Abstract

There are small pieces of evidence, suggesting that South America’s hydrological cycle is changing, which impacts its water availability and, consequently, the Earth’s surface due to its elastic response to the surface mass loading/unloading. Therefore, we analyzed 3 to 15 years of vertical crustal displacements (VCDs) due to mass loadings using 292 Global Positioning System (GPS) stations in South America, which are essential for studies related to tectonic phenomena, for example. Thus, we investigated whether the intra-annual variabilities of the displacements could be reduced using modeled VCDs and inverted displacements from Gravity Recovery and Climate Experiment (GRACE) harmonic solutions (Release 06). The modeled VCDs come from the combination of nontidal atmospheric and ocean loadings with the hydrological loadings from the land-surface model (GLDAS) and reanalysis (MERRA). We found that the highest amplitudes of VCDs of the annual signals are concentrated mainly over the Amazon Rainforest and Brazilian Highlands. However, the results also show different behavior throughout other physiographic provinces of South America, which shows low water capabilities as “sensed” by GRACE and described by the GLDAS and MERRA models. Accordingly, when we disregard the stations over the Andes Mountains and Patagonia in the analysis, the highest reduction in the variability of GPS-observed VCDs is achieved while using GRACE (79% of the sites), MERRA (75% of the sites), and GLDAS (74% of the sites). For these stations, the amplitudes (and phases) of the annual signals depicted by the geodetic sensors generally agree, while those from GLDAS and MERRA explain only approximately 50% of the deformation. However, in the southwest region of South America (between the latitude bands of − 40° to − 30°), GPS annual signals, which reached up to 11 mm, are much larger than those from GRACE and the models due to the existence of lakes that are not resolved in global analysis. These inconsistencies between GPS-observed VCDs and those derived from GRACE and the other models require further investigation, specifically for Chile.

Highlights

  • South America is known for its complex dynamic processes related to topographical, geological, geophysical, hydrological, and climate features (Hinze et al 1982; Hughes et al 2009; Solman 2013; Flament et al 2015; Novello et al 2018)

  • An annual signal was clearly visible in the observed as well as the loading derived from Gravity Recovery and Climate Experiment (GRACE) and combined loading models (CLMs)

  • In this study, we analyzed vertical crustal deformation (VCD) due to surface mass loadings using data from Global Positioning System (GPS), GRACE, and data derived from combined models (CLM-Global Land Data Assimilation System (GLDAS) and CLM-Modern-Era Retrospective Analysis for Research and Applications (MERRA)), over the main physiographic provinces of South America

Read more

Summary

Introduction

South America is known for its complex dynamic processes related to topographical, geological, geophysical, hydrological, and climate features (Hinze et al 1982; Hughes et al 2009; Solman 2013; Flament et al 2015; Novello et al 2018). The continent is of interest in investigating the magnitude and distribution of crustal deformations and their implications in different fields of study, such as geodesy, hydrology, geophysics, and climate change (e.g., Ferreira et al 2018). This is because of the critical rates of crustal deformation in the Andes dominated by the different phases and wavelengths of the earthquake deformation cycle (Khazaradze and Klotz 2003; Melnick et al 2017). Among all space geodesy techniques dedicated to positioning, only GPS is widespread through South America (e.g., Jin and Zhu 2003; Ray et al 2007)

Methods
Results
Discussion
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.