Scaling effects of standing crop residues on the wind profile

被引:19
作者
Aiken, RM
Nielsen, DC
Ahuja, LR
机构
[1] Kansas State Univ, NW Res Ext Ctr, Colby, KS 67701 USA
[2] USDA ARS, Cent Great Plains Res Stn, Washington, DC 20250 USA
[3] USDA ARS, Great Plains Syst Res, Washington, DC 20250 USA
关键词
D O I
10.2134/agronj2003.1041
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Standing senescent stems increase the aerodynamic roughness of the surface, reducing wind energy available for momentum transfer at the soil surface, such as for wind erosion, and also the soil-atmosphere convective exchanges of heat, water vapor, and trace gases. We conducted studies to determine the predictive accuracy of an algorithm derived for plant canopies to scale effects of standing crop residues on the wind profile. We used this algorithm to calculate aerodynamic properties (displacement height and roughness length) of standing crop residues related to the log wind profile equation. We also calculated apparent roughness length from wind profiles measured under neutral stability conditions over stems of wheat (Triticum aestivum L.), corn (Zea mays L.), millet (Panicum miliaceum L.), and sunflower (Helianthus annuas L.) using calibrated single-needle and cup anemometers. A least-squares fit of roughness length calculated by an algorithm derived for crop canopies indicated a systematic, positive bias when it was applied to standing stems. After adjusting for bias, calculated windspeeds generally were contained in 80% confidence intervals for observations above and within the crop stubble. Predictive root mean square errors (RMSE) within profiles ranged from 0.6 to 4.6% of reference wind speed. The nonlinear forms of the scaling algorithms are consistent with theory and wind tunnel observations, representing an advance over parameterization schemes assuming a linear relation with residue height. This advance warrants evaluation of the adjusted algorithm for simulation of microclimate in the soil-residue-crop canopy regime. Application to momentum transfer problems requires further investigation of drag partitioning.
引用
收藏
页码:1041 / 1046
页数:6
相关论文
共 31 条
[1]   Energy balance simulation for surface soil and residue temperatures with incomplete cover [J].
Aiken, RM ;
Flerchinger, GN ;
Farahani, HJ ;
Johnsen, KE .
AGRONOMY JOURNAL, 1997, 89 (03) :404-415
[2]   A TRANSIENTLY HEATED NEEDLE ANEMOMETER [J].
BLAND, WL ;
NORMAN, JM ;
CAMPBELL, GS ;
CALISSENDORFF, C ;
MILLER, EE .
AGRICULTURAL AND FOREST METEOROLOGY, 1995, 74 (3-4) :227-235
[3]   THE PHYSICAL-ENVIRONMENT OF 2 SEMI-ARID TROPICAL SOILS WITH PARTIAL SURFACE MULCH COVER [J].
BRISTOW, KL ;
ABRECHT, DG .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1989, 27 (03) :577-587
[4]  
Campbell GS, 1973, INTRO ENV BIOPHYSICS
[5]   A 4-LAYER MODEL FOR THE HEAT-BUDGET OF HOMOGENEOUS LAND SURFACES [J].
CHOUDHURY, BJ ;
MONTEITH, JL .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1988, 114 (480) :373-398
[6]  
Denmead O. T., 1985, The forest-atmosphere interaction. Proceedings of the forest environmental measurements conference held at Oak Ridge, Tennessee, October 23-28, 1983, P421
[7]   LAGRANGIAN AND K-THEORY APPROACHES IN MODELING EVAPORATION FROM SPARSE CANOPIES [J].
DOLMAN, AJ ;
WALLACE, JS .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1991, 117 (502) :1325-1340
[8]   CROP RESIDUE REMOVAL AND SOIL PRODUCTIVITY WITH NO-TILL CORN, SORGHUM, AND SOYBEAN [J].
DORAN, JW ;
WILHELM, WW ;
POWER, JF .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1984, 48 (03) :640-645
[9]  
Doren D. M. Van Jr., 1978, ASA [American Society of Agronomy] Special Publication, P49
[10]   Crop residue effects on aerodynamic processes and wind erosion [J].
Hagen, LJ .
THEORETICAL AND APPLIED CLIMATOLOGY, 1996, 54 (1-2) :39-46