Changes between Version 71 and Version 72 of DevelopmentActivities/ORCHIDEE-CNP
- Timestamp:
- 2016-03-02T18:02:01+01:00 (8 years ago)
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DevelopmentActivities/ORCHIDEE-CNP
v71 v72 17 17 This subroutine calculates the scaling functions based on the stoichiometric ratio of labile plant tissue (reserve, labile and leaf) which are used to scale root uptake, biological N2 fixation, and biochemical mineralization. It currently supports scaling functions based on the P-to-N ratio, N-to-C ratio and P-to-C ratio. All other combinations will cause a 'STOP', but could be easily implemented if needed. 18 18 19 == New input file with USDA soil orders == 20 We use the USDA soil order map of Sun et al. (in revision). The gap filling of the missing values was done like this 19 == New input files == 20 === USDA soil orders === 21 We use the USDA soil order map of Sun et al. (in revision) with the dominant soil order per pixel. The gap filling of the missing values was done like this 21 22 (see script /home/users/dgoll/ORC_data/USDA_soilorders/try_2_fill/fill_deserts.ksh): 22 23 … … 30 31 Figure 1: USDA soil orders: Alfisols(1), Andisols(2), Aridisols(3), Entisols(4), Gelisols(5), Histosols(6), Inceptisols(7), Mollisols(8), Oxisols(9), Spodosols(10),Ultisols(11), Vertisols(12) 31 32 32 33 === GliM lithology === 34 We use the GliM lithology map by Hartmann & Moosdorf (2012). We account for subgrid scale heterogeneity by reading the fractional coverage of each of the 16 classes. 33 35 34 36 [[Image(lith_dom_map.png)]]