Found the:
They say in that abstract:
"An electrical resistivity survey conducted by the Wenner method at closely spaced electrode spacings was used to determine the vertical extent and resistivity of the frozen ground. This survey was effective in determining the thickness of 3 feet for the frozen ground and a resistivity of 1000 ohm-meters. Beneath the frozen ground the resistivity decreased to 40 ohm meters."
As you can see there can not be a word about grounding with such soil resistivity. And that was measured in New York, not on pole where you have perma frost. I was over arctic circle for 3 months in Siberia. There is no such thing as ground there. I mean you have surface that is earth, but 2m below is perma Ice and nothing melted down for god knows how long (Siberia was green valley in a time of mamuts) . Winter is 9 months in year and they can not have cultive plants, Trees with shallow roots, grass. Situation is a bit better in woods because you have something like vegetation accumulating for some time so the soil resistivity can go under those data for New York.
Problem is in general water on arctic you have almost pure water, no mineral salts in ice, and they are the one that are conducting electricity, and all the gruound is saturated with such ice. So resistivity per meter goes maybe 2 - 10 times more than that data for New York. You don't have that down limit of 40ohm, because everything is perma ice.
And here is an abstract I found of one research work considdering this subject I think you will get all you need from it:
"comparative study of the results of vertical electrical soundings (VES) and magnetotelluric soundings (MTS) carried out at Seymour and James Ross Islands (NE of Antarctic Peninsula) is conducted. Frozen ground thickness, estimated by VES, is compared with permafrost thickness estimates, obtained using: (a) steady geothermal heat flow, inferred from the depths of conductive layers in the crust and upper mantle estimated by MTS, and (b) mean annual air temperatures (MAAT). At Seymour Island, 250 m of permafrost thickness, in equilibrium with an inferred heat flow of 72 mW/m2 (corresponding to a geothermal gradient of 0.037 °C/m) and with an MAAT of ?9.4 °C, is estimated for the upper terrace (about 200 m a.s.l.). This value is consistent with the frozen ground thickness (200 m in the upper terrace) previously estimated by VES. Magnetotelluric soundings carried out in the northwestern region of James Ross Island (volcanic island with recent activity) suggest a magma chamber with top at about 7 km depth in the crust. From the depth of this conductive body, a heat flow of 145 mW/m2 and a geothermal gradient of 0.074 °C/m are estimated, suggesting 67 m of permafrost thickness in the upper terraces (35 m a.s.l.) of this island in equilibrium with the estimated steady heat flow and an MAAT=?5°C. The frozen ground thickness estimated by VES lies between 40 and 45 m for the same terrace. The differences between frozen ground thickness and permafrost thickness in both islands could be attributed to a cryopeg, according to the high salinity beneath the frozen ground suggested by MT soundings....
As you can see if you download
You can expect the sand/loam over there (no biomass to create better ground) with around 500 000 ohm-cm resistivity which is some 200 times more than general ground and that is on normal temperature and x10 times on temperature you will measure it so you should count on 2 000 multiply factor to an normal grounding that you would calculate in bad soil next to your doorstep. I believe you know now why I told you that grounding system is impossible in such conditions...
Anyway in that file above you have some methods for measuring ground resistivity but I am not certain will you get any data because currents are to low to be measured....
You would need a gear that puts a lightning in ground to get accurate data.