Asthenospheric flow estimates in the Atlantic realm based on Poiseuille/Couetteflow models
Authors: Wang Zhirui , Bunge Hans-Peter , Stotz Ingo , Vilacis Baurier Berta , Hayek Valencia Jorge Nicolas , Friedrich Anke 
Published: March 2022

&lt;p&gt;&lt;span&gt;Mantle convection has profound effects on the Earth&amp;#8217;s surface, such as inducing vertical motion, which is commonly termed dynamic topography. Sophisticated mantle convection models have been used to study current and past dynamic topography. But many input parameters, like complex rheologies and thermo-chemical flow properties remain poorly known, requiring ad-hoc model parameterization and long range extrapolation. This makes it attractive to explore simple analytic models of upper mantle flow. The existence of a weak asthenosphere allows one to explore upper mantle in the context of Poiseuille/Couette flow. The latter provides an geodynamically plausible link between flow properties and dynamic topography. Here we construct simple upper mantle flow models parameterized in terms of sources/sinks (plumes/slab) of Poiseuille/Couette flow. Our approach provides physical insight into the pattern of upper mantle flow, makes it easy to assess uncertainties of key model parameters, such as poorly resolved asthenospheric thickness and viscosity, and can be extended back in time, given first-order estimates of plume and subduction flux deduced from geological records. Importantly, it demands low computational cost relative to a time dependent geodynamic models. We present results for the Atlantic realm, and link our estimates of upper mantle flow history to Base Hiatus Surfaces (BHS) recently developed by Friedrich etal., (2018), Vibe etal., (2018), Carena etal., (2019), &amp;#160;Hayek metal., (2020) and Hayek metal., (2021). The latter serve as proxy for inferring past dynamic topography variations. We also relate our calculations to seismically inferred anisotropy, as a further proxy for upper mantle flow. Our results indicate that asthenospheric flow pattern can be explained through the concept of source to sink and that this flow type is testable against first order seismic and geologic observables.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;&lt;span&gt;References:&amp;#160;&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Carena, S., Bunge, H. P., &amp; Friedrich, A. M. (2019). Analysis of geological hiatus surfaces across Africa in the Cenozoic and implications for the timescales of convectively-maintained topography.&amp;#160;Canadian Journal of Earth Sciences,&amp;#160;56(12), 1333-1346.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Friedrich, A. M., Bunge, H. P., Rieger, S. M., Colli, L., Ghelichkhan, S., &amp; Nerlich, R. (2018). Stratigraphic framework for the plume mode of mantle convection and the analysis of interregional unconformities on geological maps.&amp;#160;Gondwana Research,&amp;#160;53, 159-188.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Hayek, J. N., Vilac&amp;#237;s, B., Bunge, H. P., Friedrich, A. M., Carena, S., &amp; Vibe, Y. (2020). Continent-scale Hiatus Maps for the Atlantic Realm and Australia since the Upper Jurassic and links to mantle flow induced dynamic topography.&amp;#160;Proceedings of the Royal Society A,&amp;#160;476(2242), 20200390.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Hayek, J. N., Vilac&amp;#237;s, B., Bunge, H. P., Friedrich, A. M., Carena, S., &amp; Vibe, Y. (2021). Correction: Continent-scale Hiatus Maps for the Atlantic Realm and Australia since the Upper Jurassic and links to mantle flow-induced dynamic topography.&amp;#160;Proceedings of the Royal Society A,&amp;#160;477(2251), 20210437.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span&gt;Vibe, Y., Friedrich, A. M., Bunge, H. P., &amp; Clark, S. R. (2018). Correlations of oceanic spreading rates and hiatus surface area in the North Atlantic realm.&amp;#160;Lithosphere,&amp;#160;10(5), 677-684.&lt;/span&gt;&lt;/p&gt;