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M25 Speed cameras
Tom Anderson wrote:
Anyway, my proposal is for *all* heights to be measured as distance from the centre of mass of the earth. SOLVED! Why not measure heights from the centre of mass of the earth-moon system? That would abolish the need for tide tables because the tide would be at a fixed height... although the land would go up and down. ;-) |
M25 Speed cameras
On Thu, Feb 14, 2008 at 12:13:05PM -0000, John Rowland wrote:
Have you downloaded the latest software? My latest download introduced an option under "Safety preferences" to choose a sound for when you go over the speed limit. I've never actually tried it, though. Oh, cool, didn't know about that - thanks! -- David Cantrell | Nth greatest programmer in the world Irregular English: you have anecdotes; they have data; I have proof |
M25 Speed cameras
On Fri, 15 Feb 2008 00:56:55 +0000, Tom Anderson wrote:
On Thu, 14 Feb 2008, R.C. Payne wrote: Tom Anderson wrote: On Wed, 13 Feb 2008, Tom Anderson wrote: On Wed, 13 Feb 2008, Old Central wrote: IIRC the use of GPS to determine heights is a complex topic. You need to determine the spheroid and geoid separation in relation to the grid used and so on. Remember that many countires use by the different versions of these for their mapping and with different origins. If you want to know the height above local sea level, then yes, you need a map of the geoid. But nobody uses that. In the UK, we use height above the OSGB36 datum, Hang on, no, that's rubbish. We do use the local sea level, aka Ordnance Datum Newlyn. Well whenever I am using GPS these days [1], I can find my altitude by reference to my watch and a copy of Reed's Almanac. And that leads me to the question, what sea level are you taking? Certainly most charts I've found (Admiralty and Imray) use LAT [2] as their datum for points below MHWS [3], and MHWS for heights on dry land. Really? I know about LAT, but i'm surprised to hear that land heights are measured from MHWS. OS maps use the Newlyn datum, which is the mean sea level at Newlyn back in 1915 or something; that's carried through the country by levelling, so the datum is an gravitational isopotential surface. MHWS is not only a high, not mean, tide, but is something that's affected by local seabed topography, and so is not an isopotential surface. That means it won't be parallel to the Newlyn datum, so not only will Admiralty heights be different to OS heights, but the difference will vary across the country! Horses for courses, though. Nautical charts use LAT as a datum because depths are there so you can work out if you're going to run aground and that lets them have tide values which are always positive. Plus, it means that when you see a blue bit on a chart, you know it's always underwater. You couldn't use LAT for land heights, because it's not defined on land. I suppose they use MHWS on land because it has a similar property - anything with a positive height is always above water. Hang on, how do they determine MHWS on land? Are you sure they don't use ODN? It irks me that the Newlyn datum is a mean sea level, and not LAT. But then i suppose it's natural to define an isopotential surface that way, because it's the sea level you'd have if you got rid of the moon. Except it's not, because of topographic effects. I think. In conclusion, geomatics is hard. Anyway, my proposal is for *all* heights to be measured as distance from the centre of mass of the earth. SOLVED! The thing to appreicaite is that the purpose of a chart is not to record what the sea is like, it is a tool to allow you to sail around on it safely. By charting depths below LAT, you are in the position that if you navigated entirely ignoring tides, only considering your draught and the chart depth, you will not run aground. If you consider what a mariner might want heigts above MHWS for, there are only two uses: air draught under bridges and power lines, or using the hieght of something to determine distance (eg dipping lights). For air draught, if you apply the same principel as with depths, if you ignore tides, only consider your mast height and the charted clearance, you will be OK with a height above MHWS. Robin PS I've never come across HAT, as the opposite of LAT. Both MHWS and MLWS are talked about, as well as MHWN and MLWN. |
M25 Speed cameras
In uk.transport.london message ,
