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Commuting time map
Dear All
I hope I've come to the right place to ask this question. I was commenting with a colleague recently how she (living in Sevenoaks) takes a similar amount of time as me (in Raynes Park) to get into work (we're based in Monument). It made me wonder if anyone has re-designed a London travel map in terms of time frame of reference - i.e. shortest time taken to get to a major London station (e.g. Waterloo, Victoria, London Bridge, Liverpool Street etc.) from around the south-east? Just interested from a commuting viewpoint. Regards Richard |
Commuting time map
Richard Dixon wrote:
Dear All I hope I've come to the right place to ask this question. I was commenting with a colleague recently how she (living in Sevenoaks) takes a similar amount of time as me (in Raynes Park) to get into work (we're based in Monument). It made me wonder if anyone has re-designed a London travel map in terms of time frame of reference - i.e. shortest time taken to get to a major London station (e.g. Waterloo, Victoria, London Bridge, Liverpool Street etc.) from around the south-east? Just interested from a commuting viewpoint. There is software available to companies involved in transport planning which can plot "isochrones" (contours of time) of public transport journey time to a specific point in London. Unfortunately I can't immediately see any available on the internet. -- Dave Arquati Imperial College, SW7 www.alwaystouchout.com - Transport projects in London |
Commuting time map
Dave Arquati wrote in
: There is software available to companies involved in transport planning which can plot "isochrones" (contours of time) of public transport journey time to a specific point in London. Unfortunately I can't immediately see any available on the internet. Thanks - if you are able to find anything then please report back - it's something I'd often wondered about and would have thought something would have been available ! Many thanks Richard |
Commuting time map
Richard Dixon wrote:
Dave Arquati wrote in : There is software available to companies involved in transport planning which can plot "isochrones" (contours of time) of public transport journey time to a specific point in London. Unfortunately I can't immediately see any available on the internet. Thanks - if you are able to find anything then please report back - it's something I'd often wondered about and would have thought something would have been available ! Unfortunately it's not openly available as those companies use the software to provide information to clients, e.g. when assessing an office relocation scheme, they can provide the client with maps showing which areas become closer temporally to the new location, and which become further away, plotting the change in journey time as a set of isochrones. It's pretty interesting stuff; I did have a paper version of one, but I'm not sure where I put it, otherwise I'd scan it in to show you. -- Dave Arquati Imperial College, SW7 www.alwaystouchout.com - Transport projects in London |
Commuting time map
On Mon, 21 Feb 2005 20:17:15 +0000, Dave Arquati wrote:
It's pretty interesting stuff; I did have a paper version of one, but I'm not sure where I put it, otherwise I'd scan it in to show you. You get strange bubbles in areas where express trains stop. Slough and Reading would be in the same isochrone for places in zone 1 for example, but Maidenhead and Twyford would be "higher". Of course time of day and mode of travel makes a difference too. -- Everything I write here is my personal opinion, and should not be taken as fact. |
Commuting time map
Richard Dixon wrote [...] I was commenting with a colleague recently how she (living in Sevenoaks) takes a similar amount of time as me (in Raynes Park) to get into work (we're based in Monument). It made me wonder if anyone has re-designed a London travel map in terms of time frame of reference - i.e. shortest time taken to get to a major London station (e.g. Waterloo, Victoria, London Bridge, Liverpool Street etc.) from around the south-east? Just interested from a commuting viewpoint. I think it can't be done on a flat map without rearranging the order of stations on each line. Thus your Raynes Park (23' am peak) will have to be shown as further out than Surbiton (18') as will Wimbledon (19'). Commuters from West Byfleet were complaining that with the new timetable they had only stopping trains in the morning peak (40') but they do have a fast return service (26'). So West Byfleet must be shown as further out than Wokng (26' & 23') and possibly as far out as Farnborough (36' & 39'). Best of luck to anyone trying to generate such a map. -- Mike D |
Commuting time map
