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三峡水库香溪河库湾水-气界面热交换过程及水体稳定性
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作者 杨忠勇 张亚超 +4 位作者 汤正阳 纪道斌 崔玉洁 李昌文 吴家阳 《湖泊科学》 EI CAS CSCD 北大核心 2023年第2期730-742,共13页
水库或湖泊的热分层结构是其动力与环境过程的重要研究方面,虽然很多学者针对水体分层结构和演变机理开展了大量研究,但水体通过水-气界面与大气进行热交换的过程,各气象因子的贡献机理等研究成果还很缺乏。本文基于三峡水库香溪河库湾2... 水库或湖泊的热分层结构是其动力与环境过程的重要研究方面,虽然很多学者针对水体分层结构和演变机理开展了大量研究,但水体通过水-气界面与大气进行热交换的过程,各气象因子的贡献机理等研究成果还很缺乏。本文基于三峡水库香溪河库湾2019年3月-2020年2月期间的水温、水位及气象等监测数据,针对水-气界面热交换过程如何影响水温垂向结构及表层水体湍流混合作用开展研究。结果表明,(1)香溪河水体年内呈高温期分层、低温期混合的基本特征,高温期混合层深度小于8 m,低温期混合层深度超过30 m。(2)太阳短波辐射是香溪河水体的主要热源,潜热通量和长波辐射是香溪河水体的主要冷源,感热通量贡献极小。(3)香溪河平均风速较弱,约为1.6 m/s,主要通过增强潜热和感热通量的方式影响水体垂向稳定性结构特征,其机械扰动作用较弱。(4)表层水体湍能通量在高温期较低(10^(-7)m^(3)/s3量级),此时水体处于分层状态,风应力大概率主导表层水体湍流发育;低温期表层水体湍能通量较高(10^(-6)m^(3)/s3量级),此时潜热通量和长波辐射主导表层水体湍流发育。 展开更多
关键词 三峡 香溪河库湾 -界面通量 分层 风应力 表层湍流
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Water, CO_2 and Energy Exchange at Vegetation-air Interface
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作者 肖丽 《Agricultural Science & Technology》 CAS 2012年第9期1908-1914,共7页
[Objective] The aim was to analyze water and heat fluxes, CO2 fluxes and energy balance in wheat ecosystem in Luancheng County of Hebei Province. [Method] Based on data of water and heat flux, and CO2 fluxes, routine ... [Objective] The aim was to analyze water and heat fluxes, CO2 fluxes and energy balance in wheat ecosystem in Luancheng County of Hebei Province. [Method] Based on data of water and heat flux, and CO2 fluxes, routine meteorological and biomass data in Luancheng in 2008, water and heat fluxes, CO2 fluxes and energy balance in wheat ecosystem were explored. [Result] The results showed that latent and sensible heat and CO2 fluxes were of obvious daily and seasonal changes; latent and sensible heat fluxes shaped an inverted U in daily change, and CO2 fluxes were of a U-shape; daily flux peak differed significantly. Furthermore, the change of latent heat, sensible heat and CO2 fluxes were closely related to environ- mental factors. Detailedly, the three were sensitive to light intensity and net radiation, and correlation coefficients were 0.92, 0.66, 0.65 and 0.90, 0.69, 0.74, respectively. Besides, the fluxes, sensitive to temperature, proved better in sunny day, especially for latent flux which is more sensitive to water in soils after precipitation. In addition, closure degree of energy balance in wheat fields was 0.91 and non-closure, caused by measurement error and neglection of heat storage, was observed, too. What's more. closure degree differed in months and time periods within a day. [Conclusion] The research concluded water and heat fluxes, CO2 fluxes, transport mechanisms and concerning factors, providing scientific reference for revealing mechanism of evapo- ration and heat dissipation of canopy, relationship between photosynthesis and water use efficiencyand energy distribution mechanism. 展开更多
关键词 Latent heat flux Sensible heat flux CO2 flux Energy balance Environ-mental factors
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香溪河初冬降温过程中垂向混合结构特征分析 被引量:4
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作者 杨忠勇 钱门亮 +3 位作者 纪道斌 周哲轩 姚仕明 范中亚 《中国环境科学》 EI CAS CSCD 北大核心 2021年第6期2862-2870,共9页
基于2018年11月29日~12月15日三峡水库支流香溪河峡口站点的水文气象等实测数据,讨论了香溪河初冬一次典型降温过程中水体的垂向混合结构动力过程,以及水-气界面的热通量和风应力在其中的贡献机制.结果表明,该时段香溪河表层约8m水深范... 基于2018年11月29日~12月15日三峡水库支流香溪河峡口站点的水文气象等实测数据,讨论了香溪河初冬一次典型降温过程中水体的垂向混合结构动力过程,以及水-气界面的热通量和风应力在其中的贡献机制.结果表明,该时段香溪河表层约8m水深范围的垂向混合结构呈显著的日间弱分层,夜间强混合模式,且日间分层时段较短,仅发生在正午前后的约4h内(最大浮力频率约2×10^(-4)s^(-1)).水-气界面的能量输入或耗散过程对水体分层混合过程的贡献显著大于风应力对水体的机械扰动作用.太阳短波辐射是表层水体日间吸热从而分层的主要驱动力,长波辐射在夜间放热过程中处于主导地位,潜热和感热过程在水体放热过程中作用相当.风应力以机械扰动的方式对水体混合模式的影响极小(湍能通量最大值2×10^(-7)m^(3)/s^(3)),主要集中在表层水体约0.5m内,但其可通过影响潜热和感热的方式显著增强中层水体混合特征.由于研究时段香溪河水温较低,蒸发放热较小,而水-气温差相对较大,风应力通过感热驱动的湍能通量(8×10^(-7)m^(3)/s^(3))略大于潜热(7×10^(-7)m^(3)/s^(3)). 展开更多
关键词 香溪河 垂向混合过程 湍能通量 水-气热通量 风应力
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NUMERICAL EXPERIMENTS ON THE IMPACTS OF SEA SPRAY ON TROPICAL CYCLONES
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作者 郑静 费建芳 +3 位作者 王元 黄小刚 李启明 吴宏毅 《Journal of Tropical Meteorology》 SCIE 2009年第1期54-58,共5页
The latest version of sea spray flux parameterization scheme developed by Andreas is coupled with the PSU/NCAR model MM5 in this paper. A western Pacific tropical cyclone named Nabi in 2005 is simulated using this cou... The latest version of sea spray flux parameterization scheme developed by Andreas is coupled with the PSU/NCAR model MM5 in this paper. A western Pacific tropical cyclone named Nabi in 2005 is simulated using this coupled air-sea spray modeling system to study the impacts of sea spray evaporation on the evolution of tropical cyclones. The results demonstrate that sea spray can lead to a significant increase of heat fluxes in the air-sea interface, especially the latent heat flux, the maximum of which can increase by up to about 35% - 80% The latent heat flux seems to be more important than the sensible heat flux for the evolution of tropical cyclones. Regardless of whether sea spray fluxes have been considered, the model can always simulate the track of Nabi well, which seems to indicate that sea spray has little impact on the movement of tropical cyclones. However, with sea spray fluxes taken into account in the model, the intensity of a simulated tropical cyclone can have significant increase. Due to the enhancement of water vapor and heat from the sea surface to the air caused by sea spray, the warm core structure is better-defined, the minimum sea level pressure decreases and the vertical speed is stronger around the eye in the experiments, which is propitious to the development and evolution of tropical cyclones. 展开更多
关键词 numerical simulation tropical cyclone sea spray parameterization scheme
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