2013
DOI: 10.1007/s00190-013-0642-3
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Comparative analysis of different environmental loading methods and their impacts on the GPS height time series

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Cited by 100 publications
(88 citation statements)
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References 39 publications
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“…Quite different from the MERRA and GLDAS model, the NCEP-R-2 model yields very small STD value at most of places around the globe, while the STD of the NCEP-R-1 model is very large, especially for the central North America and Eurasia. Since our results on the NCEP-R-1 model is quite similar as that from (Jiang et al 2013), we only show the results from the NCEP-R-2 model only hereafter. The Fig.…”
Section: Comparison Of the Weekly Loading Time Series Between Modelsmentioning
confidence: 65%
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“…Quite different from the MERRA and GLDAS model, the NCEP-R-2 model yields very small STD value at most of places around the globe, while the STD of the NCEP-R-1 model is very large, especially for the central North America and Eurasia. Since our results on the NCEP-R-1 model is quite similar as that from (Jiang et al 2013), we only show the results from the NCEP-R-2 model only hereafter. The Fig.…”
Section: Comparison Of the Weekly Loading Time Series Between Modelsmentioning
confidence: 65%
“…To remove this environmental signal from the GPS data, the CWS mass models are required to predict surface displacements. However, these CWS model induced vertical surface displacement are often not consistent with one another and with the seasonal changes in the position of the GPS markers (Jiang et al 2013). Currently, the most frequent used CWS mass models are the soil moisture (SM) plus snow water equivalent (SWE) from the monthly Global Land Data Assimilation System (GLDAS) 1 (Rui 2011) and the six-hourly National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) global reanalysis datasets (R-1) (Kalnay et al 1996), with spatial resolutions as 1 ı 1 ı and 1:875 ı .1:8889 1:9048/ ı respectively.…”
Section: Introductionmentioning
confidence: 90%
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“…4 We did not include the SWE data above the latitude of 60.5N. This area includes Greenland and most Arctic regions; GLDAS does not model snow dynamics well in these regions (Rui 2011;Jiang et al 2013).…”
Section: Data Descriptionmentioning
confidence: 99%