To: hgs@buhu.se Subject: Deleted mail to loading From : loading Content-type: text/plain Deleted mail: From MAILER-DAEMON Fri Mar 2 17:25:54 2012 Return-Path: <>--- Subject: Undelivered Mail Returned to Sender Content-Type: text/plain; charset=us-ascii This is the mail system at host buhu.chalmers.se. I'm sorry to have to inform you that your message could not be delivered to one or more recipients. It's attached below. For further assistance, please send mail to postmaster. If you do so, please include this problem report. You can delete your own text from the attached returned message. The mail system (expanded from ): unknown user: "secret3162" --D257860607A.1330705554/buhu.chalmers.se Content-Description: Delivery report Content-Type: message/delivery-status Reporting-MTA: dns; buhu.chalmers.se X-Postfix-Queue-ID: D257860607A X-Postfix-Sender: rfc822; loading@buhu.chalmers.se Arrival-Date: Fri, 2 Mar 2012 17:25:54 +0100 (CET) Final-Recipient: rfc822; secret3162@buhu.chalmers.se Original-Recipient: rfc822; secret3162 Action: failed Status: 5.1.1 Diagnostic-Code: X-Postfix; unknown user: "secret3162" --D257860607A.1330705554/buhu.chalmers.se Content-Description: Undelivered Message Content-Type: message/rfc822 Received: by buhu.chalmers.se (Postfix, from userid 3001) id D257860607A; Fri, 2 Mar 2012 17:25:54 +0100 (CET) To: secret3162@buhu.chalmers.se Subject: Ocean loading values results From: Loading@buhu.chalmers.se Content-type: text/plain Message-Id: <20120302162554.D257860607A@buhu.chalmers.se> Date: Fri, 2 Mar 2012 17:25:54 +0100 (CET) $$ Ocean loading displacement $$ $$ Calculated on froste using olfg/olmpp of H.-G. Scherneck $$ $$ COLUMN ORDER: M2 S2 N2 K2 K1 O1 P1 Q1 MF MM SSA $$ $$ ROW ORDER: $$ AMPLITUDES (m) $$ RADIAL $$ TANGENTL EW $$ TANGENTL NS $$ PHASES (degrees) $$ RADIAL $$ TANGENTL EW $$ TANGENTL NS $$ $$ Displacement is defined positive in upwards, South and West direction. $$ The phase lag is relative to Greenwich and lags positive. The $$ Gutenberg-Bullen Greens function is used. In the ocean tide model the $$ deficit of tidal water mass has been corrected by subtracting a uniform $$ layer of water with a certain phase lag globally. $$ $$ Complete : No interpolation of ocean model was necessary $$ _PP : Ocean model has been interpolated near the station $$ (PP = Post-Processing) $$ $$ CMC: YES (corr.tide centre of mass) $$ $$ Ocean tide model: NAO.99b $$ $$ END HEADER $$ TENC $$ NAO.99b_PP ID: 2012-03-02 17:25:54 $$ Computed by OLCMC/OLMPP by H G Scherneck, Onsala Space Observatory, 2012 $$ TENC, RADI TANG lon/lat: 120.9157 23.2778 2341.16 .00775 .00301 .00194 .00087 .00822 .00744 .00270 .00158 .00059 .00046 .00048 .00729 .00272 .00132 .00074 .00551 .00359 .00175 .00066 .00034 .00016 .00013 .00284 .00094 .00043 .00026 .00423 .00206 .00131 .00032 .00051 .00025 .00015 159.3 155.3 150.6 148.1 -64.7 -88.3 -66.5 -99.0 -151.7 -158.0 -176.1 109.7 137.8 96.2 133.6 -136.6 -159.7 -138.9 -164.4 135.4 86.5 15.6 -46.1 -21.2 -55.8 -26.9 -97.3 -117.0 -100.8 -114.6 1.4 -9.7 -6.0 $$ END TABLE $$ END TABLE --D257860607A.1330705554/buhu.chalmers.se-- Content-Type: message/delivery-status Reporting-MTA: dns; buhu.chalmers.se X-Postfix-Queue-ID: D257860607A X-Postfix-Sender: rfc822; loading@buhu.chalmers.se Arrival-Date: Fri, 2 Mar 2012 17:25:54 +0100 (CET) Final-Recipient: rfc822; secret3162@buhu.chalmers.se Original-Recipient: rfc822; secret3162 Action: failed Status: 5.1.1 Diagnostic-Code: X-Postfix; unknown user: "secret3162" --D257860607A.1330705554/buhu.chalmers.se Content-Description: Undelivered Message Content-Type: message/rfc822 Received: by buhu.chalmers.se (Postfix, from userid 3001) id D257860607A; Fri, 2 Mar 2012 17:25:54 +0100 (CET) To: secret3162@buhu.chalmers.se Subject: Ocean loading values results From: Loading@buhu.chalmers.se Content-type: text/plain Message-Id: <20120302162554.D257860607A@buhu.chalmers.se> Date: Fri, 2 Mar 2012 17:25:54 +0100 (CET) $$ Ocean loading displacement $$ $$ Calculated on froste using olfg/olmpp of H.