Correction to the datum/ellipsoid explanation below.

The NAD83 datum does use the GRS80 ellipsoid. The NAD27 datum uses the Clarke 
1866 ellipsoid. Woops!

Dave 

On Aug 3, 2011, at 9:07 AM, David Blodgett wrote:

> Dear Phil,
> 
>> I would have thought that if a particular piece of
>> data analysis is at a resolution that requires a geodetic datum to be
>> specified then,
> 
> The problem here is that there is no analysis that does not require this 
> information. While some choose to assume that all data uses the same datum 
> and drop those terms of analysis out of their math, that does not mean the 
> information is not there.
> 
>> giving the user the
>> opportunity to select the one s/he believes to be the most appropriate
>> for the task in hand.
> 
> 
> Having personally been in this situation, it took me two years to track down 
> exactly the right geographic transformation to apply to accurately apply 
> radar data to the landscape. It is unfair to expect that a terrestrial 
> modeler understand the handling of geographic data in climate and forecasting 
> applications to such an extent that they are comfortable making such a 
> decision.
> 
> Your argument about darwinian evolution of data use would cause a massive set 
> back in interdisciplinary science. This one minor inclusion of necessary 
> metadata would allow a broad community of users to more easily leverage data 
> using the climate and forecasting metadata conventions. Since the CF 
> community does disregard datum metadata, they could continue to silo 
> themselves from the rest of the environmental modeling community. Or, they 
> could extend a bit of an olive branch and recognize that this information is 
> critical and required for most terrestrial applications that consume 
> atmospheric data.
> 
> Regarding the difference between GRS 80 and WGS 84 ellipsoids, they are 
> different by small fractions of a meter. 
>> From wikipedia: The very small difference in the flattening thus results in 
>> a—very theoretical—difference of 0.105 mm in the semi polar axis. For most 
>> purposes, the differing polar axes can be merged to 6 356 752.3 m, with the 
>> inverse flattening rounded to 298.257.
> 
> 
> You are referring to the NAD83 Datum which uses the Clarke 1866 ellipsoid 
> which does fit the continental united states better than the GRS80/WGS84 
> ellipsoid. 
> 
> Cheers,
> 
> Dave B
> 
> On Aug 3, 2011, at 8:48 AM, Bentley, Philip wrote:
> 
>> Dear Heiko,
>> 
>>> I hope CF could define a default datum, e.g. the GRS1980 
>>> Authalic Sphere, since this matches most closely with 
>>> existing software (netcdf-java). This would make live easier 
>>> for the software-developers who have to use something if 
>>> nothing is given.
>> 
>> I'm not sure that defining a default datum for CF is the right way to go
>> in this instance. I would have thought that if a particular piece of
>> data analysis is at a resolution that requires a geodetic datum to be
>> specified then, in absentia the actual one being defined in metadata,
>> it's not clear to me that using some semi-arbitrary, and potentially
>> invalid, default datum is any better than giving the user the
>> opportunity to select the one s/he believes to be the most appropriate
>> for the task in hand.
>> 
>> The current CF conventions include a (fairly minimal) set of metadata
>> attributes which can be used to describe the basic properties of the
>> coordinate reference system associated with a given dataset. The onus
>> then is on data producers to utilise those metadata attributes to
>> describe their data to the fullest extent possible. Furthermore, other
>> non-CF attributes may be used to augment the standard set - over time
>> some of these additional attributes would no doubt find their way into
>> the CF specification.
>> 
>> Ultimately, if end-users consider that a given dataset has insufficient
>> metadata to justify its use within a particular context, then they can
>> always choose to ignore that dataset. With the passage of time - and in
>> true Darwinian fashion - such datasets (and their producers) will find
>> that they are increasingly disregarded/overlooked in analyses. Hopefully
>> this would galvanise such data producers into improving the quality of
>> their spatial metadata!
>> 
>> Regards,
>> Phil
>> 
>> 
>> PS: if a default datum were to be encoded into the CF conventions, I'd
>> imagine that the WGS84 datum would be the way to go rather than GRS80
>> which, if I understand correctly, has somewhat more of a bias towards
>> use over the North American continent. That said, I suspect the
>> differences between the 2 datums are sufficiently small as to get lost
>> in the underflow for many metocean research applications.
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