Hello Karl,
There have been extensive debates in the observational oceanographic community 
on the concept of 'sea surface temperature' - much of it on this list led by 
Craig Donlan - that resulted in the addition of 
sea_surface_foundation_temperature, sea_surface_skin_temperature and 
sea_surface_subskin_temperature in 2008, giving four SST Standard Names, not 
three. If you dig back into the archives you'll find the case was very strongly 
argued and for that reason alone I would counsel against deprecating 
sea_surface_skin_temperature.
I totally agree that sea_surface_temperature is an imprecise term which is why 
Craig's community argued so strongly for its augmentation, but I'm pretty sure 
that the scope of their considerations was open water and not water under sea 
ice. Whilst I agree that surface_temperature and sea_surface_skin_temperature 
should theoretically be numerically equal to my (observationally-biased) 
viewpoint the former is a measurement in the atmosphere (based on the CF 
definition of surface) whilst the latter is a measurement in the water column. 
Again, I would counsel against deprecating sea_surface_skin_temperature.
As regards land skin temperature I really don't have any experience in that 
domain, but my feelings are that labelling a measurement of terra firma as the 
temperature of the lower boundary of the atmosphere is pushing implied 
semantics too far. Consequently, I would support the new Standard Name.
Cheers, Roy.
Please note that I now work part-time from Tuesday to Thursday.  E-mail 
response on other days is possible but not guaranteed!

From: CF-metadata [mailto:cf-metadata-boun...@cgd.ucar.edu] On Behalf Of Karl 
Taylor
Sent: 19 June 2013 21:44
To: cf-metadata@cgd.ucar.edu
Subject: Re: [CF-metadata] new standard name: land_surface_skin_temperature

Dear all,

I think for any conceivable purposes land_surface_skin_temperature is identical 
to surface_temperature.  If not, the definition should explain how they differ. 
  Is there really an important difference between the temperature 
representative of the top few micrometers and the temperature of the top few 
molecules of the surface?  I know in models there isn't.   Also, over land 
presumably some sensors are inferring this temperature from radiation emitted 
by some combination of both vegetation and bare ground.   "upper boundary of 
the land" sounds like bare ground to me, so maybe this should be clarified.

Rather than define land_surface_skin_temperature to maintain consistency with 
sea_surface_skin_temperature, I would prefer to deprecate 
sea_surface_skin_temperature in favor of surface_temperature.   As Jonathon G. 
recalled, there was some rather extensive discussion about 
sea_surface_skin_temperature when it was proposed, which should be reviewed 
before deciding to deprecate.  [I can't remember it, and I don't think I 
participated in that earlier discussion, but I can't see a need for 
skin_temperature.]

Reading over the 3 standard names relevant to SST (surface_temperature, 
sea_surface_temperature, sea_surface_skin_temperature) here are some comments:

For *models*:  In ice-free regions all three quantities are identical.  In 
sea-ice-covered (or partially sea-ice-covered) regions only 
sea_surface_skin_temperature and sea_surface_temperature are identical 
(although one might argue that sea_surface_skin_temperature should not be 
defined under sea ice because longwave radiative fluxes are normally neglected 
between the sea ice and ocean below.)  Globally all three are the same if 
cell_method="area: mean where ice_free_sea".

For *observations*:  There is a difference between sea_surface_skin_temperature 
and sea_surface_temperature.  In addition sea_surface_temperature is imprecise 
because it depends on the measuring device (e.g., ship intake temp., bucket 
temp. ).  In ice-free regions sea_surface_skin_temperature should be nearly 
identical to surface_temperature (How big can the difference be between a 
weighted average of temperature over the top 10-20 micrometers of the ocean and 
the temperature of the top few molecules of the ocean??).  One might argue that 
sea_surface_skin_temperature should not be defined under sea ice because the 
radiometers used to measure it would not normally penetrate the sea-ice.  If 
so, then surface_temperature with a cell_method="area: mean where ice_free_sea" 
 would be the same as "sea_surface_skin_temperature" and they both would 
undefined under sea ice.  They would, of course, differ from 
sea_surface_temperature.

