利用QuikSCAT风资料对季风低气压中尺度预报的改进:以印度为例

P. Sinha, A. Chandrasekar
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引用次数: 3

摘要

西南印度季风在孟加拉湾上空形成季风洼地,为该国东部和中部地区提供了丰富的降雨。由于这些低气压形成于海上,这是一个数据匮乏的地区,卫星数据只能提供气象系统的信息来源。此外,对于短期预测,准确的初始条件对于更好的模型性能至关重要。在这项研究中,利用快速散射计(QuikSCAT)数据的三维变分(3DVAR)同化效应,利用天气研究与预报(WRF)模式系统模拟了2006年9月2-5日和9月27-30日形成的两个季风低气压(MDs)。国家环境预报中心-全球预报(NCEP-GFS)场用于初始和侧向边界条件。本研究采用两个模型运行;第一次是没有任何数据同化的控制(CTRL)或基础运行,另一次是使用3DVAR同化来同化QuikSCAT数据的3DVAR运行。两次运行的模式结果相互比较,并与热带降雨测量任务(TRMM)观测和全球分析(GFS-ANL)场进行了比较。季风低气压相对涡度的时间和面积平均垂直廓线结果表明,3DVAR与GFS-ANL的吻合程度比CTRL更接近。此外,3DVAR运行更好地模拟了众所周知的季风低压(低层冷核和高层暖核)的温度结构。虽然摄取QuikSCAT数据对2006年9月27日至30日形成的低气压的模拟降水有明显而显著的积极影响,但对2006年9月2日至5日形成的另一个低气压,QuikSCAT同化对模拟降水的改善作用很小。与上述观察结果一致,对于吸收了QuikSCAT观测数据的模型运行,在技能得分的定量测量方面有明显的改进,偏差更低,假警报更低,几乎所有降雨阈值的检测概率更高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improvement of Mesoscale Forecasts of Monsoon Depressions Through Assimilation of QuikSCAT Wind Data: Two Case Studies Over India
Monsoon depressions form during the Southwest Indian Monsoon over the Bay of Bengal and provide copious rainfall over the eastern and central parts of the country. Since these depressions form over sea, a region of data scarcity, satellite data provides only source of information of the meteorological system. Furthermore, for short-range prediction, it is extremely important to have accurate initial conditions for better model performance. In this study, effects of three dimensional variational (3DVAR) assimilation of the Quick Scatterometer (QuikSCAT) data is used in the simulation of two monsoon depressions (MDs) that formed during 2-5 September and 27-30 September 2006 using the Weather Research and Forecast (WRF) modeling system. The National Center for Environmental Prediction - Global Forecast (NCEP-GFS) fields were used for the initial and lateral boundary conditions. Two model runs were employed in this study; first a control (CTRL) or a base run without any data assimilation and another a 3DVAR run in which QuikSCAT data was assimilated using the 3DVAR assimilation. The model results from both runs were compared with one another as well as with Tropical Rainfall Measurement Mission (TRMM) observations and Global Analysis (GFS-ANL) fields. The results of the time and area averaged vertical profile of relative vorticity over monsoon depressions indicate that the 3DVAR run is in closer agreement with GFS-ANL as compared to the CTRL run. Furthermore, the well-known temperature structure of a monsoon depression (cold core at low levels and warm core at upper levels) is better simulated by the 3DVAR run. While there is a clear and marked positive impact of ingesting the QuikSCAT data in terms of simulated precipitation for the depression that formed during 27-30 September 2006, improvement in the simulated rainfall due to QuikSCAT assimilation is slight for the other depression that formed during 2-5 September 2006. Consistent with the above observations, there is a clear improvement in the quantitative measures of the skill scores with lower bias, lower false alarms and higher probability of detection for almost all rainfall thresholds for the model runs which have assimilated the QuikSCAT observations.
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