1) turbulent flux
湍通量
1.
A preliminary estimation on NCEP reanalysis turbulent flux by buoy data;
利用浮标资料初步评估NCEP再分析湍通量
2) Turbulence flux
湍流通量
1.
Atmospheric turbulence flux data and land surface temperature data of Tibet are analyzed in this paper.
分析了西藏的湍流通量数据和地表温度数据,提出了表征地表温度变化特征的地表温度特征量。
2.
In this paper, we talk about how to delete noise, wild points and filter nonlinear trends, how nonlinear trends contribute fake turbulence flux by having influence on self-relation func- tion and integral scale.
讨论了非线性趋势对时间序列的自相关函数、积分时间尺度等的影响，并估算了其最终对湍流通量的影响，指出有效地去除野点、噪音和非线性趋势以及非线性趋势对时间序列的自相关函数、积分时间尺度等的影响，可以减少其对湍流通量产生较大的虚假贡献。
3) turbulent flux
湍流通量
1.
A primary study on turbulent fluxes over surface layer in the region of cropland to grassland conversion in southern Ningxia;
宁南退耕还草区近地面湍流通量观测初报
2.
Based on the mean field data of wind,temperature and the turbulent field data from Beijing 325 m Meteorological Tower,the characteristics of mesoscale and turbulent fluxes during the strong dust storm weather from 18 to 22 March 2002 are discussed.
应用大气所325 m铁塔的湍流资料和梯度资料,对2003年3月20~23日影响北京的一次强沙尘天气过程的中尺度通量和湍流通量进行了分析,结果表明:冷空气的影响是从上层开始的。
3.
In this paper,turbulent flux over canopy of field crops was calculated using Profile Gradient Method derived from Monin Obhov Similarity Theory and drag coefficient,Stanton number and Dalton number were also further defined.
根据农田植被层上方的温湿风梯度观测资料，采用基于莫宁－奥布霍夫相似理论的廓线梯度法计算了农田植被层上方的湍流通量，进而确定出拖曳系数、斯坦顿数和道尔顿数。
4) turbulent fluxes
湍流通量
1.
Based on data from the dust storm monitoring station over Hunshandake Desert Area,Inner Mongolia,the maximum values of micrometeorological variables, turbulent fluxes and dust concentration in the surface layer are compared for eight dust events in the spring of 2004,and the characteristics of micrometeorology and radiation components in the strongest dust storm event in March 27-28 are analyzed.
利用内蒙古浑善达克沙地沙尘暴实验探测资料,给出2004年春季多次沙尘天气过程近地面微气象学要素、湍流通量及沙尘浓度的极值对比,重点分析了3月27—28日强沙尘暴过境时近地面微气象学要素和辐射分量的变化特征。
2.
The differences of turbulent fluxes and heat budget over the rice paddy and dry farming land are presented in term of the eddy covariance and profile methods based on the radiation components, turbulent and related data observed in Anhui province supported by national 973 rainstorm program from June 11 to July 20, 2001.
利用973暴雨项目2001年6月10日—7月20日在安徽境内旱地和稻田观测的近地层辐射平衡分量、涡动相关和廓线资料，计算分析了不同下垫面的辐射平衡、湍流通量和热量收支差异，并用实测的强迫变量和SiB2模式对稻田和旱地不同生长期的湍流通量进行模拟试验和对比。
3.
The features of surface albedo, water and heat flux, CO2 flux, bulk transfer coefficients and energy balance in different underlying surface and growing period have been investigated based on the data of turbulent fluxes observed by Eddy Covariance method, radiation balance components and profile data over cropland in Huaihe River Basin from Sept.
通过分析2007年9月～2008年8月年在淮河流农田下垫面采用涡动相关法(Eddy Covariance,简称EC)测得的地气间湍流通量以及辐射平衡分量和廓线资料,研究淮河流域农田地气相互作用日、季变化特征,分析了农田不同下垫面以及作物不同生长期地表反照率、水热通量、CO2通量、总体输送系数以及能量平衡比率等的变化规律,并且将涡度法与梯度法测得的感热、潜热和动量通量进行对比分析,以期能够全面深入了解农田生态系统的湍流输送特征。
5) Turbulent heat flux
湍流热通量
1.
The turbulent heat flux and latent heat flux in rows are calculated with М.
и布德柯法计算了株间的湍流热通量和潜热通量。
2.
In the context of field observations at Shentou (112°17′ E, 39°18′ S) in September～October 1988, calculation is carried out of frictional velocity, characteristic temperature and turbulent momentum flux, with turbulent heat flux dealt with by two methods.
用两种不同的方法计算了湍流热通量，并按稳定度进行了分类统计和做了采样各天的热通量日变化分析。
6) Turbulent heat fluxes
湍流热通量
1.
Evaluation of daily NCEP2 turbulent heat fluxes during southwest monsoon in South China Sea;
南海西南季风期NCEP2湍流热通量的质量分析
补充资料：传质通量
分子式：
CAS号：
性质：又称传质通量。单位时间、单位面积所传过去的物质质量，用符号N表示，其单位为kg/(m2·s)。
CAS号：
性质：又称传质通量。单位时间、单位面积所传过去的物质质量，用符号N表示，其单位为kg/(m2·s)。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条