[GRASS-user] Re: [GRASS-dev] New version of the r.landscape.evol.py Landscape Evolution module uploaded to the GRASS Addons repository.

2010-04-28 Thread Michael Barton
The reality is that this kind of modeling works well and is accurate for the 
new MFD routine in r.watershed but does not work nearly as well with 
r.terraflow or with SFD in r.watershed. 

Helena originally proposed this for r.flow, which is how we started out several 
years ago. However, as we developed this modeling script, we learned that a 
full hydrology model worked better than the flow lines information generated by 
r.flow. So we switched to r.terraflow. However, the routines of r.terraflow 
produced numerous 'artifacts' in the way of anomalous spikes and pits that 
could self-amplify over multiple iterations. We used smoothing routines to get 
rid of these. This worked OK, but affected both accuracy of estimating 
erosion/deposition and the speed of calculation (median smoothers take awhile 
to run). We have a paper coming out that uses this version of r.landscape.evol 
(the previous version that is still in addons and downloadable). The old 
version does what it can to work around the limitations of the watershed 
routines that are now standard in GRASS 6.4

Running with the new r.watershed and MFD, however, does not create the kind of 
artifacts we saw with r.terraflow and does not require post facto smoothing. 
This makes it much faster and more accurate in its erosion/deposition 
estimates. Also, the smoothing never was able to completely eliminate the 
terraflow artifacts, but these simply don't exist with r.watershed and MFD. I 
guess I don't see the point of dumbing down the new version of the script to 
work with GRASS 


C. Michael Barton
Director, Center for Social Dynamics & Complexity 
Professor of Anthropology, School of Human Evolution & Social Change
Arizona State University

voice:  480-965-6262 (SHESC), 480-727-9746 (CSDC)
fax:  480-965-7671 (SHESC),  480-727-0709 (CSDC)
www: www.public.asu.edu/~cmbarton, http://csdc.asu.edu










On Apr 28, 2010, at 12:02 PM, Isaac Ullah wrote:

>I suppose that is true from a programmatic point of view, but from 
> scientific point of view, the fact is that MFD makes the module so much more 
> useful that it's pointless to run it with r.terraflow (or SFD r.watershed). 
> Actually, I imagine that including the flag to run r.landscape.evol.py with 
> SFD terraflo/r.watershed is actually being disingenuous, as I'm not even sure 
> that the stream erosion equation can even make valid output using SFD (I need 
> to test this, but my feeling is that it will produce overly-large estimates). 
> 
> I guess that means, then, that I am advocating for backporting of 6.5 
> version of r.watershed to 6.4. Why put out the next stable version of GRASS 
> with clearly inferior capabilities? This IMO is simple guaranteeing the quick 
> obsolescence of the stable GRASS version for anyone actually interested in 
> doing state-of-the-art, cutting-edge, robust research with it. It would make 
> much more sense to me (as a scientist who uses GIS as a tool) to include the 
> best available version of modules in a new release. I understand that one 
> does not want to "break" any dependencies (and thus one should generally try 
> to avoid changing the number/arrangement of module inputs), but surely this 
> can be done for situations where the benefits so greatly outweigh these 
> costs? I imagine that only myself and perhaps a few other scripters will have 
> dependencies on r.watershed, and we can easily amend our scripts to be 
> compatible...
> 
> Cheers,
> 
> Isaac
> 
> On Wed, Apr 28, 2010 at 11:30 AM, Markus Metz 
>  wrote:
> Isaac Ullah wrote:
> > Yes, this is certainly true. We have kept backwards compatibility with a
> > flag to use r.terraflow if the user has GRASS 6.4 or less.
> 
> GRASS 6.4 is the next stable release for some time to come, thus new
> addons for GRASS 6.x should IMHO be tailored for 6.4. Either you
> advocate the backporting of the 6.5 version of r.watershed to 6.4 ;-)
> or you make r.terraflow the default, with a flag indicating to use
> r.watershed.
> 
> Anyway, IMHO, newly updated addons should run in 6.4 with the default 
> settings.
> 
> Markus M
> 
> >
> Markus Metz wrote:
> >>
> >> Isaac Ullah wrote:
> >> >
> >> >
> >> > [The new "r.landscape.evol.py"] takes advantage of the advanced MFD flow
> >> > routing capabilities of the newly
> >> > updated r.watershed module, which produced more accurate stream
> >> > networks,
> >> > and flow accumulation values.
> >>
> >> Nice, but "r.landscape.evol.py" works only with the GRASS 6.5 version
> >> of r.watershed, otherwise
> >> r.terraflow must be used. Contrary to the 6.5 version, the 6.4 version
> >> of r.watershed only supports SFD (D8) and only integer DEMs, floating
> >> point DEMs are truncated to integer(, and it's slower and uses more
> >> memory).
> >>
> >> Markus M
> >
> >
> >
> > --
> > Isaac I Ullah, M.A.
> >
> > Archaeology PhD Candidate,
> > ASU School of Evolution and Social Change
> >
> > Research Assistant,
> > Mediterranean Landscape Dy