-G. Scherneck $$ $$ COLUMN ORDER: M2 S2 N2 K2 K1 O1 P1 Q1 MF MM SSA $$ $$ ROW ORDER: $$ AMPLITUDES (m) $$ RADIAL $$ TANGENTL EW $$ TANGENTL NS $$ PHASES (degrees) $$ RADIAL $$ TANGENTL EW $$ TANGENTL NS $$ $$ Displacement is defined positive in upwards, South and West direction. $$ The phase lag is relative to Greenwich and lags positive. The $$ Gutenberg-Bullen Greens function is used. In the ocean tide model the $$ deficit of tidal water mass has been corrected by subtracting a uniform $$ layer of water with a certain phase lag globally. $$ $$ Complete : No interpolation of ocean model was necessary $$ _PP : Ocean model has been interpolated near the station $$ (PP = Post-Processing) $$ $$ CMC: YES (corr.tide centre of mass) $$ $$ Ocean tide model: NAO.99b $$ $$ END HEADER $$ TENC $$ NAO.99b_PP ID: 2012-03-02 17:25:54 $$ Computed by OLCMC/OLMPP by H G Scherneck, Onsala Space Observatory, 2012 $$ TENC, RADI TANG lon/lat: 120.9157 23.2778 2341.16 .00775 .00301 .00194 .00087 .00822 .00744 .00270 .00158 .00059 .00046 .00048 .00729 .00272 .00132 .00074 .00551 .00359 .00175 .00066 .00034 .00016 .00013 .00284 .00094 .00043 .00026 .00423 .00206 .00131 .00032 .00051 .00025 .00015 159.3 155.3 150.6 148.1 -64.7 -88.3 -66.5 -99.0 -151.7 -158.0 -176.1 109.7 137.8 96.2 133.6 -136.6 -159.7 -138.9 -164.4 135.4 86.5 15.6 -46.1 -21.2 -55.8 -26.9 -97.3 -117.0 -100.8 -114.6 1.4 -9.7 -6.0 $$ END TABLE $$ END TABLE --D257860607A.1330705554/buhu.chalmers.se-- Content-Type: message/rfc822 Received: by buhu.chalmers.se (Postfix, from userid 3001) id D257860607A; Fri, 2 Mar 2012 17:25:54 +0100 (CET) To: secret3162@buhu.chalmers.se Subject: Ocean loading values results From: Loading@buhu.chalmers.se Content-type: text/plain Message-Id: <20120302162554.D257860607A@buhu.chalmers.se> Date: Fri, 2 Mar 2012 17:25:54 +0100 (CET) $$ Ocean loading displacement $$ $$ Calculated on froste using olfg/olmpp of H.-G. Scherneck $$ $$ COLUMN ORDER: M2 S2 N2 K2 K1 O1 P1 Q1 MF MM SSA $$ $$ ROW ORDER: $$ AMPLITUDES (m) $$ RADIAL $$ TANGENTL EW $$ TANGENTL NS $$ PHASES (degrees) $$ RADIAL $$ TANGENTL EW $$ TANGENTL NS $$ $$ Displacement is defined positive in upwards, South and West direction. $$ The phase lag is relative to Greenwich and lags positive. The $$ Gutenberg-Bullen Greens function is used. In the ocean tide model the $$ deficit of tidal water mass has been corrected by subtracting a uniform $$ layer of water with a certain phase lag globally. $$ $$ Complete : No interpolation of ocean model was necessary $$ _PP : Ocean model has been interpolated near the station $$ (PP = Post-Processing) $$ $$ CMC: YES (corr.tide centre of mass) $$ $$ Ocean tide model: NAO.99b $$ $$ END HEADER $$ TENC $$ NAO.99b_PP ID: 2012-03-02 17:25:54 $$ Computed by OLCMC/OLMPP by H G Scherneck, Onsala Space Observatory, 2012 $$ TENC, RADI TANG lon/lat: 120.9157 23.2778 2341.16 .00775 .00301 .00194 .00087 .00822 .00744 .00270 .00158 .00059 .00046 .00048 .00729 .00272 .00132 .00074 .00551 .00359 .00175 .00066 .00034 .00016 .00013 .00284 .00094 .00043 .00026 .00423 .00206 .00131 .00032 .00051 .00025 .00015 159.3 155.3 150.6 148.1 -64.7 -88.3 -66.5 -99.0 -151.7 -158.0 -176.1 109.7 137.8 96.2 133.6 -136.6 -159.7 -138.9 -164.4 135.4 86.5 15.6 -46.1 -21.2 -55.8 -26.9 -97.3 -117.0 -100.8 -114.6 1.4 -9.7 -6.0 $$ END TABLE $$ END TABLE --D257860607A.1330705554/buhu.chalmers.se-- Subject: Ocean loading values results