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Effect of Horizontal Resolution on the Representation of the Global Monsoon Annual Cycle in AGCMs

机译:水平分辨率对AGCM中全球季风年周期表示的影响

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摘要

The sensitivity of the representation of the global monsoon annual cycle to horizontal resolution is compared in three AGCMs:the Met Office Unified Model-Global Atmosphere 3.0;the Meteorological Research Institute AGCM3;and the Global High Resolution AGCM from the Geophysical Fluid Dynamics Laboratory.For each model,we use two horizontal resolution configurations for the period 1998-2008.Increasing resolution consistently improves simulated precipitation and low-level circulation of the annual mean and the first two annual cycle modes,as measured by the pattern correlation coefficient and equitable threat score.Improvements in simulating the summer monsoon onset and withdrawal are region-dependent.No consistent response to resolution is found in simulating summer monsoon retreat.Regionally,increased resolution reduces the positive bias in simulated annual mean precipitation,the two annual-cycle modes over the West African monsoon and Northwestern Pacific monsoon.An overestimation of the solstitial mode and an underestimation of the equinoctial asymmetric mode of the East Asian monsoon are reduced in all high-resolution configurations.Systematic errors exist in lower-resolution models for simulating the onset and withdrawal of the summer monsoon.Higher resolution models consistently improve the early summer monsoon onset over East Asia and West Africa,but substantial differences exist in the responses over the Indian monsoon region,where biases differ across the three low-resolution AGCMs.This study demonstrates the importance of a multi-model comparison when examining the added value of resolution and the importance of model physical parameterizations for simulation of the Indian monsoon.
机译:在以下三个AGCM中比较了全球季风年周期表示对水平分辨率的敏感性:Met Office统一模型-全球大气3.0;气象研究所AGCM3;以及地球物理流体动力学实验室的全球高分辨率AGCM。在1998-2008年期间,每个模型都使用两个水平分辨率配置。通过模式相关系数和公平威胁评分来衡量,提高分辨率会持续改善年平均模式和前两个年度周期模式的模拟降水和低空环流。模拟夏季季风起伏和撤出的改进取决于区域。模拟夏季季风后退没有发现对分辨率的一致响应。区域分辨率的提高减少了模拟年平均降水量的正偏差,这两个区域的整个年周期模式西非季风和西北太平洋季风在所有高分辨率构造中,东亚季风的孤立模式和对等对称非对称模式的低估都被减少了。在模拟夏季季风的爆发和退缩的低分辨率模型中存在系统误差。东亚和西非发生了初夏季风,但印度季风地区的响应存在实质性差异,三个低分辨率AGCM的偏差都不同。这项研究表明,在检查附加项时进行多模型比较的重要性分辨率的价值以及模拟印度季风的模型物理参数化的重要性。

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  • 来源
    《大气科学进展(英文版)》 |2018年第8期|1003-1020|共18页
  • 作者单位

    LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters,Nanjing University of Information Science & Technology, Nanjing 210044, China;

    LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China;

    National Centre for Atmospheric Science and Department of Meteorology, University of Reading,Reading RG6 6BB, United Kingdom;

    Met Office Hadley Centre, Exeter, EX1 3PB, United Kingdom;

    Met Office Hadley Centre, Exeter, EX1 3PB, United Kingdom;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
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  • 入库时间 2022-08-19 03:55:46
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