Dear Andy

Yes, that looks good - a sufficient amount of information. Thanks very much.
Happy bank holiday.

Jonathan

----- Forwarded message from "Saulter, Andrew" 
<[email protected]> -----

> Date: Fri, 4 May 2018 08:34:30 +0000
> From: "Saulter, Andrew" <[email protected]>
> To: "[email protected]" <[email protected]>
> Subject: Re: [CF-metadata] proposed additional names for sea_surface_wave
>       parameters
> 
> Dear Jonathon,
> 
> Before I put in a version for all the components, does the form of the below 
> look OK?
> 
> sea_surface_wave_directional_spread
> units: degree
> Directional spread represents the (one-sided) directional width of the wave 
> directional spectrum, S(t,x,y,f,theta) where t is time, x and y are 
> horizontal coordinates (such as longitude and latitude), f is frequency and 
> theta is direction. For a given mean wave (beam) direction the quantity 
> approximates half the root mean square width about the beam axis, as derived 
> either directly from circular moments or via the Fourier components of the 
> wave directional spectrum. 
> 
> Many thanks
> Andy
> 
> 
> -----Original Message-----
> From: CF-metadata [mailto:[email protected]] On Behalf Of 
> Jonathan Gregory
> Sent: 03 May 2018 17:33
> To: [email protected]
> Subject: Re: [CF-metadata] proposed additional names for sea_surface_wave 
> parameters
> 
> Dear Andy
> 
> Yes, I agree, that is a sufficiently different quantity that it can't clearly 
> be seen as a statistic describable by cell_methods and so needs its own name.
> Maybe you could add something more to the definition.
> 
> Best wishes and thanks
> 
> Jonathan
> 
> ----- Forwarded message from "Saulter, Andrew" 
> <[email protected]> -----
> 
> > Date: Thu, 3 May 2018 10:34:03 +0000
> > From: "Saulter, Andrew" <[email protected]>
> > To: "[email protected]" <[email protected]>
> > Subject: Re: [CF-metadata] proposed additional names for sea_surface_wave
> >     parameters
> > 
> > Thanks Jonathon,
> > 
> > Re the directional_spread parameters in section 4, the "one-sided 
> > directional width" as its described in Holthuijsen's book (Waves in Oceanic 
> > and Coastal Waters) is perhaps more precisely defined by Tucker and Pitt 
> > (Waves in Ocean Engineering) as "half the beam-width as usually described: 
> > that is, it is from the beam axis to the root mean square width".
> > 
> > So in principle there is a statistical relationship between this value and 
> > a mean_wave_direction that is also computed from moments of the directional 
> > wave spectrum. However, there is a lot of detail here; first Tucker and 
> > Pitt note that this is an approximation. Rather more detail is given by 
> > Kuik et al. (1988, 
> > https://doi.org/10.1175/1520-0485(1988)018%3C1020:AMFTRA%3E2.0.CO;2 ) who 
> > explain potential differences in calculation of directional characteristics 
> > using linear or circular moments - the latter being necessary for wave 
> > measurements, where spreading is then estimated based on the Fourier 
> > components of the directional wave spectrum rather than a direct 
> > calculation of directional spectrum statistics.
> > 
> > So the parameter feels a bit more complex and nuanced than a cell_methods 
> > application to wave_direction would allow. I think giving it its own name 
> > is more appropriate in this case?
> > 
> > Cheers
> > Andy
> > 
> > 
> > -----Original Message-----
> > From: CF-metadata [mailto:[email protected]] On Behalf 
> > Of Jonathan Gregory
> > Sent: 02 May 2018 13:32
> > To: [email protected]
> > Subject: [CF-metadata] proposed additional names for sea_surface_wave 
> > parameters
> > 
> > Dear Andy
> > 
> > Your new proposals of sections 1-3 following existing patterns, as you say, 
> > and look fine to me.
> > 
> > For those of section 4, can you say precisely what "one-sided directional 
> > width" means? The way you describe it, I wonder whether it could be 
> > described as a processed version of the wave_direction theta. For example, 
> > if it was the standard deviation of theta, cell_methods could describe it.
> > 
> > Best wishes
> > 
> > Jonathan
> > 
> > ----- Forwarded message from "Saulter, Andrew" 
> > <[email protected]> -----
> > 
> > > Date: Wed, 2 May 2018 07:28:05 +0000
> > > From: "Saulter, Andrew" <[email protected]>
> > > To: "[email protected]" <[email protected]>
> > > Subject: Re: [CF-metadata] proposed additional names for sea_surface_wave
> > >   parameters
> > > 
> > > Adding a minor amendment to the units for the 
> > > 'wave_energy_at_variance_spectral_density_maximum' parameters. These 
> > > should be 'm2 s' rather than 'm2s' in order to be parsed by UDUNITS.