Re: [GRASS-user] New version of the r.landscape.evol.py Landscape Evolution module uploaded to the GRASS Addons repository.

2010-04-28 Thread MORREALE Jean Roc

Le 27/04/2010 23:59, Isaac Ullah a écrit :

Dear GRASS users/developers,

 I'm happy to announce that the Mediterranean Landscapes Dynamics Project
has released a brand new version of our landscape evolution script "
r.landscape.evol.py". It can be downloaded from the GRASS ADDONS SVN
Repository in the LandDyn directory (
http://trac.osgeo.org/grass/browser/grass-addons/LandDyn).

   "r.landscape.evol.py" calculates erosion and deposition values for a
region (DEM) given climactic (rainfall) and environmental (vegetation and
soils) conditions. It can iteratively calculate these values over multiple
time-steps, and will produce new surface DEM's for each time step (using the
previous DEM as input in the next time step). "r.landscape.evol.py" uses
process-based transport equations to calculate erosion/deposition
differently for different parts of the landscape (ie. flat areas,
hillslopes, mass movement, small channels, streams).



Hi,

Could you give me more precisions on the recursive aspect and its 
limits, for exemple do you think that your model could be applied to a 
nord europe hydrologic setting ? The testcase shown on your website is a 
wadi bordering the Jordan rift valley which is quite a different beast.


I'm also curious about how far back in time you did push your experiment 
and on the way you did extrapolate the neolithic period settings.


Regards,

MORREALE Jean Roc


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Re: [GRASS-user] Problem after import using r.in.ascii

2010-04-28 Thread Glynn Clements

Hanlie Pretorius wrote:

> I have an existing CSV file that has the headers lat, long and precip.
> The precipitation is a floating point number to two decimal places.
> The coordinates in the CSV file define the centre of a quarter degree
> square. The first set of coordinates in the file is -19.625,15.875.
> 
> Becuase the TRMM data defines the centre of the square, I subtracted
> 0.125 from the first set of coordinates to get the north-west corner
> of the raster. And I added 0.125 to the last coordinate in the CSV
> file, which is -34.875,34.125, to get the south-east corner of the
> raster.

This seems wrong; positive-X is east, positive-Y is north, so you
should be adding to north and east, subtracting from south and west.

> In the CSV file, the latitude stays constant for 74 rows while the
> longitude increments in quarter degree steps. The whole file contains
> 4588 rows, so a grid of the data should have 74 rows and 62 columns,
> right?
> 
> So I reformatted the data to 74 rows and 62 columns and added the header:
> 
> north: -19.5
> south: -35.0

> east:  15.75
> west:  34.25

Positive-X is east, so either east and west are the wrong way around,
or they should both be negative, or this represents a span of 341.5
degrees.

> rows:  74
> cols:  62
> null:  -319.99
> 
> 
> The output of g.region -p is:
> 
> projection: 3 (Latitude-Longitude)
> zone:   0
> datum:  wgs84
> ellipsoid:  wgs84
> north:  18S
> south:  36S

> west:   15E
> east:   35E

Here, east and west have been swapped relative to what you say above.

> nsres:  0:15
> ewres:  0:15
> rows:   72
> cols:   80
> cells:  5760
> 
> 
> I then imported the reformatted file using the command:
> 
> r.in.ascii -f input="3B42RT.2010032409.6.bin.sa.grass"\
> output="2010032409.6.precip" \
> title="Precipitation 2010032409.6"\
> mult=1.0 or read from header nv="* or read from header"
> 
> 
> When imported, I get two thin strips of data on the sides of the
> image. The raster shouldn't contain any nulls (the text file doesn't
> contain the value -319.99), so something is wrong.
> 
> r.info gives a very strange resolutions:
> 
> 
>  |   Type of Map:  raster   Number of Categories: 255
>  |   Data Type:FCELL
>  |   Rows: 74
>  |   Columns:  62
>  |   Total Cells:  4588
>  |Projection: Latitude-Longitude
>  |N: 19:30SS:35S   Res: 0:12:34.054054
>  |E: 15:45EW: 34:15E   Res: 5:30:29.032258

The west edge is east of the east edge, resulting in a span of 341.5
degrees. 341.5 / 62 = 5.508064516129032 = 5:30:29.032258.

