- Timestamp:
- Mar 7, 2012, 4:09:27 PM (13 years ago)
- File:
-
- 1 edited
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trunk/LMDZ.MARS/README
r563 r567 1444 1444 value was asked to user, but twice! Once is enough. 1445 1445 1446 == 07/03/12 == AC 1447 ******************************************************** 1448 >> UPDATE ON PARAMETERS TO SET TO USE THE THERMALS MODEL 1449 ******************************************************** 1450 1451 >> IN CALLPHYS.DEF << 1452 --------------------- 1453 1454 - calltherm = .true. > activates the thermals 1455 - callrichsl = .true. > activate the Richardson Monin Obukhov surface layer 1456 with subgrid gustiness, and the yamada4 diffusion model from earth (corrected version of vdif_kc) 1457 - leave calladj = .true. > so that the convective adjustment may work ABOVE the PBL. 1458 1459 >> IN RUN.DEF << 1460 ---------------- 1461 1462 - 96 physicial timesteps per day (the internal sub-timestep of thermals will adapt 1463 so that it costs only 10% more CPU time to go from "48pdt+thermals" to "96pdt+thermals".) 1464 > this has to be respected because of a coupling between the radiative transfer and thermals 1465 > if you really wish to run with 48 pdt/day, you may want to deactive the thermals... 1466 1467 >> USEFULL DIAGNOSTICS << 1468 ------------------------- 1469 1470 - activating the thermals will automatically add 3 2D-outputs to diagfi.nc files: 1471 > zmax_th : interpolated boundary layer height (m) 1472 > hfmax_th : maximum vertical eddy heat flux reached in thermals (K.m/s) 1473 > wstar : free convection velocity reached in thermals (m/s) 1474 1475 A rule of thumb for determining the mean velocities in subgrid-scale structures is: 1476 1477 Mean updraft velocity : ~ wstar 1478 Maximum updraft velocity : ~ 2 or 3.*wstar 1479 Mean downdraft velocity : ~ 0.66*wstar 1480 Maximum absolute value of downdraft velocity : ~ 2.*wstar 1481 1482 >> AT COMPILATION TIME << 1483 ------------------------- 1484 1485 - +1 vertical level during the compilation, and then using the updated z2sig.def 1486 1487 >> UPDATED Z2SIG.DEF << 1488 ----------------------- 1489 1490 - one level has been added in the PBL, so that to reach 150km you have to compile with 1491 33 vertical levels instead of 32. 1492 1493 10.00000 H: atmospheric scale height (km) (used as a reference only) 1494 0.0020736 1495 0.015735 1496 0.0600151 1497 0.163344 1498 0.36358 1499 0.708007 1500 1.25334 1501 2.06571 1502 3.22069 1503 4.80327 1504 6.90787 1505 9.63834 1506 13.108 1507 18.9666 1508 25.0626 1509 31.5527 1510 38.4369 1511 45.4369 1512 52.4369 1513 59.4369 1514 66.4369 1515 73.4369 1516 80.4369 1517 87.4369 1518 94.4369 1519 101.4369 1520 108.437 1521 115.437 1522 122.437 1523 129.437 1524 136.437 1525 143.437 1526 150.437 1527 157.437 1528 164.437 1529 171.437 1530 178.437 1531 185.437 1532 192.437 1533 199.437 1534 206.437 1535 213.437 1536 220.437 1537 227.437 1538 234.437 1539 241.437 1540 248.437 1541 255.437 1542 262.437 1543 269.437 1544 276.437 1545 283.437 1546 290.437 1547 297.437 1548 304.437 1549 311.437 1550 318.437 1551 325.437 1552 332.437 1553 339.437 1554 346.437 1555 353.437 1556 360.437 1557 367.437 1558 374.437 1559 381.437 1560 388.437 1561 395.437 1562 1563 ******************************************************** 1564 >> END OF UPDATE ON PARAMETERS FOR THE THERMALS MODEL 1565 ********************************************************
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