"Michael R N Dolbear" wrote in message news:01c51865$f9eab800$LocalHost@default... Richard Dixon wrote [...] I was commenting with a colleague recently how she (living in Sevenoaks) takes a similar amount of time as me (in Raynes Park) to get into work (we're based in Monument). It made me wonder if anyone has re-designed a London travel map in terms of time frame of reference - i.e. shortest time taken to get to a major London station (e.g. Waterloo, Victoria, London Bridge, Liverpool Street etc.) from around the south-east? Just interested from a commuting viewpoint. I think it can't be done on a flat map without rearranging the order of stations on each line. Thus your Raynes Park (23' am peak) will have to be shown as further out than Surbiton (18') as will Wimbledon (19'). Commuters from West Byfleet were complaining that with the new timetable they had only stopping trains in the morning peak (40') but they do have a fast return service (26'). So West Byfleet must be shown as further out than Wokng (26' & 23') and possibly as far out as Farnborough (36' & 39'). Best of luck to anyone trying to generate such a map. -- Mike D You do it like a weather chart or OS map with contours. The contours represent the points of equal time and yes some places further out will have less travel minutes. peter |
Commuting time map
peter wrote:
I think it can't be done on a flat map without rearranging the order of stations on each line. Thus your Raynes Park (23' am peak) will have to be shown as further out than Surbiton (18') as will Wimbledon (19'). Commuters from West Byfleet were complaining that with the new timetable they had only stopping trains in the morning peak (40') but they do have a fast return service (26'). So West Byfleet must be shown as further out than Wokng (26' & 23') and possibly as far out as Farnborough (36' & 39'). Best of luck to anyone trying to generate such a map. -- Mike D You do it like a weather chart or OS map with contours. The contours represent the points of equal time and yes some places further out will have less travel minutes. peter However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. Whereas, in the example that Mike gave, the isochrones will have to cross. That will make it rather hard to read. |
Commuting time map
"Stephen Osborn" wrote in message
... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. Whereas, in the example that Mike gave, the isochrones will have to cross. No, they won't. It's just the same as a weather map, it's just a map where every point has a real number associated with it. Draw two isochrones crossing each other, write various times on the isochrones and on the spaces between them, and you'll see that it can't happen. -- John Rowland - Spamtrapped Transport Plans for the London Area, updated 2001 http://www.geocities.com/Athens/Acro...69/tpftla.html A man's vehicle is a symbol of his manhood. That's why my vehicle's the Piccadilly Line - It's the size of a county and it comes every two and a half minutes |
Commuting time map
John Rowland wrote:
"Stephen Osborn" wrote in message ... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. Whereas, in the example that Mike gave, the isochrones will have to cross. No, they won't. It's just the same as a weather map, it's just a map where every point has a real number associated with it. Draw two isochrones crossing each other, write various times on the isochrones and on the spaces between them, and you'll see that it can't happen. I was accepting Mike's point that "I think it can't be done on a flat map without rearranging the order of stations on each line." Using Mike's example, a 'railway straight line' runs Wimbledon, Raynes Park & Surbiton in that order. The isochrone passes through Wimbledon & Surbiton (ignoring the 1 minute difference) but not through Raynes Park. That arrangement is possible on an OS map or weather chart as, say, two maxima (M) can be separated by a minimum (m) so there will be places with the same value but they are not linked by a contour / isobar. For example a1 & a2 in the diagram below: a b a a a b b a a a M a1 b m b a2 M a a a b b a a a b a Here the contours / isobars that a1 & a2 sit on have different centres. For a travel map to be of use, every point on it has to share share the same centre. regards Stephen |
Commuting time map
Richard Dixon wrote:
Dear All I hope I've come to the right place to ask this question. I was commenting with a colleague recently how she (living in Sevenoaks) takes a similar amount of time as me (in Raynes Park) to get into work (we're based in Monument). It made me wonder if anyone has re-designed a London travel map in terms of time frame of reference - i.e. shortest time taken to get to a major London station (e.g. Waterloo, Victoria, London Bridge, Liverpool Street etc.) from around the south-east? Just interested from a commuting viewpoint. I've seen such a map, but I can't remember exactly where, though it may have been North Greenwich station. There were two versions: one showing the situation before the Jubilee was extended, and one after. |
Commuting time map
