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Indian Ocean surface winds from NCMRWF analysis as compared to QuikSCAT and moored buoy winds

机译:来自NCMRWF分析的印度洋地表风与QuikSCAT和系泊浮标风的比较

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The quality of the surface wind analysis at the National Centre for Medium Range Weather Forecasts (NCMRWF), New Delhi over the tropical Indian Ocean and its improvement in 2001 are examined by comparing it with in situ buoy measurements and satellite derived surface winds from NASA QuikSCAT satellite (QSCT) during 1999, 2000 and 2001. The NCMRWF surface winds su ered from easterly bias of 1.0-1.5 ms-1 in the equatorial Indian Ocean (IO) and northerly bias of 2.0-3.0 ms-1 in the south equatorial IO during 1999 and 2000 compared to QSCT winds. The amplitude of daily variability was also underestimated compared to that in QSCT. In particular, the amplitude of daily variability of NCMRWF winds in the eastern equatorial IO was only about 60% of that of QSCT during 1999 and 2000. The NCMRWF surface winds during 2001 have significantly improved with the bias of the mean analyzed winds considerably reduced everywhere bringing it to within 0.5 ms-1 of QSCT winds in the equatorial IO. The amplitude and phase of daily and intraseasonal variability are very close to that in QSCT almost everywhere during 2001. It is shown that the weakness in the surface wind analysis during 1999 and 2000 and its improvement in 2001 are related to the weakness in simulation of precipitation by the forecast model in the equatorial IO and its improvement in 2001.
机译:通过将其与原位浮标测量值和来自NASA QuikSCAT的卫星得出的地表风进行比较,检验了新德里国家热带海洋上空的新德里国家中型天气预报中心(NCMRWF)的地表风分析质量及其在2001年的改进。卫星(QSCT)在1999年,2000年和2001年期间发生。NCMRWF地表风受到赤道印度洋(IO)的东偏1.0-1.5 ms-1和南赤道IO的北偏2.0-3.0 ms-1的影响与QSCT风相比,在1999年和2000年期间。与QSCT相比,每日变化幅度也被低估了。特别是,赤道东部IO的NCMRWF风的日变化幅度在1999年和2000年仅为QSCT的60%左右。2001年期间NCMRWF地表风有了明显改善,平均分析风的偏差在各个地方都大大减小了使它达到赤道IO的QSCT风的0.5 ms-1之内。每日和季节内变化的幅度和相位在2001年几乎所有地方都与QSCT的非常接近。表明1999和2000年的地面风分析的弱点和2001年的改进与降水模拟中的弱点有关赤道IO的预报模型及其2001年的改进。

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