1 | SUBROUTINE nightingale(u, v, u_10m, v_10m, paprs, pplay, |
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2 | . cdragh, cdragm, t, q, ftsol, tsol, |
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3 | . pctsrf, lmt_dmsconc, lmt_dms) |
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4 | c |
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5 | USE dimphy |
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6 | USE indice_sol_mod |
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7 | IMPLICIT NONE |
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8 | c |
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9 | INCLUDE "dimensions.h" |
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10 | INCLUDE "YOMCST.h" |
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11 | c |
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12 | REAL u(klon,klev), v(klon,klev) |
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13 | REAL u_10m(klon), v_10m(klon) |
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14 | REAL ftsol(klon,nbsrf) |
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15 | REAL tsol(klon) |
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16 | REAL paprs(klon,klev+1), pplay(klon,klev) |
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17 | REAL t(klon,klev) |
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18 | REAL q(klon,klev) |
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19 | REAL cdragh(klon), cdragm(klon) |
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20 | REAL pctsrf(klon,nbsrf) |
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21 | REAL lmt_dmsconc(klon) ! concentration oceanique DMS |
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22 | REAL lmt_dms(klon) ! flux de DMS |
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23 | c |
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24 | REAL ustar(klon), obklen(klon) |
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25 | REAL u10(klon), u10n(klon) |
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26 | REAL tvelocity, schmidt_corr |
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27 | REAL t1, t2, t3, t4, viscosity_kin, diffusivity, schmidt |
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28 | INTEGER i |
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29 | c |
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30 | CALL bl_for_dms(u, v, paprs, pplay, cdragh, cdragm, |
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31 | . t, q, tsol, ustar, obklen) |
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32 | c |
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33 | DO i=1,klon |
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34 | u10(i)=SQRT(u_10m(i)**2+v_10m(i)**2) |
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35 | ENDDO |
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36 | c |
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37 | CALL neutral(u10, ustar, obklen, u10n) |
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38 | c |
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39 | DO i=1,klon |
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40 | c |
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41 | c tvelocity - transfer velocity, also known as kw (cm/s) |
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42 | c schmidt_corr - Schmidt number correction factor (dimensionless) |
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43 | c Reference: Nightingale, P.D., G. Malin, C. S. Law, J. J. Watson, P.S. Liss |
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44 | c M. I. Liddicoat, J. Boutin, R.C. Upstill-Goddard. 'In situ evaluation |
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45 | c of air-sea gas exchange parameterizations using conservative and |
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46 | c volatile tracers.' Glob. Biogeochem. Cycles, 14:373-387, 2000. |
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47 | c compute transfer velocity using u10neutral |
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48 | c |
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49 | tvelocity = 0.222*u10n(i)*u10n(i) + 0.333*u10n(i) |
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50 | c |
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51 | c above expression gives tvelocity in cm/hr. convert to cm/s. 1hr =3600 sec |
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52 | |
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53 | tvelocity = tvelocity / 3600. |
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54 | |
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55 | c compute the correction factor, which for Nightingale parameterization is |
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56 | c based on how different the schmidt number is from 600. |
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57 | c correction factor based on temperature in Kelvin. good |
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58 | c only for t<=30 deg C. for temperatures above that, set correction factor |
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59 | c equal to value at 30 deg C. |
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60 | |
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61 | IF (ftsol(i,is_oce) <= 303.15) THEN |
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62 | t1 = ftsol(i,is_oce) |
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63 | ELSE |
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64 | t1 = 303.15 |
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65 | ENDIF |
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66 | |
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67 | t2 = t1 * t1 |
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68 | t3 = t2 * t1 |
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69 | t4 = t3 * t1 |
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70 | viscosity_kin = 3.0363e-9*t4 - 3.655198e-6*t3 + 1.65333e-3*t2 |
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71 | + - 3.332083e-1*t1 + 25.26819 |
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72 | diffusivity = 0.01922 * exp(-2177.1/t1) |
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73 | schmidt = viscosity_kin / diffusivity |
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74 | schmidt_corr = (schmidt/600.)**(-.5) |
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75 | c |
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76 | lmt_dms(i) = tvelocity * pctsrf(i,is_oce) |
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77 | . * lmt_dmsconc(i)/1.0e12 * schmidt_corr * RNAVO |
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78 | c |
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79 | IF (lmt_dmsconc(i)<=1.e-20) lmt_dms(i)=0.0 |
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80 | c |
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81 | ENDDO |
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82 | c |
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83 | END |
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