https://csdms.colorado.edu/csdms_wiki/api.php?action=feedcontributions&feedformat=atom&user=Danielgc 2026-04-29T19:13:36Z User contributions MediaWiki 1.44.2 https://csdms.colorado.edu/csdms_wiki/index.php?title=Reference:Reference-019894&diff=439264 2024-03-12T16:40:43Z

<p>Danielgc: Created page with &quot;{{CSDMS reference template cargo |DOIentry=https://doi.org/10.1029/2002JB002073 }} {{RefsInt1 |FeatureRef=Yes |PublicationClusterID=0 |MS_PublicationClusterID=0 |Semantic_ID=0 |PublicationWhatKindOf=a module application description |PublicationHPCCYesno=No |PublicationNrofModels=coupled modules }} {{RefsInt2 |PublicationMultipleModelsCargo=TISC }} {{RefsInt3 |PublicationAnimationsCargo=https://www.youtube.com/watch?v=q___eADYvJM }}&quot;</p> <hr /> <div>{{CSDMS reference template cargo<br /> |DOIentry=https://doi.org/10.1029/2002JB002073<br /> }}<br /> {{RefsInt1<br /> |FeatureRef=Yes<br /> |PublicationClusterID=0<br /> |MS_PublicationClusterID=0<br /> |Semantic_ID=0<br /> |PublicationWhatKindOf=a module application description<br /> |PublicationHPCCYesno=No<br /> |PublicationNrofModels=coupled modules<br /> }}<br /> {{RefsInt2<br /> |PublicationMultipleModelsCargo=TISC<br /> }}<br /> {{RefsInt3<br /> |PublicationAnimationsCargo=https://www.youtube.com/watch?v=q___eADYvJM<br /> }}</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Reference:Reference-001965&diff=245912 2020-04-24T03:55:22Z

<p>Danielgc: Created page with &quot;{{CSDMS reference template cargo |DOIentry=doi:10.1371/journal.pone.0132252 }} {{RefsInt1 |FeatureRef=No |PublicationClusterID=0 |MS_PublicationClusterID=0 |PublicationWhatKin...&quot;</p> <hr /> <div>{{CSDMS reference template cargo<br /> |DOIentry=doi:10.1371/journal.pone.0132252<br /> }}<br /> {{RefsInt1<br /> |FeatureRef=No<br /> |PublicationClusterID=0<br /> |MS_PublicationClusterID=0<br /> |PublicationWhatKindOf=a module overview describing a module<br /> |PublicationHPCCYesno=No<br /> |PublicationNrofModels=coupled modules<br /> }}<br /> {{RefsInt2<br /> |PublicationMultipleModelsCargo=TISC<br /> }}<br /> {{RefsInt3}}</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Reference:Reference-001964&diff=245911 2020-04-24T03:52:57Z

<p>Danielgc: Created page with &quot;{{CSDMS reference template cargo |DOIentry=DOI: 10.1029/2018GC008176 }} {{RefsInt1 |FeatureRef=Yes |PublicationClusterID=0 |MS_PublicationClusterID=0 |PublicationWhatKindOf=a...&quot;</p> <hr /> <div>{{CSDMS reference template cargo<br /> |DOIentry=DOI: 10.1029/2018GC008176<br /> }}<br /> {{RefsInt1<br /> |FeatureRef=Yes<br /> |PublicationClusterID=0<br /> |MS_PublicationClusterID=0<br /> |PublicationWhatKindOf=a module overview describing a module<br /> |PublicationHPCCYesno=No<br /> |PublicationNrofModels=a single module<br /> }}<br /> {{RefsInt2<br /> |PublicationMultipleModelsCargo=TISC<br /> }}<br /> {{RefsInt3}}</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TISC&diff=245910 2020-04-24T03:50:25Z

