Application of the Procedure. This procedure applies to medical appointments for all employees entitled to sick leave, the employee’s significant other and children and may be extended to other family members as determined by the Human Resources Manager. APPENDIX B Keewatin-Xxxxxxxx District School Board 800 Policy Section:Facilities & Equipment 804 Policy Name: Temporary Closing of Schools/Early Dismissal
Application of the Procedure. ERS and ENVISAT IPTA processing was applied in the Zermatt test area using SAR data of ascending (30 ERS scenes between 1992.09.05 and 2000.07.19 respectively 26 ENVISAT scenes between 2002.10.06 and 2010.09.15) and descending (31 ERS scenes between 1995.07.25 and 1999.10.13 respectively 29 ENVISAT scenes between 2002.11.06 and 2010.10.20) orbits (Fig. 21). Only summer images acquired between May and October were considered because of the presence of snow-cover. As a first step, all ERS and ENVISAT SLCs were co-registered to the same ERS reference SLC of the corresponding orbit geometry.
Application of the Procedure. This procedure applies to medical appointments for all employees entitled to sick leave, the employee’s significant other and children and may be extended to other family members as determined by the Human Resources Manager. APPENDIX D OCL – “Grandfathered” Library Technicians and Head Secretaries as at May 10, 2005 (ratification of the 2004-2007 Collective Agreement) First Name Last Name Job Title Description Xxxxxx Xxxxxx Elementary Head Secretary Lakewood School Xxxxxx Xxxxxx Library Technician Riverview School Xxxxx Xxxxxxxxxx Library Technician Beaver Brae High School Xxxxxx Pilipishen Library Technician Xxxxxxx Xxxx School Xxxxx Xxxxxx Library Technician Dryden High School Xxxxxxx Xxxx Library Technician Xxxxx Xxxxxxxxx District High Xxxxxxx Xxxxxx Library Technician Lakewood School Xxxxxxx Xxxxx Library Technician Keewatin School Xxxxxxx Xxxx Library Technician Valleyview School Xxxxx Xxxxxxxx Library Technician Evergreen School Xxxxxxxxx Xxxxxx Library Technician New Prospect Public School Xxxx Xxxx Library Technician Pinewood School Xxxxxxx Xxxxxxxx Library Technician Red Lake Xxxxxx School Xxxxx Xxxxx Library Technician Wabigoon/Oxdrift School Xxxxxxx Xxxxxx LMC Officer – Library Lakewood School Xxxxxxxx Xxxxxxxxxx Secondary Head Secretary Xxxxx Xxxxxxxxx District High Xxxxxxxx Xxxxxx Secondary Head Secretary Xxxxxx High School Xxxxx Xxxxxx Secondary Head Secretary Red Lake District High School Xxxx Xxxxxxxx Secondary Head Secretary Beaver Brae High School Xxxxxx Xxxxx Secondary Head Secretary Ignace District High School APPENDIX E OCL JOB SECURITY LIST First Name Last Name Job Title Location Hours/Day Months/Year Xxxxx Xxxxxx Library Technician Dryden High School 7 12 Xxxx Xxxxxx Secondary Secretary Xxxxx Xxxxxxxxx District High 3.25 10 Xxxxxx Xxxxxx Elementary Head Secretary Lakewood School 7 12 Xxxxxx Xxxxxxx Elementary Secretary Golden Learning Centre 7 10 Xxxx Xxxxx Secondary Secretary Xxxxx Xxxxxxxxx District High 6.5 12 Xxxxxx Xxxxx Secondary Head Secretary Ignace District High School 7 12 Xxxxxxxx Xxxxxxx Elementary Secretary Keewatin School 7 10 Xxxxxxx Xxxxxx LMC Officer – Library Lakewood School 3.25 10 Xxxxxx Xxxxxxxx Secondary Secretary Beaver Brae High School 6.5 12 Xxxxx Xxxxxxxxx Secondary Secretary Red Lake District High School 6.5 12 Xxxxxxx Xxxxx Elementary Secretary Wabigoon School 3.25 10 Xxxxx Xxxxxxxxx Secondary Secretary Dryden High School 6.5 10 Xxxxx Xxxxxxxx Elementary Secretary Oxdrift School 6.5 10 Xxxxxx Xxxxxx Libra...
