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&#xD;
We present here the processed line aeromagnetic data acquired using scintrex cesium magnetometers mounted on the BAS aerogeophysical equiped Twin Otter. &#xD;
Data are provided as XYZ ASCII line data.</gco:CharacterString>
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Jordan, T., &amp; Ferraccioli, F. (2020). Processed high resolution line aeromagnetic data over Pine Island Glacier Ice Shelf (2010-2011) (Version 1.0) [Data set]. UK Polar Data Centre, Natural Environment Research Council, UK Research &amp; Innovation. https://doi.org/10.5285/84B382C3-6B6F-4524-9807-EC7941E5620D&#xD;
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Also included in the database is a subset of lines from the BBAS survey of the catchment of Pine Island glacier. This subset includes three flow-parallel tie lines and shorter line segments roughly transverse to flow. These lines have been levelled to the high resolution grid of the PIG mouth survey, but not included in microlevelling given their contrasting orientation. &#xD;
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MagR- Raw magnetic total field intensity data (nT). &#xD;
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TCorr- Tiptank corrections (nT). These include DC shifts and gradients due to aircraft noice, etc. Dummy values if not applicable. &#xD;
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SCorr- Any DC shift applied. A +12 nT shift has been applied to P lines in the database to adjust their level to that of the rest of the survey.&#xD;
MagF- Final mag value before levelling. MagF= MagRTC- SCorr- ACorr&#xD;
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&#xD;
Basic channel description:&#xD;
  Line name Line Number &#xD;
  Flight ID Sequential flight number&#xD;
   x x projected meters*&#xD;
   y y projected meters*&#xD;
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   Lat Latitude WGS 1984, &#xD;
   Height_WGS1984 Aircraft altitude (meters) in WGS 1984, &#xD;
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&#xD;
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Latitude of natural origin:   -71&#xD;
Longitude of natural origin:    0&#xD;
Scale factor at natural origin:                     0.994&#xD;
False easting    0&#xD;
False northing    2072760.109&#xD;
&#xD;
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Aeromagnetic data acquired as part of BBAS project in 2004 was used for levelling. See related dataset:  	https://doi.org/10.5285/485e6b9b-d033-441f-8c98-b2d0efcb1d63
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