Model:TOPOG: Difference between revisions

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{{Model identity
|Model type=Tool
}}
{{Start models incorporated}}
{{End a table}}
{{Model identity2
|ModelDomain=Terrestrial, Hydrology
|Spatial dimensions=2D, 3D
|Spatialscale=Landscape-Scale, Regional-Scale, Watershed-Scale
|One-line model description=TOPOG is a terrain analysis-based hydrologic modelling package
|Extended model description=TOPOG describes how water moves through landscapes; over the land surface, into the soil, through the soil and groundwater and back to the atmosphere via evaporation. Conservative solute movement and sediment transport are also simulated.
The primary strength of TOPOG is that it is based on a sophisticated digital terrain analysis model, which accurately describes the topographic attributes of three-dimensional landscapes. It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).
We refer to TOPOG as a "deterministic", "distributed-parameter" hydrologic modelling package. The term "deterministic" is used to emphasise the fact that the various water balance models within TOPOG use physical reasoning to explain how the hydrologic system behaves. The term "distributed-parameter" means that the model can account for spatial variability inherent in input parameters such as soil type, vegetation and climate.
}}
{{Start model keyword table}}
{{Model keywords
|Model keywords=landscape
}}
{{Model keywords
|Model keywords=catchment
}}
{{End a table}}
{{Modeler information
{{Modeler information
|First name=Richard
|First name=Richard
|Last name=Silberstein
|Last name=Silberstein
|Type of contact=Model developer
|Type of contact=Model developer
|Institute / Organization=CSIRO
|Institute / Organization=University of Western Australia
|Postal address 1=Locked Bag 10
|Postal address 1=35 Stirling Hwy
|Town / City=Clayton
|Town / City=Nedlands
|Postal code=South VIC 3169
|Postal code=6009
|State=NO STATE
|Country=Australia
|Country=Australia
|Email address=richard.silberstein@csiro.au
|Email address=richard.silberstein@bigpond.com
|Phone=+61 3 9545 2176
|Phone=+61 400666334
|Fax=+61 3 9545 2175
}}
}}
{{Additional modeler information
{{Additional modeler information
Line 17: Line 39:
|Additional last name=Rahman
|Additional last name=Rahman
|Additional type of contact=Model developer
|Additional type of contact=Model developer
|Additional institute / Organization=CSIRO
|Additional institute / Organization=Flow Matters
|Additional postal address 1=Locked Bag 10
|Additional postal address 1=PO Box 272
|Additional town / City=Clayton
|Additional postal address 2=Jamison Centre
|Additional postal code=South VIC 3169
|Additional town / City=Canberra
|Additional state=NO STATE
|Additional postal code=2614
|Additional country=Australia
|Additional country=Australia
|Additional email address=joel.rahman@csiro.au
|Additional email address=joel.rahman.home@gmail.com
|Additional phone=+61 3 9545 2176
|Additional fax=+61 3 9545 2175
}}
{{Model identity
|Model type=Modular
|Categories=Hydrology, Terrestrial
|Spatial dimensions=2D, 3D
|Spatialscale=Regional-Scale, Landscape-Scale, Watershed-Scale
|One-line model description=TOPOG is a terrain analysis-based hydrologic modelling package
|Extended model description=TOPOG describes how water moves through landscapes; over the land surface, into the soil, through the soil and groundwater and back to the atmosphere via evaporation. Conservative solute movement and sediment transport are also simulated.
 
The primary strength of TOPOG is that it is based on a sophisticated digital terrain analysis model, which accurately describes the topographic attributes of three-dimensional landscapes. It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).
 