>  |   Range of data:min = 0.00  max = 7.47
> 
> 
> Can someone perhaps help me to see what's happening here?

East and west are swapped.

-- 
Glynn Clements 
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[GRASS-user] Re: [GRASS-dev] New version of the r.landscape.evol.py Landscape Evolution module uploaded to the GRASS Addons repository.

2010-04-28 Thread Markus Metz
Isaac Ullah wrote:
> Yes, this is certainly true. We have kept backwards compatibility with a
> flag to use r.terraflow if the user has GRASS 6.4 or less.

GRASS 6.4 is the next stable release for some time to come, thus new
addons for GRASS 6.x should IMHO be tailored for 6.4. Either you
advocate the backporting of the 6.5 version of r.watershed to 6.4 ;-)
or you make r.terraflow the default, with a flag indicating to use
r.watershed.

Anyway, IMHO, newly updated addons should run in 6.4 with the default settings.

Markus M

>
Markus Metz wrote:
>>
>> Isaac Ullah wrote:
>> >
>> >
>> > [The new "r.landscape.evol.py"] takes advantage of the advanced MFD flow
>> > routing capabilities of the newly
>> > updated r.watershed module, which produced more accurate stream
>> > networks,
>> > and flow accumulation values.
>>
>> Nice, but "r.landscape.evol.py" works only with the GRASS 6.5 version
>> of r.watershed, otherwise
>> r.terraflow must be used. Contrary to the 6.5 version, the 6.4 version
>> of r.watershed only supports SFD (D8) and only integer DEMs, floating
>> point DEMs are truncated to integer(, and it's slower and uses more
>> memory).
>>
>> Markus M
>
>
>
> --
> Isaac I Ullah, M.A.
>
> Archaeology PhD Candidate,
> ASU School of Evolution and Social Change
>
> Research Assistant,
> Mediterranean Landscape Dynamics Project
> ***
> isaac.ul...@asu.edu
> ul...@archaeologist.com
>
> http://www.public.asu.edu/~iullah
> ***
>
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[GRASS-user] GRASS meeting in Prague (May 1-2)

2010-04-28 Thread Martin Landa
Hi all,

please ignore this message if you are far away from Prague (Czech Republic) ;-)

In any case you are invited to the Geoinformatics FCE CTU seminar
which takes place in Prague during this weekend (May 1-2). There will
be more GRASS-related topics (talks by Markus Neteler and Markus Metz)
and more... See the program overview for details

http://geoinformatics.fsv.cvut.cz/gwiki/Main_Page#Program_Overview

Cheers, Martin

-- 
Martin Landa  * http://gama.fsv.cvut.cz/~landa
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[GRASS-user] Re: [GRASS-dev] New version of the r.landscape.evol.py Landscape Evolution module uploaded to the GRASS Addons repository.

2010-04-28 Thread Markus Metz
Isaac Ullah wrote:
>
>
> [The new "r.landscape.evol.py"] takes advantage of the advanced MFD flow 
> routing capabilities of the newly
> updated r.watershed module, which produced more accurate stream networks,
> and flow accumulation values.

Nice, but "r.landscape.evol.py" works only with the GRASS 6.5 version
of r.watershed, otherwise
r.terraflow must be used. Contrary to the 6.5 version, the 6.4 version
of r.watershed only supports SFD (D8) and only integer DEMs, floating
point DEMs are truncated to integer(, and it's slower and uses more
memory).

