Hello,
in attachment the code that was developed in python for grass 6.

In case you need to follows the tutorial (
http://istgeo.ist.supsi.ch/site/?q=node/4), i have also the other modules
specifically created and used for that.. (v.db.calc)

Markus: should I put it in the addons? I thougth it was once....

Best,
Maxi



On Mon, Apr 29, 2013 at 2:30 PM, Massimiliano Cannata <
[email protected]> wrote:

> Hello,
> in attachment the code that was developed in python for grass 6.
>
>
>
> On Mon, Apr 29, 2013 at 2:25 PM, "Peter Löwe" <[email protected]> wrote:
>
>> Michael,
>>
>> the point of contact for r.tsunami is Maxi Cannata (cc).
>>
>> AFAIK the development of r.tsunami continues, but the module remains to
>> be published.
>> One odler version of r.tsunami can be found in the slaxGIS - OSGeo Lab
>> 2008 special edition:
>>
>> http://geomatica.como.polimi.it/software/vigerGIS/slaxGIS-080805/index.php?SE=osgeolab
>>
>> FWIW, GRASS is also used to create visualisations stemming from Tsunami
>> Simulations to allow for quality checking of the models:
>>
>>  *The FOSS GIS Workbench on the GFZ Load Sharing Facility compute cluster
>> *
>> http://de.slideshare.net/loewe/egu-2012-essi-the-foss-gis
>>
>> *Tangible 3D printouts from GIS-Data: A work in progress 
>> report<http://ebooks.gfz-potsdam.de/pubman/item/escidoc:100081:1>
>> *
>>  http://ebooks.gfz-potsdam.de/pubman/item/escidoc:100081:1
>>
>>
>> Kind regards,
>> Peter
>>
>>  <[email protected]>
>>
>>
>> *Gesendet:* Samstag, 27. April 2013 um 15:54 Uhr
>> *Von:* "Michael Tiemann" <[email protected]>
>> *An:* [email protected], [email protected]
>> *Betreff:* r.tsunami status question
>>   I'm working on a talk and wanted to reference the GRASS project for
>> predicting tsunami inundation (disclosed at 2006 OSGEO conference).  The
>> wiki says that r.tsunami is part of the Grass Addons (
>> http://grasswiki.osgeo.org/wiki/Natural_Hazards) but when I look at the
>> SVN repository, I cannot find it either in Grass 5, 6, or 7 addon locations.
>>
>> Using Google, I was able to find r.tsusami listed as a code sprint item
>> that perhaps was not completed.
>>
>> Is r.tsunami dormant, renamed, or deprecated?  Thanks!
>>
>> M
>>
>>
>
>
>
> --
> *Massimiliano Cannata*
>
> Professore SUPSI in ingegneria Geomatica
>
> Responsabile settore Geomatica
>
>
> Istituto scienze della Terra
>
> Dipartimento ambiente costruzione e design
>
> Scuola universitaria professionale della Svizzera italiana
>
> Campus Trevano, CH - 6952 Canobbio
>
> Tel. +41 (0)58 666 62 14****
>
> Fax +41 (0)58 666 62 09****
>
> [email protected]
>
> *www.supsi.ch/ist*
>



-- 
*Massimiliano Cannata*

Professore SUPSI in ingegneria Geomatica

Responsabile settore Geomatica


Istituto scienze della Terra

Dipartimento ambiente costruzione e design

Scuola universitaria professionale della Svizzera italiana

Campus Trevano, CH - 6952 Canobbio

Tel. +41 (0)58 666 62 14****

Fax +41 (0)58 666 62 09****

[email protected]

*www.supsi.ch/ist*
Title: GRASS GIS: r.tsunami
GRASS logo

NAME

r.tsunami - Calculation of flooded area due to tsunami event.

KEYWORDS

tsunami, modelling

SYNOPSIS

r.tsunami
r.tsunami help
r.tsunami dtm=string rough=string size=value h=value ho=value Ho=value [runup=string] flood=string hflood=string x=value y=value [--overwrite] [--verbose] [--quiet]

Flags:

-m
Runup values [m]
-a
Calculation of total flooded area [mq]
-i
Flood height values [m]
--overwrite
Allow output files to overwrite existing files
--verbose
Verbose module output
--quiet
Quiet module output

Parameters:

dtm=string
Digital terrain model raster map name
rough=string
Roughness raster map name
size=value
Size of the neighborhood [-]
Options: 1,3,5,7,9,11,13,15,17,19,21,23,25
Default: 3
h=value
Sea depth at coastline [m]
ho=value
Sea depth at source point [m]
Ho=value
Wave height at source point [m]
runup=string
Output runup map name
flood=string
Output flooded area map name
hflood=string
Output flood height map name
x=value
X coordinate (sea point)
y=value
Y coordinate (sea point)

DESCRIPTION

r.tsunami allow to assess the maximum vertical height of the tsunami wave at the coast (run-up) and the subsequent inundation on the mainland.The procedure takes into account local morphological characteristics,vegetation and urbanization through the usage of digital terrain model and roughness raster maps.

NOTES

The digital terrain model raster map must contain null values at sea level.

AUTHORS

M.Molinari, M. Cannata (Earth Science Institute, http://istgeo.ist.supsi.ch). Implementation of the base method developed by B. Federici.

REFERENCES

  • Federici, B & Cosso, T, 2006, 'Tsunami inundation maps and damage sceneries through the GIS GRASS', proceedings of FOSS4G2006 , Lausanne, Switzerland, viewed 13 August 2008.
  • Cannata M., Federici B., Molinari M., - "Carte di inondazione dovute a tsunami mediante il GIS GRASS: applicazione all'isola di St. Lucia, Caraibi",proceedings of VIII Italian GRASS user meeting, Palermo, Italy, viewed 13 August 2008.

Last changed: $Date: 2008-05-16 12:09:06 -0700 (Fri, 16 May 2008) $


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Attachment: r.tsunami
Description: Binary data

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