We refer to TOPOG as a "deterministic", "distributed-parameter" hydrologic modelling package. The term "deterministic" is used to emphasise the fact that the various water balance models within TOPOG use physical reasoning to explain how the hydrologic system behaves. The term "distributed-parameter" means that the model can account for spatial variability inherent in input parameters such as soil type, vegetation and climate.
}}
}}
{{Model technical information
{{Model technical information
Line 45: Line 53:
|Start year development=1987
|Start year development=1987
|Does model development still take place?=Yes
|Does model development still take place?=Yes
|DevelopmentCode=Only maintenance
|DevelopmentCodeYearChecked=2020
|Model availability=As code
|Model availability=As code
|Source code availability=Through web repository
|Source code availability=Through web repository
|Source web address=http://www-data.wron.csiro.au/topog/
|Program license type=Other
|Program license type=Other
|Program license type other=PRODUCT LICENSE AGREEMENT, see website
|Program license type other=PRODUCT LICENSE AGREEMENT, see website
|OpenMI compliant=No but possible
|CCA component=No but possible
|IRF interface=No but possible
|Memory requirements=at least 32 MB core memory, preferably 64 MB
|Memory requirements=at least 32 MB core memory, preferably 64 MB
|Typical run time=--
|Typical run time=--
}}
}}
{{Input - Output description
{{Input - Output description
|Describe input parameters=See website, too many to describe:
http://www-data.wron.csiro.au/topog/
|Input format=ASCII, Binary
|Describe output parameters=--
|Output format=ASCII, Binary
|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=See website, too many to describe:
http://www-data.wron.csiro.au/topog/
|Describe key physical parameters and equations=See website, too many to describe:
http://www-data.wron.csiro.au/topog/
|Describe length scale and resolution constraints=It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).
|Describe time scale and resolution constraints=--
|Describe any numerical limitations and issues=--
}}
{{Model testing}}
{{Model testing}}
{{Users groups model}}
{{Users groups model
|Do you have current or future plans for collaborating with other researchers?=--
}}
{{Documentation model
{{Documentation model
|Provide key papers on model if any=Background:
|Manual model available=Yes
* O'LOUGHLIN, E.M. (1986): Prediction of surface saturation zones in natural catchments by topographic analysis. Water Resour. Res., 22(5): 794-804.
|Model website if any=http://www-data.wron.csiro.au/topog/
* VERTESSY, R., O'LOUGHLIN, E., BEVERLY, E. and BUTT, T. (1994): Australian experiences with the CSIRO Topog model in land and water resources management. In: P roceedings of UNESCO International Symposium on Water Resources Planning in a Changing World, Karlsruhe, Germany, June 28-30, 1994, pp. III-135-144.
|Model forum=Feed back and bugs can be reported through the website
* SHORT, D., DAWES, W.R. and WHITE, I. (1995):The practicability of using Richards' equation for general purpose soil-water dynamics models. Environment International, 21(5): 723-730.
}}
 
{{Additional comments model
Terrain analysis:
|Comments=This questionnaire is filled out by Albert Kettner, based on the TOPOG website
* HUTCHINSON, M.F. (1988): A new procedure for gridding elevation and stream line data with automatic removal of spurious pits. J. Hydrol., 106: 211-232.
}}
* DAWES, W.R. and SHORT, D.L. (1994): The significance of topology for modelling the surface hydrology of fluvial landscapes. Water Resour. Res., 30(4): 1045-1055.
{{CSDMS staff part
* BAND, L.E., VERTESSY, R.A. and LAMMERS, R. (1995): The effect of different terrain representations and resolution on simulated watershed processes. Zeitschrift für Geomorphologie, Suppl.-Bd. 101: 187-199.
|OpenMI compliant=No but possible
* MAUNDER, C.J. (1999): An automated method for constructing contour-based digital elevation models. Water Resources Research, Vol 35 No. 12: 3931-3940
|IRF interface=No but possible
|CMT component=No but possible
|CCA component=No but possible
}}
{{Start coupled table}}
{{End a table}}
{{End headertab}}
{{{{PAGENAME}}_autokeywords}}
<!-- PLEASE USE THE "EDIT WITH FORM" BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE -->


Wetness index computation:
* O'LOUGHLIN, E.M., SHORT, D.L. and DAWES, W.R. (1989): Modelling the hydrological response of catchments to landuse change. In: Proceedings of the 1989 Australian Institution of Engineers Hydrology and Water Resources Symposium. Nat. Conf. Publ., No. 89/19, pp. 335-340.
* NANDAKUMAR, N., LANE, P.N.J., VERTESSY, R.A. and O'LOUGHLIN, E.M. (1994): Prediction of soil moisture variability using wetness indices. In: Water Down Under 94: Proceedings of the Australian Institution of Engineers Hydrology and Water Resources Symposium, Adelaide, 21-25 November, 1994, Volume 3, pp. 49-54.


