[GRASS-SVN] r47929 - grass-web/trunk/intro
svn_grass at osgeo.org
svn_grass at osgeo.org
Mon Aug 29 03:17:25 EDT 2011
Author: neteler
Date: 2011-08-29 00:17:24 -0700 (Mon, 29 Aug 2011)
New Revision: 47929
Modified:
grass-web/trunk/intro/modelintegration.html
Log:
some cleanup
Modified: grass-web/trunk/intro/modelintegration.html
===================================================================
--- grass-web/trunk/intro/modelintegration.html 2011-08-28 22:38:34 UTC (rev 47928)
+++ grass-web/trunk/intro/modelintegration.html 2011-08-29 07:17:24 UTC (rev 47929)
@@ -11,83 +11,13 @@
<IMG SRC="../images/grass.smlogo.gif" alt="HOME" ALT="grasslogo" ALIGN=CENTER>
GRASS GIS - Simulation Models</H1>
-<p>
-<i>Current Topics: erosion modelling, hydrological modelling, floodplain analysis,
-wildfire spread</i>
-<p>
-<h3>Erosion modelling: ANSWERS - r.answers</h3>
-<ul>
- <li> The acronym for Areal Non-point Source Watershed Environmental Response
- Simulation model. This event-oriented, distributed parameter model is
- designed for erosion, sediment and water quality control planning on
- complex, agricultural watersheds.
- <li> It should normally be distributed in your GRASS-package. Note: ANSWERS is
- written in C and FORTRAN, and will require a C compiler and a FORTRAN
- compiler such as f77.
- <li><a href="http://soils.ecn.purdue.edu/~aggrass/models/answers/">ANSWERS
-page at Purdue</A>
- <li><a href="gdp/html_grass5/html/r.answers.html">GRASS man page r.answers</A>
-</ul>
+For topic oriented pages, see <a href="http://grass.osgeo.org/wiki/Category:Applications">GRASS GIS Applications</a> in the Wiki.
-
-<h3>Erosion modelling: AGNPS 5.0 </h3>
+<h3>Hydrological modelling</h3>
<ul>
- <li> AGricultural Non-Point Source (AGNPS) is a distributed parameter model
-developed by Agricultural Research Service (ARS) scientists and engineers. It
-predicts soil erosion and nutrient transport/loadings from agricultural
-watersheds for real or hypothetical storms i.e., it's an event-based model.
-Erosion modeling is built upon the USLE applied on a storm basis; thus, it uses
-the EI-index for single storm events. Its hydrology is based on the Soil
-Conservation Service Curve Number technique. AGNPS uses another ARS developed
-model named CREAMS to predict nutrient/pesticide and soil particle size
-generation and interaction. Here is a <A HREF=gdp/erosion/agnps/agnps.html> AGNPS Page</A>.
-Some help about using AGNPS can be found <A HREF=http://pasture.ecn.purdue.edu:80/~engelb/agen526/>here</A>.
-Note: AGNPS 5.0 is written in C.
-<p>
- References:
-<ul>
- <li> GRASS man pages: <A HREF="gdp/html_grass5/html/r.agnps50.input.html">r.agnps50.input</A>,
- <A HREF="gdp/html_grass5/html/r.agnps50.run.html">r.agnps50.run</A>, <A HREF="gdp/html_grass5/html/r.agnps50.view.html">r.agnps50.view</A>
- <li> Bragadin, G.L., Franchini, M., Morgagni, A., Todini, E. (1993): Agricultural
- non-point source nutrient loadings estimated by means of an extended version
- of AGNPS. The Bidente-Ronco case study - Part I. INGEGNERIA AMBIIENTALE,
- Vol.22, Nr.9, S. 455
-
- <li> Mitchell, J.K., Engel, B.A., Srinivasan,R., Wang, S.S.Y. (1993): Validation of AGNPS
- for Small Watersheds Using an Integrated AGNPS/GIS System. WATER RESOURCES
- BULLETIN- AMERICAN WATER RESOURCES ASSOCIATION, Vol.29, Nr.5, S. 833
- <li> Robert Alton Young, C.A. Onstad, D.D. Bosch, W.P. Anderson. (1989)
- AGNPS: A nonpoint-source pollution model for evaluating agricultural
- watersheds. Jour. of Soil and Water Conservation. v44, n2. ISSN 0022-4561
-
- <li> Srinivasan, R. and B.A. Engel, (1991), A Knowledge Based Approach
- to Extract Input Data From Gis, ASAE Paper No. 91-7045, American
- Society of Agriculatural Engineers, St. Joseph, Michigan.
