Model:Sedflux: Difference between revisions
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|Model keywords=geodynamics | |Model keywords=geodynamics | ||
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|Model keywords=stratigraphy | |||
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{{Model technical information | {{Model technical information |
Revision as of 17:29, 21 March 2011
Contact
Name | Eric Hutton |
Type of contact | Model developer |
Institute / Organization | CSDMS, INSTAAR, University of Colorado |
Postal address 1 | 1560 30th street |
Postal address 2 | |
Town / City | Boulder |
Postal code | 80305 |
State | Colorado |
Country | USA"USA" is not in the list (Afghanistan, Albania, Algeria, Andorra, Angola, Antigua and Barbuda, Argentina, Armenia, Australia, Austria, ...) of allowed values for the "Country" property. |
Email address | huttone@colorado.edu |
Phone | |
Fax |
Sedflux
Metadata
Summary
sediment transport, geodynamics, stratigraphy, Technical specs
In/Output
Process
Testing
Other
Download statistics<pbars ytitle=Downloads Title='Monthly Downloads sedflux' xlabels=true size=900x200 ymax=50 grid=true box=true cubic=true plots=open xformat=number connected=true angle=90 legend> ,Total downloads: 460 2008 - Jan,0 Feb,0 Mar,0 Apr,0 May,0 Jun,0 Jul,0 Aug,0 Sep,0 Oct,0 Nov,10 Dec,2 2009 - Jan,0 Feb,2 Mar,1 Apr,6 May,9 Jun,36 Jul,0 Aug,3 Sep,3 Oct,24 Nov,1 Dec,0 2010 - Jan,30 Feb,0 Mar,2 Apr,1 May,26 Jun,13 Jul,25 Aug,4 Sep,1 Oct,4 Nov,1 Dec,11 2011 - Jan,4 Feb,0 Mar,5 Apr,7 May,11 Jun,6 Jul,2 Aug,8 Sep,12 Oct,11 Nov,11 Dec,7 2012 - Jan,7 Feb,3 Mar,7 Apr,2 May,4 Jun,6 Jul,5 Aug,1 Sep,4 Oct,2 Nov,3 Dec,8 2013 - Jan,2 Feb,10 Mar,9 Apr,1 May,11 Jun,2 Jul,2 Aug,7 Sep,11 Oct,11 Nov,9 Dec,5 2014 - Jan,6 Feb,5 Mar,2 Apr,0 May,0 Jun,3 Jul,0 Aug,2 Sep,5 Oct,1 Nov,1 Dec,0 2015 - Jan,4 Feb,0 Mar,0 Apr,0 May,0 Jun,0 Jul,0 </pbars> sedflux-2.0 [1] [2]
Sedflux-2.0 is the newest version of the Sedflux basin-filling model. Sedflux-2.0 provides a framework within which individual process-response models of disparate time and space resolutions communicate with one another to deliver multi grain sized sediment load across a continental margin. Version 2.0 introduces a series of new process models, and the ability to operate in one of two modes to track the evolution of stratigraphy in either two or three dimensions. Additions to the 2D-mode include the addition of models that simulate
New processes in the 3D-mode include
The spatial resolution of the architecture is typically 1-25 cm in the vertical, and 10-100 m in the horizontal when operating in 2D-mode. In 3D-mode, the .... References
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