"Dave Arquati" wrote in message [snip] There is software available to companies involved in transport planning which can plot "isochrones" (contours of time) of public transport journey time to a specific point in London. Unfortunately I can't immediately see any available on the internet. When I joined my last company in 1988 the personnel dept had a printed map for London's public transport, mostly oriented to trains coming in from outer suburbia, as I recall. The map was ancient then, disintegrating, and held together with sellotape. I don't remember who published it. As a child, I remember seeing pre WW II atlases, old then, with maps of Britain, coloured like contour maps, showing time to reach London by train. I think the newer versions of Autoroute do isochrones for cars, and, of course, bikes. There's something funny, though, about the numbers Autoroute produces if you send it out on a bike at 10 mph. Every now and again I see "accessibility maps" put out by London's planning or transport people. I think they credit it to a program they have called PTAL, or some such. I wonder if you could demand a copy of the program under the Freedom of Information Act. Jeremy Parker |
Commuting time map
Aidan Stanger wrote:
Richard Dixon wrote: Dear All I hope I've come to the right place to ask this question. I was commenting with a colleague recently how she (living in Sevenoaks) takes a similar amount of time as me (in Raynes Park) to get into work (we're based in Monument). It made me wonder if anyone has re-designed a London travel map in terms of time frame of reference - i.e. shortest time taken to get to a major London station (e.g. Waterloo, Victoria, London Bridge, Liverpool Street etc.) from around the south-east? Just interested from a commuting viewpoint. I've seen such a map, but I can't remember exactly where, though it may have been North Greenwich station. There were two versions: one showing the situation before the Jubilee was extended, and one after. I remember there used to be a computer terminal in the London Transport Museum which showed you the Tube map versus a geographical one and an isochronal one. The isochronal one didn't actually show the lines though; it just showed points for the major centres like Harrow. -- Dave Arquati Imperial College, SW7 www.alwaystouchout.com - Transport projects in London |
Commuting time map
Jeremy Parker wrote:
"Dave Arquati" wrote in message [snip] There is software available to companies involved in transport planning which can plot "isochrones" (contours of time) of public transport journey time to a specific point in London. Unfortunately I can't immediately see any available on the internet. When I joined my last company in 1988 the personnel dept had a printed map for London's public transport, mostly oriented to trains coming in from outer suburbia, as I recall. The map was ancient then, disintegrating, and held together with sellotape. I don't remember who published it. As a child, I remember seeing pre WW II atlases, old then, with maps of Britain, coloured like contour maps, showing time to reach London by train. I think the newer versions of Autoroute do isochrones for cars, and, of course, bikes. There's something funny, though, about the numbers Autoroute produces if you send it out on a bike at 10 mph. Every now and again I see "accessibility maps" put out by London's planning or transport people. I think they credit it to a program they have called PTAL, or some such. I wonder if you could demand a copy of the program under the Freedom of Information Act. PTAL is a scoring system from 1 (or perhaps zero?) to 6, with 6 being the highest level of public transport accessibility. The southern portion of the King's Cross development (developers: Argent) has a PTAL score of 6, as by the time it is built, it will probably have the best public transport accessibility in the entire country. -- Dave Arquati Imperial College, SW7 www.alwaystouchout.com - Transport projects in London |
Commuting time map
Stephen Osborn wrote: John Rowland wrote: "Stephen Osborn" wrote in message ... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. This is a correct argument that two contours _indicating the same height_ must be coincident if they have at least one point in common; however consider contours marking _different_ heights; these can coincide on a non-empty set of points (eg along a vertical cliff) without necessarily coinciding everywhere. -- Larry Lard Replies to group please |
Commuting time map
Larry Lard wrote:
Stephen Osborn wrote: John Rowland wrote: "Stephen Osborn" wrote in message ... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. This is a correct argument that two contours _indicating the same height_ must be coincident if they have at least one point in common; however consider contours marking _different_ heights; these can coincide on a non-empty set of points (eg along a vertical cliff) without necessarily coinciding everywhere. -- That is true for a _literally_ vertical cliff, which does not actually occur in nature. Can you think of any other case that would be true (should "eg along a vertical cliff" actually have been "ie along a vertical cliff")? Also I still believe that, to make an accurate time map without rearranging the order of stations on each line, the isochrones would have to cross not just touch. regards Stephen |
Commuting time map
On Tue, 22 Feb 2005, Stephen Osborn wrote:
