Appendix 1 Debris Flow Inventory in Maps (Sect. 3.3)
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1 Appendix 1 Debris Flow Inventory in Maps (Sect. 3.3) Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
2 224 Appendix 1: Debris Flow Inventory in Maps
3 Appendix 1: Debris Flow Inventory in Maps 225
4 226 Appendix 1: Debris Flow Inventory in Maps
5 Appendix 1: Debris Flow Inventory in Maps 227
6 228 Appendix 1: Debris Flow Inventory in Maps
7 Appendix 1: Debris Flow Inventory in Maps 229
8 230 Appendix 1: Debris Flow Inventory in Maps
9 Appendix 1: Debris Flow Inventory in Maps 231
10 232 Appendix 1: Debris Flow Inventory in Maps
11 Appendix 1: Debris Flow Inventory in Maps 233
12 234 Appendix 1: Debris Flow Inventory in Maps
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14 236 Appendix 1: Debris Flow Inventory in Maps
15 Appendix 2 List of Aerial Photographs Used for Debris Flow Event Mapping (Sect ) Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
16 238 Appendix 2: List of Aerial Photographs
17 Appendix 3 Regional Characteristics of Debris Flow Activity in the Study Areas (Sect ) A3.1 Initiation Type Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
18 240 Appendix 3: Regional Characteristics of Debris Flow A3.2 Regolith Supply Conditions
19 Appendix 3: Regional Characteristics of Debris Flow 241 A3.3 Aspect
20 242 Appendix 3: Regional Characteristics of Debris Flow A3.4 Slope
21 Appendix 3: Regional Characteristics of Debris Flow 243 A3.5 Altitude Above Sea Level
22 244 Appendix 3: Regional Characteristics of Debris Flow A3.6 Altitude Above Catchment Exit (Relative Altitude)
23 Appendix 3: Regional Characteristics of Debris Flow 245 A3.7 Altitude and Sediment (Rock/Debris) Distribution
24 Appendix 4 Debris Flow Activity in Study Areas Through Time (Sect ) Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
25 248 Appendix 4: Debris Flow Activity in Study Areas
26 Appendix 5 Regional Characteristics of Debris Flow Events in the Study Areas (Sect ) A5.1 Initiation Type Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
27 250 Appendix 5: Regional Characteristics of Debris Flow A5.2 Regolith Supply Conditions
28 Appendix 5: Regional Characteristics of Debris Flow 251 A5.3 Aspect
29 252 Appendix 5: Regional Characteristics of Debris Flow A5.4 Slope
30 Appendix 5: Regional Characteristics of Debris Flow 253 A5.5 Altitude Above Sea Level
31 254 Appendix 5: Regional Characteristics of Debris Flow A5.6 Altitude Above Catchment Exit (Relative Altitude)
32 Appendix 6 Climate Stations Used for Temperature Interpolations (Sects , 5.2.6, and 5.2.7) The following tables list climate stations used in this study for temperature calculations. Table A6.1 specifies climate stations close to the debris flow study areas (Agent # refers to National Climate Database ID (NIWA 2010). Since the network of temperature-recording climate stations is sparse in the Southern Alps, nearby stations are identical for study areas of a given region. Climate stations are consequently grouped according to region. The stations highlighted in grey were used for frost-weathering intensity calculations (Sect ) for the study area noted in the last column. Mean annual temperature surfaces for the prediction of permafrost in the individual study areas (Sects and 5.2.7) were calculated by inter- and extrapolating between all the stations listed for the respective region. These regional lists are excerpts of Table A6.2 which lists all the South Island climate stations that were available for the calculation of mean annual temperature surfaces for the training and application of the permafrost distribution model (Sect ). Data from climate stations closest to the location of interest were denoted the highest weight in the calculations. Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
33 256 Appendix 6: Climate Stations Used for Temperature
34 Appendix 6: Climate Stations Used for Temperature 257
35 Appendix 7 Preliminary Permafrost Distribution Estimate for the Irishman Stream Valley, Central Ben Ohau Range (Sect ) The placement of miniature temperature data loggers for ground surface temperature monitoring was based on a preliminary permafrost distribution estimate for the head area of the Irishman Stream catchment and surrounding slopes. This preparatory estimate was derived from the mean toe elevation (per aspect class) of intact rock glaciers mapped in the Ben Ohau Range. Black symbols and white labels mark the logger location and corresponding site name. Basemap: Orthophotograph (Terralink ). Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
36 Appendix 8 Modelled Permafrost Extent and Frost-Weathering Intensities in the Study Areas (Sects and 5.2.7) Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
37 262 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
38 Appendix 8: Modelled Permafrost Extent and Frost-Weathering 263
39 264 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
40 Appendix 8: Modelled Permafrost Extent and Frost-Weathering 265
41 266 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
42 Appendix 8: Modelled Permafrost Extent and Frost-Weathering 267
43 268 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
44 Appendix 8: Modelled Permafrost Extent and Frost-Weathering 269
45 270 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
46 Appendix 8: Modelled Permafrost Extent and Frost-Weathering 271
47 272 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
48 Appendix 8: Modelled Permafrost Extent and Frost-Weathering 273
49 274 Appendix 8: Modelled Permafrost Extent and Frost-Weathering
50 Appendix 9 Variance Inflation Factors for Regression Analyses The variance inflation factor (VIF) is a measure for multicollinearity between predictors in a regression model (e.g. Field 2005; Gordon 2012). A VIF values greater than 10 is considered critical. Average VIF values markedly above 1 indicate that multicollinearity might be biasing the regression model. Variance inflation factors for the regression models in Sect : Springer International Publishing Switzerland 2016 K. Sattler, Periglacial Preconditioning of Debris Flows in the Southern Alps, New Zealand, Springer Theses, DOI /
51 276 Appendix 9: Variance Inflation Factors for Regression Analyses References Columbus J, Sirguey P, Tenzer R (2011) 15m DEM for New Zealand. University of Otago, National School of Surveying, New Zealand. Accessed 05 Jan 2014 Cox SC, Barrell DJA (2007) Geology of the Aoraki area, 1: Geological Map 15. GNS Science, Lower Hutt Field AP (2005) Discovering statistics using SPSS (and sex, drugs and rock'n'roll). Sage Publications, London Gordon RA (2012) Applied statistics for the social and health sciences. Routledge, New York LINZ (2009) Topo50 Maps, V 1.0. Land Information New Zealand. topography/topo-maps/topo50. Accessed 28 Feb 2016 NIWA (2010) National Climate Database. Accessed 10 Aug 2015 Rattenbury MS, Townsend DB, Johnston MR (2006) Geology of the Kaikoura area, 1: Geological Map 13. GNS Science, Lower Hutt Terralink ( ) Colour orthophotograph mosaic. Terralink International Ltd, Wellington. Index file of individual images available: Accessed 18 Nov 2015 Turnbull IM, Allibone AH, Jongens R (2010) Geology of the Fjordland area, 1: Geological Map 17. GNS Science, Lower Hutt
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