内陆小型水体水汽传输系数和Priestley-Taylor系数的量化

赵若男; 肖薇; 石立新; 赵佳玉; 谢成玉; 谢燕红; 曹畅; 张弥; 郑有飞

doi:10.3799/dqkx.2021.227

Volume 48 Issue 10

Oct. 2023

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Article Navigation > Earth Science > 2023 > 48(10): 3896-3911

Zhao Ruonan, Xiao Wei, Shi Lixin, Zhao Jiayu, Xie Chengyu, Xie Yanhong, Cao Chang, Zhang Mi, Zheng Youfei, 2023. Quantification of Water Vapor Transport Coefficient and Priestley-Taylor Coefficient over Small Inland Water Bodies. Earth Science, 48(10): 3896-3911. doi: 10.3799/dqkx.2021.227

Citation:

Zhao Ruonan, Xiao Wei, Shi Lixin, Zhao Jiayu, Xie Chengyu, Xie Yanhong, Cao Chang, Zhang Mi, Zheng Youfei, 2023. Quantification of Water Vapor Transport Coefficient and Priestley-Taylor Coefficient over Small Inland Water Bodies. Earth Science, 48(10): 3896-3911. doi: 10.3799/dqkx.2021.227

Citation:

Zhao Ruonan, Xiao Wei, Shi Lixin, Zhao Jiayu, Xie Chengyu, Xie Yanhong, Cao Chang, Zhang Mi, Zheng Youfei, 2023. Quantification of Water Vapor Transport Coefficient and Priestley-Taylor Coefficient over Small Inland Water Bodies. Earth Science, 48(10): 3896-3911. doi: 10.3799/dqkx.2021.227

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Quantification of Water Vapor Transport Coefficient and Priestley-Taylor Coefficient over Small Inland Water Bodies

doi: 10.3799/dqkx.2021.227

1.
Center on Atmospheric Environment, Nanjing University of Information Science & Technology, Nanjing 210044, China
2.
Hebei Key Laboratory of Meteorology and Ecological Environment, Shijiazhuang 050021, China
3.
Scotland Academy, Wuxi Taihu University, Wuxi 214064, China

Received Date: 2021-09-04
Available Online: 2023-10-31
Publish Date: 2023-10-25

Abstract

Abstract

Small water bodies (< 1 km²) are numerous, with area accounting for more than 40% of the total area of global inland water area, and play an important role in weather and climate system, water cycle and water resources management. In this paper, the aquaculture pond in Quanjiao County of Anhui Province was selected as a representative of small water bodies. Continuous observations of evaporation from June 2017 to May 2020 were conducted using eddy covariance technology. Data gaps were interpolated based on bulk transfer equation, and energy balance closure was forced on monthly scale. Priestley-Taylor model was used to study the effect of advection. Results indicate that the water vapor transfer coefficient of small water bodies was higher in summer and lower in winter, with a range of 1.9×10^-3 to 3.4×10^-3. The monthly water vapor transfer coefficient was significantly correlated with wind speed and the difference between water surface temperature and air temperature over small water bodies. But the transfer coefficient is not significantly correlated with water body area.The α coefficient of Priestley-Taylor model over the small water body ranged from 1.14 to 1.78, with lowest value appeared in August and highest value appeared in February, and the maximum value is higher than those over open surface of large lakes. Similar to other inland water bodies, the α coefficient over small water bodies was lower in warm season and higher in cold season, indicating that advection effect was weak in summer and strong in winter. On annual time scale, evaporation of both small and large water bodies were affected by weak advection.
- evaporation,
- small water body,
- eddy covariance,
- Priestley-Taylor model,
- water vapor transfer coefficient,
- advection,
- meteorology,
- climatology

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References(42)

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