Larry Lard wrote: Stephen Osborn wrote: John Rowland wrote: "Stephen Osborn" wrote in message ... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. This is a correct argument that two contours _indicating the same height_ must be coincident if they have at least one point in common; however consider contours marking _different_ heights; these can coincide on a non-empty set of points (eg along a vertical cliff) without necessarily coinciding everywhere. That is true for a _literally_ vertical cliff, which does not actually occur in nature. It might happen that there are no perfectly vertical cliffs, but i don't think it's impossible in principle, so that doesn't matter. Also, you do get cliffs like this: ---------/ / cliff / / / / /------- | sea | Which are a bit of a problem, as the altitude is discontinuous as you go from left to right - it goes from X feet in the air to zero without there being any intervening points. tom PS It's best not to put a "-- " before your reply; well-brought-up news software will trim everything below that from a reply. -- Destroy - kill all hippies. |
Commuting time map
"Larry Lard" wrote in message
oups.com... Stephen Osborn wrote: John Rowland wrote: "Stephen Osborn" wrote in message ... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. This is a correct argument that two contours _indicating the same height_ must be coincident if they have at least one point in common; No. There are many "saddle" points in the landscape where, say, the land is lower to the north and south, and higher to the east and west. The contour which marks the height of the saddle point runs away from the saddle point in 4 directions. It would be perverse to describe the contour as crossing itself, but the contour could meaningfully be described as touching itself at this one point. This is as true for a map of isochrones or isobars. -- John Rowland - Spamtrapped Transport Plans for the London Area, updated 2001 http://www.geocities.com/Athens/Acro...69/tpftla.html A man's vehicle is a symbol of his manhood. That's why my vehicle's the Piccadilly Line - It's the size of a county and it comes every two and a half minutes |
Commuting time map
John Rowland wrote: "Larry Lard" wrote in message oups.com... Stephen Osborn wrote: John Rowland wrote: "Stephen Osborn" wrote in message ... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. This is a correct argument that two contours _indicating the same height_ must be coincident if they have at least one point in common; No. There are many "saddle" points in the landscape where, say, the land is lower to the north and south, and higher to the east and west. The contour which marks the height of the saddle point runs away from the saddle point in 4 directions. It would be perverse to describe the contour as crossing itself, but the contour could meaningfully be described as touching itself at this one point. This is as true for a map of isochrones or isobars. Like this, yes? : [fixed width font needed] numbers are heights 0 -1 -2 -3 -2 -1 0 1 0 -1 -2 -1 0 1 2 1 0 -1 0 1 2 3 2 1 0 1 2 3 2 1 0 -1 0 1 2 1 0 -1 -2 -1 0 1 0 -1 -2 -3 -2 -1 0 Surely in this situation there is only one contour, though, and it is X-shaped. If you want to argue that there are two contours meeting in the middle, how do you decide whether it's a meeting a , or a ^ meeting a v ? Anyway, I'm not really sure this branch of this thread (?) has anything useful to say about the original problem, as raised by Michael Dolbear: "I think it can't be done on a flat map without rearranging the order of stations on each line." -- Larry Lard Replies to group please |
Commuting time map
"Larry Lard" wrote in message
ups.com... John Rowland wrote: "Larry Lard" wrote in message oups.com... There are many "saddle" points in the landscape where, say, the land is lower to the north and south, and higher to the east and west. The contour which marks the height of the saddle point runs away from the saddle point in 4 directions. It would be perverse to describe the contour as crossing itself, but the contour could meaningfully be described as touching itself at this one point. This is as true for a map of isochrones or isobars. Like this, yes? : [fixed width font needed] numbers are heights 0 -1 -2 -3 -2 -1 0 1 0 -1 -2 -1 0 1 2 1 0 -1 0 1 2 3 2 1 0 1 2 3 2 1 0 -1 0 1 2 1 0 -1 -2 -1 0 1 0 -1 -2 -3 -2 -1 0 Surely in this situation there is only one contour, though, and it is X-shaped. If you want to argue that there are two contours meeting in the middle, how do you decide whether it's a meeting a , or a ^ meeting a v ? It's a ^ meeting a v. Look at the bigger picture, which would be like this... ------- --0-0-- -0+0+0- --0-0-- ------- Anyway, I'm not really sure this branch of this thread (?) has anything useful to say about the original problem, as raised by Michael Dolbear: "I think it can't be done on a flat map without rearranging the order of stations on each line." His statement is so clearly wrong it's hard to argue with it until someone explains why they think it's right. Every public point in the 2D space has a scalar quantity associated with it, namely journey time from point X. Mathematically this is identical to the contour maps, where every point which is not inside a building has a scalar quantity associated with it, namely height above sea level. -- John Rowland - Spamtrapped Transport Plans for the London Area, updated 2001 http://www.geocities.com/Athens/Acro...69/tpftla.html A man's vehicle is a symbol of his manhood. That's why my vehicle's the Piccadilly Line - It's the size of a county and it comes every two and a half minutes |
