Characterization of Local Evapotranspiration Based on the Seasonal and Hydrometeorological Conditions

계절과 수문기상학적 조건에 따른 지역 증발산의 특성화

  • 임창수 (한국수자원공사 수자원 연구실) ;
  • 이종태 (경기대학교 공과대학 토목공학과) ;
  • 윤세의 (경기대학교 공과대학 토목공학과)
  • Published : 1996.04.01

Abstract

Meteorological and soil water content data measured from semiarid watersheds of Lucky Hills and Kendall during the summer rainy and winter periods were used to study the interrelationships between the controlling variables of the evapotranspiration, and to evaluate the effects of variables on daily actual evapotranspiration (ET) estimation. Simple and multiple linear regression (MLR) analyses were employed to evaluate the order of importance of the meteorological and soil water factors involved. The information gained was used for MLR model development. Theavailable energy and vapor pressure deficit were found to be the important variables to estimate actual ET (AET) for both periods and at both watersheds. Therefore, the important variables of evapotranspiration process in these semiarid watersheds appear to be simply the components of energy term in available energy and aerodynamic term in vapor pressure deficit of Penman potential evapotranspiration (PET) equation.

여름우기와 겨울기간 동안에 준건조 기후 유역들(Lucky Hills 그리고 Kendall) 로부터 측정된 기상학적 그리고 토양 함수량 자료를 이용하여 증발산의 조절변수들 간에 상관관계와 매일의 실제 증발산량 산정을 위한 변수들의 영향을 연구하였다. 기상학적 요소와 토양 함수량의 중요도를 알아보기 위하여 단순, 다변량선형상관분석들이 적용되어졌으며, 얻어진 정보는 다변량선형상관모델을 개발하기 위하여 사용되어졌다. 유효 에너지와 대기 증기압 차는 두 다른 유역과 계절 기간 동안에 증발산을 지배하는 중요한 변수인 것으로 판명되어졌다. 그러므로 준건조 기후 지역에 있어서 증발산 과정의 중요한 변수로는 단순히 Penman에 의해서 제안된 잠재 증발산 모형의 에너지 항에 있어서 유효 에너지와 공기 동력 항에 있어서 대기증개압차인 것으로 나타났다.

Keywords

References

  1. Ph.D. diss., State University An experimental study of the seasonal behavior of surface resistance during the growing period of soybeans (evapotranspiration, combination model, evaporation, energy balance) Ahmed, R.
  2. Multiple regression in practice Berry, W.D.;Feldman, S.
  3. Theor. Appl. Climatol. v.46 Tests of a robust eddy correlation system for sensible heat flux Blanford, J.H.;Gay, L.W.
  4. NTIS PB 252-933 Runoff studies on small watersheds Burchinal, J.C.
  5. J. Appl. Meteorol. v.6 On the direct determination of the turbulent heat flux near the ground Businger, J.A.;Miyake, M.;Dyer, A.J.;Bradley, E.F.
  6. Agron. J. v.45 Availability of soil water to plants as affected by soil misture content and meteorological conditions Denmead, O.T.;Shaw, R.H.
  7. Water Resour. Res. v.30 no.5 Runoff simulation sensitivity to remotely sensed initial soil water content Goodrich, D.C.;Schmugge, T.J.;Jackson, T.J.;Unkrich, C.L.;Keefer, T.O.;Parry, R.;Bach, L.B.;Amer, S.A.
  8. Water-Supply Paper 1648 Arizona water Harshbarger, J.W.;Lewis, D.D.;Skibitzke, H.E.;Heckler, W.L.;Kister, L.R.;Baldwin, H.L.
  9. Can. J. Plant Sci. v.38 Conversion of Latent evaporation to potential evapotranspiration Holmes, R.M.;Robertson, G.W.
  10. Nordic Hydrol. v.6 A model for estimating actual evapotranspiration from potential evapotranspiration Kristensen, K.J.;Jensen, S.E.
  11. Ecology v.35 Some relationships of evaporation rate to vapor pressure deficit and low wind velocity Kucera, C.L.
  12. Am. Meteorol. Soc. Bull. v.72 no.11 An interdisciplinary field study of the energy and water fluxes in the atmosphere-biosphere system over semiarid rangelands: Description and some preliminary results Kustas, W.P.;Goodrich, D.C.;Moran, M.S.;Amer, S.A.;Bach, L.B.;Blanford, J.H.;Chehbouni, A.;Claassen, H.;Clements, W.E.;Doraiswamy, P.C.;Dubois, P.;Clarke, T.R.;Daughtry, C.S.T.;Gellman, D.I.;Grant, T.A.;Hipps, L.E.;Huete, A.R.;Humes, K.S.;Jackson, T.J.;Keefer, T.O.;Nichols, W.D.;Parry, R.;Perry, E.M.;Pinker, R.T.;Pinter, Jr.;P.J. Qi, J.;Riggs, A.C.;Schmugge, T.J.;Shutko, A.M.;Stannard, D.I.;Swiatek, E.;Van Leeuwen, J.D.;Van Zyl, J.;Vidal, A.;Washburne, J.;Weltz, M.A.
  13. SPSS/PC+ Studentware Norusis, M.J.
  14. J. of Hydrol. v.121 Daily surface moisture model for large area semiarid land application with limited climtate data Owe, M.;Griend, Van De.
  15. Hydrological Processes HYPRE3 v.5 no.2 Rainfall interception by tress of pinus radiata and eucalyptus viminalls in 1300 mm rainfall area of southeastern new south wales: I. Gross losses and their variability Pook, E.W.;Moore, P.H.R.;Hall, T.
  16. Tech. Bull. Supercritical flow flumes for measuring sediment-laden flow Smith, R.E.;Chery, D.L.;Renard, K.G.;Gwinn, W.R.
  17. Can. J. Plant Sci. v.43 Effects of weather on evaporation from bellani plates and evapotranspiration from lysimeters Wilcox, J.C.