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Earth, Planets and Space
Fig. 6 | Earth, Planets and Space

Fig. 6

From: Updated absolute gravity rate of change associated with glacial isostatic adjustment in Southeast Alaska and its utilization for rheological parameter estimation

Fig. 6

Behavior of the load Love numbers obtained from the VM5a model for GPIM (Peltier et al. 2015). a The variation in \(-{\dot{\delta }}_n(\tau )\) with degree (n) and time (\(\tau\)). b The variation in \({\dot{h}}_n(\tau )\) with degree (n) and time (\(\tau\)). c The variation in the ratio of \(-{\dot{\delta }}_n(\tau )\) to \({\dot{h}}_n(\tau )\) with degree (n) and time (\(\tau\)). d The variation in \(-{\dot{\delta }}(\psi , \tau )\) with angular distance (\(\psi\)) and time (\(\tau\)). e The variation in \({\dot{h}}(\psi , \tau )\) with angular distance (\(\psi\)) and time (\(\tau\)). f The variation in the ratio of \(-{\dot{\delta }}(\psi , \tau )\) to \({\dot{h}}(\psi , \tau )\) with angular distance (\(\psi\)) and time (\(\tau\))

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