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1. To cite the data in any publication as follows:&#xD;
Jones, P. C., &amp; Ferraccioli, F. (2020). Processed line aerogravity data over Northern Palmer Land, Antarctic Peninsula (2002/03 season) (Version 1.0) [Data set]. UK Polar Data Centre, Natural Environment Research Council, UK Research &amp; Innovation. https://doi.org/10.5285/5388DB62-4A5E-4072-9B01-3A65785D80A0&#xD;
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2. The user recognizes the limitations of data. Use of the data is at the users' own risk, and there is no warranty as to the quality or accuracy of any data, or the fitness of the data for your intended use. The data are not necessarily fully quality assured and cannot be expected to be free from measurement uncertainty, systematic biases, or errors of interpretation or analysis, and may include inaccuracies in error margins quoted with the data.</gco:CharacterString>
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SPARC airborne gravity data and details of survey design and data processing are presented in Ferraccioli et al (2006).&#xD;
The dataset available here includes channels from raw through to filtered and upward continued free air anomalies, where data was recoverable. Data processing steps are outlined below&#xD;
&#xD;
Processing steps:&#xD;
1/ Calculate observed gravity. &#xD;
&#xD;
True spring tension (ST_real) is calculated from the posted spring tension (ST) correcting for the fact that for this survey the true spring tension approaches the posted value at 38 mGal per second.&#xD;
Beam velocity (Beam_vel) is derived from raw beam position (RB) assuming a centred difference approximation.&#xD;
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&#xD;
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&#xD;
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&#xD;
2/ Corrections to derive free air anomalies (disturbances).&#xD;
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Eotvos correction (EotvosCor) follows (Harlan, 1968).&#xD;
Latitude correction (LatCor) = 978.03185(1+0.005278895 sin2Lat- 0.000023462 sin4Lat) (IUGG 1967).&#xD;
Free air correction (FaCor) = 0.3086*Height_WGS1984. NOTE subsequent free air values are defined as gravity disturbances in geodesy, as they are referred to the ellipsoid (Hackney and Featherstone, 2003).&#xD;
Horizontal acceleration correction (HaccCor). For this survey the approximation of (Swain, 1996) was used, assuming a damping factor of 0.707, and a platform period of 4 minutes.&#xD;
&#xD;
3/ Free air anomaly and filtering.&#xD;
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&#xD;
Upward continued free air anomaly (Faacont) was produced by upward continuing free air data from the collected flight altitude to 2800 m.&#xD;
&#xD;
Channel description:&#xD;
Basic Channels    &#xD;
   Date UTC date (YYYY/MM/DD)&#xD;
   Time UTC time (HH:MM:SS.SS)&#xD;
   FlightID Sequential flight number and survey ID e.g. W12&#xD;
   Line_name Line Number e.g. LW200.1:12&#xD;
   Lon Longitude WGS 1984, for processing see readme&#xD;
   Lat Latitude WGS 1984, for processing see readme&#xD;
   x x projected meters*&#xD;
   y y projected meters*&#xD;
   Height_WGS1984 Aircraft altitude (meters) in WGS 1984, for processing see location data page&#xD;
     &#xD;
Raw gravity Channels    &#xD;
   ST Spring Tension (meter units)&#xD;
   CC Cross Coupling (meter units)&#xD;
   RB Raw beam position (Mv)&#xD;
   XACC Cross axis accelerometer (Mv)&#xD;
   LACC Long axis accelerometer (Mv)&#xD;
   Still Airborne meter still reading value (mGal)&#xD;
   Base Absolute gravity reference, from land gravity (mGal)&#xD;
     &#xD;
Calculation Channels    &#xD;
  St_real True Spring tension value (meter units)&#xD;
  Beam_vel Gravity meter beam velocity (Mv/sec)&#xD;
   Rec_grav Recalculated relative gravity (mGal)&#xD;
   Abs_grav Calculated absolute gravity (mGal)&#xD;
   VaccCor Vertical acceleration correction&#xD;
   EotvosCor Eotvos correction&#xD;
   LatCor Latitude correction&#xD;
   FaCor Free air correction&#xD;
   HaccCor Horizontal acceleration correction &#xD;
     &#xD;
Free air Channels    &#xD;
  Faa Un-filtered free air anomaly&#xD;
 FAAup Upward continued free air anomaly to altitude 2800 m&#xD;
&#xD;
*Projected coordinates (x and y) are in Polar stereographic defined as follows:&#xD;
Latitude of natural origin:   -71&#xD;
Longitude of natural origin:    0&#xD;
Scale factor at natural origin         -75.33333333333&#xD;
False easting    0&#xD;
False northing    2...(4)</gco:CharacterString>
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