Changeset 2727


Ignore:
Timestamp:
Apr 19, 2006, 5:39:16 PM (18 years ago)
Author:
sexton
Message:

updates to user manual (glossary and slump)

File:
1 edited

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  • documentation/user_manual/anuga_user_manual.tex

    r2720 r2727  
    11221122                verbose=False}
    11231123This function returns a callable object representing an initial water
    1124 displacement generated by a submarine sediment slide.
    1125 
    1126 The arguments include the downslope slide length, the water depth to the slide centre of mass,
    1127 and the bathymetric slope.
     1124displacement generated by a submarine sediment failure. These failures can take the form of
     1125a submarine slump or slide.
     1126
     1127The arguments include as a minimum, the slump or slide length, the water depth to the centre of sediment
     1128mass, and the bathymetric slope. Other slump or slide parameters can be included if they are known.
    11281129\end{funcdesc}
    11291130
     
    18501851    \item \indexedbold{\anuga} Name of software (joint development between ANU and GA)
    18511852
    1852     \item \indexedbold{domain}
    1853 
    1854     \item \indexedbold{Dirichlet boundary}
     1853    \item \indexedbold{domain} The domain of a function is the set of all input values to the function.
     1854
     1855    \item \indexedbold{Dirichlet boundary} - A Dirichlet boundary condition imposed on a differential equation
     1856 which specifies the values the solution is to take on the boundary of the domain.
    18551857
    18561858    \item \indexedbold{elevation} - refers to bathymetry and topography
    18571859
    1858     \item \indexedbold{bathymetry} offshore
    1859 
    1860     \item \indexedbold{topography} onshore
    1861 
    1862     \item \indexedbold{evolution} integration of the shallow water wave equations over time
     1860    \item \indexedbold{bathymetry} - offshore elevation
     1861
     1862    \item \indexedbold{topography} - onshore elevation
     1863
     1864    \item \indexedbold{evolution} - integration of the shallow water wave equations over time
    18631865
    18641866    \item \indexedbold{forcing term}
    18651867
    1866     \item \indexedbold{IDLE} Development environment shipped with Python
    1867 
    1868     \item \indexedbold{Manning friction coefficient}
    1869 
    1870     \item \indexedbold{mesh}    Triangulation of domain
     1868    \item \indexedbold{IDLE} - Development environment shipped with Python
     1869
     1870    \item \indexedbold{Manning friction coefficient} 
     1871
     1872    \item \indexedbold{mesh}    - Triangulation of domain
    18711873
    18721874    \item \indexedbold{meshfile}  [generic word for either .tsh or
     
    18761878    .xya file]
    18771879
    1878     \item \indexedbold{grid} evenly spaced
     1880    \item \indexedbold{grid} - evenly spaced mesh
    18791881
    18801882    \item \indexedbold{NetCDF}
     
    18841886    \item \indexedbold{pyvolution} does this really need to be here? it's a class/module?
    18851887
    1886     \item \indexedbold{conserved quantity} conserved (state, x and y momentum)
     1888    \item \indexedbold{conserved quantity} conserved (stage, x and y momentum)
    18871889
    18881890    \item \indexedbold{reflective boundary}
     
    18941896%    \item \indexedbold{try this}
    18951897
    1896     \item \indexedbold{swollen} visualisation tool
    1897 
    1898     \item \indexedbold{time boundary} defined in the manual (flog from there)
    1899 
    1900     \item \indexedbold{transmissive boundary} defined in the manual (flog from there)
    1901 
    1902     \item \indexedbold{xmomentum} conserved quantity (note, two-dimensional SWW equations say only x and y and NOT z)
    1903 
    1904     \item \indexedbold{ymomentum}  conserved quantity
    1905 
    1906     \item \indexedbold{resolution}   The maximal area of a triangular cell in a mesh
    1907 
    1908     \item \indexedbold{polygon} A sequence of points in the plane. (Arbitrary polygons can be created
     1898    \item \indexedbold{swollen} - visualisation tool
     1899
     1900    \item \indexedbold{time boundary} - defined in the manual (flog from there)
     1901
     1902    \item \indexedbold{transmissive boundary} - defined in the manual (flog from there)
     1903
     1904    \item \indexedbold{xmomentum} - conserved quantity (note, two-dimensional SWW equations say only x and y and NOT z)
     1905
     1906    \item \indexedbold{ymomentum}  - conserved quantity
     1907
     1908    \item \indexedbold{resolution} -  The maximal area of a triangular cell in a mesh
     1909
     1910    \item \indexedbold{polygon} - A sequence of points in the plane. (Arbitrary polygons can be created
    19091911    in this way.)
    19101912    \anuga represents a polygon in one of two ways. One way is to represent it as a
     
    19171919    NOTE: More can be read in the module utilities/polygon.py ....
    19181920
    1919     \item \indexedbold{easting}
    1920 
    1921     \item \indexedbold{northing}
    1922 
    1923     \item \indexedbold{latitude}
    1924 
    1925     \item \indexedbold{longitude}
    1926 
    1927     \item \indexedbold{edge}
    1928 
    1929     \item \indexedbold{vertex}
    1930 
    1931     \item \indexedbold{finite volume}
    1932 
    1933     \item \indexedbold{flux}
    1934 
    1935     \item \indexedbold{Digital Elevation Model (DEM)}
     1921    \item \indexedbold{easting} - A rectangular (x,y) coordinate measurement of distance east from a north-south reference line,
     1922usually a meridian used as the axis of origin within a map zone or projection. Easting is a UTM (Universal Transverse Mercator) Coordinate.
     1923
     1924    \item \indexedbold{northing} - A rectangular (x,y) coordinate measurement of distance north from a north-south reference line,
     1925usually a meridian used as the axis of origin within a map zone or projection. Northing is a UTM (Universal Transverse Mercator) Coordinate.
     1926
     1927
     1928    \item \indexedbold{latitude} - The angular distance on a mericlear north and south of the equator, expressed in degrees and minutes.
     1929
     1930    \item \indexedbold{longitude} - The angular distance east or west, between the meridian of a particular place on Earth and that of the
     1931Prime Meridian (located in Greenwich, England) expressed in degrees or time.
     1932
     1933    \item \indexedbold{edge} - A triangulare cell within the computational mesh can be depicted as a set of vertices joined by lines (the edges).
     1934
     1935    \item \indexedbold{vertex} - A point at which edges meet.
     1936
     1937    \item \indexedbold{finite volume} - The method evaluates the terms in the shallow water wave equationas fluxes at the surfaces of each
     1938finite volume. Because the flux entering a given volume is identical to that leaving the adjacent volume, these methods are conservative.
     1939Another advantage of the finite volume method is that it is easily formulated to allow for unstructured meshes.
     1940The method is used in many computational fluid dynamics packages.
     1941
     1942
     1943    \item \indexedbold{flux} - the amount of flow through the volume per unit time
     1944
     1945    \item \indexedbold{Digital Elevation Model (DEM)} - DEMs are digital files consisting of points of elevations,
     1946sampled systematically at equally spaced intervals.
    19361947
    19371948
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