An Approach for the Estimation of Hydrometeorological Variables Towards the Determination of Z-R Coefficients

被引:6
作者
Baltas E.A. [1 ]
Panagos D.S. [1 ]
Mimikou M.A. [1 ]
机构
[1] Department of Water Resources, Hydraulic and Maritime Engineering, National Technical University of Athens, 5 Iroon Polytechniou, Zografou, Athens
关键词
Disdrometer; JWD; Radar reflectivity; Rainfall; Z-R relationships;
D O I
10.1007/s40710-015-0119-x
中图分类号
学科分类号
摘要
An attempt is made to estimate the basic hydrometeorological variables, namely the rainfall concentration for each bin per m3, the radar reflectivity factor Z and the rainfall intensity R, and consequently to determine coefficient "a" and exponent "b" of the power law relationship Z = aRb. Data used were recorded in a period of almost 10 years, with a Joss-Walvogel RD-69 disdrometer (JWD), located in the meteorological station of the campus of National Technical University of Athens. A number of rainfall events were selected based on the following criteria: the total rainfall depth of each event was greater than 24.0 mm and the average rainfall intensity exceeded 5.0 mm/h, in order to only study events with increased flash flooding probability. Initially, Drop Size Distributions (DSDs) were calculated for these rainfall events and processed for the derivation of Z-R relationships. Such Z-R relationships were finally derived for the overall spectra of R > 5.0 mm/h and for each event separately and were compared with other Z-R relationships found in the literature. © 2015 Springer International Publishing Switzerland.
引用
收藏
页码:751 / 759
页数:8
相关论文
共 17 条
[11]  
Martins R.C.G., Machado L.A.T., Costa A.A., Characterization of the microphysics of precipitation over amazon region using radar and disdrometer data, Atmos Res, 96, pp. 388-394, (2010)
[12]  
Nzeukou A., Sauvageot H., Ochou A.D., Kebe C.M.F., Raindrop size distribution and radar parameters at Cape Verde, J Appl Meteorol, 43, pp. 90-105, (2004)
[13]  
Sempere-Tores D., Sanchez-Diezma R., Zawadzki I., Creutin J.D., Identification of stratiform and convective areas using radar data with application to the improvement of DSD analysis and Z-R relations, Phys Chem Earth, 25, pp. 985-990, (2000)
[14]  
Tenorio R.S., Kwon B.H., Z-R relationship and a severe rainfall observed by C-band radar in eastern coast of northeastern Brazil, Forth European Conference on Radar in Meteorology and Hydrology (ERAD), (2006)
[15]  
Tokey A., Short A.D., Evidence from tropical raindrop spectra of the origin of rain from stratiform versus convective clouds, J Appl Meteorol Climatol, 35, pp. 355-370, (1996)
[16]  
Uijlenhoet R., Steiner M., Smith J.A., Variability of raindrop size distributions in a squall line and implications for radar rainfall estimation, J Hydrometeorol, 4, pp. 43-61, (2003)
[17]  
Uijlenhoet R., Porra J.M., Torres D.S., Creutin J.-D., Analytical solutions to sampling effects in drop size distribution measurements during stationary rainfall: Estimation of bulk rainfall variables, J Hydrol, 328, pp. 65-82, (2006)