Dynamic water, carbon, solute and sediment balance modelling:
* BEVERLY, C.R. (1992): Background notes on the CSIRO Topog model. 1. Details of the numerical solution of the Richards equation in Topog_Yield. CSIRO Division of Water Resources, Tech. Memo. 92/12, 51 pp.
* VERTESSY, R.A., HATTON, T.J., O'SHAUGHNESSY, P.J. and JAYASURIYA, M.D.A. (1993): Predicting water yield from a mountain ash forest catchment using a terrain analysis based catchment model. J. Hydrology, 150: 665-700.
* HATTON, T.J., WALKER, J., DAWES, W. and DUNIN, F.X. (1992): Simulations of hydroecological responses to elevated CO2 at the catchment scale. Aust. J. Bot., 40: 679-696.
* DAWES, W. and HATTON, T.J. (1993): TOPOG_IRM. 1. Model Description. CSIRO Division of Water Resources, Tech. Memo. 93/5, 33 pp.
* HATTON, T.J. and DAWES, W. (1993): TOPOG_IRM. 2. Example simulations. CSIRO Division of Water Resources, Tech. Memo. 93/6.
* DAWES, W.R. and SHORT, D.L. (1993): The efficient numerical solution of differential equations for coupled water and solute dynamics: the Waves model. CSIRO Division of Water Resources, Tech. Memo. 93/18.
* HATTON, T.J., DAWES, W.R. and VERTESSY, R.A. (1995): The importance of landscape position in scaling SVAT models to catchment scale hydroecological prediction. In: R.A. Feddes (ed.) Space and Time Scale Variability and Interdependencies in Hydrological Processes, pp. 43-53 (Cambridge University Press: Cambridge).
* HATTON, T., DYCE, P., ZHANG, L. And DAWES, W. (1995): Waves - An ecohydrological model of the surface energy and water balance: sensitivity analysis. CSIRO Division of Water Resources, Tech. Memo. 95/2.
* VERTESSY, R.A., HATTON, T.J., BENYON, R.J. and DAWES, W.R. (1996): Long term growth and water balance predictions for a mountain ash (E. regnans) forest subject to clearfelling and regeneration. Tree Physiology 16:221-232.
* ZHANG, L., DAWES, W.R. and HATTON, T.J. (in press): Modelling hydrologic processes using a biophysically based model - Application of Waves to FIFE and HAPEX-MOBILHY. In press, J. Hydrology.
* DAWES, W.R., ZHANG, L., HATTON, T.J., REECE, P.H., BEALE, G. And PACKER, I. (in press): Application of a distributed parameter ecohydrological model (Topog_IRM) to a small cropping rotation catchment. In press, J. Hydrology.
* VERTESSY, R.A. DAWES, W.R., ZHANG, L., HATTON, T.J. and WALKER, J. (1996) Catchment scale hydrologic modelling to assess the water and salt balance behaviour of eucalypt plantations. CSIRO Division of Water Resources, Technical Memorandum 96/1, 23 pp.
* WU, H., RYKIEL Jr.,E.J., HATTON, T. and WALKER, J. (1994) An integrated rate methodology (IRM) for multi-factor growth rate modelling. Ecol. Modelling 73: 97-116.
* SILBERSTEIN, R.P., VERTESSY, R.A., MORRIS, J. AND FEIKMA, P.M. (1999): Modelling the effects of soil moisture and solute conditions on long term tree growth and water use: a case study from the Shepparton irrigation area, Australia. Agricultural Water Management 39:283-315
* DAVIS, S.H., VERTESSY, R.A. AND SILBERSTEIN, R.P. (1999): The sensitivity of a catchment model to soil hydraulic peoperties obtained by using different measurement techniques. Hydrol. Process. 13: 677-688
* VERTESSY, R.A. AND ELSENBEER, H. (1999): Distributed modeling of stormflow generation in an Amazonian rain forest catchment: Effects of model parameterization. Water Resources Research, Vol. 35, No. 7 2173 - 2187
* ZHU, T.X., BAND, L.E. AND VERTESSY, R.A. (1999): Continuous modelling of intermittent stormflows on a semi-arid agricultural catchment. J. Hydrology 226: 11-29
* ZHANG, L., DAWES, W.R., HATTON, T.J. HUME, I.H., O'CONNELL, M.G., MITCHELL, D.C., MILTHORP, P.L. AND YEE, M. (1999): Estimating episodic recharge under different crop/pasture rotations in the Mallee region. Part 1. Experiments and model calibration. Agricultural Water Management 42:219-235
* ZHANG, L., DAWES, W.R., HATTON, T.J. HUME, I.H., O'CONNELL, M.G., MITCHELL, D.C., MILTHORP, P.L. AND YEE, M. (1999): Estimating episodic recharge under different crop/pasture rotations in the Mallee region. Part 2. Recharge control by agronomic practices. Agricultural Water Management 42:237-249
* SILBERSTEIN, R.P. AND VERTESSY, R.A. TOPOG_Scenario - A tool for exploring hydrologic possibilities. 2nd Inter-Regional Conference on Environment-Water 99


|Manual model available=Yes
}}
{{Additional comments model}}
<!-- PLEASE USE THE "EDIT WITH FORM" BUTTON TO EDIT ABOVE CONTENTS; CONTINUE TO EDIT BELOW THIS LINE -->
==Introduction==
==Introduction==


