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--- | ||
title: 'Introduction to Geospatial Concepts' | ||
teaching: 10 | ||
exercises: 2 | ||
bibliography: references.bib | ||
zotero: true | ||
--- | ||
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::: questions | ||
- How ... | ||
::: | ||
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::: objectives | ||
- Describe ... | ||
::: | ||
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## The shape of the Earth | ||
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The shape of the Earth is approximately a sphere which is slightly wider than it is tall, and which is called **ellipsoid**. The true shape of the Earth is an irregular ellipsoid, the so-called **geoid** (@fig-earth). | ||
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![The shape of the Earth. Source: United Nations Statistics Division and International Cartographic Association (2012a)](https://unstats.un.org/unsd/geoinfo/ungegn/docs/_data_icacourses/_ImagesModules/_selfstudy/S06_images/S06_03_a00.jpg){#fig-earth} | ||
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The most common and basic representation of the position of points on the Earth is the combination of the **geographical latitude and longitude**. | ||
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![Geographical latitude and longitude. Source: van der Marel (2014).](fig/latlon.png) | ||
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**Meridians** are **vertical** circles with constant longitude, called **great circles**, which run from the North Pole to the South Pole. **Parallels** are **horizontal** circles with constant latitude, which are called **small circles**. Only the equator (the largest parallel) is also a great circle. | ||
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The black lines in @fig-latlon show the equator and the prime meridian running through Greenwich, with latitude and longitude labels. The red dotted lines show the meridian and parallel running through Karachi, Pakistan (25°45’N, 67°01’E). | ||
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## Map projection | ||
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**Map projection** is a systematic transformation of the latitudes and longitudes of locations on the surface of an ellipsoid into locations on a plane. It is a transformation of the three-dimensional Earth’s surface into its two-dimensional representation on a sheet of paper or computer screen (see @fig-projection for a comparison with flattening of an orange peel). | ||
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![Map projection represented as flattening an orange peel. Source: Data Carpentry (2023)](https://datacarpentry.org/organization-geospatial/fig/orange-peel-earth.jpg){#fig-projection} | ||
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Many different map projections are in use for different purposes. Generally, they can be categorised into the following groups: cylindrical, conic, and azimuthal (see @fig-projections). | ||
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![Cylindrical, conic, and azimuthal map projections. Source: Knippers (2009)](https://kartoweb.itc.nl/geometrics/Bitmaps/Intro%201.9a.gif){#fig-projections} | ||
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Each map projection introduces a **distortion** in geometrical elements – **distance**, **angle**, and **area**. Depending on which of these geometrical elements are more relevant for a specific map, we can choose an appropriate map projection. **Conformal projections** are the best for preserving angles between any two curves; **equal area (equivalent) projections** preserve the area or scale; **equal distance (conventional) projections** are the best for preserving distances. | ||
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## Coordinate reference systems (CRS) | ||
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A **coordinate reference system (CRS)** is a coordinate-based local, regional or global system for locating geographical entities, which uses a specific map projection. It defines how the two-dimensional, projected map relates to real places on the Earth. | ||
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All coordinate reference systems are included in a public registry called the **EPSG Geodetic Parameter Dataset (EPSG registry)**, initiated in 1985 by a member of the European Petroleum Survey Group (EPSG). Each CRS has a unique **EPSG code**, which makes it possible to easily identify them among the large number of CRS. This is particularly important for transforming spatial data from one CRS to another. | ||
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Some of the most commonly used CRS in the Netherlands are the following: | ||
