Update information and changelog. (#143)

Esteban82 · web-flow · commit d7069bae3c91 · 2026-01-22T15:37:37.000-03:00
diff --git a/docs/changes.rst b/docs/changes.rst
@@ -1,6 +1,15 @@
 Changelog
 ---------
 
+2026-01-22
+^^^^^^^^^^
+
+- ``earth_faa``: Update dataset source from version 32 to 33.
+- ``earth_faaerror``: Update dataset source from version 32 to 33.
+- ``earth_edfl``: Update dataset source from version 32 to 33.
+- ``earth_ndfl``: Update dataset source from version 32 to 33.
+- ``earth_vgg``: Update dataset source from version 32 to 33.
+
 2025-08-13
 ^^^^^^^^^^
 
diff --git a/docs/earth-edefl.rst b/docs/earth-edefl.rst
@@ -12,7 +12,7 @@ Both geodynamic and geophysical studies have an interest in the study of the Ear
 gravity field and are often used in conjunctions with bathymetric or topographic relief
 to assess the degree of isostasy.
 `David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html>`_
-have provided altimetry-based marine FAA and similar grids since 1995. The latest version 32 is now
+have provided altimetry-based marine FAA and similar grids since 1995. The latest version 33 is now
 available for remote use in GMT. Over land these grids are filled in by the EGM2008 model
 [Pavlis et al., 2012]. This dataset contains the east-west deflection of the vertical
 in micro-radians. Polar regions beyond ±80˚ are not covered and are set to NaN.
diff --git a/docs/earth-faa.rst b/docs/earth-faa.rst
@@ -12,7 +12,7 @@ Both geodynamic and geophysical studies have an interest in the study of the Ear
 gravity field and are often used in conjunctions with bathymetric or topographic relief
 to assess the degree of isostasy.
 `David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html>`_
-have provided altimetry-based marine FAA and similar grids since 1995. The latest version 32 is now
+have provided altimetry-based marine FAA and similar grids since 1995. The latest version 33 is now
 available for remote use in GMT. Over land these grids are filled in by the EGM2008 model [Pavlis et al., 2012].
 Polar regions beyond ±80˚ are not covered and are set to NaN.
 
diff --git a/docs/earth-faaerror.rst b/docs/earth-faaerror.rst
@@ -9,7 +9,7 @@ IGPP Earth Free-Air Anomaly Uncertainty
    :align: center
 
 `David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html>`_
-have provided altimetry-based marine FAA and similar grids since 1995. The latest version 32 is now
+have provided altimetry-based marine FAA and similar grids since 1995. The latest version 33 is now
 available for remote use in GMT. Over land these grids are filled in by the EGM2008 model [Pavlis et al., 2012].
 Polar regions beyond ±80˚ are not covered and are set to NaN.
 This data is a companion to the FAA anomalies but contains the uncertainty of each
diff --git a/docs/earth-ndefl.rst b/docs/earth-ndefl.rst
@@ -12,7 +12,7 @@ Both geodynamic and geophysical studies have an interest in the study of the Ear
 gravity field and are often used in conjunctions with bathymetric or topographic relief
 to assess the degree of isostasy.
 `David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html>`_
-have provided altimetry-based marine FAA and similar grids since 1995. The latest version 32 is now
+have provided altimetry-based marine FAA and similar grids since 1995. The latest version 33 is now
 available for remote use in GMT. Over land these grids are filled in by the EGM2008 model
 [Pavlis et al., 2012]. This dataset contains the north-south deflection of the vertical
 in micro-radians. Polar regions beyond ±80˚ are not covered and are set to NaN.
diff --git a/docs/earth-vgg.rst b/docs/earth-vgg.rst
@@ -11,7 +11,7 @@ IGPP Earth Vertical Gravity Gradient
 Marine geophysicists and in particular researchers of plate tectonics have an interest in derivatives of the Earth's
 gravity field as such anomalies may highlight smaller-scale features, such as seafloor tectonic scars and seamounts.
 `David Sandwell and colleagues <https://topex.ucsd.edu/marine_grav/mar_grav.html>`_
-have provided altimetry-based marine vertical gravity gradients (VGG) and similar grids since 1995. The latest version 32 is now
+have provided altimetry-based marine vertical gravity gradients (VGG) and similar grids since 1995. The latest version 33 is now
 available for remote use in GMT. Over land, these grids are filled in by predictions of the EGM2008 model [Pavlis et al., 2012].
 Polar regions beyond ±80˚ are not covered and are set to NaN.
 
