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	<title>DGGS/Proj/pt/DT - Revision history</title>
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		<title>Admin: Sync V45 (Force Parity)</title>
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		<updated>2026-01-25T11:55:09Z</updated>

		<summary type="html">&lt;p&gt;Sync V45 (Force Parity)&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Disdyakis_30.png|thumb]]&lt;br /&gt;
Projection onto a 120-sided polyhedron [[wikipedia:Disdyakis triacontahedron|&amp;#039;&amp;#039;&amp;#039;D&amp;#039;&amp;#039;&amp;#039;isdyakis &amp;#039;&amp;#039;&amp;#039;T&amp;#039;&amp;#039;&amp;#039;riacontahedron]] (is a Catalan solid with 120 identical triangular faces), proposed in 2020 by https://www.mdpi.com/2220-9964/9/5/315&lt;br /&gt;
&lt;br /&gt;
Below is the 120-faced polyhedron:&lt;br /&gt;
&lt;br /&gt;
[[file:Disdyakis_30_net.svg|center|580px]]&lt;br /&gt;
&lt;br /&gt;
Each of the 120 faces corresponds to a projection plane of the &amp;quot;Slice and Dice projection&amp;quot; type (van Leeuwen and Strebe).&lt;br /&gt;
&lt;br /&gt;
== Slice and Dice projection ==&lt;br /&gt;
The van Leeuwen and Strebe projection, originally oriented towards equilateral triangles, was optimized for &amp;#039;&amp;#039;&amp;#039;less angular distortion in isosceles triangles&amp;#039;&amp;#039;&amp;#039; in the same year, https://www.arxiv.org/pdf/2008.13670v1 but published only in 2021, https://doi.org/10.1145/3460521&lt;br /&gt;
&lt;br /&gt;
The DT projection uses isosceles triangles, so optimization is pending analysis.&lt;br /&gt;
&lt;br /&gt;
Besides the [https://doi.org/10.1559/152304006779500687 original closed], and some description in the cited articles, the equal-area &amp;quot;Slice and Dice&amp;quot; projection (van Leeuwen and Strebe) is described in https://www.researchgate.net/publication/250016113_A_Slice-and-Dice_Approach_to_Area_Equivalence_in_Polyhedral_Map_Projections (where we can request from the author).&lt;br /&gt;
&lt;br /&gt;
== Modeling the rhombic triacontahedron ==&lt;br /&gt;
The assembly of 4 by 4 faces results in a [[wikipedia:Rhombic triacontahedron|Rhombic triacontahedron]] with 120/4=30 quadrilateral faces, used as L0 of a [[Generalized Geohash/pt|GGeohash]].&lt;br /&gt;
&lt;br /&gt;
[[File:RhombicTriacontahedron-30facesFrom120.png|340px]] [[File:Rhombictriacontahedron_net.svg|340px]]&lt;br /&gt;
&lt;br /&gt;
On the faces of the [[wikipedia:Rhombic triacontahedron]], the smaller angle of the rhombus is 63.43°, closer to 90° than the rhombus of the [[DGGS/Proj/ISEA]] projection, therefore superior (with capacity) also in the cell shape.&lt;br /&gt;
&lt;br /&gt;
Recent works by Liang et al. 2022 re-equated the [[DGGS/Proj/Planos concorrentes|construction]] of the quadrilaterals of the projection, https://doi.org/10.1080/17538947.2022.2130459&lt;br /&gt;
[[File:Tjde a 2130459 f0007 ob.png|center|thumb|680px|Same &amp;#039;&amp;#039;Rhombic triacontahedron&amp;#039;&amp;#039; in alternative construction.]]&lt;br /&gt;
[[File:Fig3-dingEtAll2024.png|center|semmoldura|680x680px]]&lt;br /&gt;
&lt;br /&gt;
== Local country adjustment ==&lt;br /&gt;
[[File:ProjDT-BR-dobras1.png|thumb|380px|Example of possible altitude adjustment over Brazil.]]&lt;br /&gt;
&lt;br /&gt;
Still under study if truly viable... Complementary strategies, using [[DGGS/Proj/Planos_concorrentes#Proposta_da_re-proje%C3%A7%C3%A3o_linear_em_planos_concorrentes|Proposal of linear re-projection (hinges)]], for adjustment to the country&amp;#039;s terrain, or at least its median altitude. The strategy may utilize:&lt;br /&gt;
&lt;br /&gt;
* Change of ellipsoid radius, so that the geoid better tangents the median altitude. Not well-regarded due to causing undesirable side effects in positioning.&lt;br /&gt;
&lt;br /&gt;
* Change in the choice of the &amp;quot;secant plane to the ellipsoid&amp;quot;. This allows some compatibility between the two, DGGS and [[DNGS]], as they use the same polygons in the projection (solid angles are preserved).&lt;br /&gt;
&lt;br /&gt;
In the use of DT for each DNGS (each country), the choice of quadrilaterals no longer has a greater commitment to the &amp;#039;&amp;#039;rhombic triacontahedron&amp;#039;&amp;#039;, it is free. The commitment returns to m&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt; as a reference.&lt;br /&gt;
The &amp;quot;compatibility&amp;quot; between DNGS and DGGS (based on DT projection) would only be in the use of the reference projection and simplicity in the conversion algorithms between grids.&lt;br /&gt;
&lt;br /&gt;
== ISEA Conversion ==&lt;br /&gt;
H3 Uber and several other implementations of the DGGS standard made use of the ISEA projection, which seemed the most suitable until the 2020s. According to [https://doi.org/10.1080/17538947.2024.2324952 Huang et al. 2024], in &amp;#039;&amp;#039;&amp;quot;Bidirectional mapping between rhombic triacontahedron and icosahedral hexagonal discrete global grid systems&amp;quot;&amp;#039;&amp;#039;,&lt;br /&gt;
&lt;br /&gt;
: The icosahedron is currently the mainstream polyhedron in research and application of discrete global grid systems (DGGS). However, compared to the rhombic triacontahedron (RT), the icosahedron has disadvantages, such as lower sphere-fitting accuracy, greater projection distortion, and difficulty in incorporating the matrix structure for geospatial data storage.&lt;br /&gt;
&lt;br /&gt;
The article demonstrates efficient techniques for converting the &amp;quot;legacy ISEA&amp;quot; in the DT projection.&lt;br /&gt;
&lt;br /&gt;
The illustration below shows how the rhombus can serve as a reference for 3 types of tiles:&lt;br /&gt;
[[File:Tjde a 2130459 f0004 oc.png|center|thumb|620x620px]]&lt;br /&gt;
&lt;br /&gt;
PS: see also article https://doi.org/10.3390/ijgi11120595&lt;br /&gt;
&lt;br /&gt;
== See also ==&lt;br /&gt;
&lt;br /&gt;
* [[DGGS/Proj/ISEA]]&lt;br /&gt;
* Usage in https://www.mdpi.com/2220-9964/11/6/322 for distance transform Canada&lt;br /&gt;
[[Category:Public]]&lt;/div&gt;</summary>
		<author><name>Admin</name></author>
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