Changeset 2297 for trunk/LMDZ.GENERIC/README
- Timestamp:
- Apr 26, 2020, 7:45:46 PM (5 years ago)
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- 1 edited
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trunk/LMDZ.GENERIC/README
r2283 r2297 1512 1512 Everybody should be using AU, that's all. 1513 1513 1514 == 24/02/2020 (r224 4) == JVO1514 == 24/02/2020 (r2245) == JVO 1515 1515 + Add a 'versH2H2cia' int key in callphys that allows two values (2011 or 2018) to 1516 1516 deal with updated HITRAN file (for interpolateH2H2.F90) from 2018 that includes the … … 1533 1533 + Add a sanity check in callcorrk instead of leaving out-of-bounds planckir indexes. 1534 1534 1535 1535 == 26/04/2020 (r2297) == JVO 1536 Add a generic n-layer aerosol scheme to replace the former buggy 2-layer scheme as well as the hard-coded NH3 cloud. 1537 It can be called using 'aeronlay=.true.' in callphys.def, and set the number of layers (up to 4) with 'nlayaero'. 1538 Then, the following parameters are read as arrays of size nlayaero in callphys.def (separated by blank space) 1539 1540 *aeronlay_tauref (Optical depth of aerosol layer at ref wavelenght) 1541 *aeronlay_lamref (Ref wavelenght (m)) 1542 *aeronlay_choice (Choice for vertical profile - 1:tau follows atm scale height btwn top and bottom - 2:tau follows it own scale height) 1543 *aeronlay_pbot (Bottom pressure (Pa)) 1544 *aeronlay_ptop (Top pressure (Pa) - useful only if choice=1) 1545 *aeronlay_sclhght (Ratio of aerosol layer scale height / atmospheric scale height - useful only if choice=2 ) 1546 *aeronlay_size (Particle size (m)) 1547 *optprop_aeronlay_vis File for VIS opt properties. 1548 *optprop_aeronlay_ir File for IR opt properties. 1549 1550 +Extra info : 1551 + In addition of solving the bug from 2-layer it enables different optical properties. 1552 + The former scheme are left for retrocompatibility (for now) but you should use the new one. 1553 + See aeropacity.F90 for the calculations 1554 + Each layer can have different optical properties, size of particle ... 1555 + You have different choices for vertical profile of the aerosol layers : 1556 * aeronlay_choice = 1 : Layer tau is spread between ptop and pbot following atm scale height. 1557 * aeronlay_choice = 2 : Layer tau follows its own scale height above cloud deck (pbot). 1558 In this case ptop is dummy and sclhght gives the ratio H_cl/H_atm. 1559 1560 + The reference wavelenght for input optical depth is now read as input (aeronlay_lamref) 1561 + Following the last point some comment is added in suaer_corrk about the 'not-really-dummy'ness of IR lamref..
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