> > > 
> > > Andy
> > > 
> > > From: CF-metadata [mailto:[email protected]] On 
> > > Behalf Of Saulter, Andrew
> > > Sent: 01 May 2018 09:27
> > > To: [email protected]
> > > Subject: [CF-metadata] proposed additional names for 
> > > sea_surface_wave parameters
> > > 
> > > Hi all,
> > > 
> > > Please find proposals for some additional sea_surface_wave parameters, 
> > > which will be provided as part of Met Office operational forecast 
> > > products in the near future. Hopefully nothing too contentious as mostly 
> > > an extension of some existing CF names.
> > > 
> > > 
> > > 1.       Addition of 'tertiary_swell' names for existing wave parameters 
> > > defined under 'wind_wave', 'primary_swell' and 'secondary_swell' 
> > > categories. So would add:
> > > 
> > > sea_surface_tertiary_swell_wave_from_direction
> > > units: degree
> > > The quantity with standard name 
> > > sea_surface_tertiary_swell_wave_from_direction is the direction from 
> > > which the third most energetic swell waves are coming. Swell waves are 
> > > waves on the ocean surface and are the low frequency portion of a bimodal 
> > > wave frequency spectrum. The tertiary swell wave is the third most 
> > > energetic swell wave. The phrase "from_direction" is used in the 
> > > construction X_from_direction and indicates the direction from which the 
> > > velocity vector of X is coming. The direction is a bearing in the usual 
> > > geographical sense, measured positive clockwise from due north.
> > > 
> > > sea_surface_tertiary_swell_wave_mean_period
> > > units: s
> > > The quantity with standard name 
> > > sea_surface_tertiary_swell_wave_mean_period is the mean period of the 
> > > third most energetic swell waves. Swell waves are waves on the ocean 
> > > surface and are the low frequency portion of a bimodal wave frequency 
> > > spectrum. The tertiary swell wave is the third most energetic wave in the 
> > > low frequency portion of a bimodal wave frequency spectrum. A period is 
> > > an interval of time, or the time-period of an oscillation. Wave period is 
> > > the interval of time between repeated features on the waveform such as 
> > > crests, troughs or upward passes through the mean level. Wave mean period 
> > > is the mean period measured over the observation duration.
> > > 
> > > sea_surface_tertiary_swell_wave_significant_height
> > > Swell waves are waves on the ocean surface and are the low frequency 
> > > portion of a bimodal wave frequency spectrum. The tertiary swell wave is 
> > > the third most energetic wave in the low frequency portion of a bimodal 
> > > wave frequency spectrum. Significant wave height is a statistic computed 
> > > from wave measurements and corresponds to the average height of the 
> > > highest one third of the waves, where the height is defined as the 
> > > vertical distance from a wave trough to the following wave crest.
> > > 
> > > 
> > > 
> > > 2.       Addition of peak wave period parameter to 'wind_wave', 
> > > 'primary_swell', 'secondary_swell' and 'tertiary_swell' categories. This 
> > > follows the existing standard for 
> > > 'sea_surface_wave_period_at_variance_spectral_density_maximum' and adds:
> > > 
> > > sea_surface_wind_wave_period_at_variance_spectral_density_maximum
> > > units: s
> > > The quantity with standard name 
> > > sea_surface_wind_wave_period_at_variance_spectral_density_maximum is the 
> > > period of the most energetic waves within the wind wave component of a 
> > > sea. Wind waves are waves on the ocean surface and are the high frequency 
> > > portion of a bimodal wave frequency spectrum. A period is an interval of 
> > > time, or the time-period of an oscillation. The phrase 
> > > "wave_period_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave period, describes the period of the most energetic waves within a 
> > > given sub-domain of the wave spectrum.
> > > 
> > > sea_surface_primary_swell_wave_period_at_variance_spectral_density_m
> > > ax
> > > imum
> > > units: s
> > > The quantity with standard name 
> > > sea_surface_primary_swell_wave_period_at_variance_spectral_density_maximum
> > >  is the period of the most energetic waves within the primary swell wave 
> > > component of a sea. Swell waves are waves on the ocean surface and are 
> > > the low frequency portion of a bimodal wave frequency spectrum. The 
> > > primary swell wave is the most energetic wave component in the low 
> > > frequency portion of a bimodal wave frequency spectrum. A period is an 
> > > interval of time, or the time-period of an oscillation. The phrase 
> > > "wave_period_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave period, describes the period of the most energetic waves within a 
> > > given sub-domain of the wave spectrum.