<p>Danielgc: </p> <hr /> <div>{{Model identity<br /> |Model also known as=tAo3D<br /> |Model type=Single<br /> }}<br /> {{Start models incorporated}}<br /> {{End a table}}<br /> {{Model identity2<br /> |ModelDomain=Terrestrial, Hydrology, Geodynamic, Climate<br /> |Spatial dimensions=2D, 3D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=TISC integrates quantitative models of lithospheric flexure, fault deformation, and surface mass transport (erosion/transport/sedimentation) along drainage networks.<br /> |Extended model description=TISC is a computer program that simulates the evolution of 3D large-scale sediment transport together with tectonic deformation and lithospheric vertical movements on geological time scales. Particular attention is given to foreland sedimentary basin settings. TISC (formerly called tao3D) stands for Tectonics, Isostasy, Surface Transport, and Climate.<br /> <br /> *hydrology/climate<br /> The drainage river network is calculated following the maximum slope along the evolving topography. Based on the runoff distribution, the water discharge at any cell of the network is calculated as the water collected from tributary cells plus the precipitation at that cell. Lake evaporation is accounted for, enabling the model to study close endorheic basins. Both topography and the network evolves as a result of erosion, sedimentation and tectonic processes. <br /> <br /> *river sediment transport<br /> Sediment carrying capacity is a function of water discharge and slope and determines whether a river is eroding or depositing. Suspended sediments resulting from erosion are transported through the fluvial network until they are deposited or they leave the model domain (explicit mass conservation).<br /> <br /> *lithospheric flexure<br /> A elastic and/or viscoelastic plate approach is used to calculate the vertical movements of the lithosphere caused by the mass redistribution. In the classical lithospheric flexural model, the lithosphere is assumed to rest on a fluid asthenosphere and behave as a thin plate when submitted to external forces.<br /> <br /> *tectonic deformation<br /> Tectonic modification of the relieve and the correspondent loading of the lithosphere are calculated using a cinematic vertical shear approach (preserving the vertical thickness of the moving units during displacement). <br /> }}<br /> {{Start model keyword table}}<br /> {{Model keywords<br /> |Model keywords=fluvial morphodynamics<br /> }}<br /> {{Model keywords<br /> |Model keywords=geodynamics<br /> }}<br /> {{Model keywords<br /> |Model keywords=Bedrock Erosion<br /> }}<br /> {{Model keywords<br /> |Model keywords=groundwater<br /> }}<br /> {{Model keywords<br /> |Model keywords=isostasy<br /> }}<br /> {{Model keywords<br /> |Model keywords=orographic precipitattion<br /> }}<br /> {{Model keywords<br /> |Model keywords=evaporation<br /> }}<br /> {{Model keywords<br /> |Model keywords=lake<br /> }}<br /> {{End a table}}<br /> {{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1997<br /> |Does model development still take place?=Yes<br /> |DevelopmentCode=Only maintenance<br /> |DevelopmentCodeYearChecked=2020<br /> |Model availability=As code, As teaching tool<br /> |Source code availability=Through web repository<br /> |Source web address=https://sites.google.com/site/daniggcc/software/tisc<br /> |Program license type=GPL v3<br /> |Memory requirements=32 GB<br /> |Typical run time=minutes to days<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see software documentation<br /> |Input format=ASCII<br /> |Output format=ASCII<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=No<br /> }}<br /> {{Process description model<br /> |Describe processes represented by the model=TISC is a geodynamic numerical model combining computer modeling techniques to investigate the interplay between lithospheric-scale tectonics and erosion/sedimentation at the Earth's surface. TISC is a code that integrates the calculation of lithospheric flexure, kinematic fault deformation, and surface mass transport (erosion/transport/sedimentation) along drainage networks. In other words, TISC is a software that simulates the evolution of 3D large-scale sediment transport together with tectonic deformation and lithospheric isostatic movements on geological time scales. TISC stands for Tectonics, Isostasy, Surface transport, and Climate. <br /> <br /> Take a look at the documentation wiki and download TISC at GitHub. TISC is available for Linux / OS X platforms only.<br /> <br /> Download TISC from the github repository<br /> See also the Open Forum.<br /> <br /> The Landscape Evolution Model (LEM) component of TISC can deal with closed (internally-drained, endorheic) basins and finds the equilibrium between precipitation in drainage basins and evaporation in terminal lakes. Orographic precipitation is also calculated. Relative to other existing LEMs (Child, Cascade, Eros, ...), TISC explicitly handles lakes forming in local topographic minima, finding the outlet of such water bodies, and accounting for their role as hydrological and sedimentary sinks. It also accounts for internal drainage (endorheism) depending on the collected runoff and the lake's surface evaporation, explicitly calculating the extension of the resulting closed-drainage lakes. It also tracks sediment horizons in the sedimentary basins. TISC uses a fixed rectangular mesh for the finite-difference method. Water flow is at steady state. <br /> <br /> Particular attention is given to the formation of sedimentary basins, with a full track of the source-to-sink balance between erosion and sedimentation. Further information in these papers (G-C, 2002, Basin Res., G-C et al., 2003) showing first results of this numerical model.<br /> |Describe key physical parameters and equations=Most updated description is at <br /> <br /> For the surface process and climatic (orographic precipitation) parts only:<br /> Garcia-Castellanos, D., Jiménez-Munt, I., 2015. Topographic evolution and climate aridification during continental collision: insights from computer simulations. PLOS ONE, doi:10.1371/journal.pone.0132252 [pdf] [pdf]<br /> }}<br /> {{Model testing}}<br /> {{Users groups model}}<br /> {{Documentation model<br /> |Manual model available=No<br /> |Model website if any=https://sites.google.com/site/daniggcc/software/tisc<br /> }}<br /> {{Additional comments model}}<br /> {{CSDMS staff part<br /> |OpenMI compliant=No but possible<br /> |IRF interface=No but possible<br /> |CMT component=No but possible<br /> |CCA component=No but possible<br /> }}<br /> {{Start coupled table}}<br /> {{End a table}}<br /> {{End headertab}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> <br /> <br /> <br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == References ==<br /> &lt;br&gt;{{AddReferenceUploadButtons}}&lt;br&gt;&lt;br&gt;<br /> {{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}&lt;br&gt;<br /> {{Include_featured_references_models_cargo}}&lt;br&gt;<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> {{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TAo&diff=245909 2020-04-24T03:48:32Z

