Changes between Version 5 and Version 6 of 2012WP/2012Action_institutions_INGV
- Timestamp:
- 2011-11-15T17:35:39+01:00 (13 years ago)
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2012WP/2012Action_institutions_INGV
v5 v6 40 40 ''' Main tasks:''' Test of different parameterizations for the turbulent part of the wind drag coefficient. [[BR]] 41 41 ''' Science Reviewer:''' [[BR]] 42 ''' System Reviewer: ''' '''[[BR]]43 Deadline:''' '''[[BR]]44 Priority:''' '''[[BR]]45 Principal Investigator :''' Mario Adani (mario.adani@bo.ingv.it) [[BR]]42 ''' System Reviewer: ''' [[BR]] 43 ''' Deadline:''' [[BR]] 44 ''' Priority:''' [[BR]] 45 ''' Principal Investigator :''' Mario Adani (mario.adani@bo.ingv.it) [[BR]] 46 46 47 47 === '''INGV.3 — River lateral open boundary conditions''' === 48 ''' Motivation:''' A proper representation of river volume inflow. In case of large runoff, including 49 the river effects only in the surface water balance (Evaporation minus 50 Precipitation minus runoff/area) could limit the model capability in reproducing 51 the dynamics in the Region Of Fresh water Influence (ROFI). An open lateral 52 boundary condition with a vertical current profile is preferable. [[BR]] 48 ''' Motivation:''' A proper representation of river volume inflow. In case of large runoff, including the river effects only in the surface water balance (Evaporation minus Precipitation minus runoff/area) could limit the model capability in reproducing the dynamics in the Region Of Fresh water Influence (ROFI). An open lateral boundary condition with a vertical current profile is preferable. [[BR]] 53 49 ''' Status:''' [[BR]] 54 50 ''' Main tasks :''' [[BR]] 55 51 ''' Science Reviewer:''' [[BR]] 56 ''' System Reviewer:''' '''[[BR]]57 Deadline:''' '''[[BR]]58 Priority:''' '''[[BR]]59 Principal Investigator :''' Paolo Oddo (paolo.oddo@bo.ingv.it) [[BR]]52 ''' System Reviewer:''' [[BR]] 53 ''' Deadline:''' [[BR]] 54 ''' Priority:''' [[BR]] 55 ''' Principal Investigator :''' Paolo Oddo (paolo.oddo@bo.ingv.it) [[BR]] 60 56 61 57 === '''INGV.4 — Wave-current interaction''' === 62 ''' Motivation:''' full coupling of a wave model 63 with NEMO.In two steps: [[BR]] 64 a. Step1. By the end of 2012. Linear superposition of the Stokes velocity 65 field, computed from an offline wave model, with circulation velocity 66 from OGCM. [[BR]] 67 b. Step2. By the end of 2013. Implementation of all the wave-ogcm coupling 68 terms in the model equations. [[BR]] 58 ''' Motivation:''' full coupling of a wave model with NEMO.In two steps: [[BR]] 59 a. Step1. By the end of 2012. Linear superposition of the Stokes velocity field, computed from an offline wave model, with circulation velocity from OGCM. [[BR]] 60 b. Step2. By the end of 2013. Implementation of all the wave-ogcm coupling terms in the model equations. [[BR]] 69 61 ''' Status:''' [[BR]] 70 62 ''' Main tasks:''' [[BR]] 71 63 ''' Science Reviewer:''' [[BR]] 72 ''' System Reviewer:''' ''' [[BR]] Deadline:''' ''' [[BR]] Priority:''' ''' [[BR]] Principal Investigator :''' Mario Adani (mario.adani@bo.ingv.it) [[BR]] 64 ''' System Reviewer:''' [[BR]] 65 ''' Deadline:''' [[BR]] 66 ''' Priority:''' [[BR]] 67 ''' Principal Investigator :''' Mario Adani (mario.adani@bo.ingv.it) [[BR]] 73 68 74 69 === '''INGV.5 — Atmospheric forcing interpolation''' === 75 ''' Motivation:''' An issue that still need 76 investigation for the NEMO air-sea physics concerns the horizontal interpolation 77 of the input atmospheric fields. In the current version of the NEMO code, all the 78 external fields are interpolated into the model T-Grid, then fluxes computed, and 79 finally momentum fluxes interpolated into the corresponfing U and V-grids. 80 Another possibility is to interpolate the input atmospheric data into all the 81 necessary grids (U, V and T) and apply the bulk directly into the correct model 82 grid. This requires some testing. [[BR]] 70 ''' Motivation:''' An issue that still need investigation for the NEMO air-sea physics concerns the horizontal interpolation of the input atmospheric fields. In the current version of the NEMO code, all the 71 external fields are interpolated into the model T-Grid, then fluxes computed, and finally momentum fluxes interpolated into the corresponfing U and V-grids. Another possibility is to interpolate the input atmospheric data into all the necessary grids (U, V and T) and apply the bulk directly into the correct model grid. This requires some testing. [[BR]] 83 72 ''' Status:''' [[BR]] 84 73 ''' Main tasks:''' [[BR]]
