2022
DOI: 10.1016/j.jag.2022.102822
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Assessment of ERA-Interim and ERA5 reanalysis data on atmospheric corrections for InSAR

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Cited by 10 publications
(3 citation statements)
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“…In the case that the meteorological reanalysis data of ERA5 and the acquisition time of SAR image data are not completely synchronized, four variables, including air temperature, potential, specific humidity, and barometric pressure values, are extracted from the pressure layers closest to the acquisition time of the SAR images, assuming that the atmospheric parameters of the two adjacent moments are linearly varying [23]. The reanalysis parameters of each layer are interpolated to the grounding point using a bilinear interpolation method to calculate the ZTD and to compensate for the height difference between the grounding point and the atmosphere layers [24]. Then the hydrostatic delay and the wet delay of the main image and the auxiliary image are calculated respectively.…”
Section: Era5 Dataset Correction Methodsmentioning
confidence: 99%
“…In the case that the meteorological reanalysis data of ERA5 and the acquisition time of SAR image data are not completely synchronized, four variables, including air temperature, potential, specific humidity, and barometric pressure values, are extracted from the pressure layers closest to the acquisition time of the SAR images, assuming that the atmospheric parameters of the two adjacent moments are linearly varying [23]. The reanalysis parameters of each layer are interpolated to the grounding point using a bilinear interpolation method to calculate the ZTD and to compensate for the height difference between the grounding point and the atmosphere layers [24]. Then the hydrostatic delay and the wet delay of the main image and the auxiliary image are calculated respectively.…”
Section: Era5 Dataset Correction Methodsmentioning
confidence: 99%
“…In addition to considering natural vegetation factors, this study also takes into account the influence of meteorological parameters on atmospheric CO 2 concentration. Given the significant impact of meteorological factors on the temporal and spatial variations of CO 2 concentration, key meteorological factors affecting concentration include wind speed, temperature, and humidity [33,34]. ERA5, the fifth-generation ECMWF global climate and weather reanalysis dataset, features a spatial resolution of 0.25 • × 0.25 • and a temporal resolution of 1 h, distributed on a grid.…”
Section: Meteorological Datamentioning
confidence: 99%
“…Therefore, researchers have attempted to correct the tropospheric delay in InSAR using external auxiliary data, which estimated the zenith total delay (ZTD) in the line-of-sight (LOS) direction for each SAR data acquisition moment using external auxiliary data. The commonly used external data sources fall into several categories: meteorological reanalysis data represented by ERA5 (European Center for Medium-Range Weather Forecasts Reanalysis v5) [ 29 , 30 , 31 , 32 , 33 , 34 , 35 , 36 ]; numerical weather forecast models represented by WRF (weather research and forecasting model) [ 37 , 38 , 39 , 40 ]; precipitable water vapor (PWV) products represented using MERIS (medium-resolution imaging spectrometer), Sentinel-3 OLCI (ocean and land color instrument); and MODIS (moderate-resolution imaging spectroradiometer) [ 41 , 42 , 43 , 44 ]. These data types originate from different sensors, and exhibit spatial continuity, clearly representing the lateral heterogeneity of tropospheric water vapor content.…”
Section: Introductionmentioning
confidence: 99%