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data/argo_glors_ostia_ssh.zarr/sealevel_err_ugosa/.zarray

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+{
+  "shape": [
+    6637381
+  ],
+  "chunks": [
+    2048
+  ],
+  "dtype": "<f4",
+  "fill_value": "NaN",
+  "order": "C",
+  "filters": null,
+  "dimension_separator": ".",
+  "compressor": {
+    "id": "blosc",
+    "cname": "lz4",
+    "clevel": 5,
+    "shuffle": 1,
+    "blocksize": 0
+  },
+  "zarr_format": 2
+}

data/argo_glors_ostia_ssh.zarr/sealevel_err_ugosa/.zattrs

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+{
+  "long_name": "sealevel err_ugosa collocated at profile point",
+  "description": "err_ugosa from SEALEVEL_GLO_PHY_L4_MY_008_047, sampled at the EN4 profile latitude, longitude, and JULD.",
+  "source_product": "SEALEVEL_GLO_PHY_L4_MY_008_047",
+  "source_variable": "err_ugosa",
+  "collocation": "linear spatial interpolation and nearest temporal sample",
+  "units": "m/s",
+  "source_attrs": {
+    "comment": "The formal mapping error represents a purely theoretical mapping error. It mainly traduces errors induced by the constellation sampling capability and consistency with the spatial/temporal scales considered, as described in Le Traon et al (1998) or Ducet et al (2000)",
+    "grid_mapping": "crs",
+    "long_name": "Formal mapping error on zonal geostrophic velocity anomalies",
+    "standard_name": "surface_geostrophic_eastward_sea_water_velocity_assuming_sea_level_for_geoid standard_error",
+    "units": "m/s"
+  },
+  "_ARRAY_DIMENSIONS": [
+    "profile"
+  ]
+}