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lines changed Original file line number Diff line number Diff line change 1- IGPP Earth East-West Deflections
2- --------------------------------
1+ IGPP Earth East-West Deflection
2+ -------------------------------
33.. figure :: /_static/igpp.png
44 :align: right
55 :scale: 20 %
@@ -14,7 +14,7 @@ to assess the degree of isostasy.
1414`David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html >`_
1515have provided altimetry-based marine FAA and similar grids since 1995. The latest version 32 is now
1616available for remote use in GMT. Over land these grids are filled in by the EGM2008 model
17- [Pavlis et al., 2012]. This data set contains the east-west deflections of the vertical
17+ [Pavlis et al., 2012]. This dataset contains the east-west deflection of the vertical
1818in micro-radians. Polar regions beyond ±80˚ are not covered and are set to NaN.
1919
2020Usage
@@ -60,7 +60,8 @@ We scale and reformat the original data to take up very little space so that dow
6060from the servers are as fast as possible. For the EDEFL grid this means
6161we chose 1/32 micro-radians as the smallest data unit, which is well below the uncertainties in the
6262model. Data are scaled and shifted to fit in a short integer grid that is highly compressed
63- by netCDF lossless compression and chunking. The data are reported in micro-radians.
63+ by netCDF lossless compression and chunking. The data are reported in micro-radians, where
64+ positive (negative) values indicate a deflection to the east (west).
6465
6566Data References
6667~~~~~~~~~~~~~~~
Original file line number Diff line number Diff line change 1- IGPP Earth South- North Deflections
2- ----------------------------------
1+ IGPP Earth North-South Deflection
2+ ---------------------------------
33.. figure :: /_static/igpp.png
44 :align: right
55 :scale: 20 %
@@ -14,7 +14,7 @@ to assess the degree of isostasy.
1414`David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html >`_
1515have provided altimetry-based marine FAA and similar grids since 1995. The latest version 32 is now
1616available for remote use in GMT. Over land these grids are filled in by the EGM2008 model
17- [Pavlis et al., 2012]. This data set contains the south- north deflections of the vertical
17+ [Pavlis et al., 2012]. This dataset contains the north-south deflection of the vertical
1818in micro-radians. Polar regions beyond ±80˚ are not covered and are set to NaN.
1919
2020Usage
@@ -60,7 +60,8 @@ We scale and reformat the original data to take up very little space so that dow
6060from the servers are as fast as possible. For the NDEFL grid this means
6161we chose 1/32 micro-radians as the smallest data unit, which is well below the uncertainties in the
6262model. Data are scaled and shifted to fit in a short integer grid that is highly compressed
63- by netCDF lossless compression and chunking. The data are reported in micro-radians.
63+ by netCDF lossless compression and chunking. The data are reported in micro-radians, where
64+ positive (negative) values indicate a deflection to the north (south).
6465
6566Data References
6667~~~~~~~~~~~~~~~
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