{"id":538,"date":"2023-08-04T18:41:46","date_gmt":"2023-08-04T18:41:46","guid":{"rendered":"https:\/\/4ddynamicearth.tudelft.nl\/?page_id=538"},"modified":"2023-08-17T10:00:28","modified_gmt":"2023-08-17T10:00:28","slug":"task-2","status":"publish","type":"page","link":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/the-project\/task-2\/","title":{"rendered":"Task 2: Satellite gravity-rate data sensitivity to the 3D viscosity structure in contrast to the more classical GIA studies"},"content":{"rendered":"\t\t
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Task 2: Satellite gravity-rate data sensitivity to the 3D viscosity structure in contrast to the more classical GIA studies<\/h2>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t
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This task has two major components to understand the aspects of the Earth\u2019s viscosity, for which close collaboration in a multi-disciplinary context is needed: A numerical implementation of high-resolution 3D Earth mantle structure & computing resulting flow and GIA in terms of deformation and gravitational anomalies, an analysis of new data\/observational models and their uncertainties. Both aspects will be combined to develop a globally consistent earth dynamic simulation model.<\/p>

The outputs of this WP are the effect of different viscosity and lithosphere structures on the observed gravity, gravity-rate, dynamic topography, surface velocities, and anisotropy of the mantle, both for GIA and the mantle convection process.\u00a0<\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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The different components from mantle convection modelling that make up the total geoid. It consists of the dynamic topography part, the dynamic CMB part, and the gravitational signal from the mantle anomalies. The presented model is based on WINTERC-G (upper 400km) and SMEAN2. Modelling was done with the SFEC code.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t
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The following sensitivity studies will be produced:<\/p>

\u2022 1D viscosity sensitivity to gravity, gravity-rate and dynamic topography.
\u2022 3D viscosity sensitivity to gravity, gravity-rate and dynamic topography.
\u2022 1D lithosphere elastic thickness sensitivity to gravity, gravity-rate and dynamic topography.
\u2022 3D lithosphere elastic structure sensitivity to gravity, gravity-rate and dynamic topography.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t

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A closed-loop numerical simulation of Next Generation Gravity Mission (NGGM) for extracting mantle viscosity from the long-term gravity field.<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t
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Workpackages Task 2<\/h2>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t
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\n\t\t\t\t\t\t\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/i><\/span>\n\t\t\t\t\t\t\t\t<\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\tWP 2100: Sensitivity study of geodynamic model to gravity-change observations<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t

\u2022 Changing the 1D viscosity and density structure of the mantle. <\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t

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\n\t\t\t\t\t\t\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/i><\/span>\n\t\t\t\t\t\t\t\t<\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\tWP 2200: Sensitivity study of geodynamic model to gravity-change observations<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t

\u2022 Changing the 3D viscosity and density structure of the mantle.
\u2022 Different boundary conditions .<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t

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\u2022 Viscous vs. viscoelastic codes.<\/p>

\u2022 Compare to seismic results enhanced with Root (2020) approach.
\u2022 1D-3D lithosphere effects.<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t

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\n\t\t\t\t\t\t\t\t\t\t\t\t\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/i><\/span>\n\t\t\t\t\t\t\t\t<\/i><\/span>\n\t\t\t\t\t\t\t\t\t\t\t\t\t<\/span>\n\t\t\t\t\t\t\t\t\t\t\t\tWP 2400: Assess the uncertainty of secular gravity data for a combined GRACE, GRACE-FO and NGGM mission scenario.<\/a>\n\t\t\t\t\t<\/div>\n\n\t\t\t\t\t
<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t
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\u2022 Effect of 3D viscosity, density, and temperature structure on GIA observables.
\u2022 Sensitivity of melt content, crustal structure, and composition.

<\/p><\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"

Task 2: Satellite gravity-rate data sensitivity to the 3D viscosity structure in contrast to the more classical GIA studies This task has two major components to understand the aspects of the Earth\u2019s viscosity, for which close collaboration in a multi-disciplinary context is needed: A numerical implementation of high-resolution 3D Earth mantle structure & computing resulting… Read More »Task 2: Satellite gravity-rate data sensitivity to the 3D viscosity structure in contrast to the more classical GIA studies<\/span><\/a><\/p>\n","protected":false},"author":2,"featured_media":0,"parent":14,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"page-templates\/template-pagebuilder-full-width.php","meta":{"neve_meta_sidebar":"","neve_meta_container":"","neve_meta_enable_content_width":"off","neve_meta_content_width":100,"neve_meta_title_alignment":"","neve_meta_author_avatar":"","neve_post_elements_order":"","neve_meta_disable_header":"","neve_meta_disable_footer":"","neve_meta_disable_title":"","footnotes":""},"class_list":["post-538","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/pages\/538","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/comments?post=538"}],"version-history":[{"count":53,"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/pages\/538\/revisions"}],"predecessor-version":[{"id":784,"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/pages\/538\/revisions\/784"}],"up":[{"embeddable":true,"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/pages\/14"}],"wp:attachment":[{"href":"https:\/\/4ddynamicearth.tudelft.nl\/index.php\/wp-json\/wp\/v2\/media?parent=538"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}