Markus M
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Re: [GRASS-user] Extract coordinates of vertices/nodes

2010-04-28 Thread Markus Metz
2010/4/28 Micha Silver 
>
> On 04/28/2010 12:12 PM, Sophie Leguedois wrote:
>>
>> Greetings,
>>
>> Being quite in Grass, I am trying to find  a way to extract geographic
>> coordinates of vertices and nodes (by the way I am struggling a little to
>> understand the differences between those two concepts) for polygons or
>>
>
> This might help:
> http://grass.osgeo.org/wiki/Vectordata

In short, vertices are all the points that make up a line, a line may
consist of one or more vertices. In GRASS, nodes are the start and end
points of a line, so each line is linked to two nodes. These nodes are
used internally to maintain vector topology:
http://grass.osgeo.org/grass64/manuals/html64_user/vectorintro.html
Section: Vector model and topology
>
>> lines. Do you have any idea how to proceed?
>>
>
> Probably with v.to.points -v
>
There is some useful information in the v.to.points manual about how
to link the extracted points to the original lines.

Markus M
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[GRASS-user] i.atcorr returns all NULL values

2010-04-28 Thread Brian Walters
Hello,
I'm using i.atcorr to perform atmospheric corrections on Landsat 5 TM data
and something peculiar seems to happen arbitrarily to some of the data.  For
the most part everything works fine, but for some of the bands the result is
a raster layer that is filled with nothing but NULL values.  For example, I
have images from 3 dates over the same area.  All the layers are integer and
scaled from 0 - 255, and the elevation layer I'm using is also integer.  All
bands from the first date and the last date run through i.atcorr with no
problems, as do bands 3, 4, 5, & 7 from the middle date.  However, bands 1
and 2 from the middle date return all NULLs.  I have tried many things,
including running i.atcorr on a small subset of the band (same result),
changing the date by a day or two in the* *icnd.txt file (same result), and
changing the band to TM5 band 3 in the icnd.txt file (this ran normally).  I
can't figure out why bands 1 and 2 would run normally on two of my dates and
why bands 3-5,7 would run on this particular date yet bands 1 and 2 result
in the NULL values.  Anyone else have this problem and any clues as to why
i.atcorr is doing this?  Any help would be greatly appreciated.

Here is the text of my icnd.txt file for band 1:
7
6 23 15.966 -84.165 44.587
2
1
14.16
-0.262
-1000
25

The command I'm running:
i.atcorr -r -o iimg=peak_b1_...@mich
ialt=elevat...@michicnd=atcorr_paramfiles/atcorr_peak_B1.txt
oimg=peak_B1_atm_corr

I'm using GRASS version 6.4.0RC6

Thanks,
Brian
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Re: [GRASS-user] TopoFlow and GRASS (or any continuous distributed hydrologic model)

2010-04-28 Thread M S
r.gwflow can help with the groundwater flow.

The r.watershed module can help with where streams in basins originate
and go to the outlet.  The add-on of r.stream.extract can use
weighting parameters to adjust where the streams start (eg. increase
accumulation in wet areas, decrease accumulation in dry, and
montgomery's exponent for adjusting accumulation thresholds to have
more streams in steep areas or flat areas).

These modules will help illustrate where streams begin based on
contributing area/accumulation.  The USGS gauging stations are a good
way to validate your model.

For long term, or rain-fall event orientated analysis, r.water.sim
seems applicable.  It will output depths and discharge rates based on
rainfall and other input parameters.  Validating these simulation
results seems reasonable if you have real time data for a given rain
event with corresponding discharge rates or depths at stations in the
watershed of interest.

I have not looked at the HydroFOSS as an addon, but it indicates it
factors in evapotranspiration.
http://www.foss4g2006.org/contributionDisplay.py?contribId=157&sessionId=40&confId=1

Good luck and please post back any updates.

