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Articles

Mitigating atmospheric effects in InSAR measurements through high-resolution data assimilation and numerical simulations with a weather prediction model

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Pages 2129-2147 | Received 30 Oct 2014, Accepted 30 Jan 2015, Published online: 20 Apr 2015
 

Abstract

Repeat-pass spaceborne interferometric synthetic aperture radar (InSAR) is commonly used to measure surface deformation; phase delays due to atmospheric water vapour may have significant impact on the accuracy of these measurements. In recent years, there has been a growing interest in using forecasts and analyses from numerical weather prediction (NWP) models – which can provide good estimates of the atmospheric state – to correct for atmospheric phase delays. In this study, three separate estimates of atmospheric water vapour content from NWP output are used in combination with Environmental Satellite (Envisat) Advanced Synthetic Aperture Radar (ASAR) data over the Pearl River Delta region in South China to mitigate atmospheric distortion. The NWP-based estimates are derived from: (1) interpolation of National Centers for Environmental Prediction (NCEP) Final Operational Global Analysis (FNL) data; (2) Weather Research and Forecasting (WRF) model simulations initialized with FNL analysis without additional data assimilation; and (3) WRF simulations initialized with a three-dimensional variational (3DVar) data assimilation system that ingests additional meteorological observations. The accuracy of the atmospheric corrections from these different NWP model outputs is further verified quantitatively with precipitable water vapour (PWV) data from several ground-based global positioning system (GPS) stations in Hong Kong. Inter-comparison shows a good agreement between the PWV derived from the WRF-3DVar simulations and the GPS measurements, suggesting that atmospheric correction by convection-permitting WRF simulations initialized with mesoscale data assimilation may effectively mitigate atmospheric distortion in InSAR measurements, especially for coastal areas.

Acknowledgements

The InSAR data were provided by the European Space Agency via the ESA-MOST Dragon 3 Cooperation Program (ID: 10665). The GPS data were provided by Hong Kong Satellite Positioning Reference Station Network. The NCEP GFS-FNL data are available via the NCAR Research Data Archive (NCEP 2000). The simulation computing was performed at the Texas Advanced Computing Center (TACC). The authors sincerely acknowledge and thank Yonghui Weng, Yue Ying, and Yunji Zhang at Pennsylvania State University and Jian Jiao, Xi’ai Cui, and Siting Xiong at Peking University for their help and invaluable contributions. We also sincerely appreciate the kind suggestions and comments from the reviewer and the editor.

Additional information

Funding

This work was supported by the National Natural Science Foundation of China [41171267] and the National Science and Technology Support Programme of China [2012BAH29B03]. The first author is jointly supported by the Chinese Scholarship Council (CSC) and Pennsylvania State University.

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