<p>Danielgc: </p> <hr /> <div>{{Model identity<br /> |Model type=Single<br /> }}<br /> {{Start models incorporated}}<br /> {{End a table}}<br /> {{Model identity2<br /> |ModelDomain=Terrestrial, Geodynamic<br /> |Spatial dimensions=2D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=tAo is a software designed to model the interplay between lithosphere flexure and surface transport (erosion/sedimentation), particularly during the formation of orogens and foreland sedimentary basins (see details).<br /> |Extended model description=This pseudo-2D (cross-section, 1 independent variable x) numerical model permits calculating 1D lithospheric flexure with different rheologies, in combination with faulting, loading, and erosion/deposition. The programs are developed in C for Linux platforms, graphic output is produced using GMT scripts, and standard PCs match the CPU and memory requirements. The software is available for free under a GPL license.<br /> }}<br /> {{Start model keyword table}}<br /> {{Model keywords<br /> |Model keywords=geodynamics<br /> }}<br /> {{End a table}}<br /> {{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1995<br /> |Does model development still take place?=No<br /> |DevelopmentCode=Only maintenance<br /> |DevelopmentCodeYearChecked=2020<br /> |Model availability=As code<br /> |Source code availability=Through web repository<br /> |Source web address=https://sites.google.com/site/daniggcc/software/tao<br /> |Program license type=GPL v3<br /> |Memory requirements=16Gb<br /> |Typical run time=minutes<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see documentation along with source code, also available here:<br /> https://sites.google.com/site/daniggcc/software/tao<br /> |Input format=ASCII<br /> |Output format=ASCII<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=Yes<br /> |Other visualization software=GMT recommended<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model<br /> |Do you have current or future plans for collaborating with other researchers?=some collaborations:<br /> <br /> Emry, E.L., D.A. Wiens, D. Garcia-Castellanos, 2014. Faulting within the Pacific plate at the Mariana Trench: Implications for plate interface coupling and subduction of hydrous minerals, J. Geophys. Res. Solid Earth, 119, doi: 10.1002/2013JB010718 <br /> <br /> Saura, E., Garcia-Castellanos, D., Casciello, E., Parravano, V., Urruela, A., Vergés, J., 2015. Modeling the flexural evolution of the Amiran and Mesopotamian foreland basins of NW Zagros (Iran-Iraq). Tectonics. doi:10.1002/2014TC003660<br /> }}<br /> {{Documentation model<br /> |Manual model available=Yes<br /> |Model manual=-<br /> |Model website if any=-<br /> |Model forum=-<br /> }}<br /> {{Additional comments model}}<br /> {{CSDMS staff part<br /> |OpenMI compliant=No but possible<br /> |IRF interface=No but possible<br /> |CMT component=No but possible<br /> |CCA component=No but possible<br /> }}<br /> {{Start coupled table}}<br /> {{End a table}}<br /> {{End headertab}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> <br /> <br /> <br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == References ==<br /> &lt;br&gt;{{AddReferenceUploadButtons}}&lt;br&gt;&lt;br&gt;<br /> {{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}&lt;br&gt;<br /> {{Include_featured_references_models_cargo}}&lt;br&gt;<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> {{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TAo&diff=245908 2020-04-24T03:41:08Z