> > > 
> > > sea_surface_secondary_swell_wave_period_at_variance_spectral_density
> > > _m
> > > aximum
> > > units: s
> > > The quantity with standard name 
> > > sea_surface_secondary_swell_wave_period_at_variance_spectral_density_maximum
> > >  is the period of the most energetic waves within the secondary swell 
> > > wave component of a sea. Swell waves are waves on the ocean surface and 
> > > are the low frequency portion of a bimodal wave frequency spectrum. The 
> > > secondary swell wave is the most energetic wave component in the low 
> > > frequency portion of a bimodal wave frequency spectrum. A period is an 
> > > interval of time, or the time-period of an oscillation. The phrase 
> > > "wave_period_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave period, describes the period of the most energetic waves within a 
> > > given sub-domain of the wave spectrum.
> > > 
> > > sea_surface_tertiary_swell_wave_period_at_variance_spectral_density_
> > > ma
> > > ximum
> > > units: s
> > > The quantity with standard name 
> > > sea_surface_tertiary_swell_wave_period_at_variance_spectral_density_maximum
> > >  is the period of the most energetic waves within the tertiary swell wave 
> > > component of a sea. Swell waves are waves on the ocean surface and are 
> > > the low frequency portion of a bimodal wave frequency spectrum. The 
> > > tertiary swell wave is the third most energetic wave component in the low 
> > > frequency portion of a bimodal wave frequency spectrum. A period is an 
> > > interval of time, or the time-period of an oscillation. The phrase 
> > > "wave_period_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave period, describes the period of the most energetic waves within a 
> > > given sub-domain of the wave spectrum.
> > > 
> > > 
> > > 
> > > 3.       Addition of energy_at_variance_spectral_density_maximum 
> > > parameter to existing 'wind_wave', 'primary_swell', 'secondary_swell' and 
> > > 'tertiary_swell' categories. This follows the existing standard for 
> > > 'sea_surface_wave_energy_at_variance_spectral_density_maximum' and adds:
> > > 
> > > sea_surface_wind_wave_energy_at_variance_spectral_density_maximum
> > > units: m2s
> > > The quantity with standard name 
> > > sea_surface_wind_wave_energy_at_variance_spectral_density_maximum is the 
> > > energy of the most energetic waves within the wind wave component of a 
> > > sea. Wind waves are waves on the ocean surface and are the high frequency 
> > > portion of a bimodal wave frequency spectrum. The phrase 
> > > "wave_energy_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave energy, describes the maximum value of the 
> > > wave_variance_spectral_density within a given sub-domain of the wave 
> > > spectrum.
> > > 
> > > sea_surface_primary_swell_wave_energy_at_variance_spectral_density_m
> > > ax
> > > imum
> > > units: m2s
> > > The quantity with standard name 
> > > sea_surface_primary_swell_wave_energy_at_variance_spectral_density_maximum
> > >  is the energy of the most energetic waves within the primary swell wave 
> > > component of a sea. Swell waves are waves on the ocean surface and are 
> > > the low frequency portion of a bimodal wave frequency spectrum. The 
> > > primary swell wave is the most energetic wave component in the low 
> > > frequency portion of a bimodal wave frequency spectrum. The phrase 
> > > "wave_energy_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave energy, describes the maximum value of the 
> > > wave_variance_spectral_density within a given sub-domain of the wave 
> > > spectrum.
> > > 
> > > sea_surface_secondary_swell_wave_energy_at_variance_spectral_density
> > > _m
> > > aximum
> > > units: m2s
> > > The quantity with standard name 
> > > sea_surface_primary_swell_wave_energy_at_variance_spectral_density_maximum
> > >  is the energy of the most energetic waves within the secondary swell 
> > > wave component of a sea. Swell waves are waves on the ocean surface and 
> > > are the low frequency portion of a bimodal wave frequency spectrum. The 
> > > secondary swell wave is the second most energetic wave component in the 
> > > low frequency portion of a bimodal wave frequency spectrum. The phrase 
> > > "wave_energy_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave energy, describes the maximum value of the 
> > > wave_variance_spectral_density within a given sub-domain of the wave 
> > > spectrum.
> > > 
> > > sea_surface_tertiary_swell_wave_energy_at_variance_spectral_density_
> > > ma
> > > ximum
> > > units: m2s
> > > The quantity with standard name 
> > > sea_surface_tertiary_swell_wave_energy_at_variance_spectral_density_maximum
> > >  is the energy of the most energetic waves within the tertiary swell wave 
> > > component of a sea. Swell waves are waves on the ocean surface and are 
> > > the low frequency portion of a bimodal wave frequency spectrum. The 
> > > tertiary swell wave is the third most energetic wave component in the low 
> > > frequency portion of a bimodal wave frequency spectrum. The phrase 
> > > "wave_energy_at_variance_spectral_density_maximum", sometimes called peak 
> > > wave energy, describes the maximum value of the 
> > > wave_variance_spectral_density within a given sub-domain of the wave 
> > > spectrum.