-
- <li> Srinivasan, R. and B.A. Engel, (1991), GIS: A Tool For Visualization
- and Analyzation, ASAE Paper No. 91-7574, ASAE, St. Joseph, Michigan.
-
- <li> Srinivasan, R., Engel, B.A., Wright, J.R., Lee, J.G.(1994):
- The Impact of GIS-derived Topographic Attributes on the Simulation of
- Erosion Using AGNPS. APPLIED ENGINEERING IN AGRICULTURE , Vol.10,
- Nr.4, S. 561
-
+ <li> See <a href="http://grass.osgeo.org/wiki/Hydrological_Sciences">Hydrological Sciences</a>
</ul>
-</ul>
-<h3> Erosion modelling: KINEROS - r.kineros</h3>
-<ul>
- <li> KINEROS represents a watershed as a set of related elements.
- Elements may be hillslopes, channels or ponds. A computational order
- must be specified so that boundary conditions for an element, such as
- the amount of water contributed by lateral hillslopes and upstream
- tributaries, are available.
-<p>(Smith et al., in press; Woolhiser et al., 1990).
- <li><a href="gdp/html_grass4/html/r.kineros.html">GRASS man page r.kineros</A>
-</ul>
-
-
-<hr>
<h3>Rainfall-runoff modelling: TOPMODEL - r.topmodel</h3>
<ul>
<li> TOPMODEL is a rainfall-runoff model that bases its distributed
@@ -99,71 +29,13 @@
that the predictions conform as far as possible to the user's perceptions
of how a catchment works. The distributed outputs from the model
help in such assessments.
- <li><a href="http://www.es.lancs.ac.uk/hfdg/topmodel.html">TOPMODEL page at
+ <li><a href="http://web.archive.org/web/20050731101409/http://www.es.lancs.ac.uk/hfdg/topmodel.html">TOPMODEL page at
Lancaster University</A>
- <li><a href="gdp/html_grass5/html/r.topmodel.html">GRASS man page r.topmodel</A>
- <li><a href="gdp/html_grass5/html/r.topidx.html">GRASS man page r.topidx</A>
- <li><a href="http://www.es.lancs.ac.uk/hfdg/TOPMODEL/new-bibliog.html">TopModel Bibliography</A>
+ <li><a href="gdp/html_grass64/html/r.topmodel.html">GRASS man page r.topmodel</A>
+ <li><a href="gdp/html_grass64/html/r.topidx.html">GRASS man page r.topidx</A>
+ <li><a href="http://web.archive.org/web/20050731101409/http://www.es.lancs.ac.uk/hfdg/TOPMODEL/new-bibliog.html">TopModel Bibliography</A>
</ul>
-<h3>Storm water runoff: r.water.fea</h3>
-<ul>
-<li> r.water.fea is an interactive program that allows the user to simulate
- storm water runoff analysis using the finite element numerical technique.
-Infiltration is calculated using the Green and Ampt formulation. r.water.fea
-computes and draws hydrographs for every basin as well as at stream junctions
-in an analysis area. It also draws animation maps at the basin level. The
-software is available within GRASS 4.x/5.x.
-<li><a href="http://www.coe.ou.edu/emgis/software/rwaterfea.htm">r.water.fea</A>
-developed at University of Oklahoma by Dr. B.E. Vieux
- <li><a href="gdp/html_grass5/html/r.water.fea.html">GRASS man page r.water.fea</A>
-</ul>
-
-<h3>Hydrologic modelling: r.hydro.CASC2D</h3>
-<ul>
-<li><a href=http://www.engr.uconn.edu/~ogden/casc2d/casc2d_home.html>CASC2D
-page at University of Connecticut</a>
-<li>r.hydro.CASC2D is a physically-based, distributed, raster
-hydrologic model which simulates the hydrologic response of a watershed
-subject to a given rainfall field. Input rainfall is allowed to vary in
-space and time. Major components of the model include interception,
-infiltration, and surface runoff routing. Interception is a process whereby
-rainfall is retained by vegetation. Interception is estimated using an
-empirical three parameter model. Infiltration is the process whereby
-rainfall or surface water is pulled into the soil by capillary and
-gravity forces. The Green and Ampt equation with four parameters is applied
-to model the event-based infiltration. For continuous soil moisture
-accounting, redistribution of soil moisture can also be simulated whenever
-the non-intercepted rainfall intensity falls below the saturated hydraulic
-conductivity of the soil. The redistribution option requires two more soil
-hydraulic parameters. Excess rainfall becomes surface runoff and is routed
-as overland flow and subsequently as channel flow. The overland flow routing
-formulation is based on a two-dimensional explicit finite difference (FD)
-technique, while two different FD techniques, one explicit and
-one implicit, provide options for routing one-dimensional channel flow.
