Evaluating seasonal loading models and their impact on global and regional reference frame alignment

Seasonal variations are observed in GPS time series, but are not included in the International Terrestrial Reference Frame (ITRF) models. Unmodeled seasonal variations at sites used for reference frame alignment are aliased into the reference frame parameters and bias all coordinates in the transformed solution. We augment ITRF2008 with seasonal loading models based either on Gravity Recovery and Climate Experiment (GRACE) measurements or a suite of models for atmospheric pressure, continental hydrology, and nontidal ocean loading. We model the seasonal components using either annual and semiannual terms or a nonparametric approach. When we include a seasonal variation model, the weighted root-mean-square misfit after seven-parameter transformation decreases for 70–90% of the daily GPS solutions depending on the network and seasonal model used, relative to a baseline case using ITRF2008. When seasonal variations are included in the reference frame solution, the observed seasonal variations are more consistent with the GRACE-based model at 80–85% of the GPS sites that were not used in the frame alignment. The suite of forward models performs nearly as well as the GRACE-based model for North America, but substantially worse for other parts of the world. We interpret these findings to mean that the use of ITRF2008 without seasonal terms causes the amplitude of seasonal variations in the coordinate time series to be damped down relative to the true loading deformation and that the observed GPS time series are more consistent with a TRF model that includes seasonal variations. At present, a seasonal model derived from GRACE captures seasonal variations more faithfully than one based on hydrologic models.

[1]  Peter Steigenberger,et al.  Vertical deformations from homogeneously processed GRACE and global GPS long-term series , 2011 .

[2]  Xavier Collilieux,et al.  Comparison of very long baseline interferometry, GPS, and satellite laser ranging height residuals from ITRF2005 using spectral and correlation methods , 2007 .

[3]  Jian Wang,et al.  Bedrock displacements in Greenland manifest ice mass variations, climate cycles and climate change , 2012, Proceedings of the National Academy of Sciences.

[4]  Jim R. Ray,et al.  Sub-daily alias and draconitic errors in the IGS orbits , 2011, GPS Solutions.

[5]  B. D. Tapley,et al.  Satellite Gravity Measurements Confirm Accelerated Melting of Greenland Ice Sheet , 2006, Science.

[6]  T. Dixon,et al.  Accelerating uplift in the North Atlantic region as an indicator of ice loss , 2010 .

[7]  D. Rowlands,et al.  Recent glacier mass changes in the Gulf of Alaska region from GRACE mascon solutions , 2008, Journal of Glaciology.

[8]  Xavier Collilieux,et al.  IGS contribution to the ITRF , 2009 .

[9]  J. Freymueller,et al.  Seasonal hydrological loading in southern Alaska observed by GPS and GRACE , 2012 .

[10]  J. Ray,et al.  Anomalous harmonics in the spectra of GPS position estimates , 2008 .

[11]  Zuheir Altamimi,et al.  Strategies to mitigate aliasing of loading signals while estimating GPS frame parameters , 2011, Journal of Geodesy.

[12]  Z. Altamimi,et al.  ITRF2008: an improved solution of the international terrestrial reference frame , 2011 .

[13]  Xavier Collilieux,et al.  Hydrological deformation induced by the West African Monsoon: Comparison of GPS, GRACE and loading models , 2012 .

[14]  Jürgen Kusche,et al.  Surface mass redistribution inversion from global GPS deformation and Gravity Recovery and Climate Experiment (GRACE) gravity data , 2005 .

[15]  J. Wahr,et al.  A comparison of annual vertical crustal displacements from GPS and Gravity Recovery and Climate Experiment (GRACE) over Europe , 2007 .

[16]  N. G. Val’es,et al.  CNES/GRGS 10-day gravity field models (release 2) and their evaluation , 2010 .

[17]  Mike P. Stewart,et al.  GPS height time series: Short‐period origins of spurious long‐period signals , 2007 .

[18]  M. Bevis,et al.  Spread of ice mass loss into northwest Greenland observed by GRACE and GPS , 2010 .

[19]  K. Heki Seasonal Modulation of Interseismic Strain Buildup in Northeastern Japan Driven by Snow Loads , 2001, Science.

[20]  Xavier Collilieux,et al.  Quality assessment of GPS reprocessed terrestrial reference frame , 2011 .

[21]  Michael B. Heflin,et al.  Large‐scale global surface mass variations inferred from GPS measurements of load‐induced deformation , 2003 .

[22]  M. Bouin,et al.  Correlated errors in GPS position time series: Implications for velocity estimates , 2011 .

[23]  M. Tamisiea,et al.  On seasonal signals in geodetic time series , 2012 .

[24]  T. Dixon,et al.  Slow slip events in Costa Rica detected by continuous GPS observations, 2002–2011 , 2012 .

[25]  Jeffrey T. Freymueller,et al.  Seasonal Position Variations and Regional Reference Frame Realization , 2009 .

[26]  Peter Steigenberger,et al.  Generation of a consistent absolute phase-center correction model for GPS receiver and satellite antennas , 2007 .

[27]  Guillaume Ramillien,et al.  Detecting hydrologic deformation using GRACE and GPS , 2009 .

[28]  M. Zhong,et al.  Contributions of thermal expansion of monuments and nearby bedrock to observed GPS height changes , 2009 .

[29]  K. Heki Snow load and seasonal variation of earthquake occurrence in Japan , 2003 .

[30]  J. Ray,et al.  Effect of the satellite laser ranging network distribution on geocenter motion estimation , 2009 .

[31]  Jeffrey T. Freymueller,et al.  Seasonal and long-term vertical deformation in the Nepal Himalaya constrained by GPS and GRACE measurements , 2012 .

[32]  J. Avouac,et al.  Seasonal variations of seismicity and geodetic strain in the Himalaya induced by surface hydrology as revealed from GPS monitoring, seismic monitoring and GRACE measurements , 2007 .

[33]  W. Farrell Deformation of the Earth by surface loads , 1972 .

[34]  Jeffrey P. Walker,et al.  THE GLOBAL LAND DATA ASSIMILATION SYSTEM , 2004 .

[35]  Xavier Collilieux,et al.  Impact of loading effects on determination of the International Terrestrial Reference Frame , 2010 .

[36]  D. Alsdorf,et al.  Seasonal fluctuations in the mass of the Amazon River system and Earth's elastic response , 2005 .

[37]  D. Chambers,et al.  Estimating Geocenter Variations from a Combination of GRACE and Ocean Model Output , 2008 .

[38]  Y. Bock,et al.  Anatomy of apparent seasonal variations from GPS‐derived site position time series , 2001 .

[39]  S. Schwartz,et al.  Slow slip events and seismic tremor at circum‐Pacific subduction zones , 2007 .

[40]  Haiying Gao,et al.  Source parameters and time‐dependent slip distributions of slow slip events on the Cascadia subduction zone from 1998 to 2008 , 2010 .

[41]  F. Bryan,et al.  Time variability of the Earth's gravity field: Hydrological and oceanic effects and their possible detection using GRACE , 1998 .

[42]  G. Blewitt,et al.  A New Global Mode of Earth Deformation: Seasonal Cycle Detected , 2001, Science.

[43]  Carl Wunsch,et al.  Global ocean circulation during 1992-1997, estimated from ocean observations and a general circulation model , 2002 .