Mark

On Wed, Apr 28, 2010 at 11:28 AM, stephen sefick  wrote:
> I would like to be able to model groundwater and surface water flow
> for some particular watersheds with usgs gauging stations.  The
> gauging stations are to help parameterize/validate the modeled
> discharge.  I would then like to be able to try and predict
> probability of intermittance, or, in other words, where permenant flow
> starts in the watersheds under investigation.  I think that D8 flow
> algorithm based distributed hydrologic models are the way to do this.
> If I am wrong I would greatly appreciate this being pointed out.  I
> was wondering if there were any implementations for long-term
> simulation (I would like to account for different water years).  Also,
> I would like to, at the least, use GRASS as a preprocessor for gridded
> rainfall and Evapotranspiration time series (along with whatever else
> may be necessary input data).  I have looked into GSSHA, but don't not
> have the resources for acquiring the WMS software needed to drive the
> model ($1500), and it looks like TopoFlow for the Colorado CSMDS
> modelling group would work.  If there are any suggestions, comments,
> or criticisms of my decisions for trying to attack this problem please
> point them out.  Thank you all very much for your wonderful help.
> kindest regards,
>
> Stephen Sefick
>
> On Thu, Apr 22, 2010 at 8:54 AM, Rich Shepard  
> wrote:
>> On Thu, 22 Apr 2010, stephen sefick wrote:
>>
>>> I would like to simulate the hydrology of a watershed.  Does anyone have
>>> guidance for this particular endeavor- especially with the help of GRASS
>>> GIS as a raster processor, or engine for model analysis?
>>
>>  There are several hydrologic modules available for your use. The raster
>> manual (r.*) has details on each, and the wiki has a section on hydrological
>> modeling.
>>
>>  The question you need to answer in order to get more focused help here is
>> just what it is you want to do. What problem are you trying to solve? What
>> behavior(s) do you want to explore? Specificity, and telling us what you've
>> done so far to educate yourself, goes a long way to helping you.
>>
>> Rich
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>>
>
>
>
> --
> Stephen Sefick
>
> Let's not spend our time and resources thinking about things that are
> so little or so large that all they really do for us is puff us up and
> make us feel like gods.  We are mammals, and have not exhausted the
> annoying little problems of being mammals.
>
>                                                                -K. Mullis
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Re: [GRASS-user] TopoFlow and GRASS (or any continuous distributed hydrologic model)

2010-04-28 Thread stephen sefick
I would like to be able to model groundwater and surface water flow
for some particular watersheds with usgs gauging stations.  The
gauging stations are to help parameterize/validate the modeled
discharge.  I would then like to be able to try and predict
probability of intermittance, or, in other words, where permenant flow
starts in the watersheds under investigation.  I think that D8 flow
algorithm based distributed hydrologic models are the way to do this.
If I am wrong I would greatly appreciate this being pointed out.  I
was wondering if there were any implementations for long-term
simulation (I would like to account for different water years).  Also,
I would like to, at the least, use GRASS as a preprocessor for gridded
rainfall and Evapotranspiration time series (along with whatever else
may be necessary input data).  I have looked into GSSHA, but don't not
have the resources for acquiring the WMS software needed to drive the
model ($1500), and it looks like TopoFlow for the Colorado CSMDS
modelling group would work.  If there are any suggestions, comments,
or criticisms of my decisions for trying to attack this problem please
point them out.  Thank you all very much for your wonderful help.
kindest regards,

Stephen Sefick

On Thu, Apr 22, 2010 at 8:54 AM, Rich Shepard  wrote:
> On Thu, 22 Apr 2010, stephen sefick wrote:
>
>> I would like to simulate the hydrology of a watershed.  Does anyone have
>> guidance for this particular endeavor- especially with the help of GRASS
>> GIS as a raster processor, or engine for model analysis?
>
>  There are several hydrologic modules available for your use. The raster
> manual (r.*) has details on each, and the wiki has a section on hydrological
> modeling.
>
>  The question you need to answer in order to get more focused help here is
> just what it is you want to do. What problem are you trying to solve? What
> behavior(s) do you want to explore? Specificity, and telling us what you've
> done so far to educate yourself, goes a long way to helping you.
>
> Rich
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-- 
Stephen Sefick

Let's not spend our time and resources thinking about things that are
so little or so large that all they really do for us is puff us up and
make us feel like gods.  We are mammals, and have not exhausted the
annoying little problems of being mammals.

-K. Mullis
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[GRASS-user] Problem after import using r.in.ascii

2010-04-28 Thread Hanlie Pretorius
Greetings Herbivores,

This is the first time that I've created a location and mapset fo my
own and I'm trying to import TRMM precipitation data into GRASS using
r.in.ascii.

I have an existing CSV file that has the headers lat, long and precip.
The precipitation is a floating point number to two decimal places.
The coordinates in the CSV file define the centre of a quarter degree
square. The first set of coordinates in the file is -19.625,15.875.

Becuase the TRMM data defines the centre of the square, I subtracted
0.125 from the first set of coordinates to get the north-west corner
of the raster. And I added 0.125 to the last coordinate in the CSV
file, which is -34.875,34.125, to get the south-east corner of the
raster.

In the CSV file, the latitude stays constant for 74 rows while the
longitude increments in quarter degree steps. The whole file contains
4588 rows, so a grid of the data should have 74 rows and 62 columns,
right?