== History ==
== History ==


== Papers ==
== References  ==
<br>{{AddReferenceUploadButtons}}<br><br>
{{#ifexist:Template:{{PAGENAME}}-citation-indices|{{{{PAGENAME}}-citation-indices}}|}}<br>
{{Include_featured_references_models_cargo}}<br>


== Issues ==
== Issues ==


== Help ==
== Help ==
{{#ifexist:Model_help:{{PAGENAME}}|[[Model_help:{{PAGENAME}}]]|}}


== Input Files ==
== Input Files ==


== Output Files ==
== Output Files ==
== Download ==
== Source ==

Latest revision as of 20:16, 16 September 2020



TOPOG


Metadata

Also known as
Model type Tool
Model part of larger framework
Note on status model
Date note status model
Incorporated models or components:
Spatial dimensions 2D, 3D
Spatial extent Landscape-Scale, Regional-Scale, Watershed-Scale
Model domain Terrestrial, Hydrology
One-line model description TOPOG is a terrain analysis-based hydrologic modelling package
Extended model description TOPOG describes how water moves through landscapes; over the land surface, into the soil, through the soil and groundwater and back to the atmosphere via evaporation. Conservative solute movement and sediment transport are also simulated.

The primary strength of TOPOG is that it is based on a sophisticated digital terrain analysis model, which accurately describes the topographic attributes of three-dimensional landscapes. It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).

We refer to TOPOG as a "deterministic", "distributed-parameter" hydrologic modelling package. The term "deterministic" is used to emphasise the fact that the various water balance models within TOPOG use physical reasoning to explain how the hydrologic system behaves. The term "distributed-parameter" means that the model can account for spatial variability inherent in input parameters such as soil type, vegetation and climate.

Keywords:

landscape, catchment,

Name Richard Silberstein
Type of contact Model developer
Institute / Organization University of Western Australia
Postal address 1 35 Stirling Hwy
Postal address 2
Town / City Nedlands
Postal code 6009
State
Country Australia
Email address richard.silberstein@bigpond.com
Phone +61 400666334
Fax


Name Joel Rahman
Type of contact Model developer
Institute / Organization Flow Matters
Postal address 1 PO Box 272
Postal address 2 Jamison Centre
Town / City Canberra
Postal code 2614
State
Country Australia
Email address joel.rahman.home@gmail.com
Phone
Fax


Supported platforms
Unix
Other platform
Programming language

Fortran77, C

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 Only maintenance
When did you indicate the 'code development status'? 2020
Model availability As code
Source code availability
(Or provide future intension)
Through web repository
Source web address http://www-data.wron.csiro.au/topog/
Source csdms web address
Program license type Other
Program license type other PRODUCT LICENSE AGREEMENT, see website
Memory requirements at least 32 MB core memory, preferably 64 MB
Typical run time --


Describe input parameters See website, too many to describe:

http://www-data.wron.csiro.au/topog/

Input format ASCII, Binary
Other input format
Describe output parameters --
Output format ASCII, Binary
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 See website, too many to describe:

http://www-data.wron.csiro.au/topog/

Describe key physical parameters and equations See website, too many to describe:

http://www-data.wron.csiro.au/topog/

Describe length scale and resolution constraints It is intended for application to small catchments (up to 10 km2, and generally smaller than 1 km2).
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:
Model website if any http://www-data.wron.csiro.au/topog/
Model forum / discussion board Feed back and bugs can be reported through the website
Comments This questionnaire is filled out by Albert Kettner, based on the TOPOG website


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
Richard Silberstein
Rahman
Nr. of publications: 10
Total citations: 963
h-index: 5
m-quotient: 0.13
Qrcode TOPOG.png
Link to this page



Introduction

History

References




Nr. of publications: 10
Total citations: 963
h-index: 5
m-quotient: 0.13



Featured publication(s)YearModel describedType of ReferenceCitations
O'Loughlin, E. M.; 1986. Prediction of Surface Saturation Zones in Natural Catchments by Topographic Analysis. Water Resources Research, 22, 794–804. 10.1029/WR022i005p00794
(View/edit entry)
1986 TOPOG
Model overview 714
Vertessy, R.A.; Hatton, T.J.; O'Shaughnessy, P.J.; Jayasuriya, M.D.A.; 1993. Predicting water yield from a mountain ash forest catchment using a terrain analysis based catchment model. Journal of Hydrology, 150, 665–700. 10.1016/0022-1694(93)90131-R
(View/edit entry)
1993 TOPOG
Model overview 186
See more publications of TOPOG


Issues

Help

Input Files

Output Files