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- **World Geodetic System 1984 (WGS84)** is the best known global reference system (EPSG:4326). | ||
- **European Terrestrial Reference System 1989 (ETRS89)** is the standard coordinate system for Europe (EPSG:4258). | ||
- The most popular projected CRS in the Netherlands is ‘Stelsel van de Rijksdriehoeksmeting (RD)’ registered in EPSG as **Amersfoort / RD New (EPSG:28992)**. | ||
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The main parameters of each CRS are the following: | ||
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- **Datum** is a model of the shape of the Earth, which specifies how a coordinate system is linked to the Earth, e.g. how to define the origin of the coordinate axis – where (0,0) is. It has angular units (degrees). | ||
- **Projection** is mathematical transformation of the angular measurements on the Earth to linear units (e.g. meters) on a flat surface (paper or a computer screen). | ||
- **Additional parameters**, such as a definition of the centre of the map, are often necessary to create the full CRS. | ||
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In this workshop, we use two CRS shown in @tbl-crs. | ||
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| | WGS 84 (EPSG:4326) | Amersfoort / RD New (EPSG:28992) | | ||
|-----------------|----------------------------|----------------------------| | ||
| Units | degrees | meters | | ||
| Projection | Geographic (uses latitude and longitude for coordinates) | | | ||
| | Dynamic (relies on a datum which is not plate-fixed) | Static (relies on a datum which is plate-fixed) | | ||
| Celestial body | Earth | | | ||
| Datum | World Geodetic System 1984 ensemble | Amersfoort | | ||
| Method | Lat/long (Geodetic alias) | Oblique Stereographic Alternative | | ||
| Prime meridian | Greenwich | | | ||
| Ellipsoid | | Bessel 1841 | | ||
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: Main properties of WGS 84 and Amersfoort / RD New coordinate reference systems {#tbl-crs} | ||
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## Map scale | ||
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**Map scale** measures the ratio between distance on a map and the corresponding distance on the ground. For example, on a 1:100 000 scale map, 1cm on the map equals 1km (100 000 cm) on the ground. Map scale can be expressed in the following three ways: | ||
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- Verbal: 1 centimetre represents 250 meters | ||
- Fraction: 1:25000 | ||
- Graphic: | ||
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::: callout | ||
# Useful resources | ||
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- Campbell, J., Shin, M. E. (2011). Essentials of Geographic Information Systems. Textbooks. 2. <https://digitalcommons.liberty.edu/textbooks/2> (Accessed 22-01-2024) | ||
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- Data Carpentry (2023): Introduction to Geospatial Concepts. Coordinate Reference Systems. <https://datacarpentry.org/organization-geospatial/03-crs.html> (Accessed 22-01-2024) | ||
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- GeoRepository (2024): EPSG Geodetic Parameter Dataset <https://epsg.org/home.html> (Accessed 22-01-2024) | ||
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- Klokan Technologies GmbH (2022) <https://epsg.io/> (Accessed 22-01-2024) | ||
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- United Nations Statistics Division and International Cartographic Association (2012b): UNGEGN-ICA webcourse on Toponymy. <https://unstats.un.org/unsd/geoinfo/ungegn/docs/_data_icacourses/2012_Home.html> (Accessed 22-01-2024) | ||
::: | ||
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::: keypoints | ||
- Use `.md` files for episodes when you want static content | ||
- Use `.Rmd` files for episodes when you need to generate output | ||
- Run `sandpaper::check_lesson()` to identify any issues with your lesson | ||
- Run `sandpaper::build_lesson()` to preview your lesson locally | ||
::: |
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@article{vandermarel2014, | ||
title = {Reference Systems for Surveying and Mapping. Lecture Notes}, | ||
author = {van der Marel, Hans}, | ||
year = {2014}, | ||
date = {2014}, | ||
langid = {en} | ||
} |
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{ | ||
"R": { | ||
"Version": "4.3.0", | ||
"Repositories": [ | ||
{ | ||
"Name": "CRAN", | ||
"URL": "https://cran.rstudio.com" | ||
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] | ||
}, | ||
"Packages": { | ||
"renv": { | ||
"Package": "renv", | ||
"Version": "1.0.3", | ||
"OS_type": null, | ||
"Repository": "CRAN", | ||
"Source": "Repository" | ||
} | ||
} | ||
} |
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library/ | ||
local/ | ||
cellar/ | ||
lock/ | ||
python/ | ||
sandbox/ | ||
staging/ |
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