– Notice of Service Changes WSRN – Effective December 1
Transcription
– Notice of Service Changes WSRN – Effective December 1
WSRN – Notice of Service Changes NOTICE OF SERVICE CHANGES – Effective December 1st, 2014 The WSRN is now in its 13th year of development and operations; the dedication of the many partners (infrastructure contributors, sponsors, equipment vendors, scientific, and academic partners) plus those supporting operations through annual contributions, have built the WSRN into one a much lauded example of public/private cooperation. Several elements of upgraded hardware/software, and changes in the National Spatial Reference System have prompted the WSRN to make some changes – these will not disrupt services – but there will be some changes – please read in detail. WSRN CHANGES Summary: The WSRN operates dual systems (dual banks of servers and NTRIP casters for real-time access) and the older of the two systems will be retired on Dec 1st, 2014. A new set of redundant servers and caster will be deployed at that time to replace the old ones. But, the legacy reference framework (NAD93-CORS 96) on the old casters will be discontinued at that time and both the primary and new redundant systems and casters will operate on the NAD832011 reference framework. CHANGES SHOULD BE TRANSPARENT TO EXISTING ACCOUNT HOLDERS (see the FAQ – frequently asked question – section at the end of this email. 1. NAD83-CORS96 Epoch 2002.00 will no longer be supported – Effective December 1st 2014. The WSRN constrains all stations to the National Spatial Reference System (NSRS), via the active control component of the NSRS maintained by the Nation Geodetic Survey (NGS). The NGS ceased support of NAD93-CORS96 in 2012, and the reference positions for controlling CORS have gone out of tolerance (due to velocity) we are unable to continue to constrain to the legacy NAD83-CORS96 Epoch 2002.00 values. The old values are straining the capabilities of the software to maintain decent solutions; it is time to move forward. 2. No more 156.74.250.185 Caster. The legacy servers and caster (i.e. with the caster IP of 156.74.250.185, nicknamed “185 server” or “CORS96 server”) will be retired on December 1st, 2014. Several of the physical servers in this old bank have been running for 13 years straight, are aging, no-longer supported, and are running an older version of the software 3. The www.wsrn3.org website will not change. The current website will still offer the very same static files for post-processing freely and openly to the public (via WSRN participant logins or “guest” logins) and the “Reference Data Shop” link (one you’ve logged in) or via the archive at Central Washington University: ftp.panga.cwu.edu/pub/data/ . There will be no changes in static file formats or files offered. 4. The Primary real-time caster and Reference Framework. Most users have already transitioned to the newer “NAD38-2011” servers and NTRIP caster: 156.74.250.108 (nicknamed the :108 server” or “2011 server”) and all stations run NAD83-2011 Epoch 2010.00. This newer reference framework is consistent with the published values for NGS CORS, the NGS OPU and OPS-RS online positioning services, and is constrained to WSRN station that are also part of the NGS CORS network. 5. Pending Redundant System caster and reference framework. To replace the retiring legacy servers a brand new bank of servers has been installed and will be configured and tested. Users will have a fallback caster (IP to be determined when commissioned) to the primary “108” caster; all usernames, passwords, mountpoint names, subnets, etc will be the same. There will be no changes to solution types or formats - users will be able to switch from one caster to the other by only changing the caster IP. 6. Update Account System. Updated accounting procedures and software are already running on the newer “108” servers, and there are regular audits. There should be no changes apparent to the end user. New test accounts have automatic expiration dates but otherwise the WSRN does not change anything about valid user accounts without calling the users first. Anniversary dates for all new accounts are at the 15th or month, with first invoices prorated to the 15th, and existing given a one-time adjustment to the 15th upon renewal. The login databases of the retiring “185” server will be discontinued on Dec 1st 2014 but all valid logins have been added to the newer “108” server already. Do not hesitate to contact if you have questions, but please read the following FAQ first: FAQ – Frequently Asked Questions about the WSRN Dec 1st 2014 Changes How much of a shift is there between NAD83-CORS96 Epoch 2002.00 and NAD83-2011 epoch 2010.00? It varies around the state. The positional changes in the reference framework are threefold: the NGS has had improved data, computational approaches have improved, and the biggest factor has been the “Epoch” change in the velocities due to plate movement. NAD38-2011 is a multi-year solution, a full 8 years of data and velocity. NAD83-2011 is an upgrade on many levels; a lot of the noise and inconsistencies in CORS96 (and older realizations) have been addressed. To give you an idea of just how much velocity can come into play; in Seattle, over a 25 year period there is a s much as 0.5’ of shift. Example differences between NAD83-CORS96 Epoch 2002.00 and NAD38-20911 Epcoh 2010.00 run around 0.15’ (in the central Puget Sound area, more on the coast, and less further east, but this can vary. Vertical differences are typically only a few hundredths (but see entry below about Geoid models). What can I do about the