Analysis and evaluation of Observing System Simulation Experiments (OSSEs) forecast data for Indian summer monsoon

M. Deshpande, P. Mukhopadhyay, M. Masutani, Zaizhong Ma, L. Riishojgaard, M. Hardesty, D. Emmitt, T. N. Krishnamurti, B. Goswami
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Abstract

An attempt is made here to evaluate the skill of forecast during boreal summer monsoon regime over the Indian region using the Observation Simulation System Experiment (OSSE) with Doppler Wind LIDAR (DWL) onboard International Space Station (ISS), assimilated in the initial condition. Through various techniques such as pattern correlation, root mean square error etc, we found that there is some positive impact of assimilating the DWL data on the forecast particularly at the lower tropospheric level. Impact on lowering the RMSE is seen for wind fields in the 850 and 500 hPa over Indian domain but not much impact is seen over larger domain. The moisture field and cloud also show marginal impact due to assimilation of DWL. This indicates that possibly due to lower spatial resolution of DWL data and more data gap over Indian and surrounding oceanic region, the impact on forecast is less. However, it shows the promise that monsoon being a convectively coupled system; increase in spatial data by DWL may better resolve the low level wind and subsequently the low level shear which is important for convection trigger in boundary layer.
印度夏季风观测系统模拟试验(OSSEs)预报资料分析与评价
本文利用国际空间站(ISS)机载多普勒风激光雷达(DWL)的观测模拟系统实验(OSSE),在初始条件下同化,对印度地区北方夏季风状态的预报能力进行了评价。通过模式相关、均方根误差等技术分析,我们发现同化DWL资料对对流层低层的预报有一定的积极影响。在印度地区,850和500 hPa风场对RMSE的降低有影响,但在更大的地区没有太大影响。由于DWL的同化,水汽场和云也表现出边际影响。这说明可能是由于DWL数据空间分辨率较低,印度洋及周边海域数据差距较大,对预报影响较小。然而,它显示了季风是对流耦合系统的前景;DWL增加的空间数据可以更好地解析低层风和低层切变,而低层切变是触发边界层对流的重要因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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