<p>Danielgc: </p> <hr /> <div>{{Model identity<br /> |Model type=Single<br /> }}<br /> {{Start models incorporated}}<br /> {{End a table}}<br /> {{Model identity2<br /> |ModelDomain=Terrestrial, Geodynamic<br /> |Spatial dimensions=2D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=tAo is a software designed to model the interplay between lithosphere flexure and surface transport (erosion/sedimentation), particularly during the formation of orogens and foreland sedimentary basins (see details).<br /> |Extended model description=This pseudo-2D (cross-section, 1 independent variable x) numerical model permits calculating 1D lithospheric flexure with different rheologies, in combination with faulting, loading, and erosion/deposition. The programs are developed in C for Linux platforms, graphic output is produced using GMT scripts, and standard PCs match the CPU and memory requirements. The software is available for free under a GPL license.<br /> }}<br /> {{Start model keyword table}}<br /> {{Model keywords<br /> |Model keywords=geodynamics<br /> }}<br /> {{End a table}}<br /> {{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1995<br /> |Does model development still take place?=No<br /> |DevelopmentCode=Only maintenance<br /> |DevelopmentCodeYearChecked=2020<br /> |Model availability=As code<br /> |Source code availability=Through web repository<br /> |Source web address=https://sites.google.com/site/daniggcc/software/tao<br /> |Program license type=GPL v3<br /> |Memory requirements=16Gb<br /> |Typical run time=minutes<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see documentation along with source code, also available here:<br /> https://sites.google.com/site/daniggcc/software/tao<br /> |Input format=ASCII<br /> |Output format=ASCII<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=Yes<br /> |Other visualization software=GMT recommended<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model<br /> |Do you have current or future plans for collaborating with other researchers?=-<br /> }}<br /> {{Documentation model<br /> |Manual model available=Yes<br /> |Model manual=-<br /> |Model website if any=-<br /> |Model forum=-<br /> }}<br /> {{Additional comments model}}<br /> {{CSDMS staff part<br /> |OpenMI compliant=No but possible<br /> |IRF interface=No but possible<br /> |CMT component=No but possible<br /> |CCA component=No but possible<br /> }}<br /> {{Start coupled table}}<br /> {{End a table}}<br /> {{End headertab}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> <br /> <br /> <br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == References ==<br /> &lt;br&gt;{{AddReferenceUploadButtons}}&lt;br&gt;&lt;br&gt;<br /> {{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}&lt;br&gt;<br /> {{Include_featured_references_models_cargo}}&lt;br&gt;<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> {{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=User:Danielgc&diff=15071 2010-09-01T10:12:12Z

