Climatology of Near-Surface Daily Peak Wind Gusts Across Scandinavia: Observations and Model Simulations

被引:5
|
作者
Minola, Lorenzo [1 ]
Azorin-Molina, Cesar [2 ]
Guijarro, Jose A. [3 ]
Zhang, Gangfeng [4 ,5 ,6 ]
Son, Seok-Woo [7 ]
Chen, Deliang [1 ]
机构
[1] Univ Gothenburg, Dept Earth Sci, Reg Climate Grp, Gothenburg, Sweden
[2] CSIC, CIDE, Ctr Invest Desertificac, Valencia, Spain
[3] State Meteorol Agcy AEMET, Palma De Mallorca, Spain
[4] Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing, Peoples R China
[5] Beijing Normal Univ, Minist Civil Affairs, Acad Disaster Reduct & Emergency Management, Beijing, Peoples R China
[6] Beijing Normal Univ, Minist Educ, Beijing, Peoples R China
[7] Seoul Natl Univ, Sch Earth & Environm Sci, Seoul, South Korea
基金
瑞典研究理事会; 中国国家自然科学基金;
关键词
SWEDEN; SPEED; HOMOGENIZATION; EUROPE; TRENDS; PART;
D O I
10.1029/2020JD033534
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
An observed daily peak wind gusts (DPWG) dataset over Scandinavia, consisting of time series from 127 meteorological stations across Finland, Norway and Sweden, has been created. This dataset provides high-quality and homogenized near-surface DPWG series for Scandinavia, spanning the longest available time period (1996-2016). The aim of this study is to evaluate the ability of two regional climate models (RCMs) in simulating DPWG winds. According to the observed DPWG climatology, meteorological stations are classified into three regions for which wind conditions are influenced by similar physical processes: coast, inland and mountain. Smaller-scale DPWG features of the three regions are only captured when coarser general circulation models or reanalyses are downscaled by a RCM. Dynamic downscaling is thus needed to achieve more realistic simulations of DPWG when compared to their driving models. The performances of the RCMs are found to be more dependent on model dynamics and physics (such as gust parametrization) than on the boundary conditions provided by the driving models. We also found that the RCMs cannot accurately simulate observed DPWG in inland and mountainous areas, suggesting the need for higher horizontal resolution and/or better representation of relevant boundary-layer processes.
引用
收藏
页数:17
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