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Investigating the Impact of Climate Change on Dust Storms Over Kuwait by the Middle of the Century Simulated by WRF Dynamical Downscaling.

机译:通过WRF动态降尺度模拟,研究气候变化对本世纪中叶之前科威特沙尘暴的影响。

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摘要

The aim of this study is to examine the impact of climate change on future dust storms in Kuwait. Dust storms are more frequent in summertime in the Arabian Peninsula, and can be highly influential on the climate and the environment in the region. In this study, the influence of climate change in the Middle East and especially in Kuwait was investigated by high-resolution (48, 12, and 4 km grid spacing) dynamic downscaling using the WRF (Weather Research & Forecasting) model. The WRF dynamic downscaling was forced by reanalysis using the National Centers for Environment Prediction (NCEP) model for the years 1997, 2000, and 2008. The downscaling results were first validated by comparing NCEP model outputs with the observational data. The global climate change dynamic downscaling model was run using current WRF regional climate model (RCM) simulations (2006--2010) and WRF-RCM climate simulations of the future (2056--2060). They were used to compare results between the present and the middle of the century. In general, the dominant features from (NCEP) runs were consistent with each other, as well as with WRF-RCM results. The influence of climate change in the Middle East and Kuwait can be projected from the differences between the current and model future run. The average temperature showed a positive trend in the future, as in other studies. The temperature was predicted to increase by around 0.5-2.5 °C over the next 50 years. No significant change in mean sea level pressure patterns was projected. However, amongst other things, a change in the trend of the surface wind speeds was indicated during summertime. As a result, the increase in temperature and the decline in wind speed in the future indicate a reduction in dust storm days in Kuwait by the middle of the century.
机译:这项研究的目的是研究气候变化对科威特未来沙尘暴的影响。夏季,阿拉伯半岛的沙尘暴更为频繁,并且可能对该地区的气候和环境产生重大影响。在这项研究中,使用WRF(天气研究与预报)模型通过高分辨率(48、12和4 km网格间距)动态缩小研究了中东和特别是科威特气候变化的影响。通过使用1997、2000和2008年美国国家环境预测中心(NCEP)模型进行的重新分析,对WRF动态降级进行了强制。降级结果首先通过将NCEP模型输出与观测数据进行比较来验证。使用当前的WRF区域气候模型(RCM)模拟(2006--2010)和未来的WRF-RCM气候模拟(2056--2060)来运行全球气候变化动态降尺度模型。它们被用来比较当前与本世纪中叶之间的结果。通常,(NCEP)运行的主要特征彼此一致,并且与WRF-RCM结果一致。可以从当前运行和未来运行之间的差异来预测气候变化对中东和科威特的影响。像其他研究一样,未来的平均温度显示出正趋势。预计在接下来的50年中,温度将升高约0.5-2.5°C。预计平均海平面压力模式无明显变化。但是,除其他外,夏季期间表明了地面风速趋势的变化。结果,未来温度升高和风速下降表明到本世纪中叶科威特的沙尘暴天数减少。

著录项

  • 作者

    Alsarraf, Hussain.;

  • 作者单位

    The University of Nebraska - Lincoln.;

  • 授予单位 The University of Nebraska - Lincoln.;
  • 学科 Climate change.;Meteorology.;Atmospheric sciences.
  • 学位 Ph.D.
  • 年度 2013
  • 页码 125 p.
  • 总页数 125
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:41:16

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