<p>Danielgc: </p> <hr /> <div>{{Signup information member<br /> |First name member=Daniel<br /> |Last name member=Garcia-Castellanos<br /> |Institute member=ICTJA-CSIC<br /> |City member=Barcelona<br /> |Postal code member=08028<br /> |State member=NO STATE<br /> |Country member=Spain<br /> |Confirm email member=daniggcc@gmail.com<br /> |Website member=http://cuba.ictja.csic.es/~danielgc/<br /> |Working group member=Terrestrial Working Group<br /> }}</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TAo&diff=15070 2010-09-01T10:07:17Z

<p>Danielgc: </p> <hr /> <div>{{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model identity<br /> |Model type=Single<br /> |Spatial dimensions=2D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=tAo is a software designed to model the interplay between lithosphere flexure and surface transport (erosion/sedimentation), particularly during the formation of orogens and foreland sedimentary basins (see details). <br /> |Extended model description=This 2D (cross-section) numerical model permits calculating 1D lithospheric flexure with different rheologies, in combination with faulting, loading, and erosion/deposition. The programs are developed in C for Linux platforms, graphic output is produced using GMT scripts, and standard PCs match the CPU and memory requirements. The software is available for free under a GPL license.<br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1995<br /> |Does model development still take place?=Yes<br /> |Model availability=As code<br /> |Source web address=http://cuba.ictja.csic.es/~danielgc/tao/<br /> |Program license type=GPL v3<br /> |OpenMI compliant=No not possible<br /> |CCA component=No not possible<br /> |IRF interface=No not possible<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see documentation along with source code, also available here:<br /> http://cuba.ija.csic.es/~danielgc/tao/<br /> |Input format=ASCII<br /> |Output format=ASCII<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=Yes<br /> |Other visualization software=GMT recommended<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model<br /> |Do you have current or future plans for collaborating with other researchers?=-<br /> }}<br /> {{Documentation model<br /> |Provide key papers on model if any=-<br /> |Manual model available=Yes<br /> |Model manual=-<br /> |Model website if any=-<br /> |Model forum=-<br /> }}<br /> {{Additional comments model}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == Papers ==<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==<br /> <br /> == Download ==<br /> <br /> == Source ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=File:Tao.info.txt&diff=15069 2010-09-01T10:06:20Z

<p>Danielgc: </p> <hr /> <div></div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TISC&diff=15020 2010-08-31T17:32:30Z

