sea_water_x_velocity_due_to_parameterized_mesoscale_eddies
A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized mesoscale eddies occur on a spatial scale of many tens of kilometres and an evolutionary time of weeks. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. Parameterized mesoscale eddies are represented in ocean models using schemes such as the Gent-McWilliams scheme. sea_water_x_velocity_due_to_parameterized_mesoscale_eddies is used in some parameterisations of lateral diffusion in the ocean.
List containing this term version:
CF (48)
CF (49)
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CF (81)
CF (82)
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CF (84)
CF (85)
CF (86)
Proposls with this term version:
Proposal: Jonathan Gregory / Stephen Griffies / Alison Pamment [New standard names for OMIP: physics]
There are no aliases for this term
This term is alaised by
A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. bolus_sea_water_x_velocity is used in some parameterisations of lateral diffusion in the ocean.
List containing this term version:
Proposls with this term version:
Proposal: Jonathan Gregory / Stephen Griffies / Alison Pamment [New standard names for OMIP: physics]
A velocity is a vector quantity. "x" indicates a vector component along the grid x-axis, positive with increasing x. The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. Parameterized mesoscale eddies occur on a spatial scale of many tens of kilometres and an evolutionary time of weeks. Reference: James C. McWilliams 2016, Submesoscale currents in the ocean, Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, volume 472, issue 2189. DOI: 10.1098/rspa.2016.0117. Parameterized mesoscale eddies are represented in ocean models using schemes such as the Gent-McWilliams scheme. sea_water_x_velocity_due_to_parameterized_mesoscale_eddies is used in some parameterisations of lateral diffusion in the ocean.
List containing this term version:
CF (48)
CF (49)
CF (50)
CF (51)
CF (52)
CF (53)
CF (54)
CF (55)
CF (56)
CF (57)
CF (58)
CF (59)
CF (60)
CF (61)
CF (62)
CF (63)
CF (64)
CF (65)
CF (66)
CF (67)
CF (68)
CF (69)
CF (70)
CF (71)
CF (72)
CF (73)
CF (74)
CF (75)
CF (76)
CF (77)
CF (78)
CF (79)
CF (80)
CF (81)
CF (82)
CF (83)
CF (84)
CF (85)
CF (86)
Proposls with this term version:
Proposal: Jonathan Gregory / Stephen Griffies / Alison Pamment [New standard names for OMIP: physics]
