Coordinate variable data and header information for model SGLOBE-rani-true-xi.nc

netcdf SGLOBE-rani-true-xi {
dimensions:
	depth = 37 ;
	latitude = 89 ;
	longitude = 180 ;
variables:
	float depth(depth) ;
		depth:long_name = "depth below earth surface" ;
		depth:units = "kilometer " ;
		depth:positive = "down " ;
	float latitude(latitude) ;
		latitude:long_name = "Latitude; positive north" ;
		latitude:units = "degrees_north" ;
		latitude:standard_name = "latitude" ;
	float longitude(longitude) ;
		longitude:long_name = "Longitude; positive east" ;
		longitude:units = "degrees_east" ;
		longitude:standard_name = "longitude" ;
	float xi(depth, latitude, longitude) ;
		xi:long_name = "Radial anisotropy in (SH/SV)^2" ;
		xi:units = "dimensionless" ;
		xi:valid_range = -1000.f, 1000.f ;
		xi:missing_value = 99999.f ;
		xi:_FillValue = 99999.f ;

// global attributes:
		:title = "SGLOBE-rani" ;
		:id = "SGLOBE-rani" ;
		:summary = "SGLOBE-rani is a global radially anisotropic shear wave speed model \n",
			" with radial anisotropy allowed in the whole mantle. It is based on a seismic data set of over 43M seismic surface wave (fundamental \n",
			" and overtones) and body wave measurements. It models simultaneously crustal thickness and mantle structure, and its reference model is PREM. \n",
			" NOTE: Kustowski et al., 2008 and Chang et al., 2014 showed that the anisotropic structure in the lowermost mantle retrieved from global \n",
			" tomographic inversions can be strongly affected by leakage effects, so we discourage interpreting SGLOBE-rani\'s anisotropic structure below ~1500 km depth.\n",
			" " ;
		:keywords = "radial anisotropy, anisotropy, shear wave, s wave, velocity" ;
		:Metadata_Conventions = "Unidata Dataset Discovery v1.0" ;
		:creator_name = "Sung-Joon Chang and Ana M.G. Ferreira" ;
		:creator_url = "http://seismo.kangwon.ac.kr/downloads.htm" ;
		:creator_email = "sjchang@kangwon.ac.kr, a.ferreira@ucl.ac.uk" ;
		:institution = "Kangwon National University and University College London" ;
		:acknowledgment = "This research was initially supported by the Leverhulme Trust (project F/00 204/AS), \n",
			" followed by support by NERC project NE/K005669/1 and by the Korea Meteorological Administration Research and \n",
			" Development Program under grant CATER-2014-8030. This study was also supported by 2013 Research Grant from \n",
			" Kangwon National University. It was carried out initially on the High Performance Computing Cluster supported \n",
			" by the Research and Specialist Computing Support services at the University of East Anglia followed by the national \n",
			" UK supercomputing facilities HECToR and Archer. A.M.G.F. also thanks funding by the European Commission\'s Initial \n",
			" Training Network project QUEST (contract FP7- PEOPLEITN-2008-238007; www.quest-itn.org).\n",
			"" ;
		:references = " Chang, S.-J., A.M.G. Ferreira, J. Ritsema, H.J. van Heijst, and J.H. Woodhouse (2015), Joint inversion for global isotropic and radially anisotropic mantle structure including crustal thickness perturbations, Journal of Geophysical Research, 120, 4278-4300, doi:10.1002/2014JB011824.\n",
			"" ;
		:history = "ver 1.1" ;
		:comment = "model converted to netCDF by Sung-Joon Chang\n",
			"2017-10-09 IRIS DMC: removed xi:add_offset = \"0.f\" and xi:scale_factor = \"1.f\" to \n",
			" avoid errors when reading with MATLAB \n",
			"2018-10-22 changed valid_range from string to array of numbers" ;
		:geospatial_lat_min = -88. ;
		:geospatial_lat_max = 88. ;
		:geospatial_lat_units = "degrees_north" ;
		:geospatial_lat_resolution = 2. ;
		:geospatial_lon_min = 0. ;
		:geospatial_lon_max = 358. ;
		:geospatial_lon_units = "degrees_east" ;
		:geospatial_lon_resolution = 2. ;
		:geospatial_vertical_min = 25 ;
		:geospatial_vertical_max = 2800 ;
		:geospatial_vertical_units = "kilometer" ;
		:geospatial_vertical_resolution = 100 ;
		:geospatial_vertical_positive = "down" ;
		:time_coverage_start = "start" ;
		:time_coverage_end = "present" ;
data:

 depth = 25, 50, 100, 150, 200, 250, 300, 350, 400, 450, 500, 550, 600, 650, 
    700, 750, 800, 900, 1000, 1100, 1200, 1300, 1400, 1500, 1600, 1700, 1800, 
    1900, 2000, 2100, 2200, 2300, 2400, 2500, 2600, 2700, 2800 ;

 latitude = -88, -86, -84, -82, -80, -78, -76, -74, -72, -70, -68, -66, -64, 
    -62, -60, -58, -56, -54, -52, -50, -48, -46, -44, -42, -40, -38, -36, 
    -34, -32, -30, -28, -26, -24, -22, -20, -18, -16, -14, -12, -10, -8, -6, 
    -4, -2, 0, 2, 4, 6, 8, 10, 12, 14, 16, 18, 20, 22, 24, 26, 28, 30, 32, 
    34, 36, 38, 40, 42, 44, 46, 48, 50, 52, 54, 56, 58, 60, 62, 64, 66, 68, 
    70, 72, 74, 76, 78, 80, 82, 84, 86, 88 ;

 longitude = 0, 2, 4, 6, 8, 10, 12, 14, 16, 18, 20, 22, 24, 26, 28, 30, 32, 
    34, 36, 38, 40, 42, 44, 46, 48, 50, 52, 54, 56, 58, 60, 62, 64, 66, 68, 
    70, 72, 74, 76, 78, 80, 82, 84, 86, 88, 90, 92, 94, 96, 98, 100, 102, 
    104, 106, 108, 110, 112, 114, 116, 118, 120, 122, 124, 126, 128, 130, 
    132, 134, 136, 138, 140, 142, 144, 146, 148, 150, 152, 154, 156, 158, 
    160, 162, 164, 166, 168, 170, 172, 174, 176, 178, 180, 182, 184, 186, 
    188, 190, 192, 194, 196, 198, 200, 202, 204, 206, 208, 210, 212, 214, 
    216, 218, 220, 222, 224, 226, 228, 230, 232, 234, 236, 238, 240, 242, 
    244, 246, 248, 250, 252, 254, 256, 258, 260, 262, 264, 266, 268, 270, 
    272, 274, 276, 278, 280, 282, 284, 286, 288, 290, 292, 294, 296, 298, 
    300, 302, 304, 306, 308, 310, 312, 314, 316, 318, 320, 322, 324, 326, 
    328, 330, 332, 334, 336, 338, 340, 342, 344, 346, 348, 350, 352, 354, 
    356, 358 ;
}