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Validation of INSAT-3D Atmospheric Motion Vectors for Monsoon 2015

机译:2015年季风INSAT-3D大气运动矢量的验证

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Atmospheric Motion Vector (AMV) over Indian Ocean and surrounding region is one of the most important sources of tropospheric wind information assimilated in numerical weather prediction (NWP) system. Earlier studies showed that the quality of Indian geo-stationary satellite Kalpana-1 AMVs was not comparable to that of other geo-stationary satellites over this region and hence not used in NWP system. Indian satellite INSAT-3D was successfully launched on July 26, 2013 with upgraded imaging system as compared to that of previous Indian satellite Kalpana-1. INSAT-3D has middle infrared band (3.80 - 4.00 μm) which is capable of night time pictures of low clouds and fog. Three consecutive images of 30-minutes interval are used to derive the AMVs. New height assignment scheme (using NWP first guess and replacing old empirical GA method) along with modified quality control scheme were implemented for deriving INSAT-3D AMVs. In this paper an attempt has been made to validate these AMVs against in-situ observations as well as against NCMRWF's NWP first guess for monsoon 2015. AMVs are subdivided into three different pressure levels in the vertical viz. low (1000 - 700 hPa), middle (700 - 400 hPa) and high (400 - 100 hPa) for validation purpose. Several statistics viz. normalized root mean square vector difference; biases etc. have been computed over different latitudinal belt. Result shows that the general mean monsoon circulations along with all the transient monsoon systems are well captured by INSAT-3D AMVs, as well as the error statistics viz., RMSE etc of INSAT-3D AMVs is now comparable to other geostationary satellites.
机译:印度洋及周边地区的大气运动矢量(AMV)是数值天气预报(NWP)系统中吸收的对流层风信息的最重要来源之一。较早的研究表明,印度对地静止卫星Kalpana-1 AMV的质量无法与该地区其他对地静止卫星相提并论,因此未在NWP系统中使用。印度卫星INSAT-3D已于2013年7月26日成功发射,其成像系统与之前的印度卫星Kalpana-1相比已升级。 INSAT-3D具有中红外波段(3.80-4.00μm),可用于夜间低云和雾的照片。 30分钟间隔的三个连续图像用于导出AMV。实施了新的高度分配方案(使用NWP首先猜测并替换了旧的经验GA方法)以及改进的质量控制方案,以得出INSAT-3D AMV。在本文中,我们尝试通过现场观测以及NCMRWF针对2015年季风的NWP首次验证来验证这些AMV。AMV在垂直方向上分为三个不同的压力水平。低(1000-700 hPa),中(700-400 hPa)和高(400-100 hPa)进行验证。几个统计信息。归一化均方根矢量差;在不同的纬度带上已计算出偏差等。结果表明,INSAT-3D AMV很好地捕获了一般平均季风环流以及所有瞬态季风系统,INSAT-3D AMV的误差统计值,RMSE等现在可以与其他地球静止卫星相媲美。

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