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Copy file name to clipboardExpand all lines: CHANGELOG.md
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For non-gridded or sparse data, the raster and contour marks implement a variety of spatial interpolation methods to populate the raster grid. The *barycentric* interpolation method, shown below with data from the [Great Britain aeromagnetic survey](https://www.bgs.ac.uk/datasets/gb-aeromagnetic-survey/), uses barycentric coordinates from a Delaunay triangulation of the samples (small black dots).
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For non-gridded or sparse data, the raster and contour marks implement a variety of [spatial interpolation methods](./README.md#spatial-interpolation) to populate the raster grid. The *barycentric* interpolation method, shown below with data from the [Great Britain aeromagnetic survey](https://www.bgs.ac.uk/datasets/gb-aeromagnetic-survey/), uses barycentric coordinates from a Delaunay triangulation of the samples (small black dots).
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[<imgsrc="./img/ca55.webp"width="650"alt="A map showing the varying intensity of the magnetic field as periodically observed from an airplane flying in an approximate grid pattern">](https://observablehq.com/@observablehq/plot-raster)
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TK, alternate visualization as contours.
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The same data, as filled contours in projected coordinates:
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Naturally, the raster and contour mark work with Plot’s [projection system](./README.md#projection-options), allowing spatial samples to be shown in any geographic projections and in conjunction with other geographic data. The *equirectangular* projection is the natural choice for this gridded water vapor data from [NASA Earth Observations](https://neo.gsfc.nasa.gov/view.php?datasetId=MYDAL2_M_SKY_WV&date=2022-11-01).
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[<imgsrc="./img/ca55-contours.webp"width="650"alt="A map showing the varying intensity of the magnetic field as periodically observed from an airplane flying in an approximate grid pattern">](https://observablehq.com/@observablehq/plot-raster)
Naturally, the raster and contour mark support Plot’s [projection system](./README.md#projection-options), allowing spatial samples to be shown in any geographic projection and in conjunction with other geographic data. The *equirectangular* projection is the natural choice for this gridded global water vapor dataset from [NASA Earth Observations](https://neo.gsfc.nasa.gov/view.php?datasetId=MYDAL2_M_SKY_WV&date=2022-11-01).
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[<imgsrc="./img/water-vapor.png"width="650"alt="A map of global atmospheric water vapor, showing a higher concentration of water vapor near the equator">](https://observablehq.com/@observablehq/plot-raster)
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