曹润祥, 李发文, 李建柱, 冯平. 天津平原区城市化地区蒸散发特征[J]. 水科学进展, 2021, 32(3): 366-375. DOI: 10.14042/j.cnki.32.1309.2021.03.005
引用本文: 曹润祥, 李发文, 李建柱, 冯平. 天津平原区城市化地区蒸散发特征[J]. 水科学进展, 2021, 32(3): 366-375. DOI: 10.14042/j.cnki.32.1309.2021.03.005
CAO Runxiang, LI Fawen, LI Jianzhu, FENG Ping. Exploring evapotranspiration characteristics in urbanized areas of Tianjin plain[J]. Advances in Water Science, 2021, 32(3): 366-375. DOI: 10.14042/j.cnki.32.1309.2021.03.005
Citation: CAO Runxiang, LI Fawen, LI Jianzhu, FENG Ping. Exploring evapotranspiration characteristics in urbanized areas of Tianjin plain[J]. Advances in Water Science, 2021, 32(3): 366-375. DOI: 10.14042/j.cnki.32.1309.2021.03.005

天津平原区城市化地区蒸散发特征

Exploring evapotranspiration characteristics in urbanized areas of Tianjin plain

  • 摘要: 为揭示城市蒸散发特征,采用考虑人为热影响的SEBS-Urban模型计算天津平原区2015—2017年逐月蒸散量。使用两步验证法对结果进行检验,首先利用MODIS MOD16产品对非建成区模拟结果合理性进行验证,其次利用城市耗水(UWD)模型得到的天津大学卫津路校区月蒸散量对建成区模拟结果验证。在SEBS-Urban模拟结果基础上,检验Budyko方程在城市化地区的适用性。结果表明:① SEBS-Urban模型精度可靠,体现了蒸散发项在城市地表能量平衡与二元水循环中的相合性;②人为热或社会侧的耗水会导致蒸散发量增加,建成区增幅达85%~115%,整个研究区增幅为7.2%~8.7%;③ Budyko方程在研究区具有较好的拟合效果,可应用于城市地区。本研究成果可为城市化地区蒸散发研究提供必要的参考。

     

    Abstract: To reveal the characteristics of urban-based evapotranspiration, a SEBS-Urban model was applied to estimate the monthly evapotranspiration(ET) that occurred in the plain area of Tianjin over 2015—2017 considering anthropogenic heat release. A two-step verification method was used. First, a comparative analysis was performed with the MODIS MOD16 products for rural areas. Second, the urban water dissipation (UWD) framework was used to assess the model's performance in built-up areas. The feasibility of the Budyko formula was explored based on the SEBS-Urban results. Three key results were obtained: ① The SEBS-Urban model is reliable, and the results of the built-up area ET analysis are consistent from the perspectives of an urban surface energy balance and a dualistic water cycle. ② The ET increment ranges up to 85%~115% for the built-up area but only 7.2%~8.7% for the whole study area after including considerations for anthropogenic heat. ③ The Budyko formula obtained good results for estimating evapotranspiration in the study area, suggesting that it can also be applied to urban areas. The results of this study can provide a necessary reference for studies on evapotranspiration in urbanized areas.

     

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