> > > 
> > > 
> > > 
> > > 4.       And finally... Addition of 'directional_spreading' parameter to 
> > > 'sea_surface_wave', 'wind_wave', 'primary_swell', 'secondary_swell' and 
> > > 'tertiary_swell' categories. Giving the additional parameters:
> > > 
> > > sea_surface_wave_directional_spread
> > > units: degree
> > > Directional spread is the (one-sided) directional width of the wave 
> > > directional spectrum, S(t,x,y,f,theta) where t is time, x and y are 
> > > horizontal coordinates (such as longitude and latitude), f is frequency 
> > > and theta is direction.
> > > 
> > > sea_surface_wind_wave_directional_spread
> > > units: degree
> > > The quantity with standard name sea_surface_wind_wave_directional_spread 
> > > is the directional width of the wind wave component of a sea. Wind waves 
> > > are waves on the ocean surface and are the high frequency portion of a 
> > > bimodal wave frequency spectrum. The phrase "wave_directional_spread" 
> > > describes is the (one-sided) directional width within a given sub-domain 
> > > of the wave directional spectrum, S(t,x,y,f,theta) where t is time, x and 
> > > y are horizontal coordinates (such as longitude and latitude), f is 
> > > frequency and theta is direction .
> > > 
> > > sea_surface_primary_swell_wave_directional_spread
> > > units: degree
> > > The quantity with standard name 
> > > sea_surface_primary_swell_wave_directional_spread is the directional 
> > > width of the primary swell wave component of a sea. Swell waves are waves 
> > > on the ocean surface and are the low frequency portion of a bimodal wave 
> > > frequency spectrum. The primary swell wave is the most energetic wave 
> > > component in the low frequency portion of a bimodal wave frequency 
> > > spectrum. The phrase "wave_directional_spread" describes is the 
> > > (one-sided) directional width within a given sub-domain of the wave 
> > > directional spectrum, S(t,x,y,f,theta) where t is time, x and y are 
> > > horizontal coordinates (such as longitude and latitude), f is frequency 
> > > and theta is direction .
> > > 
> > > sea_surface_secondary_swell_wave_directional_spread
> > > units: degree
> > > The quantity with standard name 
> > > sea_surface_secondary_swell_wave_directional_spread is the directional 
> > > width of the secondary swell wave component of a sea. Swell waves are 
> > > waves on the ocean surface and are the low frequency portion of a bimodal 
> > > wave frequency spectrum. The secondary swell wave is the second most 
> > > energetic wave component in the low frequency portion of a bimodal wave 
> > > frequency spectrum. The phrase "wave_directional_spread" describes is the 
> > > (one-sided) directional width within a given sub-domain of the wave 
> > > directional spectrum, S(t,x,y,f,theta) where t is time, x and y are 
> > > horizontal coordinates (such as longitude and latitude), f is frequency 
> > > and theta is direction .
> > > 
> > > sea_surface_tertiary_swell_wave_directional_spread
> > > units: degree
> > > The quantity with standard name 
> > > sea_surface_secondary_swell_wave_directional_spread is the directional 
> > > width of the tertiary swell wave component of a sea. Swell waves are 
> > > waves on the ocean surface and are the low frequency portion of a bimodal 
> > > wave frequency spectrum. The tertiary swell wave is the third most 
> > > energetic wave component in the low frequency portion of a bimodal wave 
> > > frequency spectrum. The phrase "wave_directional_spread" describes is the 
> > > (one-sided) directional width within a given sub-domain of the wave 
> > > directional spectrum, S(t,x,y,f,theta) where t is time, x and y are 
> > > horizontal coordinates (such as longitude and latitude), f is frequency 
> > > and theta is direction .
> > > 
> > > 
> > > Phew!
> > > Many thanks
> > > Andy
> > > 
> > > Andy Saulter
> > > Surge, Waves and Metocean Projects Manager Met Office  FitzRoy Road 
> > > Exeter  Devon EX1 3PB
> > > Tel: +44 (0)1392 884703  Fax: +44 (0)1392 885681 
> > > [email protected]<mailto:[email protected].
> > > uk
> > > > http://www.metoffice.gov.uk
> > > 
> > 
> > > _______________________________________________
> > > CF-metadata mailing list
> > > [email protected]
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> > 
> > 
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