On quality of radar rainfall with respect to temporal and spatial resolution for application to urban areas

被引：5

作者：

Yoon, Jungsoo ^{[1
]}

Joo, Jingul ^{[2
]}

Yoo, Chulsang ^{[3
]}

Hwang, Seokhwan ^{[4
]}

Lim, Sanghun ^{[4
]}

机构：

[1] Korea Meteorol Adm, Weather Radar Ctr, Seoul, South Korea

[2] Dongshin Univ, Dept Civil Engn, Naju Si 520714, Jeollanam Do, South Korea

[3] Korea Univ, Coll Engn, Sch Civil Environm & Architectural Engn, Seoul, South Korea

[4] Korea Inst Civil Engn & Bldg Technol, Water Resources Res Div, Goyang Si, South Korea

来源：

METEOROLOGICAL APPLICATIONS | 2017年 / 24卷 / 01期

关键词：

temporal resolution; spatial resolution; quantitative quality measures; radar rainfall; gauge rainfall; QUANTITATIVE PRECIPITATION ESTIMATION; VERTICAL PROFILES; SIZE DISTRIBUTION; SAMPLING ERRORS; REFLECTIVITY; IDENTIFICATION; VARIABILITY; CALIBRATION;

D O I：

10.1002/met.1601

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

In this study the quality of radar rainfall with respect to temporal and spatial resolution was examined. Gwangdeoksan Radar and the Korea Institute of Civil Engineering and Building Technology (KICT) Radar were used for this purpose, along with the automatic weather systems data within Seoul. In addition, several quantitative quality measures were applied to examine the resolution. A negative bias of more than 40% in the radar rainfall of Gwangdeoksan Radar occurred with changes in the temporal and spatial resolution. However, the negative bias in the radar rainfall of KICT Radar was less than 10%. The mean square error in the radar rainfall of Gwangdeoksan Radar ranged from 5.5 to 0.4 mm(2) h(-2) and the mean square error in the radar rainfall of KICT Radar ranged from 30.2 to 1.5 mm(2) h(-2). The correlation co-efficient of the accumulated time of 30 min was more than 0.7, which increased by 30% from the correlation co-efficient of the accumulated time of 10 min. The bias in the radar rainfall of Gwangdeoksan Radar was still large with changes in the temporal and spatial resolution. However, the radar rainfall of KICT Radar was quantitatively similar to the gauge rainfall, and so the radar rainfall did not need any further quantitative correction.

引用

页码：19 / 30

页数：12

共 35 条

[1]

Anagnostou EN, 2004, J HYDROMETEOROL, V5, P110, DOI 10.1175/1525-7541(2004)005<0110:HREFXP>2.0.CO

[2]

[3]

ANDRIEU H, 1995, J APPL METEOROL, V34, P225, DOI 10.1175/1520-0450(1995)034<0225:IOVPOR>2.0.CO

[4]

[5] Radar calibration - Some simple approaches [J].

Atlas, D .

BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2002, 83 (09) :1313-1316

[6]

Battan L.J., 1973, RADAR OBSERVATION AT, V1st

[7] On the sensitivity of urban hydrodynamic modelling to rainfall spatial and temporal resolution [J].

Bruni, G. ;

Reinoso, R. ;

van de Giesen, N. C. ;

Clemens, F. H. L. R. ;

ten Veldhuis, J. A. E. .

HYDROLOGY AND EARTH SYSTEM SCIENCES, 2015, 19 (02) :691-709

[8] The quantitative precipitation estimation system for Dallas-Fort Worth (DFW) urban remote sensing network [J].

Chen, Haonan ;

Chandrasekar, V. .

JOURNAL OF HYDROLOGY, 2015, 531 :259-271

[9]

Free AD, 2007, 23 C INT INF PROC SY

[10] Rain drop size distribution variability and impact on X-band polarimetric radar retrieval: Results from the AMMA campaign in Benin [J].

Gosset, Marielle ;

Zahiri, Eric-Pascal ;

Moumouni, Sounmaila .

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2010, 136 :243-256

← 1 2 3 4 →