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首页> 外文期刊>Advances in space research >Study of tropospheric delay over Indian region from MODIS, NCEP/NCAR data and ground based water vapor measurements at Kolkata
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Study of tropospheric delay over Indian region from MODIS, NCEP/NCAR data and ground based water vapor measurements at Kolkata

机译:根据MODIS,NCEP / NCAR数据和加尔各答地面水汽测量结果,研究印度对流层对流层延迟

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A priori estimation of delays with error variance of atmospheric radio wave propagation is important for precise position estimation and integrity of the system like Global Positioning System (GPS). Tropospheric effects are less severe than the ionospheric counterpart, but behave in a complex manner, making it difficult to isolate them. In this present paper, a ground based radiometer has been utilized to study the characteristics of tropospheric delay and compared it with the MODIS satellite observations over Kolkata (22.57°N, 88.37°E). Results indicate a good agreement between radiometer and MODIS data except the monsoon months. A climatology of spatial and temporal variation of dry and wet tropospheric delay over the Indian subcontinent have also been estimated using MODIS data and NCEP-NCAR reanalysis data for 2008-2012. The spatial variations of dry delay over Indian region are observed to be in the range of 120-250 cm with limited seasonal variability. However, the wet delay varies from 20 cm in winter months to 45 cm during monsoon period in the coastal and central Indian region. Further analysis reveals that the contribution of wet delays in total delay is significant only along the Indo-Gangetic plain. This indicates that extra precaution is needed in handling tropospheric delay for this region due to fast varying nature of water vapor.
机译:具有大气无线电波传播误差方差的延迟的先验估计对于精确的位置估计和像全球定位系统(GPS)这样的系统的完整性很重要。对流层效应没有电离层效应严重,但其作用方式复杂,难以隔离。在本文中,地面辐射计已被用于研究对流层延迟的特征,并将其与MODIS卫星在加尔各答(22.57°N,88.37°E)上的观测结果进行了比较。结果表明,除季风月份外,辐射计与MODIS数据之间的一致性很好。还使用MODIS数据和NCEP-NCAR再分析数据(2008-2012年)估算了印度次大陆上干对流层和湿对流层延迟的时空变化气候学。在印度地区,干旱延迟的空间变化在120-250 cm范围内,季节性变化有限。然而,在印度沿海和中部地区,湿延迟时间从冬季的20厘米到季风期的45厘米不等。进一步的分析表明,湿延迟在总延迟中的贡献仅在沿印度—恒河平原地区才有意义。这表明由于水蒸气的快速变化性质,在处理该区域的对流层延迟时需要采取额外的预防措施。

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