-Through a step function, a depression depth may be specified, below which no
-overland flow will be routed.
- <li><a href="gdp/html_grass5/html/r.hydro.CASC2D.html">GRASS man page
-r.hydro.CASC2D</A>
-</ul>
-
-<h3>SWAT hydrologic model</h3>
-The Soil and Water Assessment Tool (SWAT) is the hydrologic model
-used in the SWAT/GRASS linkage (USDA/Arnold and others, 1995). SWAT
-is a continuous-time, basin-scale hydrologic model capable of
-complex long-term simulations including hydrology, pesticide and
-nutrient cycling, and erosion and sediment transport. It is a river basin scale model
-developed to quantify the impact of land management practices in
-large, complex watersheds. SWAT is a public domain model actively
-supported by the USDA Agricultural Research Service at the
-Grassland, Soil and Water Research Laboratory in Temple, TX.
-
-<ul>
-<li><a href="http://www.brc.tamus.edu/swat/">SWAT main page</a>
-<li><a href="http://www.brc.tamus.edu/swatgrass/index.html">Full SWAT-GRASS man page with references</a>
-</ul>
-<hr>
-
<h3>Watershed Calculation: r.watershed</h3>
<ul>
<li> The series of programs provided within the watershed menu is
@@ -179,36 +51,12 @@
5. Coding stream segments/finding segment lengths
6. Finding subwatershed basins
</pre>
- <li><a href="gdp/html_grass5/html/r.watershed.html">GRASS man page
-r.watershed</A>
+ <li><a href="gdp/html_grass64/html/r.watershed.html">GRASS man page r.watershed</A>
</ul>
-
-
-<h3>Floodplain Analysis: f.input etc.</h3>
+<h3>Landscape Analysis: r.le and r.li</h3>
<ul>
-<li>f.input reads the results of the HEC-2 Water Surface Profile model
-and generates a vector map of water surface elevations at hydraulic
-sections. The user supplies to f.input a vector map of the hydraulic
-cross sections used in the HEC-2 model along with the HEC-2 model
-results.
-<li>f.econ takes as input the results of f.wsurf along with a
-user-supplied vector map of building sites and two ASCII files of
-economic data. As output f.econ generates a vector map of total
-damage to each building in the floodplain along with a summary ASCII
-report of flood damages categorized by building types (residential,
-public, ...) and damage type (structure or content). f.econ also
-reports areal extent of flooding.
-<li> f.reach provides floodwater statistics, including areal extent of
-flooding, average flood depth, and volume of water, calculated on a
-reach-by-reach basis.
-</ul>
-
-<hr>
-
-<h3>Landscape Analysis: r.le</h3>
-<ul>
<li> Since the 1970s, with the availability of satellite data, there has
been an increasing interest in the structure of the earth on the scale of kilometers
or hundreds of kilometers.
@@ -247,8 +95,10 @@
options for graphing or statistically analyzing the results of
the analyses. External software must be used.
</ul>
- <li><a href="gdp/landscape/">Postscript documentation</A> (check also the
- related manual pages)
+ <li><a href="gdp/landscape/">Postscript documentation</A>
+ <li><a href="gdp/html_grass64/html/r.le.html">GRASS man page r.le</A>
+ <li><a href="gdp/html_grass64/html/r.li.html">GRASS man page r.li</A>
+</ul>
<hr>
@@ -270,25 +120,16 @@
<li> r.spreadpath - Recursively traces the least cost path
backwards to cells from which the cumulative cost was
determined.
- <li><a href="gdp/html_grass5/html/r.ros.html">GRASS man page
-r.ros</A>
- <li><a href="gdp/html_grass5/html/r.spread.html">GRASS man page
-r.spread</A>
- <li><a href="gdp/html_grass5/html/r.spreadpath.html">GRASS man page
-r.spreadpath</A>
+ <li><a href="gdp/html_grass64/html/r.ros.html">GRASS man page r.ros</A>
+ <li><a href="gdp/html_grass64/html/r.spread.html">GRASS man page r.spread</A>
+ <li><a href="gdp/html_grass64/html/r.spreadpath.html">GRASS man page r.spreadpath</A>
</ul>
-<hr>
-<ul>
- <li><A HREF=http://pasture.ecn.purdue.edu/~aggrass/models/> Model integration in GRASS</A> - Collection of Bernie Engel.
-</ul>
-
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