Fri, 15 Feb 2008 01:33:44, John Rowland n.co.uk posted: Tom Anderson wrote: Anyway, my proposal is for *all* heights to be measured as distance from the centre of mass of the earth. SOLVED! Why not measure heights from the centre of mass of the earth-moon system? That would abolish the need for tide tables because the tide would be at a fixed height... although the land would go up and down. Earth radius 4000 miles, Moon distance 240000 miles. Ratio of masses 81. The barycentre is therefore 3000 miles from the Earth's centre, 1000 miles down. So you're suggesting a tidal range of 6000 miles from high to low. -- (c) John Stockton, nr London, UK. Turnpike v6.05 IE 6. Web URL:http://www.merlyn.demon.co.uk/ - FAQish topics, acronyms, & links. I find MiniTrue useful for viewing/searching/altering files, at a DOS prompt; free, DOS/Win/UNIX, URL:http://www.idiotsdelight.net/minitrue/ unsupported. |
M25 Speed cameras
On Fri, 15 Feb 2008, John Rowland wrote:
Tom Anderson wrote: Anyway, my proposal is for *all* heights to be measured as distance from the centre of mass of the earth. SOLVED! Why not measure heights from the centre of mass of the earth-moon system? That would abolish the need for tide tables because the tide would be at a fixed height... SPLENDID IDEA. although the land would go up and down. A minor detail. A slightly bigger 'although' is that it wouldn't work - sea level isn't just a constant distance from the earth-moon barycentre. If it was, there'd only be one tide a day, wouldn't there? tom -- natural disasters, unexplained phenomena, chaos, chance, tattooing, |
M25 Speed cameras
In uk.transport.london message Pine.LNX.4.64.0802150035150.18870@urchin
..earth.li, Fri, 15 Feb 2008 00:39:03, Tom Anderson posted: Am i right in thinking that you couldn't calculate height if the satellites were all equidistant from you? Yes, if they are co-planar; not, I think, otherwise. But then you wouldn't be able to calculate position at all. No. For example, if more than two satellites are equidistant from you and randomly placed the surface of a sphere, then you must be at the centre of the sphere. Is there a configuration where you can get a fix in XY but not Z? S1 .. S2 ___________________TA______________ - You X - If the satellites are co-planar, you cannot determine the sign of your height measured from that plane; and if you are either very near to or very far from that plane your height measurement becomes inaccurate. In terrestrial use : At sea, the altitude is already known to within a few metres. On land, the altitude is already known to within about +-5km. In the air, the altitude is already known to within about +-15km. In those cases, the usable satellites are always above a horizontal plane through the receiver. AIUI, commercially-available GPS receivers will refuse to give an answer if above some specific altitude; that is to annoy D-I-Y ICBM makers. There could also be a speed limit. -- (c) John Stockton, nr London, UK. Turnpike v6.05 MIME. Web URL:http://www.merlyn.demon.co.uk/ - FAQish topics, acronyms, & links. Proper = 4-line sig. separator as above, a line exactly "-- " (SonOfRFC1036) Do not Mail News to me. Before a reply, quote with "" or " " (SonOfRFC1036) |
M25 Speed cameras
On Fri, 15 Feb 2008, R.C. Payne wrote:
On Fri, 15 Feb 2008 00:56:55 +0000, Tom Anderson wrote: On Thu, 14 Feb 2008, R.C. Payne wrote: Tom Anderson wrote: On Wed, 13 Feb 2008, Tom Anderson wrote: On Wed, 13 Feb 2008, Old Central wrote: IIRC the use of GPS to determine heights is a complex topic. You need to determine the spheroid and geoid separation in relation to the grid used and so on. Remember that many countires use by the different versions of these for their mapping and with different origins. If you want to know the height above local sea level, then yes, you need a map of the geoid. But nobody uses that. In the UK, we use height above the OSGB36 datum, Hang on, no, that's rubbish. We do use the local sea level, aka Ordnance Datum Newlyn. Well whenever I am using GPS these days [1], I can find my altitude by reference to my watch and a copy of Reed's Almanac. And that leads me to the question, what sea level are you taking? Certainly most charts I've found (Admiralty and Imray) use LAT [2] as their datum for points below MHWS [3], and MHWS for heights on dry land. Really? I know about LAT, but i'm surprised to hear that land heights are measured from MHWS. OS maps use the Newlyn datum, which is the mean sea level at Newlyn back in 1915 or something; that's carried through the country by levelling, so the datum is an gravitational isopotential surface. MHWS is not only a high, not mean, tide, but is something that's affected by local seabed topography, and