RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 19, ES5003, doi:10.2205/2019ES000675, 2019


Figure 6. The same rates but residuals are now relative to the GIA model by Milne et al. (2001). The "absolute" GIA rates relative to the Earth's center of mass were converted to rates relative to MSL assuming a geoid rise of 6% of the absolute rates and a MSL rise of 1.3 mm/yr (1892–1991).


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Citation: Kaftan Vladimir, Jaakko Mäkinen (2019), Fennoscandian uplift study as an example of Russian-Finnish cooperation in Arctic geodesy (Advisory), Russ. J. Earth Sci., 19, ES5003, doi:10.2205/2019ES000675.


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