Monsoonal precipitation over Peninsular Malaysia in the CMIP6 HighResMIP experiments: the role of model resolution

被引:24
|
作者
Liang, Ju [1 ]
Tan, Mou Leong [2 ]
Hawcroft, Matthew [3 ,4 ]
Catto, Jennifer L. [1 ]
Hodges, Kevin I. [5 ]
Haywood, James M. [1 ,3 ]
机构
[1] Univ Exeter, Coll Engn Math & Phys Sci, Exeter EX4 4QE, Devon, England
[2] Univ Sains Malaysia, Sch Humanities, Geog Sect, GeoInformat Unit, Usm Pulau Pinang 11800, Malaysia
[3] Met Off, Exeter EX1 3PB, Devon, England
[4] Univ Southern Queensland, Toowoomba, Qld 4300, Australia
[5] Univ Reading, Dept Meteorol, Reading RG6 6ET, Berks, England
基金
英国自然环境研究理事会;
关键词
CMIP6; HighResMIP; Precipitation; Peninsular Malaysia; Model resolution; REGIONAL CLIMATE; VERTICAL RESOLUTION; MARITIME CONTINENT; EXTREME PRECIPITATION; HORIZONTAL RESOLUTION; SOUTHEAST-ASIA; DIURNAL CYCLE; WINTER MONSOON; EAST-COAST; RAINFALL;
D O I
10.1007/s00382-021-06033-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study investigates the ability of 20 model simulations which contributed to the CMIP6 HighResMIP to simulate precipitation in different monsoon seasons and extreme precipitation events over Peninsular Malaysia. The model experiments utilize common forcing but are run with different horizontal and vertical resolutions. The impact of resolution on the models' abilities to simulate precipitation and associated environmental fields is assessed by comparing multi-model ensembles at different resolutions with three observed precipitation datasets and four climate reanalyses. Model simulations with relatively high horizontal and vertical resolution exhibit better performance in simulating the annual cycle of precipitation and extreme precipitation over Peninsular Malaysia and the coastal regions. Improvements associated with the increase in horizontal and vertical resolutions are also found in the statistical relationship between precipitation and monsoon intensity in different seasons. However, the increase in vertical resolution can lead to a reduction of annual mean precipitation compared to that from the models with low vertical resolutions, associated with an overestimation of moisture divergence and underestimation of lower-tropospheric vertical ascent in the different monsoon seasons. This limits any improvement in the simulation of precipitation in the high vertical resolution experiments, particularly for the Southwest monsoon season.
引用
收藏
页码:2783 / 2805
页数:23
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