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A Review of the Bowen Ratio Surface Energy Balance Method for Quantifying Evapotranspiration and other Energy Fluxes

鲍恩比率 潜热 显热 能量平衡 蒸散量 可用能量 涡度相关法 水蒸气 表面能 环境科学 行星边界层 热流密度 传热 大气科学 气象学 热力学 湍流 能量(信号处理) 物理 生态系统 生物 量子力学 生态学
作者
Suat Irmak,Kari E. Skaggs,Sumantra Chatterjee
出处
期刊:Transactions of the ASABE [American Society of Agricultural and Biological Engineers]
卷期号:: 1657-1674 被引量:31
标识
DOI:10.13031/trans.57.10686
摘要

<italic>Abstract.</italic> The Bowen ratio energy balance (BREB) method of indirect measurement of latent and sensible heat fluxes and other major components of the surface energy balance is accepted as one of the robust approaches in the fields of agricultural engineering, micrometeorology, water resources research, hydrology, and related disciplines. The adoption of this technology in quantification of surface energy fluxes in practical applications is mainly attributed to the method's performance and robustness in measurement of such fluxes for various agro-ecosystem surfaces in different climates. The method determines the Bowen ratio (β) by means of measured gradients of atmospheric temperature and air moisture content (actual water vapor pressure) and applies β in the energy balance equation to solve for the latent and sensible heat flux. The main assumption in the Bowen ratio theory is that the energy transfer coefficients for latent heat (KV) and sensible heat fluxes (KH) are equal. This assumption is made because all energy scalars are carried by the same eddies and, therefore, these scalars are associated at the same boundary layer of the evaporating surface. A basic criterion of this method is that the air temperature and water vapor pressure are measured (above an evaporating surface) at such heights that the horizontal gradient of air temperature and water vapor pressure can be neglected. The equality (or similarity) assumption (KV = KH) has been proven to be valid for a range of field and vegetation surfaces in various climates. However, the assumption has also been proven invalid for some heterogeneous vegetation surfaces. Nevertheless, successful application of the BREB method to measure surface energy fluxes has been reported for many different types of terrestrial surfaces, including agricultural fields, grasslands, forestry, lakes, wetlands, ocean, etc. This article reviews the history; the main scientific, theoretical, and technical principles; the operational characteristics; and some of the advances in instrumentation of the BREB method. Some studies utilizing the BREB method are also presented.

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