<p>Danielgc: </p> <hr /> <div>{{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model identity<br /> |Model type=Single<br /> |Categories=Terrestrial<br /> |Spatial dimensions=2D, 3D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=TISC integrates quantitative models of lithospheric flexure, fault deformation, and surface mass transport (erosion/transport/sedimentation) along drainage networks. <br /> |Extended model description=TISC is a computer program that simulates the evolution of 3D large-scale sediment transport together with tectonic deformation and lithospheric vertical movements on geological time scales. Particular attention is given to foreland sedimentary basin settings. TISC (formerly called tao3D) stands for Tectonics, Isostasy, Surface Transport, and Climate.<br /> <br /> *hydrology/climate<br /> The drainage river network is calculated following the maximum slope along the evolving topography. Based on the runoff distribution, the water discharge at any cell of the network is calculated as the water collected from tributary cells plus the precipitation at that cell. Lake evaporation is accounted for, enabling the model to study close endorheic basins. Both topography and the network evolves as a result of erosion, sedimentation and tectonic processes. <br /> <br /> *river sediment transport<br /> Sediment carrying capacity is a function of water discharge and slope and determines whether a river is eroding or depositing. Suspended sediments resulting from erosion are transported through the fluvial network until they are deposited or they leave the model domain (explicit mass conservation).<br /> <br /> *lithospheric flexure<br /> A elastic and/or viscoelastic plate approach is used to calculate the vertical movements of the lithosphere caused by the mass redistribution. In the classical lithospheric flexural model, the lithosphere is assumed to rest on a fluid asthenosphere and behave as a thin plate when submitted to external forces.<br /> <br /> *tectonic deformation<br /> Tectonic modification of the relieve and the correspondent loading of the lithosphere are calculated using a cinematic vertical shear approach (preserving the vertical thickness of the moving units during displacement). <br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1997<br /> |Does model development still take place?=Yes<br /> |Model availability=As code<br /> |Source code availability=Through web repository<br /> |Source web address=http://cuba.ictja.csic.es/~danielgc/TISC<br /> |Program license type=GPL v3<br /> |OpenMI compliant=No not possible<br /> |CCA component=No not possible<br /> |IRF interface=No not possible<br /> |Typical run time=minutes to days<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see software documentation<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=No<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model}}<br /> {{Documentation model<br /> |Manual model available=No<br /> }}<br /> {{Additional comments model}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == Papers ==<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==<br /> <br /> == Download ==<br /> <br /> == Source ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TISC&diff=15019 2010-08-31T17:25:26Z

<p>Danielgc: </p> <hr /> <div>{{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model identity<br /> |Categories=Terrestrial<br /> |Spatial dimensions=2D, 3D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=TISC is a numerical model that integrates quantitative models of lithospheric flexure, fault deformation, and surface mass transport (erosion/transport/sedimentation) along drainage networks. In other words, TISC is a computer program that simulates the evolution of 3D large-scale sediment transport together with tectonic deformation and lithospheric vertical movements on geological time scales. Particular attention is given to foreland sedimentary basin settings. <br /> <br /> TISC (formerly called tao3D) stands for Tectonics, Isostasy, Surface Transport, and Climate.<br /> |Extended model description=river drainage<br /> The drainage river network is calculated following the maximum slope along the evolving topography. Based on the runoff distribution, the water discharge at any cell of the network is calculated as the water collected from tributary cells plus the precipitation at that cell. Lake evaporation is accounted for, enabling the model to study close endorheic basins. Both topography and the network evolves as a result of erosion, sedimentation and tectonic processes. <br /> <br /> river sediment transport<br /> Sediment carrying capacity is a function of water discharge and slope and determines whether a river is eroding or depositing. Suspended sediments resulting from erosion are transported through the fluvial network until they are deposited or they leave the model domain (explicit mass conservation).<br /> <br /> lithospheric flexure<br /> A elastic and/or viscoelastic plate approach is used to calculate the vertical movements of the lithosphere caused by the mass redistribution. In the classical lithospheric flexural model, the lithosphere is assumed to rest on a fluid asthenosphere and behave as a thin plate when submitted to external forces.<br /> <br /> tectonic deformation<br /> Tectonic modification of the relieve and the correspondent loading of the lithosphere are calculated using a cinematic vertical shear approach (preserving the vertical thickness of the moving units during displacement). <br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1997<br /> |Does model development still take place?=Yes<br /> |Model availability=As code<br /> |Source code availability=Through web repository<br /> |Source web address=http://cuba.ictja.csic.es/~danielgc/TISC<br /> |Program license type=GPL v3<br /> |OpenMI compliant=No not possible<br /> |CCA component=No not possible<br /> |IRF interface=No not possible<br /> |Typical run time=minutes to days<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see software documentation<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=No<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model}}<br /> {{Documentation model<br /> |Manual model available=No<br /> }}<br /> {{Additional comments model}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == Papers ==<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==<br /> <br /> == Download ==<br /> <br /> == Source ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=User:Danielgc&diff=15018 2010-08-31T17:21:50Z

