Model:FUNDY: Difference between revisions

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{{End a table}}
{{End a table}}
{{Model identity2
{{Model identity2
|Categories=Coastal, Marine
|ModelDomain=Coastal, Marine
|Spatial dimensions=3D
|Spatial dimensions=3D
|Spatialscale=Continental
|Spatialscale=Continental
|One-line model description=a 3-D diagnostic model for continental shelf circulation studies
|One-line model description=a 3-D diagnostic model for continental shelf circulation studies
|Extended model description=It solves the linearized shallow water equations forced by tidal or other barotropic boundary conditions, wind or a density gradient using linear finite elements.  
|Extended model description=It solves the linearized shallow water equations forced by tidal or other barotropic boundary conditions, wind or a density gradient using linear finite elements.
}}
}}
{{Start model keyword table}}
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|Postal code=03755
|Postal code=03755
|State=New Hampshire
|State=New Hampshire
|Country=USA
|Country=United States
|Email address=Christopher.E.Naimie@dartmouth.edu
|Email address=Christopher.E.Naimie@dartmouth.edu
|Phone=603-646-2119
|Phone=603-646-2119
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}}
}}
{{Model technical information
{{Model technical information
|Supported platforms=Windows
|Supported platforms=Linux
|Programming language=Fortran77
|Programming language=Fortran77
|Code optimized=Single Processor
|Code optimized=Single Processor
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}}
}}
{{Process description model
{{Process description model
|Describe processes represented by the model=The model is forced by tidal or other barotropic boundary conditions, wind, and/or fixed baroclinic pressure gradient, all acting at a single frequency (including zero) and specified by the user.  
|Describe processes represented by the model=The model is forced by tidal or other barotropic boundary conditions, wind, and/or fixed baroclinic pressure gradient, all acting at a single frequency (including zero) and specified by the user.
}}
}}
{{Model testing}}
{{Model testing}}
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{{Documentation model
{{Documentation model
|Manual model available=Yes
|Manual model available=Yes
|Model manual=Three-dimensional diagnostic model for baroclinic wind-driving and tidal circulation in shallow seas.pdf,  
|Model manual=Three-dimensional diagnostic model for baroclinic wind-driving and tidal circulation in shallow seas.pdf,
}}
}}
{{Additional comments model}}
{{Additional comments model}}
{{CSDMS staff part
{{CSDMS staff part
|OpenMI compliant=No not possible
|OpenMI compliant=No but possible
|CCA component=No not possible
|CCA component=No but possible
|IRF interface=No not possible
|IRF interface=No but possible
|CMT component=Not yet
|CMT component=No but possible
}}
}}
{{Start coupled table}}
{{Start coupled table}}
{{End a table}}
{{End a table}}
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==Introduction==
==Introduction==
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== History ==
== History ==


== Papers ==
== References  ==
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== Issues ==
== Issues ==


== Help ==
== Help ==
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== Input Files ==
== Input Files ==


== Output Files ==
== Output Files ==
== Download source code ==

Latest revision as of 20:17, 16 September 2020



FUNDY


Metadata

Also known as
Model type Single
Model part of larger framework
Note on status model
Date note status model
Incorporated models or components:
Spatial dimensions 3D
Spatial extent Continental
Model domain Coastal, Marine
One-line model description a 3-D diagnostic model for continental shelf circulation studies
Extended model description It solves the linearized shallow water equations forced by tidal or other barotropic boundary conditions, wind or a density gradient using linear finite elements.
Keywords:

continental shelf circulation, hydrodynamics,

Name Christopher Naimie
Type of contact Technical contact
Institute / Organization Dartmouth College
Postal address 1 Thayer School of Engineering
Postal address 2
Town / City Hanover
Postal code 03755
State New Hampshire
Country United States
Email address Christopher.E.Naimie@dartmouth.edu
Phone 603-646-2119
Fax 603-646-3856


Supported platforms
Linux
Other platform
Programming language

Fortran77

Other program language
Code optimized Single Processor
Multiple processors implemented
Nr of distributed processors
Nr of shared processors
Start year development 1987
Does model development still take place? Yes
If above answer is no, provide end year model development
Code development status
When did you indicate the 'code development status'?
Model availability
Source code availability
(Or provide future intension)
Through web repository
Source web address http://www-nml.dartmouth.edu/Software/fundy/
Source csdms web address
Program license type Other
Program license type other
Memory requirements
Typical run time


Describe input parameters
Input format ASCII
Other input format
Describe output parameters
Output format ASCII
Other output format
Pre-processing software needed? No
Describe pre-processing software
Post-processing software needed? No
Describe post-processing software
Visualization software needed? No
If above answer is yes
Other visualization software


Describe processes represented by the model The model is forced by tidal or other barotropic boundary conditions, wind, and/or fixed baroclinic pressure gradient, all acting at a single frequency (including zero) and specified by the user.
Describe key physical parameters and equations
Describe length scale and resolution constraints
Describe time scale and resolution constraints
Describe any numerical limitations and issues


Describe available calibration data sets
Upload calibration data sets if available:
Describe available test data sets
Upload test data sets if available:
Describe ideal data for testing


Do you have current or future plans for collaborating with other researchers?
Is there a manual available? Yes
Upload manual if available: Media:Three-dimensional diagnostic model for baroclinic wind-driving and tidal circulation in shallow seas.pdf
Model website if any
Model forum / discussion board
Comments


This part will be filled out by CSDMS staff

OpenMI compliant No but possible
BMI compliant No but possible
WMT component No but possible
PyMT component
Is this a data component
Can be coupled with:
Model info
Christopher Naimie
Nr. of publications: 2
Total citations: 13
h-index: 1
m-quotient: 0.05
Qrcode FUNDY.png
Link to this page



Introduction

History

References




Nr. of publications: 2
Total citations: 13
h-index: 1
m-quotient: 0.05



Featured publication(s)YearModel describedType of ReferenceCitations
Mupparapu, Prashant; Brown, Wendell S.; 2002. Role of convection in winter mixed layer formation in the Gulf of Maine, February 1987: ROLE OF CONVECTION IN WINTER MIXED LAYER. Journal of Geophysical Research: Oceans, 107, 22–1-22-18. 10.1029/1999JC000116
(View/edit entry)
2002 FUNDY
Model application 13
See more publications of FUNDY


Issues

Help

Input Files

Output Files