shift between NAD83-CORS96 Epoch 2002.00 and NAD83-2011 epoch 2010.00? Most users simply start new projects on the new reference, or localize to project references or legacy published values – localization, calibration, adjustment (the term varies in different surveying and mapping software) now is good time to learn how to use those localization features and establish best practices for your crews. The earth continues to move – no geodetic coordinates can be truly frozen in time and space. There are published NAD83-2011 Epoch 2010.00 values on passive monuments available from the NGS: http://www.ngs.noaa.gov/cgi-bin/datasheet.prl and WSDOT: http://www.wsdot.wa.gov/monument/ . Note that many of the passive marks were not reobserved to derive the new values, but may have just been recomputed – users have found instances of differences between observed and published due to subsidence or other disturbances. Be sure to check more than one monument if using published values. NGS’s OPUS is another source for NAD83-2011 Epoch 2010.00 positions. If there are no verified published passive marks near your work area, static sessions of carried lengths (depending on the precision you require) can be automatically processed through the NGS OPUS portal: http://www.ngs.noaa.gov/OPUS/ . Note that OPUS-RS will not work for some northern and western regions of the state, and regular OPUS may not work well in some of the same areas, and that you may need to wait a day (some CORS stations used in OPUS only send data daily) and updated orbit data to be used in the OPUS solution. Session lengths vary, but some users report that 2 to 4 sessions can often match NGS. WSDOT, and WSRN values. What Geoid Model should I use? It is highly recommended by the NGS that is you are working within the NAD83-2011 Epoch 2010.00 reference framework that you use their hybrid Geoid model GEOID 2012A (or newer) as the underlying data is on the same reference realization – do not mix and match. Though the newest geoid has weaknesses around the state most early adopters of the 2011 have been reporting improved results for geoid derived orthometric elevations; especially in determining localized differences. Will the WSRN turn off my logins if I have not renewed my account? NO. The WSRN will always contact you first. The only exception is test logins; they will automatically expire at the end of 90 days – we try to contact you before expiration Will there be changes to logins or mountpoints in the new system? NO. The same usernames, passwords, and mountpoint names were ported over to the new server. The port of the casters is the same (8080) and only the last 3 digits of the caster Ip have changed from 185 to 108 Is the solution different? Fundamentally no, but there have been improvements to the software and algorithms, plus the new reference framework is much tighter. Uses will notice that they do not match an old CORS96 value, but that is a reference framework change and has nothing to do to with solution quality. Do I choose “NAD83-2011” in the datum selection for my data collector software? Typically, NO. DC software typically do the transformation from ITRF (WGS84 et al) to NAD83 (Moldensky) transparent to the user without intervention. In some DC software you need to choose “No Transformation” so you do not do a “double transformation” (as the WSRN is already on NAD83). Or you simply pick “NAD83” (and not NAD83-2011). If you notice your results are about 4’ horizontal by 1.3’ vertical off published 2011, then you are probably doing a double transformation (the underlying ellipsoids are offset by 2m at earth center and around here the respective ellipsoids are separated around 4’x1.3’). Does the new caster have Glonass? YES. For several years, all but handful of WSRN stations have been Glonass capable and Glonass is in all solutions. The few stations that do not have Glonass are operated by Unavco PBO (National Science Foundation funded) and were deployed without Glonass – SC03, P401, P402, etc. But this is about to change. PBO is proposing to allow interested parties to sponsor the upgrade of their sites to Glonass capability (contact me if you’d like to do this, an investment of that kind would vest a user as a WSRN partial-station sponsor partner). PACWA – the new coastal subnet. On the old “185” servers, the NW and SW subnets covered the Pacific coast area; overlapping at Gray’s harbor. The new “108” servers have a new subnet for the Pacific coast region; this works better for maintaining solutions and subnet geodesy as there is substantial velocity and atmospheric effects in that region – better to treat it separately. (See attached map). Support of other formats. The new servers will support (as standard services) RTCM3.1 and CMR+ (though users are encouraged to migrate over to RTCM3.1 (we kept CMR+ for users of some legacy equipment and RTCM3 (forward) continues to be developed as an open format by the international RTCM committee). Over the past decade, some users have requested other formats and network solution types, like mater-auxiliary and FKP; we’ve implemented, they’ve tried them, they found no advantage over VRS or single base, and then we’ve discontinued. Other format requests will still be evaluated on a case-by-case basis, but note that users have settled on these and we can only field requests if there is some compelling need (e.g. compatibility with legacy gear). As there appears to be no one using RTCM2.3 (and older format that uses much more bandwidth) we are discontinuing RTCM2.3 on the newer servers. Gavin Schrock, PLS [email protected] www.wsrn3.org 206-684-5630