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For the geosciences based on the data obtained from the modern geodetic measurements, GIA (Glacial Isostatic Adjustment) is important to study the Earth’s viscoelastic structure and dynamics, and the environmental problem of the Erath.
Following two topicst will be introduced; / Experience at Ny-Ålesund lesund, , Svalbard in the Arctic, / Japan–US joint observation project in Southern Alaska started in 2005**. ** Abstract #053 of P41 by Freymueller et al. last day talk closely relates to the 2 nd topics.
Page 1: Application of modern geodetic meas
Page 5 and 6: Geodetic observations at Ny-Ålesun
Page 7 and 8: Absolute gravity observations • R
Page 9 and 10: Possible origins that we studied; (
Page 11 and 12: Sensitivity test of the PGR rate La
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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