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Computation of the PDIM effect Method: Convolution of the changing mass with the loading Green’s function (for the PREM earth model) over the main 16 glaciers approximated their shape with elliptical cylinder. Results: Uplift: 2.04 mm/yr Gravity: -0.53 μGal/yr SVAL model by Hagedoorn & Wolf (2003) For a mean melting rate of -45 cm/yr over Svalbard that was inferred from glaciology data.
Sensitivity test of the PGR rate Large ice model ● : ARC3+ANT4 ▼ : ICE-3G (large ice model) Small ice model: ○ : ANU+ANT4 Computed by Okuno
Page 1 and 2: Application of modern geodetic meas
Page 3 and 4: Following two topicst will be intro
Page 5 and 6: Geodetic observations at Ny-Ålesun
Page 7 and 8: Absolute gravity observations • R
Page 9: Possible origins that we studied; (
Page 13 and 14: A geophysical interpretation Assume
Page 15 and 16: Japan-US joint observation project
Page 17 and 18: Rapid Uplift Rate Observed in South
Page 19 and 20: Summary of the study by Alaskan gro
Page 21 and 22: GPS measurements 100 km after C. F.
Page 23 and 24: Observation and study in this proje
Page 25 and 26: Absolute gravityg measurement in So
Page 27 and 28: Tide Gauge Stations 100 km after C.
Page 29 and 30: Summary / Experiences in Svalbard a
Page 31: Observed displacement rates • NS

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