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The map server Web tool is designed to permit rapid browsing of the MODIS Mosaic of Antarctica (MOA) data set, and provide readily accessible images for figures, field planning, presentations, etc. This tool was created at the University of New Hampshire by Dr. Mark Fahnestock and Mr. Norman Vine. The MOA Web-based map server contains several pre-stretched versions of the MOA data set, allowing both high-contrast areas (for example, glaciers and mountains) and low-contrast areas (for example, ice shelves, plateau surface) to be displayed with the full information content of MOA.
Note: The map server also allows users to view the RAMP AMM-1 125 m backscatter image from 1997.
Use the radio buttons to select zoom options: In, Pan, or Out. Zooming or panning is accomplished by clicking the Refresh/Query button or a location in the large zoomed image. Clicking a location in the small reference image pans to that location at the current zoom level.
The Size field refers to the zoom rate. Zoom is limited to integer steps, 1-25. Note that zooming out by one integer (Use 3 as an example.) and then zooming in by another (for example, 4) gives a fractional increase in zoom (1.33; 4/3=In/Out=1.33).
|Layer Options||Description||Range of Surface Brightness Values|
|moa_uhc||MOA surface image, ultra-high contrast||15875 - 16125|
|moa_vhc||MOA surface image, very high contrast||15800 - 16200|
|moa_hc||MOA surface image, high contrast||15500 - 16500|
|moa||MOA surface image, nominal contrast||15000 - 17000|
|moa_lc||MOA surface image, low contrast||12000 - 20000|
|moa_vlc||MOA surface image, very low contrast||9000 - 23000|
|moa_ulc||MOA surface image, ultra-low contrast||1 - 32000|
|ramp||RAMP AMM-1 125 m backscatter image||1 - 255|
A graticule is a grid of location lines, in this case latitude-longitude lines, that overlays a map or image grid. On the MOA site, this is generated interactively by the Minnesota Map Server (MMS) from the projection information for MOA. The algorithm is set to produce overlay grids with approximately 3 to 10 lines in each direction. Note: There are known problems with the Graticule when it includes the 180° meridian. This layer also lacks line labels at high zoom levels.
The main two-byte MOA data set (namely, the high-pass filtered MODIS Band 1 image) is an array of numbers representing surface brightness, each value of which is in the range 1 to 65535 with an average value of about 16000. However, in order to make a one-byte MOA grey-level image that can be displayed, a portion of this 1 to 65535 range (namely, a minimum and a maximum value) is mapped into values in the range 1 to 255 using linear interpolation. A particular mapping can be represented by a minimum-maximum pair, and is referred to as a "contrast stretch."
The seven MOA image layers are versions of the main MOA data set with different contrast stretches applied. The contrast stretches are applied on-the-fly as the data are extracted from the two-byte MOA image. The stretches allow a user to enhance the features of interest to their application of the data. Low-contrast features, such as subtle ice topography on ice shelves, are best revealed by the moa_uhc (ultra-high contrast) stretch. High-contrast features, such as mountains and valleys, are best represented by the very low or ultra-low contrast stretches of MOA.
The ramp layer is a version of the Radarsat Antarctic Mapping Program (RAMP) Antarctic Mapping Mission 1 (AMM-1) synthetic aperature radar (SAR) image, compiled from data acquired by Canada's Radarsat 1 satellite during September and October of 1997 (for comparison, the MOA MODIS imagery was acquired between 20 November 2003 and 29 February 2004). This 125 m 1-byte product (grey values limited between 1 and 255) reveals details related to both topography and snow characteristics in the upper few tens of meters of the ice sheet (See RAMP Data.).
The Ctrl key can used to select both Graticule, which provides a latitude-longitude grid, and one or two of the image layers at the same time. Selecting two image layers gives a blended image, unless one of them is the ramp mosaic layer, in which case only the ramp mosaic layer is shown.
Upgrades with additional layers and the snow-grain-size image are in the development stage. See the MOA - MODIS Mosaic of Antarctica map server on the University of New Hampshire Web site. (UNH map server availability may be intermittent.)
Clicking on the Comments button will launch your email client to send a message to NSIDC User Services.
The User's Guide link will direct you to this document.
Follow this example to become familiar with the interface.
You can use your browser to save a MOA image to your hard drive. For example, using Netscape, move the cursor over the large zoomed image or the small reference image, click the right mouse button, and select Save Image As... You can then specify a directory and file name for a saved JPEG file. A similar procedure can be used with other browsers. Note: Useful information about the image, such as the projected corner pixel x and y coordinates, which is used to derive the latitudinal and longitudinal coordinates, is included in the URL.
A great deal of information is available in the URL. It is shown here with carriage returns added to improve readability. The information in bold font is followed by an explanation.
From the URL, the important pieces of information are:
The above x and y values refer to a projected coordinate system with the center of the projection at the south pole, and include the part of the image "underneath" the scale bar at the bottom of the image.
If needed, the x and y scales can be calculated using:
xscale = (urx - llx) / numcols = (601565.625000 - (-908840.625000)) / 800 = 1888.0078 meters per pixel
yscale = (ury - lly) / numrows = (550340.625000 - (-960065.625000)) / 800 = 1888.0078 meters per pixel
For MOA, investigators employed the Mapx library, which enables the addition of mapping functionality to an application to handle map projections. A map projection is a mapping between geographic latitude-longitude coordinates, usually represented in degrees on the Earth's surface, and Cartesian x-y coordinates, usually represented in meters on a plane surface. Mapx utilities provide access to predefined maps and the capability to define map projection parameters (MPP) stored in a .mpp file. These additional map projection parameters, which are independent of the view, include:
Map Projection: Polar Stereographic Ellipsoid
Map Reference Latitude: -90.0
Map Reference Longitude: 0.0
Map Second Reference Latitude: -71.0 ; latitude of true scale
Map Equatorial Radius: 6378137.0 ; wgs84 meters
Map Eccentricity: 0.081819190843 ; wgs84
This file, Moa.mpp, is available via FTP.
Converting xy corner points to latitude-longitude pairs requires some kind of map projection software package. In the case of the Mapx package (Visit Mapx: Map Transformations Library.), investigators use the xytest program included in Mapx together with Moa.mpp as follows:
> assuming map origin lat is same as ref. lat -90.000000
> assuming map origin lon is same as ref. lon 0.000000
enter lat lon -
enter x y - -908840.625000 -960065.625000
lat,lon = -77.8762579 -136.5700315 valid
x,y = -908840.6250001 -960065.6250001 valid
enter x y - 601565.625000 50340.625000
lat,lon = -84.4482155 85.2164807 valid
x,y = 601565.6250001 50340.6250000 valid
enter x y - -908840.625000 550340.625000
lat,lon = -80.2439738 -58.8033590 valid
x,y = -908840.6250001 550340.6250001 valid
enter x y - 601565.625000 -960065.625000
lat,lon = -79.6000806 147.9292345 valid
x,y = 601565.6250001 -960065.6250001 valid
lower left lat-lon = -77.8762579 -136.5700315
upper right lat-lon = -84.4482155 85.2164807
upper left lat-lon = -80.2439738 -58.8033590
lower right lat-lon = -79.6000806 147.9292345
Haran, T., J. Bohlander, T. Scambos, and M. Fahnestock compilers. 2005. MODIS mosaic of Antarctica (MOA) image map. Boulder, CO, USA: National Snow and Ice Data Center. Digital media.
For assistance or more information on this data set, contact User Services at NSIDC.