So I reformatted the data to 74 rows and 62 columns and added the header:

north:   -19.5
south:   -35.0
east:15.75
west:34.25
rows:74
cols:62
null:-319.99


The output of g.region -p is:

projection: 3 (Latitude-Longitude)
zone:   0
datum:  wgs84
ellipsoid:  wgs84
north:  18S
south:  36S
west:   15E
east:   35E
nsres:  0:15
ewres:  0:15
rows:   72
cols:   80
cells:  5760


I then imported the reformatted file using the command:

r.in.ascii -f input="3B42RT.2010032409.6.bin.sa.grass"\
output="2010032409.6.precip" \
title="Precipitation 2010032409.6"\
mult=1.0 or read from header nv="* or read from header"


When imported, I get two thin strips of data on the sides of the
image. The raster shouldn't contain any nulls (the text file doesn't
contain the value -319.99), so something is wrong.

r.info gives a very strange resolutions:


 |   Type of Map:  raster   Number of Categories: 255
 |   Data Type:FCELL
 |   Rows: 74
 |   Columns:  62
 |   Total Cells:  4588
 |Projection: Latitude-Longitude
 |N: 19:30SS:35S   Res: 0:12:34.054054
 |E: 15:45EW: 34:15E   Res: 5:30:29.032258
 |   Range of data:min = 0.00  max = 7.47


Can someone perhaps help me to see what's happening here?

Thanks
Hanlie
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[GRASS-user] osm import

2010-04-28 Thread Moritz Lennert

Hamish,

In a recent post [1], you said that to import OSM maps, one can use 
v.in.ogr, but I don't see a driver for OSM maps in ogr. Could you explain ?


Thanks !

Moritz



[1]http://lists.osgeo.org/pipermail/grass-user/2010-January/054253.html
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[GRASS-user] v.vol.idw

2010-04-28 Thread Stefania Merlo

Hi,

I was wondering what happened to the above command in the new releases  
of GRASS. I am quite sure I did use it in GRASS 5 and possibly early  
versions of 6 but it seems it got lost somewhere along the road. Is  
there any reason for this? Does anyone remember in what version of  
GRASS for Mac it was last present? I am in desperate need to use it to  
interpolate 3d points of subsoil data for comparison with v.vol.rst.


All best

Stefania


Stefania Merlo
Department of Archaeology
University of Cambridge
United Kingdom
sm...@cam.ac.uk


 “Mi piacerebbe che il mio viaggio fosse ancora lungo e costellato di  
smarrimenti, si mi piacerebbe vivere per molto tempo e commettere  
ancora mille errori, mille sbagli, ed anche un certo numero di peccati  
memorabili”! (Amin Maalouf, Il periplo di Baldassarre)


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Re: [GRASS-user] Extract coordinates of vertices/nodes

2010-04-28 Thread Micha Silver

On 04/28/2010 12:12 PM, Sophie Leguedois wrote:

Greetings,

Being quite in Grass, I am trying to find  a way to extract geographic
coordinates of vertices and nodes (by the way I am struggling a little to
understand the differences between those two concepts) for polygons or
   

This might help:
http://grass.osgeo.org/wiki/Vectordata

lines. Do you have any idea how to proceed?
   

Probably with v.to.points -v



Cheers

So.L.
   



--
Micha Silver
http://www.surfaces.co.il/
Arava Development Co.  +972-52-3665918

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[GRASS-user] Re: Extract coordinates of vertices/nodes

2010-04-28 Thread schorschli

Hi Sophie,

v.out.ascii format=standard might help. 

Here is the manual:
http://grass.itc.it/grass64/manuals/html64_user/v.out.ascii.html

Afterwards you can write a simple script to extract the coordinates from the
ascii-output.


schorschli
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[GRASS-user] Extract coordinates of vertices/nodes

2010-04-28 Thread Sophie Leguedois

Greetings,

Being quite in Grass, I am trying to find  a way to extract geographic
coordinates of vertices and nodes (by the way I am struggling a little to
understand the differences between those two concepts) for polygons or
lines. Do you have any idea how to proceed?

Cheers

So.L.
-- 
View this message in context: 
http://osgeo-org.1803224.n2.nabble.com/Extract-coordinates-of-vertices-nodes-tp4973423p4973423.html
Sent from the Grass - Users mailing list archive at Nabble.com.
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