Dear Andy, Roy and Jonathan,

I have reviewed these proposals for new sea surface wave names. Thanks once 
again for a clear and useful discussion. Consensus was reached in May, so the 
following 16 new names are accepted for publication in the standard name table:

sea_surface_tertiary_swell_wave_from_direction (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 (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 swell 
wave. 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 (m)
'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. Significant wave height is a statistic computed from wave 
measurements and corresponds to the mean 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.'

sea_surface_wind_wave_period_at_variance_spectral_density_maximum (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. Wave period is the interval of time between repeated features 
on the waveform such as crests, troughs or upward passes through the mean 
level. 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_maximum (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 swell wave. 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. 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_maximum (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 second 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. 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_maximum (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 swell wave. 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. 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_wind_wave_energy_at_variance_spectral_density_maximum (m2 s)
'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_maximum (m2 
s)
'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 swell wave. 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_maximum 
(m2 s)
'The quantity with standard name 
sea_surface_secondary_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 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_maximum (m2 
s)
'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 swell wave. 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_wave_directional_spread (degree)
'Directional spread 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. 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.'

sea_surface_wind_wave_directional_spread (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. Directional spread 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. 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.'

sea_surface_primary_swell_wave_directional_spread (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 swell wave. Directional spread 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. 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.'

sea_surface_secondary_swell_wave_directional_spread (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 in the low frequency 
portion of a bimodal wave frequency spectrum. Directional spread 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. 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.'

sea_surface_tertiary_swell_wave_directional_spread (degree)
'The quantity with standard name 
sea_surface_tertiary_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 swell wave. Directional 
spread 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. 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.'

These names will be added in the August 6th update.

Best wishes,
Alison

------
Alison Pamment                                 Tel: +44 1235 778065
NCAS/Centre for Environmental Data Archival    Email: [email protected]
STFC Rutherford Appleton Laboratory     
R25, 2.22
Harwell Oxford, Didcot, OX11 0QX, U.K.

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