globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-012-1440-y
Scopus记录号: 2-s2.0-84875757960
论文题名:
Simulating the impact of the large-scale circulation on the 2-m temperature and precipitation climatology
作者: Bowden J.H.; Nolte C.G.; Otte T.L.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2013
卷: 40, 期:2017-07-08
起始页码: 1903
结束页码: 1920
语种: 英语
英文关键词: Analysis nudging ; Bermuda high ; Interior grid nudging ; Regional climate modeling ; Spectral nudging
英文摘要: The impact of the simulated large-scale atmospheric circulation on the regional climate is examined using the Weather Research and Forecasting (WRF) model as a regional climate model. The purpose is to understand the potential need for interior grid nudging for dynamical downscaling of global climate model (GCM) output for air quality applications under a changing climate. In this study we downscale the NCEP-Department of Energy Atmospheric Model Intercomparison Project (AMIP-II) Reanalysis using three continuous 20-year WRF simulations: one simulation without interior grid nudging and two using different interior grid nudging methods. The biases in 2-m temperature and precipitation for the simulation without interior grid nudging are unreasonably large with respect to the North American Regional Reanalysis (NARR) over the eastern half of the contiguous United States (CONUS) during the summer when air quality concerns are most relevant. This study examines how these differences arise from errors in predicting the large-scale atmospheric circulation. It is demonstrated that the Bermuda high, which strongly influences the regional climate for much of the eastern half of the CONUS during the summer, is poorly simulated without interior grid nudging. In particular, two summers when the Bermuda high was west (1993) and east (2003) of its climatological position are chosen to illustrate problems in the large-scale atmospheric circulation anomalies. For both summers, WRF without interior grid nudging fails to simulate the placement of the upper-level anticyclonic (1993) and cyclonic (2003) circulation anomalies. The displacement of the large-scale circulation impacts the lower atmosphere moisture transport and precipitable water, affecting the convective environment and precipitation. Using interior grid nudging improves the large-scale circulation aloft and moisture transport/precipitable water anomalies, thereby improving the simulated 2-m temperature and precipitation. The results demonstrate that constraining the RCM to the large-scale features in the driving fields improves the overall accuracy of the simulated regional climate, and suggest that in the absence of such a constraint, the RCM will likely misrepresent important large-scale shifts in the atmospheric circulation under a future climate. © 2012 Springer-Verlag (outside the USA).
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/55043
Appears in Collections:过去全球变化的重建

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作者单位: U.S. EPA National Exposure Research Laboratory, Research Triangle Park, NC, United States; University of North Carolina, Chapel Hill, NC, United States

Recommended Citation:
Bowden J.H.,Nolte C.G.,Otte T.L.. Simulating the impact of the large-scale circulation on the 2-m temperature and precipitation climatology[J]. Climate Dynamics,2013-01-01,40(2017-07-08)
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