My conclusion is that sea_surface_skin_temperature is not needed and should be 
deprecated and for similar reasons land_surface_skin_temperature should not be 
added.  We need to retain both sea_surface_temperature and surface_temperature.

best regards,
Karl
On 6/19/13 8:32 AM, Jonathan Wrotny wrote:
Dear Jonathan G and John G,

Thanks to both of you for your replies to the questions on land surface skin 
temperature.  I do agree with Jonathan G's points and see how the land surface 
temperature is likely very similar in value to the surface (interface) 
temperature, but my opinion is that for consistency of names within the CF and 
to alleviate general confusion (e.g. the inevitable questions of why there is 
not a land surface skin temperature when there is one for the sea surface), its 
seems useful to add a standard name for land_surface_skin_temperature.  I think 
having the analogue to the sea surface quantity is complementary.  I realized, 
however, that my initial definition of land surface skin temperature was a 
little too specific in attempting to quantify the depth of the skin layer.  My 
general impression is that the depth of the land skin layer is more variable 
and not as well quantified as the depth of the sea surface skin.  Thus, I 
generalized the definition to emphasize that the skin temperature is a 
radiometric quantity and removed the reference to the skin depth.  Here is my 
current proposal:

Standard Name:  land_surface_skin_temperature


Definition:  The land surface skin temperature is the aggregate temperature of 
the "skin" of the land surface, where the "skin" is the upper boundary of the 
land which emits infrared radiation directly to space through the atmosphere.


Canonical Units:  K

Any comments are appreciated.

Sincerely,

Jonathan Wrotny

On 6/17/2013 10:17 AM, John Graybeal wrote:

As I understand it, the reason for the introduction of the skin temperature 
(and other sea surface temperatures) is that originally sea_surface_temperature 
encompassed everything (in its 100 years of use) from a bucket somewhere in the 
first 10 meters, to a satellite measuring the first few millimeters. More 
precise names were needed.



I expect a similar situation applies on land. Even if past practice may only 
penetrate the service 10 centimeters, that's noticeably different than a 
satellite measuring a few millimeters.  If that's at all true, having the 
refined term makes sense to me.



John



On Jun 17, 2013, at 05:41, Jonathan Gregory 
<j.m.greg...@reading.ac.uk><mailto:j.m.greg...@reading.ac.uk> wrote:



Dear Jonathan and Jim



In my previous email, I was trying to explain why an interface temperature

is a physical meaningful concept, which Jonathan asked about. This is actually

an applicable concept in models, as I said, and it is the idea which I (at

least) had in mind when the name was put in the standard name table. Like CF

in general, the standard name table was originally created for the purpose of

model metadata, and was later to extended to observations. This quantity is an

idealisation, not an observable quantity.



The heat capacity of a layer 12 micrometers thick is so small that I suppose

there is practically no difference between the skin temperature and the

interface temperature, on the timescales you're interested in. Is that correct,

do you think? If so, it seems to me that it would be fine to use the existing

name of surface_temperature for this quantity. You propose the new name on the

analogy of the sea_surface_skin_temperature. The same argument would apply to

that as well. I can't remember the reason why it was thought necessary to make

a distinction between surface_temperature and sea_surface_skin_temperature,

though I do recall quite a lot of discussion about it.



It is also fine to introduce land_surface_skin_temperature as well, I would

say. The data-writer has a choice. They could use surface_temperature if that

is accurate enough, but if they wish to be more precise about what material

layer it applies to, the skin temperature names could be used.



