Fig. 8From: Updated absolute gravity rate of change associated with glacial isostatic adjustment in Southeast Alaska and its utilization for rheological parameter estimationBehavior of the load Love numbers used to calculate the response to LPIM and RPIM. The load Love number for \(\tau = 2\) kyr determined from the VM5a model (orange lines in Fig. 6) is shown as the gray-colored symbol in each panel, for comparison with those obtained from the subsurface structure model (Table 3 and Fig. 7). 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 (\(\tau\))Back to article page