Evaluation of downscaled wind speeds and parameterised gusts for recent and historical windstorms in Switzerland

被引:25
作者
Stucki, Peter [1 ,2 ]
Dierer, Silke [3 ]
Welker, Christoph [1 ,2 ,4 ,5 ]
Gomez-Navarro, Juan Jose [1 ,6 ]
Raible, Christoph C. [1 ,6 ]
Martius, Olivia [1 ,2 ,4 ]
Bronnimann, Stefan [1 ,2 ]
机构
[1] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland
[2] Univ Bern, Inst Geog, Bern, Switzerland
[3] Meteotest, Bern, Switzerland
[4] Mobiliar Lab Nat Risks, Bern, Switzerland
[5] GVZ Gebaudeversicherung Kanton Zurich, Zurich, Switzerland
[6] Univ Bern, Inst Phys, Climate & Environm Phys, CH-3012 Bern, Switzerland
关键词
dynamical downscaling; 20CR; ERA-Interim; wind speed; wind gust estimation; extreme event; hazard map; Alps; gust factor; risk; WRF wind evaluation; REGIONAL CLIMATE MODEL; WINTER STORMS; 20TH-CENTURY REANALYSIS; SURFACE WIND; EXTREME; PERFORMANCE;
D O I
10.3402/tellusa.v68.31820
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Assessments of local-scale windstorm hazard require highly resolved spatial information on wind speeds and gusts. In this study, maximum (peak) sustained wind speeds on a 3-km horizontal grid over Switzerland are obtained by dynamical downscaling from the Twentieth Century Reanalysis (20CR) employing the Weather Research and Forecasting (WRF) model. Subsequently, simulated peak gusts are derived using four wind gust parameterizations (WGPs). Evaluations against observations at 63 locations in complex terrain include four high-impact windstorms (occurring in 1919, 1935, 1990, and 1999) and 14 recent windstorms (occurring between 1993 and 2011). Peak sustained wind speeds and directions are generally well simulated, although wind speeds are mostly overestimated. In general, performance and skill measures are best for locations on the Swiss Plateau and inferior for Alpine mountain and valley locations. An independent ERA-Interim WRF downscaling configuration produces overall comparable results, implying that the 20CR ensemble mean is a reliable data set in dynamical downscaling exercises. The four evaluated WGPs largely reproduce the observed gustiness, although the timing and magnitude of the peak gusts are not regularly captured. None of the WGPs stands out as single best for the complex topography of Switzerland. Differences among the WGPs are small compared to the biases inherited from the sustained-wind part in the WGP formulations. All WGPs transform overestimated peak sustained winds into underestimated peak gusts, which points to an underrepresentation of the turbulent part in the WGP formulations. The range of simulated peak gusts from downscaling all 20CR ensemble members does not reliably include the observed peak gust, indicating limited benefit in applying an ensemble approach. Despite the limitations, we infer that with spatial optimisations of the simulation (e.g. by bias correction or adaptation of the WGP schemes), downscaling of 20CR input is an efficient option for high-resolution assessments of windstorm hazard and risk in Switzerland.
引用
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页数:18
相关论文
共 59 条
[1]   Mean gust factors in complex terrain [J].
Agústsson, H ;
Olafsson, H .
METEOROLOGISCHE ZEITSCHRIFT, 2004, 13 (02) :149-155
[2]   Forecasting wind gusts in complex terrain [J].
Agustsson, H. ;
Olafsson, H. .
METEOROLOGY AND ATMOSPHERIC PHYSICS, 2009, 103 (1-4) :173-185
[3]   Estimation of bora wind gusts using a limited area model [J].
Belusic, D ;
Klaic, ZB .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2004, 56 (04) :296-307
[4]  
Benjamin S.G., 2002, NWS TECHNICAL PROCED, P1
[5]   Wind gust estimation for Mid-European winter storms: towards a probabilistic view [J].
Born, Kai ;
Ludwig, Patrick ;
Pinto, Joaquim G. .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2012, 64
[6]  
Brasseur O, 2001, MON WEATHER REV, V129, P5, DOI 10.1175/1520-0493(2001)129<0005:DAAOAP>2.0.CO
[7]  
2
[8]   Extreme winds at northern mid-latitudes since 1871 [J].
Broennimann, S. ;
Martius, O. ;
von Waldow, H. ;
Welker, C. ;
Luterbacher, J. ;
Compo, G. P. ;
Sardeshmukh, P. D. ;
Usbeck, T. .
METEOROLOGISCHE ZEITSCHRIFT, 2012, 21 (01) :13-27
[9]  
Bronnimann S., 2013, WEATHER EXTREMES 140, VG89, P7, DOI [10.4480/GB2013.G89.01, DOI 10.4480/GB2013.G89.01]
[10]  
Bronnimann S., 2014, PHYS UNSERER Z, V45, P84