참고문헌 (6)
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- MariaKolokotroni, "Urban heatisland intensity in London: Aninvestigationoftheimpactofphysical characteristicsonchangesinoutdoorair temperatureduringsummer", ScienceDirect Solar Energy, 82(11), pp.986~998 (2008)
- YinkaR, "Aspectsofthevariation insomecharacteristicsofradiationbudget within the urban canopy of Ibadan", Atmosphere Environment, 24(1), pp.9~17 (1990)
- 최동호, "하절기 실험을 통한 건물녹화용 피복재료의 복사수지 해석", 한국태양에너지학회 논문집, 30(3), pp.71~80 (2010), 한국태양에너지학회
- 최동호, "하절기 복사환경 관측을 통한 석재, 목재, 알루미늄 바닥재의 열특성 평가", 한국태양에너지학회 논문집, 28(3), pp.35~44 (2008), 한국태양에너지학회
- 류남형, "투·보수성 시멘트 콘크리트 포장의 열환경 특성(Ⅰ)", 한국조경학회지, 32(6), pp.82~94 (2005), 한국조경학회