Best wishes



Jonathan



13/06/17 13:20:03 house

On Fri, Jun 14, 2013 at 02:45:28PM -0400, Jonathan Wrotny wrote:

Date: Fri, 14 Jun 2013 14:45:28 -0400

From: Jonathan Wrotny <jwro...@aer.com><mailto:jwro...@aer.com>

User-Agent: Mozilla/5.0 (Windows NT 5.1; rv:17.0) Gecko/20130509

Thunderbird/17.0.6

To: Jim Biard <jim.bi...@noaa.gov><mailto:jim.bi...@noaa.gov>

CC: "cf-metadata@cgd.ucar.edu List"<mailto:cf-metad...@cgd.ucar.eduList> 
<cf-metadata@cgd.ucar.edu><mailto:cf-metadata@cgd.ucar.edu>

Subject: Re: [CF-metadata] new standard name: land_surface_skin_temperature



Dear Jim,



Thanks for your comments.  They all make sense to me and I'm on

board with your suggested definition.  I'll just wait for others to

comment, if needed, then we can converge on a final definition.

Sincerely,



Jonathan



On 6/14/2013 2:11 PM, Jim Biard wrote:

Jonathan,



I still don't believe that the surface temperature concept that

Jonathan Gregory has ever been what people were intending when

they make the surface_temperature standard name, but I'll abide by

whatever folks decide.



On a different front, I don't think the definition of the standard

name should include statements about technology used (measured by

an infrared radiometer?).  The definition should speak only to the

measured quantity, without reference to the way in which you

happen to be measuring it.  Likewise, there is no need for the

statement regarding variability of the quantity.  Also, the

surface in this name is not the lower boundary of the atmosphere.

It is the upper boundary of the land.  An non-volatile object in a

hard vacuum has a surface skin temperature.



Given all that, I'd suggest this for your definition:



Standard Name: land_surface_skin_temperature



Definition: The land surface skin temperature is the aggregate

temperature of the "skin" of the land surface, which extends

vertically approximately 12 micrometers below the land surface.



If people really think it needs to be spelled out even further,

add the sentence "The land surface is the upper boundary of the

land."



Grace and peace,



Jim



Jim Biard

Research Scholar

Cooperative Institute for Climate and Satellites 
<http://www.cicsnc.org/><http://www.cicsnc.org/>

Remote Sensing and Applications Division

National Climatic Data Center 
<http://www.ncdc.noaa.gov/><http://www.ncdc.noaa.gov/>

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On Jun 14, 2013, at 1:54 PM, Jonathan Wrotny 
<jwro...@aer.com<mailto:jwro...@aer.com>

<mailto:jwro...@aer.com><mailto:jwro...@aer.com>> wrote:



Dear Jonathan Gregory,



Thanks for your reply...this certainly helps to clear things up

for me.  I now better understand the meaning of the

"surface_temperature" standard name with the temperature defined

by heat fluxes at an interface, and not based on an actual

medium.



This also makes it obvious to me that my proposed standard name

"land_surface_skin_temperature" does not currently exist within

CF and could serve as an analogue to

"sea_surface_skin_temperature."  To summarize, here is my

current proposal:



Standard Name:   land_surface_skin_temperature



Definition:The surface called "surface" means the lower boundary

of the atmosphere. The land surface skin temperature is the

temperature measured by an infrared radiometer, but measurements

from microwave radiometers operating at GHz wavelengths also

exist. It represents the aggregate temperature of the skin

surface where ?skin? means the surface medium viewed by a sensor

to a vertical depth of approximately 12 micrometers.



Measurements of this quantity are subject to a large potential

diurnal cycle which is primarily due to the balance between

heating during the day by solar radiation and continual cooling

from terrestrial (long-wave) radiation emitted by the skin

surface.



Canonical Units:K





Sincerely,



Jonathan Wrotny



On 6/14/2013 1:22 PM, Jonathan Gregory wrote:

Dear Jonathan



I defer to Roy about the various sea water temperature names.



It is physically meaningful to have a temperature which doesn't relate to any

material layer. If there is no matter associated with it, it must have zero

heat capacity, so the temperature is determined by requiring an exact balance

of heat fluxes. For this to be possible, the heat fluxes concerned must depend

on the temperature, which of course they generally do. Obviously this is an

idealisation, but a surface interface temperature of this kind really can

exist in a model, although it's not an observational quantity. A model can

obtain such a temperature by solving simultaneously for the heat fluxes that

are balanced at the interface.



Best wishes



Jonathan G

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