Application of the Procedure. This procedure applies to medical appointments for all employees entitled to sick leave, the employee’s significant other and children and may be extended to other family members as determined by the Human Resources Manager. APPENDIX D Library Technicians and Head Secretaries Xxxxx Xxxxxx H Xxxxxx Library Technician Officer Library
Application of the Procedure. The multi-scale and multi-sensor SBAS analysis has been carried out by processing both descending and ascending SAR datasets relevant to the Umbria region, (Italy). In particular, the descending dataset is composed of 116 (77 ERS-1/2 and 39 ENVISAT) images and covers the April 1992-September 2010 time interval, while the ascending dataset includes 87 (36 ERS-1/2 and 51 ENVISAT) images spanning from June 1995- September 2010. As results of the regional scale SBAS analysis, low resolution deformation velocity maps and associated time series from both datasets have been produced, allowing the detection of several natural and human induced phenomena occurring in the study area. Figure 2 reports the low resolution deformation velocity map obtained by processing the descending dataset, superimposed on an amplitude SAR image of the analysed area. Such deformation velocity map reveals an overall stability of the area in the observed time interval. However, significant deformation patterns are present in the Xxxxx Umbra, where a subsidence induced by water exploitation occurs, and in the area around Perugia. We point out that the portion of Xxxxx Umbra between Assisi and Foligno has been affected by subsidence since 1992 (Figure 2c), as already shown by Xxxxxxxx et al. (2009), while the Perugia area exhibits ground deformation only since 2000. This is clearly visible in the plot reported in Figure 2b, thus demonstrating the effectiveness of the multi-scale SBAS approach to analyse and monitor large time intervals (almost 20 years) deformation phenomena, characterized by a temporal evolution of displacements that significantly deviate from a linear trend.
Application of the Procedure. ERS-ENVISAT Stitching (Merging) analysis of the area (275 km2) led to the identification of 26842 total measurement points (MP), with a point density of 97 PS/ km2. Figure 5 shows the distribution of the MPs identified compared with single ERS and ENVISAT results. The distribution of MP within the study area is homogeneous with ERS and ENVISAT results. As far as velocity field is concerned the ‘merging velocity’ corresponds generally to the average of ERS and Envisat separate velocity fields. Examples of time series are reported in Figure 6.
Application of the Procedure. Altamira has done the PSInSAR processing of the C-band satellite images for the Hungarian test sites in the framework of international cooperation of XXXXX.
Application of the Procedure. Due to the strong non linear displacement occurred in the temporal gap between ERS and ENVISAT, the ERS-ENVISAT Stitching (Merging) analysis has not been performed for the Silesian coal Basin area data. Below, the ERS and ENVISAT deformation velocity maps are reported (Figs. 10 and 11).
Application of the Procedure. Tramuntana range has been monitored using ERS-1/2 and ENVISAT data stacks in descending orbit. The Figure 12 shows a long time series obtained by joining deformation data from ERS-1/2 and ENVISAT results. The final time series covers the timeframe from 1992 to 2009. Mean annual displacement (mm/yr) Tramuntana ERS-ENVISAT Displacement time series 10,00 0,00 -100,070/05/1990 -20,00 -30,00 -40,00 -50,00 -60,00 -70,00 -80,00 -90,00 -100,00 31/01/1993 28/10/1995 24/07/1998 19/04/2001 14/01/2004 10/10/2006 06/07/2009 01/04/2012 ERS ENVISAT Date ERS 1992-2000 (descending orbit) ENVISAT 2003-2009 (descending orbit) Figure 12. ERS-ENVISAT (descending orbit) displacement time series.
Application of the Procedure. In the post-event, since March 10th 2010, the DRPC in collaboration with the Department of Earth Sciences of the University of Xxxxxxxx, installed a GB-InSAR. The system employed was designed and implemented by Ellegi-LiSAlab s.r.l. and JRC and installed on a stable support, in Sanguinera, that is located on the slope facing the San Fratello landslide, at an average distance of 3.3 km (Figure 4). Figure 4 - GB-InSAR position and its field of view. Monthly cumulative deformation maps were made through the interferometric radar data and the displacement time series of some representative points of the landslide were extracted and analyzed. An example of interferogram obtained during this campaign is shown in Figure 5. The colour of each pixel represents the LoS (line of sight) component of the displacement (Figure 6). Figure 5 - Example of a displacement map of the studied area. The interferogram in Figure 5 represents the displacements along the LoS, since monitoring (March 10th 2010) to May 31st 2011. It shows the presence of principal movements concentrated in defined areas, in the upper part of the slope. On the interferogram some representative points are displayed; the displacement time series of these points, obtained using the GB-InSAR data, are shown in Figure 6. Figure 6 - Displacement time series of ten representative points of the landslide area. The displacements were also studied by the analysis of data obtained through satellite interferometry (PS-InSAR). Especially the ENVISAT and RADARSAT-2 data stacks in descending and ascending orbits, and the COSMO-SkyMed in descending orbit were analyzed. The ENVISAT satellite, provided by ESA space agency, works in C band with a repeat cycle of 35 days (Xxxxxxxxxxx et al., 2005). The analyzed images regard data acquired between November 22nd 2003 and May 20th 2009. Because of the acquisition mode and the exposition of the instable slope, the best information about displacement is obtained from data stacks in ascending orbits. In Figure 6 the ENVISAT data, acquired in ascending orbit and elaborated with PS- InSAR technique, are shown. Vel. Landslide limits (DRPC, 2010) Figure 7 - PS ENVISAT, obtained by data acquired in ascending orbit. In red, the areas characterized by higher displacements are emphasized. The RADARSAT-2 satellite, provided by Geospacial Services International, works in C band with a repeat cycle of 24 days (Xxxxxxx et al., 2007). The analyzed images regard data acquired between Decembe...
