18-Geom-A7 Geospatial Information Systems · May 2014
Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)
National Exams — May 2014 — 04-Geom-A7 Geospatial Information Systems. Closed-book; no calculator permitted. Format: twenty-three short-answer questions of equal value (5 marks each); a candidate answers any twenty, but all twenty-three are solved in full below. Datum and coordinate conventions follow the Canadian spatial reference framework — NAD83(CSRS) horizontally and CGVD2013 vertically.
Reference texts: P. A. Longley, M. F. Goodchild, D. J. Maguire & D. W. Rhind, Geographic Information Systems and Science (4th ed., Wiley, 2015); P. Bolstad, GIS Fundamentals: A First Text on Geographic Information Systems (6th ed., XanEdu, 2019); P. A. Burrough, R. A. McDonnell & C. D. Lloyd, Principles of Geographical Information Systems (3rd ed., Oxford, 2015); M. Worboys & M. Duckham, GIS: A Computing Perspective (2nd ed., CRC, 2004); ISO 19115 Geographic information — Metadata.
Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.
Both estimate values at locations where no measurement exists, but they differ in where those locations lie relative to the sample data. Spatial interpolation estimates values within the area covered by the sample points — inside the convex hull of, and bracketed by, the known observations. Because every predicted location is surrounded by data, interpolation is generally reliable, and methods such as inverse-distance weighting, spline and kriging are designed for this bounded, "fill-in-between" situation. Spatial extrapolation estimates values outside the sampled area or beyond the range of the observations — projecting the modelled trend into a region where there are no surrounding control points. It is inherently far less reliable and carries much larger uncertainty, because the estimate rests on the assumption that the pattern observed inside the data continues unchanged outside it, which frequently fails (a trend fitted over a valley need not hold on the ridge beyond). In practice a GIS should be used to interpolate wherever possible and to extrapolate only with explicit caution: predictions beyond the data envelope should be flagged as low-confidence, and geostatistical methods such as kriging usefully report the rising prediction variance that signals this degradation as one moves outside the sampled region.