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Numerical simulations of fractional vegetation coverage influences on the convective environment over the source region of the Yellow River

机译:植被覆盖率对黄河源区对流环境影响的数值模拟

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The spatial distribution of fractional vegetation coverage (FVC) over the source region of the Yellow River (SRYR) shows heterogeneity and has changed much for vegetation degradation during the past 30 years. In this paper, three numerical tests were conducted using the Weather Research and Forecasting (WRF) model for a fair weather case and a rainy case over the SRYR. The first test used FVC derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) data, the second test took a spatial constant FVC (=50 %), and the last one deployed the model default FVC. The results showed that simulated 2-m height potential temperature decreased and specific humidity increased as FVC increased for both cases. The magnitudes of the sensible and latent heat fluxes were different over the wetland at the fair day and the rainy day. There was a divergence center near the Zoige wetland in the fair weather case but a convergent center in the rainy case. As a conclusion, when the default FVC in the WRF model were replaced by the new MODIS-derived FVC data, the root-mean-square errors (RMSEs) between measurements and the simulated 2-m height air temperature and relative humidity decreased for both cases, the mean RMSEs between measurements and the simulated 2-m height air temperature and relative humidity declined by 0.3 K and 3.0 % in the fair day, 0.4 K and 3.4 % in the rainy case. The mean differences of simulated precipitation for seven ground stations were 1.1 mm for the fair day and 4.2 mm for the rainy case. Therefore, the updated MODIS FVC has influences on the convective environment over the SRYR.
机译:在过去的30年中,黄河源区(SRYR)上的部分植被覆盖度(FVC)的空间分布表现出异质性,并且发生了很大的变化。在本文中,使用天气研究和预报(WRF)模型对SRYR上的晴天和雨天进行了三个数值测试。第一个测试使用从中等分辨率成像光谱仪(MODIS)数据得出的FVC,第二个测试采用空间常数FVC(= 50%),最后一个测试使用模型默认FVC。结果表明,两种情况下,随着FVC的增加,模拟的2 m高位势温度降低,比湿度增加。在晴天和雨天,湿地的感热通量和潜热通量的大小都不同。在天气晴朗的情况下,若尔热湿地附近有一个发散中心,而在雨天的情况中有一个发散中心。结论是,当用新的MODIS衍生的FVC数据代替WRF模型中的默认FVC时,测量值与模拟的2米高度空气温度和相对湿度之间的均方根误差(RMSE)均降低了在晴天,测量值与模拟的2米高的气温和相对湿度之间的平均RMSE下降了0.3 K和3.0%,在雨天下降了0.4 K和3.4%。七个地面站的模拟降水平均差在晴天为1.1 mm,在雨天为4.2 mm。因此,更新的MODIS FVC对SRYR上的对流环境有影响。

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