Long-term analysis of measured and simulated evapotranspiration and soil water content

被引:5
|
作者
Wegehenkel, M. [1 ]
Rummel, U. [2 ]
Beyrich, F. [2 ]
机构
[1] ZALF eV, Inst Landscape Syst Anal, Muncheberg, Germany
[2] Richard Assmann Observ, Lindenberg Meteorol Observ, German Meteorol Serv Deutsch Wetterdienst, DWD, Lindenberg, Germany
关键词
modelling; real evapotranspiration; soil water content; eddy covariance; compensatory root water uptake model; EDDY-COVARIANCE; HYDRAULIC CONDUCTIVITY; FLUX MEASUREMENTS; SURFACE; EVAPORATION; MODEL; GROUNDWATER; PATTERNS; HYDRUS; HEAT;
D O I
10.1080/02626667.2017.1332417
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
In our study, we analysed a period from 2003 to 2012 with micrometeorological data measured at a boundary-layer field site operated by the Lindenberg Meteorological Observatory -Richard-ABmann-Observatory of the German Meteorological Service (DWD). Amongst others, these data consist of real evapotranspiration (ETr) rates measured by eddy covariance and soil water contents determined by time domain reflectometry. Measured ETr and soil water contents were compared with those simulated by a simple soil-vegetation-atmosphere transfer (SVAT) scheme consisting of the FAO56 Penman-Monteith equation and the soil water flux model Hydrus-1D. We applied this SVAT scheme using uncompensatory and compensatory root water uptake (RWU). Soil water contents and ETr rates calculated using uncompensatory RWU showed an acceptable fit to the measured ones. In comparison, the use of compensatory RWU resulted in lower model performance due to higher deviations between measured and simulated soil moisture values and ETr rates during dry summer periods.
引用
收藏
页码:1532 / 1550
页数:19
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