<p>Danielgc: </p> <hr /> <div>{{Signup information member<br /> |First name member=Daniel<br /> |Last name member=Garcia Castellanos<br /> |Institute member=ICTJA-CSIC<br /> |City member=Barcelona<br /> |Postal code member=08028<br /> |State member=NO STATE<br /> |Country member=Spain<br /> |Confirm email member=daniggcc@gmail.com<br /> |Website member=http://cuba.ictja.csic.es/~danielgc/<br /> |Working group member=Terrestrial Working Group<br /> }}</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=User:Danielgc&diff=15017 2010-08-31T17:20:23Z

<p>Danielgc: </p> <hr /> <div>{{Signup information member<br /> |First name member=Daniel<br /> |Last name member=Garcia Castellanos<br /> |Institute member=ICTJA-CSIC<br /> |City member=Barcelona<br /> |Postal code member=08028<br /> |State member=NO STATE<br /> |Country member=Spain<br /> |Confirm email member=daniggcc@gmail.com<br /> |Working group member=Terrestrial Working Group<br /> }}</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TAo&diff=15015 2010-08-31T17:13:57Z

<p>Danielgc: Created page with &#039;{{Modeler information |First name=Daniel |Last name=Garcia Castellanos |Type of contact=Model developer |Institute / Organization=ICTJA-CSIC |Town / City=Barcelona |Postal code=0…&#039;</p> <hr /> <div>{{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model identity<br /> |Spatial dimensions=2D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=tAo is a software designed to model the interplay between lithosphere flexure and surface transport (erosion/sedimentation), particularly during the formation of orogens and foreland sedimentary basins (see details). This 2D (cross-section) numerical model permits calculating 1D lithospheric flexure with different rheologies, in combination with faulting, loading, and erosion/deposition. The programs are developed in C for Linux platforms, graphic output is produced using GMT scripts, and standard PCs match the CPU and memory requirements. The software is available for free under a GPL license<br /> |Extended model description=-<br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1995<br /> |Does model development still take place?=no<br /> |Model availability=As code<br /> |Source web address=http://cuba.ictja.csic.es/~danielgc/tao/<br /> |Program license type=GPL v3<br /> |OpenMI compliant=No not possible<br /> |CCA component=No not possible<br /> |IRF interface=No not possible<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see documentation along with source code<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=No<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model<br /> |Do you have current or future plans for collaborating with other researchers?=-<br /> }}<br /> {{Documentation model<br /> |Provide key papers on model if any=-<br /> |Manual model available=Yes<br /> |Model manual=-<br /> |Model website if any=-<br /> |Model forum=-<br /> }}<br /> {{Additional comments model}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == Papers ==<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==<br /> <br /> == Download ==<br /> <br /> == Source ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=File:Tisc.info.txt&diff=15013 2010-08-31T17:12:12Z

<p>Danielgc: </p> <hr /> <div></div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=Model:TISC&diff=15011 2010-08-31T17:05:18Z