Commuting time map
John Rowland wrote: "Larry Lard" wrote in message ups.com... John Rowland wrote: "Larry Lard" wrote in message oups.com... There are many "saddle" points in the landscape where, say, the land is lower to the north and south, and higher to the east and west. The contour which marks the height of the saddle point runs away from the saddle point in 4 directions. It would be perverse to describe the contour as crossing itself, but the contour could meaningfully be described as touching itself at this one point. This is as true for a map of isochrones or isobars. Like this, yes? : [fixed width font needed] numbers are heights 0 -1 -2 -3 -2 -1 0 1 0 -1 -2 -1 0 1 2 1 0 -1 0 1 2 3 2 1 0 1 2 3 2 1 0 -1 0 1 2 1 0 -1 -2 -1 0 1 0 -1 -2 -3 -2 -1 0 Surely in this situation there is only one contour, though, and it is X-shaped. If you want to argue that there are two contours meeting in the middle, how do you decide whether it's a meeting a , or a ^ meeting a v ? It's a ^ meeting a v. Look at the bigger picture, which would be like this... ------- --0-0-- -0+0+0- --0-0-- ------- I call this one 8-shaped contour, rather than two O-shaped contours that touch at one point, but I would invest about zero effort in arguing the toss. Anyway, I'm not really sure this branch of this thread (?) has anything useful to say about the original problem, as raised by Michael Dolbear: "I think it can't be done on a flat map without rearranging the order of stations on each line." His statement is so clearly wrong it's hard to argue with it until someone explains why they think it's right. Every public point in the 2D space has a scalar quantity associated with it, namely journey time from point X. Mathematically this is identical to the contour maps, where every point which is not inside a building has a scalar quantity associated with it, namely height above sea level. OK yes here I have been incorrectly thinking about something completely other. The 'it' you can't do without rearranging stations: make such a map where commuting time is represented by distance; What you *can* do: make such a map where isochrones are explicitly overlaid on a geographical map, obviating any need to rearrange stations. At some point the 'it' changed and I failed to notice... -- Larry Lard Replies to group please |
Commuting time map
On Wed, 23 Feb 2005 12:24:21 -0000, "John Rowland"
wrote: "Larry Lard" wrote in message oups.com... Anyway, I'm not really sure this branch of this thread (?) has anything useful to say about the original problem, as raised by Michael Dolbear: "I think it can't be done on a flat map without rearranging the order of stations on each line." His statement is so clearly wrong it's hard to argue with it until someone explains why they think it's right. Every public point in the 2D space has a scalar quantity associated with it, namely journey time from point X. Mathematically this is identical to the contour maps, where every point which is not inside a building has a scalar quantity associated with it, namely height above sea level. That's broadly correct, but there is a difference in that whereas height is a continuous quantity which has a value for *every* location, journey time from X only has a value at discrete locations, namely those where there are stations. So if you want to construct a contour map (or a carpet plot) on a map of (say) England then you need to interpolate between the values using a straight line or a mathematical function that does it more smoothly. Here's an example: if it takes 40 minutes to West Drayton and 25 minutes to Slough (I'm guessing these times), then where does the "30 minute contour" run? The answer is it passes somewhere between the two stations. The exact position depends on what type of interpolation you are using. Note that you don't only have to interpolate between adjacent stations on the same line - you need to interpolate between adjacent stations irrespective of whether there is a railway between them, to allow you to work out, say, where the 30 min contour line passes between Slough and Gerrard's Cross. There is software around that will do all this and take a set of (X.Y) point and plot the Z value using contours. There are three steps we need to take: * obtain the Grid Reference (X,Y) of every station in (say) the south-east. Does this data already exist? * look up the fastest peak journey time (Z) from somewhere to each station * plot the resulting data as a contour plot PaulO |
Commuting time map
Stephen Osborn wrote:
John Rowland wrote: "Stephen Osborn" wrote... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. You already have the counterexample of a vertical cliff. I have seen those in nature - although not all of the cliff was vertical, there were certainly parts that were, and they were definitely big and vertical enough for contours to meet on the map. Whereas, in the example that Mike gave, the isochrones will have to cross. No, they won't. It's just the same as a weather map, it's just a map where every point has a real number associated with it. Draw two isochrones crossing each other, write various times on the isochrones and on the spaces between them, and you'll see that it can't happen. I was accepting Mike's point that "I think it can't be done on a flat map without rearranging the order of stations on each line." Using Mike's example, a 'railway straight line' runs Wimbledon, Raynes Park & Surbiton in that order. The isochrone passes through Wimbledon & Surbiton (ignoring the 1 minute difference) but not through Raynes Park. That arrangement is possible on an OS map or weather chart as, say, two maxima (M) can be separated by a minimum (m) so there will be places with the same value but they are not linked by a contour / isobar. For example a1 & a2 in the diagram below: a b a a a b b a a a M a1 b m b a2 M a a a b b a a a b a Here the contours / isobars that a1 & a2 sit on have different centres. For a travel map to be of use, every point on it has to share share the same centre. That statement is absolutely ridiculous! I'd go so far as to say the converse is true: If they don't share the same centre then the map can clearly display the information* and is therefore useful. If they do share the same centre then it's impossible to display sufficient information clearly, therefore the map would be useless. They do have to share the same reference point, but that's all. I assume what you were trying to say was that to be useful for determining the time it would take to get between any two points on the map, every contour has to share the same centre. If that is what you mean, I'm not going to bother disputing it because it's pointless - software could do the job a lot better than any map! * The easiest way of doing so would be to set the background colour according to how long it takes to get to the reference point. I expect this would be referred to as isochromic isochrones! |
Commuting time map
Aidan Stanger wrote:
Stephen Osborn wrote: John Rowland wrote: "Stephen Osborn" wrote... However the contours on an OS map (and AFAIK isobars on a weather chart) never touch let alone cross. They can touch, but they can't cross. I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. You already have the counterexample of a vertical cliff. I have seen those in nature - although not all of the cliff was vertical, there were certainly parts that were, and they were definitely big and vertical enough for contours to meet on the map. Whereas, in the example that Mike gave, the isochrones will have to cross. No, they won't. It's just the same as a weather map, it's just a map where every point has a real number associated with it. Draw two isochrones crossing each other, write various times on the isochrones and on the spaces between them, and you'll see that it can't happen. I was accepting Mike's point that "I think it can't be done on a flat map without rearranging the order of stations on each line." Using Mike's example, a 'railway straight line' runs Wimbledon, Raynes Park & Surbiton in that order. The isochrone passes through Wimbledon & Surbiton (ignoring the 1 minute difference) but not through Raynes Park. That arrangement is possible on an OS map or weather chart as, say, two maxima (M) can be separated by a minimum (m) so there will be places with the same value but they are not linked by a contour / isobar. For example a1 & a2 in the diagram below: a b a a a b b a a a M a1 b m b a2 M a a a b b a a a b a Here the contours / isobars that a1 & a2 sit on have different centres. For a travel map to be of use, every point on it has to share share the same centre. That statement is absolutely ridiculous! I'd go so far as to say the converse is true: If they don't share the same centre then the map can clearly display the information* and is therefore useful. If they do share the same centre then it's impossible to display sufficient information clearly, therefore the map would be useless. They do have to share the same reference point, but that's all. I assume what you were trying to say was that to be useful for determining the time it would take to get between any two points on the map, every contour has to share the same centre. If that is what you mean, I'm not going to bother disputing it because it's pointless - software could do the job a lot better than any map! * The easiest way of doing so would be to set the background colour according to how long it takes to get to the reference point. I expect this would be referred to as isochromic isochrones! That's the way the isochrones I've seen have done it. It makes for a very clear and interesting picture. Comparing the difference in journey times to two locations is also done this way (i.e. set the isochrones as the difference in journey time, +/-, for reaching point B compared to reaching point A). -- Dave Arquati Imperial College, SW7 www.alwaystouchout.com - Transport projects in London |