so is not an isopotential surface. That means it won't be parallel to the Newlyn datum, so not only will Admiralty heights be different to OS heights, but the difference will vary across the country! Horses for courses, though. Nautical charts use LAT as a datum because depths are there so you can work out if you're going to run aground and that lets them have tide values which are always positive. Plus, it means that when you see a blue bit on a chart, you know it's always underwater. You couldn't use LAT for land heights, because it's not defined on land. I suppose they use MHWS on land because it has a similar property - anything with a positive height is always above water. If you consider what a mariner might want heigts above MHWS for, there are only two uses: air draught under bridges and power lines, or using the hieght of something to determine distance (eg dipping lights). For air draught, if you apply the same principel as with depths, if you ignore tides, only consider your mast height and the charted clearance, you will be OK with a height above MHWS. I didn't think of air draft, but that makes a lot of sense. For heights for sighting, though, you really want height above LAT, so you can work out the height difference between you and the object by subtracting the current tide height from its height. With MHWS, you need to know the local value for MHWS as well, although i suppose this is in your tide tables anyway. There's still an issue with deciding what MHWS is inland; do they just use MHWS at the nearest point on the coast, or the nearest standard port or something? Do they indicate which MHWS heights are measured relative to? Do they pick one reference MHWS for each chart, and indicate it in the margin? Looking at an Imray chart, i can't see any indication of how MHWS is defined. For sighting, really you want GPS-style purely geometric coordinates, as local variations in gravity and topography, as affect ODN and LAT/MHWS heights, don't come in to sighting. The more i think about it, the more all this annoys me. Okay, how about a single datum that's based on finding the lowest LAT around the British Isles, and carrying that height elsewhere via levelling? You get an isopotential, geoid-based datum, like ODN, but with the nautical advantages of LAT. It would be more conservative than LAT, though, as the datum would be below actual LAT in most places (i don't know how much by). But then, chart datum is only approximately LAT anyway, and this would mean that tidal heights would still be positive. PS I've never come across HAT, as the opposite of LAT. Both MHWS and MLWS are talked about, as well as MHWN and MLWN. Ditto. The argument for using MHWS for air drafts is really an argument for using HAT. Aha! It seems this is exactly what the UKHO are now doing - see the last item he http://easytide.ukho.gov.uk/Easytide...pport/faq.aspx tom -- natural disasters, unexplained phenomena, chaos, chance, tattooing, |
M25 Speed cameras
In article ,
John Rowland wrote: Tom Anderson wrote: Anyway, my proposal is for *all* heights to be measured as distance from the centre of mass of the earth. SOLVED! Why not measure heights from the centre of mass of the earth-moon system? That would abolish the need for tide tables because the tide would be at a fixed height... although the land would go up and down. Notice the way in which the sea stays steady as a rock whilst the buildings keep washing up and down. Nick -- Serendipity: http://www.leverton.org/blosxom (last update 4th February 2008) "The Internet, a sort of ersatz counterfeit of real life" -- Janet Street-Porter, BBC2, 19th March 1996 |
M25 Speed cameras
On Thu, Feb 14, 2008 at 12:13:05PM -0000, John Rowland wrote:
David Cantrell wrote: I use Tomtom on a Palm Treo 680. Mine turns the speed display from white to red when I exceed it (possibly when I exceed it by a certain amount, not sure). Trouble is, it's *far* too small to even see what colour the text is without taking my eyes off the road for longer than I want to. I've not found any way of getting an audible warning out of it. Have you downloaded the latest software? My latest download introduced an option under "Safety preferences" to choose a sound for when you go over the speed limit. I've never actually tried it, though. The self-update thingy seems to think that I do indeed have the latest version. No such option though. -- David Cantrell | Enforcer, South London Linguistic Massive Featu an incorrectly implemented bug |
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