Model:CSt ASMITA: Difference between revisions
From CSDMS
No edit summary |
No edit summary |
||
| Line 30: | Line 30: | ||
|Categories=Coastal, Marine | |Categories=Coastal, Marine | ||
|One-line model description=Aggregate scale morphodynamic model of integrated coastal systems | |One-line model description=Aggregate scale morphodynamic model of integrated coastal systems | ||
|Extended model description=A length-, and time-averaged representation of coastal system elements including the inner shelf, shoreface, surfzone, inlet, inlet shoals, and estuary channels and tidal flats. The multi-line nature of the morphodynamic model allows it to represent large-scale sediment transport processes with a combination time-average physics empirical relationships. A major use is to represent the interactions between system components to develop with changes in large scale forcing such as accelerated sea level rise, changes in river sediment input (ie. dams), changes in estuary tide prisms (ie. dikes) and the like. | |Extended model description=A length-, and time-averaged representation of coastal system elements including the inner shelf, shoreface, surfzone, inlet, inlet shoals, and estuary channels and tidal flats. The multi-line nature of the morphodynamic model allows it to represent large-scale sediment transport processes with a combination time-average physics empirical relationships. A major use is to represent the interactions between system components to develop with changes in large scale forcing such as accelerated sea level rise, changes in river sediment input (ie. dams), changes in estuary tide prisms (ie. dikes) and the like. | ||
}} | }} | ||
{{Start model keyword table}} | |||
{{End a table}} | |||
{{Model technical information | {{Model technical information | ||
|Supported platforms=Windows | |Supported platforms=Windows | ||
| Line 40: | Line 41: | ||
|Does model development still take place?=No | |Does model development still take place?=No | ||
|Model availability=As code, As teaching tool | |Model availability=As code, As teaching tool | ||
|Program license type=GPL v2 | |Program license type=GPL v2 | ||
|Memory requirements=Ordinary PC or laptop | |Memory requirements=Ordinary PC or laptop | ||
|Typical run time=Minutes | |Typical run time=Minutes | ||
}} | }} | ||
| Line 90: | Line 90: | ||
|Pre-processing software needed?=No | |Pre-processing software needed?=No | ||
|Post-processing software needed?=No | |Post-processing software needed?=No | ||
|Visualization software needed?=No | |Visualization software needed?=No | ||
}} | }} | ||
{{Process description model | {{Process description model | ||
|Describe processes represented by the model=Time- and length-averaged sediment transport in shelf, shoreface and surf zone environments combined with morphodynamic-driven sediment flux through inlet, along ebb tide delta and with the bay or estuar. | |Describe processes represented by the model=Time- and length-averaged sediment transport in shelf, shoreface and surf zone environments combined with morphodynamic-driven sediment flux through inlet, along ebb tide delta and with the bay or estuar. | ||
|Describe key physical parameters and equations=These are described in the extensive comments within the fortran program. | |Describe key physical parameters and equations=These are described in the extensive comments within the fortran program. | ||
|Describe length scale and resolution constraints=Typical applications involve coastal systems tens to hundreds of kilometers in extent. Very useful when there are many components in the coastal system. Although the gridded portion of the model usually use delta x and y values on the order of 100s of meters there is a sub-grid scale representation of the shoreline position with resolution of meters. | |Describe length scale and resolution constraints=Typical applications involve coastal systems tens to hundreds of kilometers in extent. Very useful when there are many components in the coastal system. Although the gridded portion of the model usually use delta x and y values on the order of 100s of meters there is a sub-grid scale representation of the shoreline position with resolution of meters. | ||
|Describe time scale and resolution constraints=Averaging time is on the order of annual averages so that individual storm events are not represented. Problems usually are scaled for years, to decades all the way up to millenia. | |Describe time scale and resolution constraints=Averaging time is on the order of annual averages so that individual storm events are not represented. Problems usually are scaled for years, to decades all the way up to millenia. | ||
|Describe any numerical limitations and issues=Probably more than we know but none come to mind. | |Describe any numerical limitations and issues=Probably more than we know but none come to mind. | ||
}} | }} | ||
{{Model testing | {{Model testing | ||
|Describe available calibration data sets=Like most morphodynamical models the user is to supply long-term coastal change data from measured data. | |Describe available calibration data sets=Like most morphodynamical models the user is to supply long-term coastal change data from measured data. | ||
|Describe available test data sets=Several papers have been published that can be used in comparison tests (simply Google Niedoroda) | |Describe available test data sets=Several papers have been published that can be used in comparison tests (simply Google Niedoroda) | ||
|Describe ideal data for testing=User supplied time history of shoreline and depth changes over time with supporting long records of short-term wave and current measurements. | |Describe ideal data for testing=User supplied time history of shoreline and depth changes over time with supporting long records of short-term wave and current measurements. | ||
}} | }} | ||
{{Users groups model | {{Users groups model | ||
|Do you have current or future plans for collaborating with other researchers?=This model continues to evolve. The users are encouraged to replace subroutine with very simplified representations of physics (eg. wave refraction and shoaling) with superior codes. They are requested to pass these back to the authors for inclusion in the new version. Similar requests are made of those using the model for interesting teaching situations. | |Do you have current or future plans for collaborating with other researchers?=This model continues to evolve. The users are encouraged to replace subroutine with very simplified representations of physics (eg. wave refraction and shoaling) with superior codes. They are requested to pass these back to the authors for inclusion in the new version. Similar requests are made of those using the model for interesting teaching situations. | ||
This model will form a basis of the SL-PR model now funded for development and use with coastal response to sea level rise problems. | This model will form a basis of the SL-PR model now funded for development and use with coastal response to sea level rise problems. | ||
}} | }} | ||
{{Documentation model | {{Documentation model | ||
| Line 121: | Line 120: | ||
}} | }} | ||
{{Additional comments model | {{Additional comments model | ||
|Comments=This model is actively under development as of the spring of 2009. | |Comments=This model is actively under development as of the spring of 2009. | ||
}} | }} | ||
{{CSDMS staff part | {{CSDMS staff part | ||
| Line 127: | Line 126: | ||
|CCA component=No but possible | |CCA component=No but possible | ||
|IRF interface=No but possible | |IRF interface=No but possible | ||
|CMT component=Not yet | |||
}} | }} | ||
{{Start coupled table}} | |||
{{End a table}} | |||
{{End headertab}} | {{End headertab}} | ||
<!-- Edit the part above to update info on other papers --> | <!-- Edit the part above to update info on other papers --> | ||
Revision as of 17:25, 23 June 2011
