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      레이저-옵티컬 디스드로미터를 활용한 대전지역의 강우에너지 특성 평가 = Evaluation of Kinetic Energy of Raindrops at Daejeon city using Laser-optical Disdrometer

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      https://www.riss.kr/link?id=A60128668

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      다국어 초록 (Multilingual Abstract)

      To evaluate the kinetic energy of the raindrops, the drop size distribution and the terminal velocity of the raindrops had been measured from January to September 2010 using the laser-optical disdrometer in KIGAM, Daejeon, Korea. The relationship between kinetic energy (KE) and rainfall intensity (I) was computed as logarithmic and exponential model, respectively, under the rainfall intensity of about 142mm/h. The exponential model is more suitable for the relationship of KE-I than the logarithmic model, because the exponential model presented better fit for KE over 50mm/h of rainfall intensity. Meanwhile, the differences of the total kinetic energy existed in rainfall events with almost same total rainfall depth, and KE values of Daejeon at high rainfall intensity underestimated rather than the others under temperate climate. Therefore, these differences of KE in rainfall events and geographical regions imply the result from the variations of rainfall intensity within a rainfall event.
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      To evaluate the kinetic energy of the raindrops, the drop size distribution and the terminal velocity of the raindrops had been measured from January to September 2010 using the laser-optical disdrometer in KIGAM, Daejeon, Korea. The relationship betw...

      To evaluate the kinetic energy of the raindrops, the drop size distribution and the terminal velocity of the raindrops had been measured from January to September 2010 using the laser-optical disdrometer in KIGAM, Daejeon, Korea. The relationship between kinetic energy (KE) and rainfall intensity (I) was computed as logarithmic and exponential model, respectively, under the rainfall intensity of about 142mm/h. The exponential model is more suitable for the relationship of KE-I than the logarithmic model, because the exponential model presented better fit for KE over 50mm/h of rainfall intensity. Meanwhile, the differences of the total kinetic energy existed in rainfall events with almost same total rainfall depth, and KE values of Daejeon at high rainfall intensity underestimated rather than the others under temperate climate. Therefore, these differences of KE in rainfall events and geographical regions imply the result from the variations of rainfall intensity within a rainfall event.

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      참고문헌 (Reference)

      1 이민부, "임진강유역의 토지이용에 따른 지표침식에 관한 연구" 대한지리학회 43 (43): 263-275, 2008

      2 이민부, "북한 회령지역의 농경지 변화에 따른 토양침식 추정" 한국지역지리학회 9 (9): 373-384, 2003

      3 기상청, "기상연보"

      4 정영상, "강원도 경사지 토양 유실 예측용 신USLE의 적용을 위한 강수 인자와 토양 침식성 인자의 검토" 32 (32): 31-38, 1999

      5 김진관, "강우입자의 물리적 특성평가: 경기도 안성시 지역을 사례로" 한국지형학회 17 (17): 49-57, 2010

      6 Miura, S, "Transport rates of surface materials on steep forested slopes induced by raindrop splash erosion" 7 : 201-211, 2002

      7 Neal., J. H, "The effect of degree of slope and rainfall characteristics on runoff and soil erosion" 280 : 1938

      8 Morgan, R. P. C, "The European Soil Erosion Model (EUROSEM): a dynamic approach for predicting sediment transport from fields and small catchments" 23 : 527-544, 1998

      9 Brown, L. C, "Storm erosivity using idealized intensity distributions" 30 : 379-386, 1987

      10 Morgan, R. P. C., "Soil erosion and conservation (Second edition)" Longman Group 1995

      1 이민부, "임진강유역의 토지이용에 따른 지표침식에 관한 연구" 대한지리학회 43 (43): 263-275, 2008

      2 이민부, "북한 회령지역의 농경지 변화에 따른 토양침식 추정" 한국지역지리학회 9 (9): 373-384, 2003

      3 기상청, "기상연보"

      4 정영상, "강원도 경사지 토양 유실 예측용 신USLE의 적용을 위한 강수 인자와 토양 침식성 인자의 검토" 32 (32): 31-38, 1999

      5 김진관, "강우입자의 물리적 특성평가: 경기도 안성시 지역을 사례로" 한국지형학회 17 (17): 49-57, 2010

      6 Miura, S, "Transport rates of surface materials on steep forested slopes induced by raindrop splash erosion" 7 : 201-211, 2002

