Climate Change Data Portal
DOI | 10.1007/s00382-020-05359-3 |
Benefits and added value of convection-permitting climate modeling over Fenno-Scandinavia | |
Lind P.; Belušić D.; Christensen O.B.; Dobler A.; Kjellström E.; Landgren O.; Lindstedt D.; Matte D.; Pedersen R.A.; Toivonen E.; Wang F. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 1893 |
结束页码 | 1912 |
卷号 | 55 |
英文摘要 | Convection-permitting climate models have shown superior performance in simulating important aspects of the precipitation climate including extremes and also to give partly different climate change signals compared to coarser-scale models. Here, we present the first long-term (1998–2018) simulation with a regional convection-permitting climate model for Fenno-Scandinavia. We use the HARMONIE-Climate (HCLIM) model on two nested grids; one covering Europe at 12 km resolution (HCLIM12) using parameterized convection, and one covering Fenno-Scandinavia with 3 km resolution (HCLIM3) with explicit deep convection. HCLIM12 uses lateral boundaries from ERA-Interim reanalysis. Model results are evaluated against reanalysis and various observational data sets, some at high resolutions. HCLIM3 strongly improves the representation of precipitation compared to HCLIM12, most evident through reduced “drizzle” and increased occurrence of higher intensity events as well as improved timing and amplitude of the diurnal cycle. This is the case even though the model exhibits a cold bias in near-surface temperature, particularly for daily maximum temperatures in summer. Simulated winter precipitation is biased high, primarily over complex terrain. Considerable undercatchment in observations may partly explain the wet bias. Examining instead the relative occurrence of snowfall versus rain, which is sensitive to variance in topographic heights it is shown that HCLIM3 provides added value compared to HCLIM12 also for winter precipitation. These results, indicating clear benefits of convection-permitting models, are encouraging motivating further exploration of added value in this region, and provide a valuable basis for impact studies. © 2020, The Author(s). |
英文关键词 | Convection-permitting climate modeling; Diurnal cycle; Extremes; Fenno-Scandinavia; HARMONIE-climate; Precipitation |
语种 | 英语 |
scopus关键词 | atmospheric convection; climate change; climate modeling; computer simulation; image resolution; parameterization; precipitation (climatology); regional climate; Fennoscandia |
来源期刊 | Climate Dynamics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/145334 |
作者单位 | Rossby Centre, Swedish Meteorological and Hydrological Institute, Folkborgsvägen 17, Norrköping, 60176, Sweden; Danish Meteorological Institute, Copenhagen, Denmark; Norwegian Meteorological Institute, Oslo, Norway; University of Copenhagen, Copenhagen, Denmark; Finnish Meteorological Institute, Helsinki, Finland |
推荐引用方式 GB/T 7714 | Lind P.,Belušić D.,Christensen O.B.,et al. Benefits and added value of convection-permitting climate modeling over Fenno-Scandinavia[J],2020,55. |
APA | Lind P..,Belušić D..,Christensen O.B..,Dobler A..,Kjellström E..,...&Wang F..(2020).Benefits and added value of convection-permitting climate modeling over Fenno-Scandinavia.Climate Dynamics,55. |
MLA | Lind P.,et al."Benefits and added value of convection-permitting climate modeling over Fenno-Scandinavia".Climate Dynamics 55(2020). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。