<p>Danielgc: Created page with &#039;{{Modeler information |First name=Daniel |Last name=Garcia Castellanos |Type of contact=Model developer |Institute / Organization=ICTJA-CSIC |Town / City=Barcelona |Postal code=0…&#039;</p> <hr /> <div>{{Modeler information<br /> |First name=Daniel<br /> |Last name=Garcia Castellanos<br /> |Type of contact=Model developer<br /> |Institute / Organization=ICTJA-CSIC<br /> |Town / City=Barcelona<br /> |Postal code=08028<br /> |Country=Spain<br /> |Email address=danielgc@ictja.csic.es<br /> }}<br /> {{Model identity<br /> |Categories=Terrestrial<br /> |Spatial dimensions=2D, 3D<br /> |Spatialscale=Continental, Regional-Scale<br /> |One-line model description=TISC is a numerical model that integrates quantitative models of lithospheric flexure, fault deformation, and surface mass transport (erosion/transport/sedimentation) along drainage networks. In other words, TISC is a computer program that simulates the evolution of 3D large-scale sediment transport together with tectonic deformation and lithospheric vertical movements on geological time scales. Particular attention is given to foreland sedimentary basin settings. <br /> <br /> TISC (formerly called tao3D) stands for Tectonics, Isostasy, Surface Transport, and Climate. <br /> <br /> |Extended model description=river drainage<br /> The drainage river network is calculated following the maximum slope along the evolving topography. Based on the runoff distribution, the water discharge at any cell of the network is calculated as the water collected from tributary cells plus the precipitation at that cell. Lake evaporation is accounted for, enabling the model to study close endorheic basins. Both topography and the network evolves as a result of erosion, sedimentation and tectonic processes. <br />   <br /> river sediment transport<br /> Sediment carrying capacity is a function of water discharge and slope and determines whether a river is eroding or depositing. Suspended sediments resulting from erosion are transported through the fluvial network until they are deposited or they leave the model domain (explicit mass conservation). <br />   <br /> lithospheric flexure<br /> A elastic and/or viscoelastic plate approach is used to calculate the vertical movements of the lithosphere caused by the mass redistribution. In the classical lithospheric flexural model, the lithosphere is assumed to rest on a fluid asthenosphere and behave as a thin plate when submitted to external forces. <br />   <br /> tectonic deformation<br /> Tectonic modification of the relieve and the correspondent loading of the lithosphere are calculated using a cinematic vertical shear approach (preserving the vertical thickness of the moving units during displacement).  <br /> <br /> }}<br /> {{Model technical information<br /> |Supported platforms=Unix, Linux, Mac OS<br /> |Programming language=C<br /> |Code optimized=Single Processor<br /> |Start year development=1997<br /> |Does model development still take place?=Yes<br /> |Model availability=As code<br /> |Source code availability=Through web repository<br /> |Source web address=http://cuba.ictja.csic.es/~danielgc/TISC<br /> |Program license type=GPL v3<br /> |OpenMI compliant=No not possible<br /> |CCA component=No not possible<br /> |IRF interface=No not possible<br /> |Typical run time=minutes to days<br /> }}<br /> {{Input - Output description<br /> |Describe input parameters=see software documentation<br /> |Pre-processing software needed?=No<br /> |Post-processing software needed?=No<br /> |Visualization software needed?=No<br /> }}<br /> {{Process description model}}<br /> {{Model testing}}<br /> {{Users groups model}}<br /> {{Documentation model<br /> |Manual model available=No<br /> }}<br /> {{Additional comments model}}<br /> &lt;!-- PLEASE USE THE &quot;EDIT WITH FORM&quot; BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE --&gt;<br /> ==Introduction==<br /> <br /> == History ==<br /> <br /> == Papers ==<br /> <br /> == Issues ==<br /> <br /> == Help ==<br /> <br /> == Input Files ==<br /> <br /> == Output Files ==<br /> <br /> == Download ==<br /> <br /> == Source ==</div>

Danielgc https://csdms.colorado.edu/csdms_wiki/index.php?title=User:Danielgc&diff=15006 2010-08-31T16:46:41Z

<p>Danielgc: </p> <hr /> <div>{{Signup information member<br /> |First name member=Daniel<br /> |Last name member=Garcia Castellanos<br /> |Institute member=ICTJA-CSIC<br /> |City member=Barcelona<br /> |Postal code member=08028<br /> |State member=NO STATE<br /> |Country member=Spain<br /> |Confirm email member=daniggcc@gmail.com<br /> }}</div>

Danielgc