function z = gsw_z_from_p(p,lat,geo_strf_dyn_height,sea_surface_geopotental)

% gsw_z_from_p                                         height from pressure
%==========================================================================
%
% USAGE:  
%  z = gsw_z_from_p(p,lat,{geo_strf_dyn_height},{sea_surface_geopotental})
%
% DESCRIPTION:
%  Calculates height from sea pressure using the computationally-efficient
%  75-term expression for specific volume in terms of SA, CT and p 
%  (Roquet et al., 2015).  Dynamic height anomaly, geo_strf_dyn_height, if
%  provided, must be computed with its p_ref = 0 (the surface).  Also if
%  provided, sea_surface_geopotental is the geopotential at zero sea 
%  pressure. This function solves Eqn.(3.32.3) of IOC et al. (2010).  
%
%  Note. Height z is NEGATIVE in the ocean. i.e. Depth is -z.  
%   Depth is not used in the GSW computer software library.  
%
%  Note that this 75-term equation has been fitted in a restricted range of 
%  parameter space, and is most accurate inside the "oceanographic funnel" 
%  described in McDougall et al. (2003).  The GSW library function 
%  "gsw_infunnel(SA,CT,p)" is avaialble to be used if one wants to test if 
%  some of one's data lies outside this "funnel".  
%
% INPUT:
%  p    =  sea pressure                                            [ dbar ]
%          ( i.e. absolute pressure - 10.1325 dbar )
%  lat  =  latitude in decimal degrees north                [ -90 ... +90 ]
%
% OPTIONAL:
%  geo_strf_dyn_height = dynamic height anomaly                 [ m^2/s^2 ]
%    Note that the refernce pressure, p_ref, of geo_strf_dyn_height must be 
%    zero (0) dbar.
%  sea_surface_geopotental = geopotential at zero sea pressure  [ m^2/s^2 ]
%
%  lat may have dimensions 1x1 or Mx1 or 1xN or MxN, where p is MxN.
%  geo_strf_dyn_height and geo_strf_dyn_height, if provided, must have 
%  dimensions MxN, which are the same as p.
%
% OUTPUT:
%  z  =  height                                                       [ m ]
%  Note. At sea level z = 0, and since z (HEIGHT) is defined to be
%    positive upwards, it follows that while z is positive in the 
%    atmosphere, it is NEGATIVE in the ocean.
%
% AUTHOR:  
%  Trevor McDougall, Claire Roberts-Thomson & Paul Barker.
%                                                      [ help@teos-10.org ]
%
% VERSION NUMBER: 3.06.12 (25th May, 2020)
%
% REFERENCES:
%  IOC, SCOR and IAPSO, 2010: The international thermodynamic equation of 
%   seawater - 2010: Calculation and use of thermodynamic properties.  
%   Intergovernmental Oceanographic Commission, Manuals and Guides No. 56,
%   UNESCO (English), 196 pp.  Available from http://www.TEOS-10.org
%
%  McDougall, T.J., D.R. Jackett, D.G. Wright and R. Feistel, 2003: 
%   Accurate and computationally efficient algorithms for potential 
%   temperature and density of seawater.  J. Atmosph. Ocean. Tech., 20,
%   pp. 730-741.
%
%  Moritz, H., 2000: Geodetic reference system 1980. J. Geodesy, 74, 
%   pp. 128-133.
%
%  Roquet, F., G. Madec, T.J. McDougall, P.M. Barker, 2015: Accurate
%   polynomial expressions for the density and specifc volume of seawater
%   using the TEOS-10 standard. Ocean Modelling, 90, pp. 29-43.
%
%  This software is available from http://www.TEOS-10.org
%
%==========================================================================

%--------------------------------------------------------------------------
% Check variables and resize if necessary
%--------------------------------------------------------------------------

if ~(nargin == 2 | nargin == 3 | nargin == 4)
   error('gsw_z_from_p: Requires two, three or four inputs')
end %if

if ~exist('geo_strf_dyn_height','var')
    geo_strf_dyn_height = zeros(size(p));
end
if ~exist('sea_surface_geopotental','var')
    sea_surface_geopotental = zeros(size(p));
end

[mp,np] = size(p);
[ml,nl] = size(lat);
[mdh,ndh] = size(geo_strf_dyn_height);
[msg,nsg] = size(sea_surface_geopotental);

if (mp ~= mdh) | (np ~= ndh)
    error('gsw_z_from_p: pressure & dynamic height anomaly need to have the same dimensions')
end
if (mdh ~= msg) | (ndh ~= nsg)
    error('gsw_z_from_p: dynamic height anomaly & the geopotential at zero sea pressure need to have the same dimensions')
end

if (ml == 1) & (nl == 1)              % lat scalar - fill to size of p
    lat = lat*ones(size(p));
elseif (nl == np) & (ml == 1)         % lat is row vector,
    lat = lat(ones(1,mp), :);              % copy down each column.
elseif (mp == ml) & (nl == 1)         % lat is column vector,
    lat = lat(:,ones(1,np));               % copy across each row.
elseif (np == ml) & (nl == 1)          % lat is a transposed row vector,
    lat = lat.';                              % transposed then
    lat = lat(ones(1,mp), :);                % copy down each column.
elseif (mp == ml) & (np == nl)
    % ok
else
    error('gsw_z_from_p: Inputs array dimensions arguments do not agree')
end %if

if mp == 1
    p = p.';
    lat = lat.';
    geo_strf_dyn_height = geo_strf_dyn_height.';
    sea_surface_geopotental = sea_surface_geopotental.';
    transposed = 1;
else
    transposed = 0;
end

%--------------------------------------------------------------------------
% Start of the calculation
%--------------------------------------------------------------------------

gamma = 2.26e-7; % If the graviational acceleration were to be regarded as 
                 % being depth-independent, which is often the case in 
                 % ocean models, then gamma would be set to be zero here,
                 % and the code below works perfectly well.
deg2rad = pi/180;
sinlat = sin(lat*deg2rad);
sin2 = sinlat.*sinlat;
B = 9.780327*(1.0 + (5.2792e-3 + (2.32e-5*sin2)).*sin2); 
A = -0.5*gamma*B;
C = gsw_enthalpy_SSO_0(p) - (geo_strf_dyn_height + sea_surface_geopotental);
z = -2*C./(B + sqrt(B.*B - 4.*A.*C));

if transposed
    z = z.';
end

end