      7 Neal., J. H, "The effect of degree of slope and rainfall characteristics on runoff and soil erosion" 280 : 1938

      8 Morgan, R. P. C, "The European Soil Erosion Model (EUROSEM): a dynamic approach for predicting sediment transport from fields and small catchments" 23 : 527-544, 1998

      9 Brown, L. C, "Storm erosivity using idealized intensity distributions" 30 : 379-386, 1987

      10 Morgan, R. P. C., "Soil erosion and conservation (Second edition)" Longman Group 1995

      11 Van Dijk, A. I. J. M, "Rainfall intensity-kinetic energy relationships: a critical literature appraisal" 261 : 1-23, 2002

      12 Kinnell, P. I. A, "Rainfall intensity-kinetic energy relationships for soil loss prediction" 45 : 153-155, 1980

      13 Ekern, P. C., "Rainfall intensity as a measure of storm erosivity" 18 : 212-216, 1954

      14 Wischmeier, W. H, "Rainfall energy and its relation to soil loss" 39 : 285-291, 1958

      15 박의정, "RUSLE와 GRID를 이용한 하천의 토양유실량 및 유사유출량 산정방법별 비교분석" 한국지리정보학회 10 (10): 112-121, 2007

      16 박지상, "RUSLE 모델을 이용한 금강 유역의 토지 이용별 토사유출량 추정" 한국물환경학회 22 (22): 619-625, 2006

      17 Renard, K. G, "Predicting soil erosion by water: a guide to conservation planning with the revised universal soil loss equation (RUSLE), USDA Agricultural Handbook" USDA 703-, 1997

      18 Wischmeier, W. H, "Predicting rainfall erosion losses, USDA Agricultural Handbook" USDA 537-, 1978

      19 Al-Durrah, M. M, "Parameters for describing soil detachmentdue to single waterdrop impact" 46 : 836-840, 1982

      20 Nearing, M. A, "Modeling soil erosion, In Soil Erosion Research Methods (Second edition)" Soil and Water Conservation Society and St. Lucie Press 127-156, 1994

      21 Fornis, R. L., "Kinetic energy-rainfall intensity relationship for central Cebu, Philippines for soil erosion studies" 300 : 20-32, 2005

      22 Meyer, L. D, "How rain intensity affects interill erosion" 24 : 1472-1475, 1981

      23 박경훈, "GIS 및 RUSLE 기법을 활용한 금호강 유역의 토양침식위험도 평가" 한국지리정보학회 6 (6): 3-36, 2003

      24 이근상, "GIS 기반에서비퇴사량 실측자료를 활용한 토양침식의 정량화에 관한 연구" 25-34, 2002

      25 Nanko, K, "Estimation of soil splash detachment rateson the forest floor of an unmanagedJapanese cypress plantation based on fieldmeasurements of throughfall drop sizesand velocities" 72 : 348-361, 2008

      26 Lal, R, "Erodibility and erosivity, In Soil Erosion Research Methods (Second edition)" Soil and Water Conservation Society and St. Lucie Press 181-208, 1994

      27 Jayawardena, A. W, "Drop size distribution and kinetic energy load of rainstorms in Hong Kong" 14 : 1069-1082, 2000

      28 IPCC, "Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change" Cambridge University Press 2007

      29 Coutinho, M. A, "Characterization of raindrop size distributions at the Vale Formoso Experimental Erosion Center" 25 : 187-197, 1995

      30 McIsaac, G. F, "Apparent geographic and atmospheric influences on raindrop sizes and rainfall kinetic energy" 45 : 663-666, 1990

      31 Nearing, M.A, "A process-based soil erosion model for USDA-Water Erosion Prediction Project technology" 32 : 1587-1593, 1989

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      학술지 이력

      학술지 이력
      연월일 이력구분 이력상세 등재구분
      2027 평가예정 재인증평가 신청대상 (재인증)
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      2018-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2015-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2011-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2009-01-01 평가 등재학술지 유지 (등재유지) KCI등재
      2006-01-01 평가 등재학술지 선정 (등재후보2차) KCI등재
      2005-01-01 평가 등재후보 1차 PASS (등재후보1차) KCI등재후보
      2004-01-01 평가 등재후보 1차 FAIL (등재후보1차) KCI등재후보
      2003-01-01 평가 등재후보학술지 선정 (신규평가) KCI등재후보
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      학술지 인용정보

      학술지 인용정보
      기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
      2016 0.68 0.68 0.65
      KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
      0.7 0.71 0.769 0.28
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