4.6 Article

High-Resolution Water Vapor Maps Obtained by Merging Interferometric Synthetic Aperture Radar and GPS Measurements

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出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2020JD033430

关键词

atmospheric water vapor; global positioning system (GPS); interferometric synthetic aperture radar (InSAR); precipitable water vapor (PWV); tropospheric delay

资金

  1. National Natural Science Fund for Distinguished Young Scholars [41925016]
  2. National Key R&D Program of China [2018YFC1503603]

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This study introduces a new method for constructing high-resolution PWV maps by fusing InSAR and GPS measurements to address the issue of InSAR observations being unable to build absolute PWV maps. The method was validated in the Southern California region and showed that the CMVE method significantly outperformed conventional methods in constructing high-resolution PWV maps.
Previous research has demonstrated several successful meteorological applications of interferometric synthetic aperture radar (InSAR) by mapping high-resolution precipitable water vapor (PWV) over large areas with satisfactory precision (e.g., 1-2 mm). InSAR, however, can only measure temporal changes in the PWV, that is, the differential PWV (Delta PWV) between two SAR acquisition epochs. The construction of absolute PWV maps using InSAR observations remains an intractable problem. We present here a new method for constructing high-resolution PWV maps by fusing InSAR and global positioning system (GPS) measurements. Our method involves: (1) extracting temporal differences in the zenith wet delays (Delta ZWD) from InSAR observations with the assistance of synchronous GPS measurements, and (2) using a constrained minimum variance estimator (CMVE) to construct the high-resolution maps of the absolute ZWDs by fusing the InSAR-Delta ZWD and the GPS-ZWD samples, and finally (3) transforming the high-resolution ZWDs to PWVs using an elevation-dependent proportionality. Only a single interferogram was needed in our method, so we did not use any temporal (i.e., time-series) hypotheses, for example, we did not assume that the average value of the temporal turbulent ZWDs was equal to zero. We validated the new method over the Southern California region using four Sentinel-1 interferograms related to eight SAR images acquired in different seasons and in different years. We also used synchronous GPS measurements from the Southern California integrated GPS network. Eight high-resolution maps of PWVs related to the eight SAR acquisitions were generated, covering similar to 250 km in area at a similar to 160 m spatial resolution. Comparisons between the CMVE method and the other two methods (GPS-only-based interpolation and time-series InSAR stacking) were conducted. Experimental results showed that the CMVE method performed significantly better than conventional methods for constructing high-resolution PWV maps, which is of great interest to a wide community of geophysicists and meteorologists.

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