- From: Thomson, Martin <Martin.Thomson@andrew.com>
- Date: Thu, 22 Apr 2010 09:00:44 +0800
- To: Steve Block <steveblock@google.com>, public-geolocation <public-geolocation@w3.org>
- Message-ID: <8B0A9FCBB9832F43971E38010638454F03E7D06C7D@SISPE7MB1.commscope.com>
Hi Steve, Some comments inline. > > I have a recommendation on x, y and z though. In this case, we do > have > > names. These should instead be labelled, East, North and Up. > OK, I'll add these names. Though I think we should keep the labels > x,y,z too. > > > I also have a problem with the use of magnetic north. I understand > the > > limitations of the measurement devices, but there are other ways of > defining > > cardinal directions that are more directly compatible with > geolocation. > Yes, you're right, we should use True North (the direction towards the > North Pole, which lies on the line of 90 latitude for the datum in > use) for the WGS84 datum (the datum used by Geolocation). Geolocation > uses True North as the reference for its heading property. That's great, thanks. > > Rather than defining "Up" to be the tangent to the gravipotential > surface, you can define up in terms of location (as a vector in > > WGS84 Cartesian coordinates): > I think that rather than defining up to be the direction of the vector > from the WGS84 origin as you suggest, I think it's more common to use > the direction perpendicular to the ground for these local coordinates. > Though we should clarify the spec to say that the ground should be > taken to be tangent to the local surface of the WGS84 spheroid. What I described wasn't the vector through the centre of the spheroid - it IS the vector tangential to the local surface. I have a brief description of this (PDF attached). > > The drawback is that in order to measure this you need to know the > relationship between magnetic north and these. Note also that > > magnetic north moves. You also need to know the relationship of the > gravipotential surface with East and North - the EGM (Earth > > Gravipotential Model) provides that. > Yes, it's true that these definitions require significant computation > to obtain the required values from the sensor data. Though we don't > require a particular level of accuracy and for many applications, the > obvious approximations (magnetic north == true north, gravity is > parallel to the Up axis) will suffice. It's not so much the computation, it's more the contextual information. The more recent high resolution EGM models are pretty large. Absolutely - I hate to suggest it, but the idea of a "magnetic" tag makes some sense. For those applications that care about the extra precision, it might be worth the additional bit (and increase of API surface area). > > Though I suspect that implementations will be forced to substitute > zero. > Why do you think this? Only that for those devices that lack the full 3 axis orientation, apps might exist that assume or require it. It's not a big deal. Let that be a decision for app makers to make. Using null seems the best approach. > >> > Would I be right in assuming that 0, 0, 0 orientation equates to a > device with the screen facing > >> > up and the top of the screen toward north? > >> Yes > > But you still have to assume this. An explicit statement might seem > a little redundant, but that small effort will pay you back. > The spec states that 'The transformation from the Earth frame to the > device frame is expressed in terms of 3 rotations', so at (0, 0, 0) > the frames are aligned by definition. It also says 'Starting with the > two frames aligned, the rotations are applied in the following > order:'. Can you suggest how you'd like to add further clarification? No, I missed that. It's good. > > Right hand rotation is well understood. Using that terminology would > be helpful. > OK, I'll add that terminology. Cheers, Martin > > Steve > > -- > Google UK Limited > Registered Office: Belgrave House, 76 Buckingham Palace Road, London > SW1W 9TQ > Registered in England Number: 3977902
Attachments
- application/pdf attachment: WhatsUp.pdf
Received on Thursday, 22 April 2010 01:04:31 UTC