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Re: Chris Little's comments on the BP - Issues 128 and 204

From: Frans Knibbe <frans.knibbe@geodan.nl>
Date: Fri, 18 Mar 2016 14:04:32 +0100
Message-ID: <CAFVDz40uPdGp=0dT6BFcM9otBVM9NxX6fp68R5i9eet6bgVN3A@mail.gmail.com>
To: Jon Blower <j.d.blower@reading.ac.uk>
Cc: SDW WG <public-sdw-wg@w3.org>
Hi Jon,

Would you be willing to try to formulate a use case from which the CRS
requirements follow? Or would it be possible to spot an existing use case
that could be elaborated a bit?

I think it is important to have a complete collection of requirements in
the UCR document, to help subsequent standardization efforts. It is
possible that some requirements can not be met, but there should at least
be awareness that they exist.

Regards,
Frans

2016-02-19 13:23 GMT+01:00 Jon Blower <j.d.blower@reading.ac.uk>:

> Hi Frans,
>
> (graceful handling of the 180º discontinuity). Do you think such a
> requirement should be included in the UCR document?
>
>
> Yes, possibly - it’s a tough question though that impacts on both data
> formats and APIs. It’s been a problem for a long time, but with no
> consistent solution identified.
>
> Polar science is another area where a cylindrical CRS is not ideal.
>>
>
> But CRS84 is not cylindrical?
>
>
> Sorry yes, you’re right. I meant that typically when we plot CRS84 we use
> an equidistant cylindrical projection (or Mercator), both of which are bad
> options for polar data. There is also an issue of interpreting polygons
> that go around the poles and the 180/-180 discontinuity. A polar projection
> of some kind would usually be a better option for recording coordinates
> (the NSIDC in the US has some useful resources on this I think).
>
> Cheers,
> Jon
>
>
>
> On 19 Feb 2016, at 12:00, Frans Knibbe <frans.knibbe@geodan.nl> wrote:
>
>
>
> 2016-02-18 9:20 GMT+01:00 Jon Blower <j.d.blower@reading.ac.uk>:
>
>> Hi Ed, Frans, all,
>>
>> [snip]
>>
>
>> One constant area of pain is the discontinuity at 180 degrees. Services
>> and software are very inconsistent about how they handle data that span
>> this discontinuity. Many people (particularly those interested in the
>> Pacific Ocean!) have expressed a need for a CRS where the discontinuity is
>> defined elsewhere (or one in which the longitude axis values are explicitly
>> allowed to “wrap”).
>>
>
> This is a remark I find interesting as a UCR editor, because it looks like
> a requirement for spatial data on the web (graceful handling of the 180º
> discontinuity). Do you think such a requirement should be included in the
> UCR document?
>
>>
>> Polar science is another area where a cylindrical CRS is not ideal.
>>
>
> But CRS84 is not cylindrical?
> Could polar science have specific requirements that should be recorded in
> the UCR document?
>
> Greetings,
> Frans
>
>
>
>>
>> Cheers,
>> Jon
>>
>>
>>
>>
>>
>> On 17 Feb 2016, at 14:44, Frans Knibbe <frans.knibbe@geodan.nl> wrote:
>>
>> Hello Ed,
>>
>> Basing requirements on what we observe on the web today could be risky.
>> I hope that with the Best Practices we can lay the foundations of a better,
>> more interoperable and more robust web in the future. Some things I think
>> we should consider in this case are:
>>
>>    - I believe the lack of a generally usable CRS impedes publication of
>>    professional geographical data. And there are other reasons why data
>>    providers need (our) best practices before publication of spatial data on
>>    the web becomes a viable option. So I think the 99% is a skewed proportion:
>>    Relatively simple, amateuristic data are easy to publish and use on
>>    the web nowadays. That could be the reason for seeing so much of it. For
>>    professional, serious data it is another matter.
>>    - Current provisioning of data in many cases may be on the web but is
>>    still monolithic in design: one database for one application. The idea of
>>    putting data on the web for everyone to use as they seem fit requires a
>>    higher level of data quality, among which is using a CRS that is not
>>    only usable for a specficic application.
>>    - Current provisioning of data on the web often does not consider
>>    durability of data. With an ever increasing coordinate error, using CRS84
>>    does not fit well with the idea of providing long lasting data.
>>    - A good generally usable CRS does not necessarily have to be
>>    something more complex than WGS84/CRS84. It could be something simpler.
>>
>> Regards,
>> Frans
>>
>> 2016-02-17 15:06 GMT+01:00 Ed Parsons <eparsons@google.com>:
>>
>>> No I disagree... For the vast majority of the current uses of spatial
>>> data on the web WGS84 is used without problem, as the GIS/Geospatial
>>> community we have still not accepted that we are the minority, the people
>>> with very specific use cases.. For 99% of the potential uses of spatial
>>> data on the web today WGS84 is fine.
>>>
