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Inter-comparison of the Penman-Monteith type model in modeling the evapotranspiration and its components in an orchard plantation of Southwest China

Author

Listed:
  • Cui, Ningbo
  • He, Ziling
  • Jiang, Shouzheng
  • Wang, Mingjun
  • Yu, Xiuyun
  • Zhao, Lu
  • Qiu, Rangjian
  • Gong, Daozhi
  • Wang, Yaosheng
  • Feng, Yu

Abstract

Crop evapotranspiration (ET) along with its components (canopy transpiration (T) and soil evaporation (E)) estimates are crucial for agroecosystem hydrological process research and developing agricultural water-saving strategies. An inter-comparison of the Penman-Monteith type model, including Penman-Monteith (PM), Shuttleworth-Wallace (S-W), Two-Patch (T-P) and topography- and vegetation-based surface energy partitioning algorithm (TVET), Clumping (CL) and developed Two patch-Two layer (T-T) model was conducted to estimate ET and its components in a kiwifruit orchard. Results showed that all models can well capture the pattern of eddy covariance-based hourly ET (ETEC), with a slope of 0.82–1.10, R2 of 0.78–0.83, and RMSE of 0.039–0.049 mm 0.5 h–1, and yield relatively reliable estimates validated by sap flow-based hourly T, with a slope of 0.93–1.16, R2 of 0.72–0.79, and RMSE 0.017–0.026 mm 0.5 h–1. All the P-M type models agreed well with the daily ETEC, with a slope of 0.88–1.21, R2 of 0.82–0.86, and RMSE of 0.55–0.88 mm d–1, respectively. S-W overestimated actual ET due to overestimation in both T and E, T-P and TVET models overestimated T but underestimated actual E as they ignored the soil contribution under the canopy. T-T model outperformed other models in daily ET, T, and E estimates, with R2 of 0.86, 0.73 and 0.73, and RMSE of 0.56, 0.39 and 0.46 mm d–1, respectively. The output ET and T of the different P-M type models were most sensitive to canopy resistance (rsc), while E is most sensitive to aerodynamic resistance between substrate and crop canopy. Net radiation was the most crucial meteorological factor affecting ET, T and E, as it directly participated in the energy balance calculation. The output T was sensitive to air temperature since it affected rsc, while E was relatively sensitive to soil water content since it greatly changed soil surface resistance.

Suggested Citation

  • Cui, Ningbo & He, Ziling & Jiang, Shouzheng & Wang, Mingjun & Yu, Xiuyun & Zhao, Lu & Qiu, Rangjian & Gong, Daozhi & Wang, Yaosheng & Feng, Yu, 2023. "Inter-comparison of the Penman-Monteith type model in modeling the evapotranspiration and its components in an orchard plantation of Southwest China," Agricultural Water Management, Elsevier, vol. 289(C).
    • Handle: RePEc:eee:agiwat:v:289:y:2023:i:c:s0378377423004067
    DOI: 10.1016/j.agwat.2023.108541
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    1. Dong, Juan & Xing, Liwen & Cui, Ningbo & Zhao, Lu & Guo, Li & Wang, Zhihui & Du, Taisheng & Tan, Mingdong & Gong, Daozhi, 2024. "Estimating reference crop evapotranspiration using improved convolutional bidirectional long short-term memory network by multi-head attention mechanism in the four climatic zones of China," Agricultural Water Management, Elsevier, vol. 292(C).

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