Rainfall-Induced Attenuation Correction for Two Operational Dual-Polarization C-Band Radars in the Netherlands

被引:4
|
作者
Overeem, Aart [1 ,2 ]
de Vries, Hylke [3 ]
Al Sakka, Hassan [4 ]
Uijlenhoet, Remko [2 ,5 ]
Leijnse, Hidde [1 ,2 ]
机构
[1] Royal Netherlands Meteorol Inst, R&D Observat & Data Technol, De Bilt, Netherlands
[2] Wageningen Univ & Res, Hydrol & Quantitat Water Management Grp, Wageningen, Netherlands
[3] Royal Netherlands Meteorol Inst, R&D Weather & Climate Modelling, De Bilt, Netherlands
[4] Leonardo Germany GmbH, Neuss, Germany
[5] Delft Univ Technol, Fac Civil Engn & Geosci, Dept Water Management, Delft, Netherlands
关键词
Precipitation; Radars; Radar observations; Rainfall; Remote sensing; BIAS ADJUSTMENT; WEATHER RADAR; FUZZY-LOGIC; PRECIPITATION; PERFORMANCE; ALGORITHMS; RETRIEVAL; RANGE; MODEL; QPE;
D O I
10.1175/JTECH-D-20-0113.1
中图分类号
P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
The Royal Netherlands Meteorological Institute (KNMI) operates two operational dual-polarization C-band weather radars providing 2D radar rainfall products. Attenuation can result in severe underestimation of rainfall amounts, particularly in convective situations that are known to have high impact on society. To improve the radar-based precipitation estimates, two attenuation correction methods are evaluated and compared: 1) modified Kraemer (MK) method, i.e., Hitschfeld-Bordan where parameters of the power-law Z(h)-k(h) relation are adjusted such that reflectivities in the entire dataset do not exceed 59 dBZ(h) and attenuation correction is limited to 10 dB; and 2) using two-way path-integrated attenuation computed from the dual-polarization moment specific differential phase K-dp (Kdp method). In both cases the open-source Python library wradlib is employed for the actual attenuation correction. A radar voxel only contributes to the computed path-integrated attenuation if its height is below the forecasted freezing-level height from the numerical weather prediction model HARMONIE-AROME. The methods are effective in improving hourly and daily quantitative precipitation estimation (QPE), where the Kdp method performs best. The verification against rain gauge data shows that the underestimation diminishes from 55% to 37% for hourly rainfall for the Kdp method when the gauge indicates more than 10 mm of rain in that hour. The improvement for the MK method is less pronounced, with a resulting underestimation of 40%. The stability of the MK method holds a promise for application to data archives from single-polarization radars.
引用
收藏
页码:1125 / 1142
页数:18
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