Commuting time map
Larry Lard wrote [...] The 'it' you can't do without rearranging stations: make such a map where commuting time is represented by distance; What you *can* do: make such a map where isochrones are explicitly overlaid on a geographical map, obviating any need to rearrange stations. At some point the 'it' changed and I failed to notice... Yes. Thank you. I really didn't do this on purpose. The OP referred to distorted maps where travel time to a central point was represented by distance. John Rowland and others (reference to 'bubbles') were considering overlays on standard geographical maps. http://www.sciencenews.org/articles/20040828/bob8.asp and links for explanation/discussion of weird maps, based on population and so forth. -- Mike D |
Commuting time map
In article ,
Paul Oter wrote: Here's an example: if it takes 40 minutes to West Drayton and 25 minutes to Slough (I'm guessing these times), then where does the "30 minute contour" run? A five minute walk from Slough Station. Next? -- Mike Bristow - really a very good driver |
Commuting time map
Dave Arquati wrote:
Aidan Stanger wrote: Stephen Osborn wrote: snip John Rowland wrote: I think you are wrong there. Contours mark places of equal height. If two contours touch at any one point then, de definito, they have to touch at *all* points, so the two contours become one contour. You already have the counterexample of a vertical cliff. I have seen those in nature - although not all of the cliff was vertical, there were certainly parts that were, and they were definitely big and vertical enough for contours to meet on the map. I am still not convinced you will find a natural cliff that is *truly* vertical (e.g. measured by a plumb line) for more than 10 metres, in order to have the contour lines coincident. I would be fascinated if you can think of an example where this is true. For a travel map to be of use, every point on it has to share share the same centre. That statement is absolutely ridiculous! Yes it is, isn't it. I had fallen into the same trap as Larry Lard (in an earlier post) had and was thinking of the distance from the centre showing the travelling time. Probably too much time looking at LU zonal maps! this would be referred to as isochromic isochrones! Nice! -- regards Stephen |
Commuting time map
Stephen Osborn wrote:
I am still not convinced you will find a natural cliff that is *truly* vertical (e.g. measured by a plumb line) for more than 10 metres, in order to have the contour lines coincident. I would be fascinated if you can think of an example where this is true. http://www.climbvertigo.ca/location-first-face.htm seems to indicate that in places, the cliff is actually overhanging. Tim (tm) -- tim at economic-truth.co.uk Xbox Live gamertag: Xexyz http://www.economic-truth.co.uk - the students' economics resource http://www.ugvm.org.uk - the uk.games.video.misc magazine The talkabout network is denied permission to reproduce this post |
Commuting time map
Tim Miller wrote:
Stephen Osborn wrote: I am still not convinced you will find a natural cliff that is *truly* vertical (e.g. measured by a plumb line) for more than 10 metres, in order to have the contour lines coincident. I would be fascinated if you can think of an example where this is true. http://www.climbvertigo.ca/location-first-face.htm seems to indicate that in places, the cliff is actually overhanging. Tim (tm) Yes but that is not vertical so the contour lines (of different heights) would not be coincident. I am struggling to get my mind around how an overhang should be shown on an OS map. -- regards Stephen |
Commuting time map
Stephen Osborn wrote:
http://www.climbvertigo.ca/location-first-face.htm seems to indicate that in places, the cliff is actually overhanging. Yes but that is not vertical so the contour lines (of different heights) would not be coincident. I am struggling to get my mind around how an overhang should be shown on an OS map. It would involve contour lines crossing. Each would have to be clearly labelled at every point. Tim (tm) -- tim at economic-truth.co.uk Xbox Live gamertag: Xexyz http://www.economic-truth.co.uk - the students' economics resource http://www.ugvm.org.uk - the uk.games.video.misc magazine The talkabout network is denied permission to reproduce this post |
Commuting time map
"Jeremy Parker" wrote in message
... Every now and again I see "accessibility maps" put out by London's planning or transport people. I think they credit it to a program they have called PTAL, or some such. I wonder if you could demand a copy of the program under the Freedom of Information Act. PTAL is not a program, it's an acronym. "public transport accessibility level" Ken's bunch are quite keen on it - basing parkign standards for development on PTAL etc. See the London Plan, e.g. p.48 http://www.london.gov.uk/mayor/strat...n_plan_all.pdf |
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