function K = sw_seck(S,T,P) % SW_SECK Secant bulk modulus (K) of sea water %========================================================================= % SW_SECK $Id: sw_seck.m,v 1.1 2003/12/12 04:23:22 pen078 Exp $ % Copyright (C) CSIRO, Phil Morgan 1992. % % USAGE: dens = sw_seck(S,T,P) % % DESCRIPTION: % Secant Bulk Modulus (K) of Sea Water using Equation of state 1980. % UNESCO polynomial implementation. % % INPUT: (all must have same dimensions) % S = salinity [psu (PSS-78) ] % T = temperature [degree C (ITS-90)] % P = pressure [db] % (alternatively, may have dimensions 1*1 or 1*n where n is columns in S) % % OUTPUT: % K = Secant Bulk Modulus [bars] % % AUTHOR: Phil Morgan 92-11-05, Lindsay Pender (Lindsay.Pender@csiro.au) % % DISCLAIMER: % This software is provided "as is" without warranty of any kind. % See the file sw_copy.m for conditions of use and licence. % % REFERENCES: % Fofonoff, P. and Millard, R.C. Jr % Unesco 1983. Algorithms for computation of fundamental properties of % seawater, 1983. _Unesco Tech. Pap. in Mar. Sci._, No. 44, 53 pp. % Eqn.(15) p.18 % % Millero, F.J. and Poisson, A. % International one-atmosphere equation of state of seawater. % Deep-Sea Res. 1981. Vol28A(6) pp625-629. %========================================================================= % Modifications % 99-06-25. Lindsay Pender, Fixed transpose of row vectors. % 03-12-12. Lindsay Pender, Converted to ITS-90. % CALLER: sw_dens.m % CALLEE: none %---------------------- % CHECK INPUT ARGUMENTS %---------------------- if nargin ~=3 error('sw_seck.m: Must pass 3 parameters') end %if % CHECK S,T,P dimensions and verify consistent [ms,ns] = size(S); [mt,nt] = size(T); [mp,np] = size(P); % CHECK THAT S & T HAVE SAME SHAPE if (ms~=mt) | (ns~=nt) error('check_stp: S & T must have same dimensions') end %if % CHECK OPTIONAL SHAPES FOR P if mp==1 & np==1 % P is a scalar. Fill to size of S P = P(1)*ones(ms,ns); elseif np==ns & mp==1 % P is row vector with same cols as S P = P( ones(1,ms), : ); % Copy down each column. elseif mp==ms & np==1 % P is column vector P = P( :, ones(1,ns) ); % Copy across each row elseif mp==ms & np==ns % PR is a matrix size(S) % shape ok else error('check_stp: P has wrong dimensions') end %if %***check_stp %-------------------------------------------------------------------- % COMPUTE COMPRESSION TERMS %-------------------------------------------------------------------- P = P/10; %convert from db to atmospheric pressure units T68 = T * 1.00024; % Pure water terms of the secant bulk modulus at atmos pressure. % UNESCO eqn 19 p 18 h3 = -5.77905E-7; h2 = +1.16092E-4; h1 = +1.43713E-3; h0 = +3.239908; %[-0.1194975]; AW = h0 + (h1 + (h2 + h3.*T68).*T68).*T68; k2 = 5.2787E-8; k1 = -6.12293E-6; k0 = +8.50935E-5; %[+3.47718E-5]; BW = k0 + (k1 + k2*T68).*T68; e4 = -5.155288E-5; e3 = +1.360477E-2; e2 = -2.327105; e1 = +148.4206; e0 = 19652.21; %[-1930.06]; KW = e0 + (e1 + (e2 + (e3 + e4*T68).*T68).*T68).*T68; % eqn 19 %-------------------------------------------------------------------- % SEA WATER TERMS OF SECANT BULK MODULUS AT ATMOS PRESSURE. %-------------------------------------------------------------------- j0 = 1.91075E-4; i2 = -1.6078E-6; i1 = -1.0981E-5; i0 = 2.2838E-3; SR = sqrt(S); A = AW + (i0 + (i1 + i2*T68).*T68 + j0*SR).*S; m2 = 9.1697E-10; m1 = +2.0816E-8; m0 = -9.9348E-7; B = BW + (m0 + (m1 + m2*T68).*T68).*S; % eqn 18 f3 = -6.1670E-5; f2 = +1.09987E-2; f1 = -0.603459; f0 = +54.6746; g2 = -5.3009E-4; g1 = +1.6483E-2; g0 = +7.944E-2; K0 = KW + ( f0 + (f1 + (f2 + f3*T68).*T68).*T68 ... + (g0 + (g1 + g2*T68).*T68).*SR ).*S; % eqn 16 K = K0 + (A + B.*P).*P; % eqn 15 return %----------------------------------------------------------------------------