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Albers Conic Equal Area
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=======================
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+ This projection, developed by Heinrich C. Albers in 1805, is predominantly used to map
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+ regions of large east-west extent, in particular the United States. It is a conic,
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+ equal-area projection, in which parallels are unequally spaced arcs of concentric
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+ circles, more closely spaced at the north and south edges of the map. Meridians, on the
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+ other hand, are equally spaced radii about a common center, and cut the parallels at
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+ right angles. Distortion in scale and shape vanishes along the two standard parallels.
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+ Between them, the scale along parallels is too small; beyond them it is too large.
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+ The opposite is true for the scale along meridians.
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+
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``Blon0/lat0/lat1/lat2/width``: Give projection center ``lon0/lat0`` and two standard
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parallels ``lat1/lat2``.
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"""
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Equidistant conic
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=================
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+ The equidistant conic projection was described by the Greek philosopher Claudius
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+ Ptolemy about A.D. 150. It is neither conformal or equal-area, but serves as a
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+ compromise between them. The scale is true along all meridians and the
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+ standard parallels.
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+
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``Dlon0/lat0/lat1/lat2/width``: Give projection center ``lon0/lat0``, two standard
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parallels ``lat1/lat2``, and the map width.
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"""
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Lambert Conic Conformal Projection
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==================================
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+ This conic projection was designed by the Alsatian mathematician Johann Heinrich
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+ Lambert (1772) and has been used extensively for mapping of regions with predominantly
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+ east-west orientation, just like the Albers projection. Unlike the Albers projection,
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+ Lambert’s conformal projection is not equal-area. The parallels are arcs of circles
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+ with a common origin, and meridians are the equally spaced radii of these circles. As
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+ with Albers projection, it is only the two standard parallels that are distortion-free.
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+
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``Llon0/lat0/lat1/lat2/width``: Give projection center ``lon0/lat0``, two standard
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parallels ``lat1/lat2``, and the map width.
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"""
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Polyconic Projection
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====================
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+ The polyconic projection, in Europe usually referred to as the American polyconic
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+ projection, was introduced shortly before 1820 by the Swiss-American cartographer
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+ Ferdinand Rodulph Hassler (1770–1843). As head of the Survey of the Coast, he was
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+ looking for a projection that would give the least distortion for mapping the coast of
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+ the United States. The projection acquired its name from the construction of each
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+ parallel, which is achieved by projecting the parallel onto the cone while it is rolled
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+ around the globe, along the central meridian, tangent to that parallel. As a
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+ consequence, the projection involves many cones rather than a single one used in
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+ regular conic projections.
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+
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+ The polyconic projection is neither equal-area, nor conformal. It is true to scale
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+ without distortion along the central meridian. Each parallel is true to scale as well,
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+ but the meridians are not as they get further away from the central meridian. As a
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+ consequence, no parallel is standard because conformity is lost with the lengthening of
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+ the meridians.
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+
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``Poly/width``: The only additional argument for the projection is the map width.
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"""
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import pygmt
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