| 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 | |
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| 5 | USE dimphy |
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| 6 | USE indice_sol_mod |
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| 7 | USE lmdz_yomcst |
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| 8 | |
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| 9 | USE lmdz_dimensions, ONLY: iim, jjm, llm, ndm |
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| 10 | IMPLICIT NONE |
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| 11 | ! |
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| 12 | |
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| 13 | |
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| 14 | REAL :: u(klon, klev), v(klon, klev) |
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| 15 | REAL :: u_10m(klon), v_10m(klon) |
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| 16 | REAL :: ftsol(klon, nbsrf) |
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| 17 | REAL :: tsol(klon) |
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| 18 | REAL :: paprs(klon, klev + 1), pplay(klon, klev) |
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| 19 | REAL :: t(klon, klev) |
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| 20 | REAL :: q(klon, klev) |
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| 21 | REAL :: cdragh(klon), cdragm(klon) |
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| 22 | REAL :: pctsrf(klon, nbsrf) |
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| 23 | REAL :: lmt_dmsconc(klon) ! concentration oceanique DMS |
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| 24 | REAL :: lmt_dms(klon) ! flux de DMS |
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| 25 | |
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| 26 | REAL :: ustar(klon), obklen(klon) |
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| 27 | REAL :: u10(klon), u10n(klon) |
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| 28 | REAL :: tvelocity, schmidt_corr |
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| 29 | REAL :: t1, t2, t3, t4, viscosity_kin, diffusivity, schmidt |
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| 30 | INTEGER :: i |
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| 31 | |
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| 32 | CALL bl_for_dms(u, v, paprs, pplay, cdragh, cdragm, & |
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| 33 | t, q, tsol, ustar, obklen) |
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| 34 | |
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| 35 | DO i = 1, klon |
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| 36 | u10(i) = SQRT(u_10m(i)**2 + v_10m(i)**2) |
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| 37 | ENDDO |
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| 38 | |
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| 39 | CALL neutral(u10, ustar, obklen, u10n) |
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| 40 | |
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| 41 | DO i = 1, klon |
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| 42 | |
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| 43 | ! tvelocity - transfer velocity, also known as kw (cm/s) |
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| 44 | ! schmidt_corr - Schmidt number correction factor (dimensionless) |
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| 45 | ! Reference: Nightingale, P.D., G. Malin, C. S. Law, J. J. Watson, P.S. Liss |
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| 46 | ! M. I. Liddicoat, J. Boutin, R.C. Upstill-Goddard. 'In situ evaluation |
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| 47 | ! of air-sea gas exchange parameterizations using conservative and |
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| 48 | ! volatile tracers.' Glob. Biogeochem. Cycles, 14:373-387, 2000. |
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| 49 | ! compute transfer velocity using u10neutral |
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| 50 | |
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| 51 | tvelocity = 0.222 * u10n(i) * u10n(i) + 0.333 * u10n(i) |
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| 52 | |
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| 53 | ! above expression gives tvelocity in cm/hr. convert to cm/s. 1hr =3600 sec |
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| 54 | |
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| 55 | tvelocity = tvelocity / 3600. |
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| 56 | |
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| 57 | ! compute the correction factor, which for Nightingale parameterization is |
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| 58 | ! based on how different the schmidt number is from 600. |
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| 59 | ! correction factor based on temperature in Kelvin. good |
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| 60 | ! only for t<=30 deg C. for temperatures above that, set correction factor |
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| 61 | ! equal to value at 30 deg C. |
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| 62 | |
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| 63 | IF (ftsol(i, is_oce) <= 303.15) THEN |
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| 64 | t1 = ftsol(i, is_oce) |
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| 65 | ELSE |
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| 66 | t1 = 303.15 |
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| 67 | ENDIF |
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| 68 | |
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| 69 | t2 = t1 * t1 |
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| 70 | t3 = t2 * t1 |
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| 71 | t4 = t3 * t1 |
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| 72 | viscosity_kin = 3.0363e-9 * t4 - 3.655198e-6 * t3 + 1.65333e-3 * t2 & |
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| 73 | - 3.332083e-1 * t1 + 25.26819 |
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| 74 | diffusivity = 0.01922 * exp(-2177.1 / t1) |
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| 75 | schmidt = viscosity_kin / diffusivity |
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| 76 | schmidt_corr = (schmidt / 600.)**(-.5) |
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| 77 | |
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| 78 | lmt_dms(i) = tvelocity * pctsrf(i, is_oce) & |
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| 79 | * lmt_dmsconc(i) / 1.0e12 * schmidt_corr * RNAVO |
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| 80 | |
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| 81 | IF (lmt_dmsconc(i)<=1.e-20) lmt_dms(i) = 0.0 |
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| 82 | |
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| 83 | ENDDO |
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| 84 | |
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| 85 | END SUBROUTINE nightingale |
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