Climate Statistics in Global Simulations of the Atmosphere, from 80 to 2.5 km Grid Spacing

IF 2.4 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of the Meteorological Society of Japan Pub Date : 2020-04-01 DOI:10.2151/JMSJ.2020-005
C. Hohenegger, L. Kornblueh, D. Klocke, T. Becker, G. Cioni, J. F. Engels, Uwe Schulzweida, B. Stevens
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引用次数: 64

Abstract

Basic climate statistics, such as water and energy budgets, location and width of the Intertropical Convergence Zone (ITCZ), trimodal tropical cloud distribution, position of the polar jet, and land sea contrast, remain either biased in coarse-resolution general circulation models or are tuned. Here, we examine the horizontal resolution dependency of such statistics in a set of global convection-permitting simulations integrated with the ICOsahedral Non-hydrostatic (ICON) model, explicit convection, and grid spacings ranging from 80 km down to 2.5 km. The impact of resolution is quantified by comparing the resolution-induced differences to the spread obtained in an ensemble of eight distinct global storm-resolving models. Using this metric, we find that, at least by 5 km, the resolution-induced differences become smaller than the spread in 26 out of the 27 investigated statistics. Even for nine (18) of these statistics, a grid spacing of 80 (10) km does not lead to significant differences. Resolution down to 5 km matters especially for net shortwave radiation, which systematically increases with the resolution because of reductions in the low cloud amount over the subtropical oceans. Further resolution dependencies can be found in the land-to-ocean precipitation ratio, in the latitudinal position and width of the Pacific ITCZ, and in the longitudinal position of the Atlantic ITCZ. In addition, in the tropics, the deep convective cloud population systematically increases at the expense of the shallow one, whereas the partition of congestus clouds remains fairly constant. Finally, refining the grid spacing systematically moves the simulations closer to observations, but climate statistics exhibiting weaker resolution dependencies are not necessarily associated with smaller biases. Corresponding author: Cathy Hohenegger, Max Planck Institute for Meteorology, Bundesstrasse 53, 20146 Hamburg, Germany E-mail: cathy.hohenegger@mpimet.mpg.de J-stage Advance Published Date: 10 November 2019 Journal of the Meteorological Society of Japan Vol. 98, No. 1 74
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全球大气模拟中的气候统计,从80到2.5公里网格间距
基本气候统计数据,如水和能源预算、热带辐合带(ITCZ)的位置和宽度、三模态热带云分布、极地急流的位置和陆海对比,在粗分辨率的环流模型中仍然存在偏差,或者进行了调整。在这里,我们在一组全球对流允许模拟中检查了这些统计数据的水平分辨率相关性,这些模拟与二十面体非流体静力(ICON)模型、显式对流和80公里至2.5公里的网格间距相结合。通过将分辨率引起的差异与在八个不同的全球风暴分辨率模型中获得的传播进行比较,可以量化分辨率的影响。使用这个指标,我们发现,在27个调查的统计数据中,有26个统计数据的分辨率引起的差异小于5公里。即使对于这些统计数据中的九(18)个,80(10)km的网格间距也不会导致显著差异。低至5公里的分辨率尤其重要,因为副热带海洋上空的低云量减少,净短波辐射会随着分辨率的增加而系统地增加。在陆地与海洋的降水比、太平洋ITCZ的纬度位置和宽度以及大西洋ITCZ的纵向位置中可以发现进一步的分辨率相关性。此外,在热带地区,深对流云的数量以浅对流云为代价系统地增加,而凝结云的分布保持相当恒定。最后,细化网格间距系统地使模拟更接近观测,但表现出较弱分辨率依赖性的气候统计数据并不一定与较小的偏差有关。通讯作者:Cathy Hohenegger,马克斯·普朗克气象研究所,德国联邦大街5320146,德国汉堡电子邮件:cathy.hohenegger@mpimet.mpg.deJ阶段进展发表日期:2019年11月10日日本气象学会学报第98卷第174期
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来源期刊
Journal of the Meteorological Society of Japan
Journal of the Meteorological Society of Japan 地学-气象与大气科学
CiteScore
6.70
自引率
16.10%
发文量
56
审稿时长
3 months
期刊介绍: JMSJ publishes Articles and Notes and Correspondence that report novel scientific discoveries or technical developments that advance understanding in meteorology and related sciences. The journal’s broad scope includes meteorological observations, modeling, data assimilation, analyses, global and regional climate research, satellite remote sensing, chemistry and transport, and dynamic meteorology including geophysical fluid dynamics. In particular, JMSJ welcomes papers related to Asian monsoons, climate and mesoscale models, and numerical weather forecasts. Insightful and well-structured original Review Articles that describe the advances and challenges in meteorology and related sciences are also welcome.
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