Dear Dirk,

a fair comment ... I withdraw my suggested re-ordering,


regards,

Martin


________________________________
From: CF-metadata <cf-metadata-boun...@cgd.ucar.edu> on behalf of Dirk Notz 
<dirk.n...@mpimet.mpg.de>
Sent: 03 July 2018 14:34
To: cf-metadata@cgd.ucar.edu
Subject: Re: [CF-metadata] SIMIP: 5 standard names and one area type for CMIP6

Dear Alison, Jonathan, Martin,

I like the names that Jonathan suggested. With Martin's definition, I
find it more difficult to figure out how to read the various parts of
the name, i.e. people could wonder about a "sea-ice maximum" etc.

Best,

 Dirk



----
Dr. Dirk Notz
http://www.mpimet.mpg.de/~notz.dirk

Am 03.07.2018 um 13:26 schrieb Martin Juckes - UKRI STFC:
> Dear Alison, Jonathan,
>
>
> I can see some benefit in the re-ordering the parts of the name, but we 
> generally start names with something more specific to the parameter (e.g. 
> sea_surface_wave_maximum_period).
>
>
> How about:
>
> sea_ice_maximum_over_coordinate_rotation_of_horizontal_shear_strain_rate 
> (s-1) and
>
> sea_ice_maximum_over_coordinate_rotation_of_horizontal_shear_stress (N m-1)?
>
>
> regards,
>
> Martin
>
> ________________________________
> From: CF-metadata <cf-metadata-boun...@cgd.ucar.edu> on behalf of Jonathan 
> Gregory <j.m.greg...@reading.ac.uk>
> Sent: 28 June 2018 14:49
> To: Pamment, Alison (STFC,RAL,RALSP)
> Cc: cf-metadata@cgd.ucar.edu
> Subject: Re: [CF-metadata] SIMIP: 5 standard names and one area type for CMIP6
>
> Dear Alison
>
> Yes, that's what I meant. Thanks for considering it.
>
> Best wishes
>
> Jonathan
>
> On Thu, Jun 28, 2018 at 01:41:23PM +0000, Alison Pamment - UKRI STFC wrote:
>> Date: Thu, 28 Jun 2018 13:41:23 +0000
>> From: Alison Pamment - UKRI STFC <alison.pamm...@stfc.ac.uk>
>> To: "'j.m.greg...@reading.ac.uk'" <j.m.greg...@reading.ac.uk>,
>>  "cf-metadata@cgd.ucar.edu" <cf-metadata@cgd.ucar.edu>
>> Subject: RE: [CF-metadata] SIMIP: 5 standard names and one area type for
>>  CMIP6
>>
>> Dear Jonathan,
>>
>> Thank you for commenting on these names. If I understand you correctly, then 
>> the two 'maximum' names and definitions would be rearranged as follows.
>>
>> maximum_over_coordinate_rotation_of_sea_ice_horizontal_shear_strain_rate 
>> (s-1)
>> '"Sea ice" means all ice floating in the sea which has formed from freezing 
>> sea water, rather than by other processes such as calving of land ice to 
>> form icebergs. Axial strain is the symmetric component of the tensor 
>> representing the gradient of internal forces (e.g. in ice). Strain rate 
>> refers to off-diagonal element(s) of the strain tensor (a single element for 
>> horizontal shear strain). "Horizontal" refers to the local horizontal in the 
>> location of the sea ice, i.e., perpendicular to the local gravity vector. 
>> Each of the strain components is defined with respect to a frame of 
>> reference. "Coordinate rotation" refers to the range of all possible 
>> orientations of the frame of reference. The shear strain has a maximum value 
>> relative to one of these orientations. The second invariant of strain rate, 
>> often referred to as the maximum shear strain [rate], is the maximum over 
>> coordinate rotations of the shear strain rate.'
>>
>> maximum_over_coordinate_rotation_of_sea_ice_horizontal_shear_stress (N m-1)
>> ' "Sea ice" means all ice floating in the sea which has formed from freezing 
>> sea water, rather than by other processes such as calving of land ice to 
>> form icebergs. Axial stress is the symmetric component of the tensor 
>> representing the gradient of internal forces (e.g. in ice). Shear stress 
>> refers to off-diagonal element(s) of the stress tensor (a single element for 
>> horizontal shear stress). "Horizontal" refers to the local horizontal in the 
>> location of the sea ice, i.e., perpendicular to the local gravity vector. 
>> Each of the stress components is defined with respect to a frame of 
>> reference. "Coordinate rotation" refers to the range of all possible 
>> orientations of the frame of reference. The shear stress has a maximum value 
>> relative to one of these orientations. The second invariant of stress, often 
>> referred to as the maximum shear stress, is the maximum over coordinate 
>> rotations of the shear stress.'
>>
>> I tend to agree that these are a little easier to understand at first sight. 
>> I'm happy to write the names and definitions this way, if Dirk and Bruno 
>> have no objections.
>>
>> N.B. I have added 'Axial' to the start of the second sentence of the 
>> definitions and replaced 'stress' with 'strain' for the first definition, as 
>> requested by Dirk.
>>
>> Best wishes,
>> Alison
>>
>> ------
>> Alison Pamment                                 Tel: +44 1235 778065
>> NCAS/Centre for Environmental Data Archival    Email: 
>> alison.pamm...@stfc.ac.uk
>> STFC Rutherford Appleton Laboratory
>> R25, 2.22
>> Harwell Oxford, Didcot, OX11 0QX, U.K.
>>
>> -----Original Message-----
>> From: CF-metadata <cf-metadata-boun...@cgd.ucar.edu> On Behalf Of Jonathan 
>> Gregory
>> Sent: 25 June 2018 14:23
>> To: cf-metadata@cgd.ucar.edu
>> Subject: Re: [CF-metadata] SIMIP: 5 standard names and one area type for 
>> CMIP6
>>
>> Dear Alison and Dirk
>>
>>> It has taken me a little while to understand this name, but I am beginning 
>>> to grasp it!
>>> sea_ice_horizontal_shear_strain_rate_maximum_over_coordinate_rotation
>>> (s-1)
>>
>> I think the concept and definition are fine, but the name could maybe be 
>> made a bit clearer. The last sentence of the definition seems clearer in 
>> turning it
>> round: could you likewise make the name
>>   maximum_over_coordinate_rotation_of_sea_ice_horizontal_shear_strain_rate
>>
>> ?
>>
>> Cheers
>>
>> Jonathan
>> _______________________________________________
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