Digital Earth Reference Model

From Pyxis public wiki
Revision as of 13:29, 2 May 2013 by Perry R. Peterson (talk | contribs)
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)
Jump to navigation Jump to search

Frequently abbreviated DERM a Digital Earth model uses a well defined discrete partitioning or grid of cells to model the Earth, as opposed to a continuous point based model developed for navigation of traditional geographic coordinate reference systems.

A Digital Earth Reference Model tends to encompasses four critical principals of a digital model namely:

  • A discrete uniform partitioning also called a Geodesic Discrete Global Grid System (a tessellation or tiling of cells over the Earth surface). Criteria for an optimized discrete global grid has been proposed by Michael Goodchild - generally, equal area cells that exhaustively cover the globe in closely packed hierarchical tessellations, each cell representing a homogeneous value:
  • A unique linear non floating point index for each discrete cell that encompasses within the index both a parent child hierarchical relationship and a coordinate system that converges uniformly to the set of all real numbers;
  • A set of mathematical relationships and operations built on the index: algebra, geometry, Boolean operations, image processing, etc; and
  • Drawing on signal processing theory, a strategy for quantizing values (preferable integers) from analog or other digital sources to each discrete cell.

A DERM is designed to work in a digital environment providing statistically valid sampling, rapid storage, processing, transmission, discovery, visualization, integration, aggregation, and transformations. See: DERM in action.

Icosahedron Snyder Equal Area Aperature 3 Hexagonal Grid