>>> Ed
>>>
>>>
>>> On Wed, 17 Feb 2016 at 13:18 Frans Knibbe <frans.knibbe@geodan.nl>
>>> wrote:
>>>
>>>> Hello,
>>>>
>>>> About the phrase " For the majority of applications a common global
>>>> CRS (WGS84) is fine": If we say it like that, it seems we are saying
>>>> that it is OK to use WGS84 as a default CRS. I think that would be the
>>>> wrong message. I think it should be only used in some very specific cases:
>>>> in which spatial resolution is higher than meter level and data are usable
>>>> for a limited time. For other cases, WGS84 or CRS84 should not be
>>>> recommended. In my mind, a best practice would be to *not* use
>>>> WGS84/CRS84 *unless* you are certain the data have a sufficiently low
>>>> spatial resolution and temporal validity.
>>>>
>>>> I think a general good practice for data publishing is not to make too
>>>> many assumptions on how data will be used (applications). Some applications
>>>> will not be hurt by wrongfully using WGS84, but you can not be sure that
>>>> other types of data usage will not suffer.
>>>>
>>>> In sessions last week, I have seen examples of geomerty encodings that
>>>> were all wrong. In combination with CRS84 extremely high coordinate
>>>> precisions were used and no temporal metadata were present. Lots of
>>>> antipatterns!
>>>>
>>>> Regards,
>>>> Frans
>>>>
>>>>
>>>>
>>>> 2016-01-14 18:55 GMT+01:00 Jeremy Tandy <jeremy.tandy@gmail.com>:
>>>>
>>>>> Thanks Chris - I've incorporated your suggestions in the Editors Draft
>>>>> and added your comments to the respective issues.
>>>>>
>>>>> Jeremy
>>>>>
>>>>> On Thu, 14 Jan 2016 at 16:20 Little, Chris <
>>>>> chris.little@metoffice.gov.uk> wrote:
>>>>>
>>>>>> Jeremy,
>>>>>>
>>>>>>
>>>>>>
>>>>>> A little late for the BPFPWD, but some text to address issues 128 and
>>>>>> 204. In American English.
>>>>>>
>>>>>>
>>>>>>
>>>>>> Chris
>>>>>>
>>>>>>
>>>>>>
>>>>>> Why
>>>>>>
>>>>>> The choice of CRS is sensitive to the intended domain of application
>>>>>> for the geospatial data. For the majority of applications a common global
>>>>>> CRS (WGS84) is fine, but high precision applications (such as precision
>>>>>> agriculture, digging holes in roads and defence) require spatial
>>>>>> referencing to be accurate to a few meters or even centimeters.
>>>>>>
>>>>>> One aspect is the confusion of precision and accuracy. Seven decimal
>>>>>> places of a latitude degree corresponds to about one centimeter. Whatever
>>>>>> the precision of the specified coordinates, the accuracy of positioning on
>>>>>> the actual earth's surface using WGS84 will only approach about a metre
>>>>>> horizontally and may have apparent errors of up to 100 metres vertically,
>>>>>> because of assumptions about reference systems, tectonic plate movements
>>>>>> and which definition of the earth's 'surface' is used.
>>>>>>
>>>>>>
>>>>>>
>>>>>> Issue 128
>>>>>>
>>>>>> Add explanation of why there are so many CRSs.
>>>>>>
>>>>>> For example, North America and Europe are receding from each other by
>>>>>> a couple of centimeters per year, whereas Australia is moving several
>>>>>> centimeters per year north-eastwards. So, for better than one meter
>>>>>> accuracy in Europe, the European Terrestrial Reference System 1989 (ETRS89)
>>>>>> was devised and it is fixed with respect to the European tectonic plate.
>>>>>> Consequently, coordinates in the ETRS89 system will change by a couple of
>>>>>> centimetres per year with respect to WGS84.
>>>>>>
>>>>>>
>>>>>>
>>>>>> Issue 204
>>>>>>
>>>>>> Need to clarify when and why people use different CRS's
>>>>>>
>>>>>> Even if a CRS, tied to a tectonic plate, is used, local coordinates
>>>>>> in some areas may still change over time, if the plate is rotating with
>>>>>> respect to the rest of the earth. Many existing useful maps pre-date GPS
>>>>>> and WGS84 based mapping, so that location errors of tens of metres, or
>>>>>> more, may exist when compared to the same location derived from a different
>>>>>> technology, and these errors may vary in size across the extent of a single
>>>>>> map.
>>>>>>
>>>>>>
>>>>>>
>>>>>> Note
>>>>>>
>>>>>> The misuse of spatial data, because of confusion about the CRS, can
>>>>>> result in catastrophic results; e.g. both the bombing of the Chinese
>>>>>> Embassy in Belgrade during the Balkan conflict and fatal incidents along
>>>>>> the East Timor border are generally attributed to spatial referencing
>>>>>> problems.
>>>>>>
>>>>>> Intended Outcome
>>>>>>
>>>>>> A Coordinate Reference System (CRS) sensitive to the intended domain
>>>>>> of application (e.g. high precision applications) for the geospatial data
>>>>>> should be chosen.
>>>>>>
>>>>>>
>>>>>>
>>>>>>
>>>>>>
>>>>>
>>>> --
>>>
>>> *Ed Parsons*
>>> Geospatial Technologist, Google
>>>
>>> Google Voice +44 (0)20 7881 4501
>>> www.edparsons.com @edparsons
>>>
>>
>>
>>
>
>
Received on Friday, 18 March 2016 13:08:12 UTC

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