Appendix A. Field and Office Validation Examples of Seven Landscape Change Types Assessed in this Study
1. Annual Variability
Annual Variability category was created to be able to model and remove polygons detected by LandTrendr that do not capture change of interest to the NCCN. Usually, these changes are associated with variability in snow cover, clouds, terrain shadows, or vegetation phenology that is not removed in the image processing steps and is of great enough magnitude to pass through filtering. Annual variability patches are generally only found in high elevations areas with subalpine vegetation, such as above the tree line. The interpreter must exercise care in determining a polygon of this class truly shows no change. The TimeSync trajectories of these changes usually show high degree of variability throughout the time period being examined and are dominated by red, brown and orange hues.
Figure A1 shows an example of a 2008 patch in Mount Rainier National Park that would be placed in the Annual Variability category. Landsat tasseled-cap image chips between 2006 and 2009 are not significantly different, except for slight variation in hues most likely related to differences in timing of snowmelt and soil moisture during the image acquisition dates.
Figure A1.
A 2008 Annual Variability patch generated by LandTrendr at Mount Rainier National Park. (a) Photo collected during field validation. Photo credit: NPS/Catharine Copass (2016). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines, magenta colors correspond to snow and bright red colors denote clouds.
Figure A1.
A 2008 Annual Variability patch generated by LandTrendr at Mount Rainier National Park. (a) Photo collected during field validation. Photo credit: NPS/Catharine Copass (2016). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines, magenta colors correspond to snow and bright red colors denote clouds.
2. Avalanche
Avalanches originate in snow receiving zones on ridges or high on the valley wall. They are typically long, linear patches, although some events can be broken up into multiple smaller patches depicting areas of greatest removal of vegetation. If the avalanche occurred in an existing avalanche chute, the TimeSync trajectory usually starts in bright greens and yellows, which are representative of low statured, mostly broadleaf vegetation—small conifers, deciduous shrubs and herbs. If swaths of forest were removed, the TimeSync trajectory will start as greenish blue, representative of mature conifer forest. As avalanches typically remove some but not all of the vegetation, the trajectory after the event is typically shown in hues of red, brown and tan. Higher magnitude avalanches occasionally traverse the valley floor and leave a large pile of downed trees in their wake, which can usually be seen in the aerial photography.
Figure A2 shows field and office validation components for a large avalanche that occurred at North Cascades National Park in 2008.
Figure A2.
A 2008 Avalanche patch generated by LandTrendr at North Cascades National Park. (a) Photo collected during field validation. Photo credit: NPS/ Chris Lauver (2011). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines and bright red (as opposed to darker red) color in the last image chip denotes clouds.
Figure A2.
A 2008 Avalanche patch generated by LandTrendr at North Cascades National Park. (a) Photo collected during field validation. Photo credit: NPS/ Chris Lauver (2011). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines and bright red (as opposed to darker red) color in the last image chip denotes clouds.
3. Fire
Figure A3 shows a 2004 fire at Mount Rainier National Park. Fires tend to leave standing trees with no foliage, which can be seen in the aerial photography as thin shadows. Fire polygons are often large. Some lower intensity fires leave behind a mix of dead and singed trees. Sometimes active burning and smoke can been seen in the aerial photography, since the aerial photos in the Pacific Northwest are usually taken in August. The trajectory in the TimeSync usually shows changing from blue and green of conifers to a mix of brighter colors where the vegetation has been completely burned, to orange for shrubby new growth (
Figure A3c).
Figure A3.
A 2004 Fire patch generated by LandTrendr at Mount Rainier National Park. (a) Photo collected during field validation. Photo credit: NPS/ Natalya Antonova (2016). (b) Pre-disturbance 2003 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2006 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of thirty six pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines.
Figure A3.
A 2004 Fire patch generated by LandTrendr at Mount Rainier National Park. (a) Photo collected during field validation. Photo credit: NPS/ Natalya Antonova (2016). (b) Pre-disturbance 2003 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2006 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of thirty six pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines.
4. Mass Movement
This category includes a variety of vegetation-removing changes that expose rock or bare ground. Larger events are typically called landslides, and are found on valley walls away from streams or creeks. Most landslides totally remove vegetation and are often persistent, such as the 2004 Goodell Creek landslide shown in
Figure A4. Some rare events, however, are better described as “soil creeps” or “slumps” and are characterized by only partial removal of vegetation. Debris flows are mass movements associated with water discharge, such as streams. Mass movements are distinguished from the riparian category in that they occur on valley walls, perpendicular to the valley floor. Riparian category is associated with changes found on the valley floor, along low gradient rivers. Mass movements are distinguished from avalanches by the magnitude of change: mass movement leaves little to no vegetation; and by shape and context. The interpreters usually look for persistent red and orange colors in the TimeSync trajectory following the event (
Figure A4c).
Figure A4.
A 2004 Mass Movement patch generated by LandTrendr at North Cascades National Park. (a) Photo collected during field validation. Photo credit: NPS/ Jon Riedel (2004). (b) Pre-disturbance 1998 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2006 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync.
Figure A4.
A 2004 Mass Movement patch generated by LandTrendr at North Cascades National Park. (a) Photo collected during field validation. Photo credit: NPS/ Jon Riedel (2004). (b) Pre-disturbance 1998 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2006 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync.
5. Progressive Defoliation
Figure A5 shows components of field and office validation for 2003 North Cascades National Park patch that falls into the Progressive Defoliation category. This category is usually assigned to landscape change polygons where forest cover still remains but has undergone slow changes in spectral values that represent a loss of greenness and wetness (
Figure A5c). Interpreting the color change in TimeSync is therefore more challenging. The interpreter usually sees a very slight dip in the trajectory with decrease in blueness and greenness. However, the decrease is not big enough to suggest change from conifer to broadleaf vegetation or bare earth (
Figure A5).
The decreasing greenness of the forest can be difficult to discern in the aerial photography. In some stands the decline is due to LandTrendr detecting individual trees which have completely died. These dead trees appear in the aerial photos as bright red or yellow. In some stands the decline is due to the tip and top limbs of a significant proportion of the trees succumbing to some pathogen. This type of decline shows up as a subtle greying of the canopy in the aerial photos and can be hard to discern if the color balance of the photos is poor. In addition, change polygons in this category can have both types of declining trees.
Figure A5.
A 2003 Progressive Defoliation patch generated by LandTrendr at North Cascades National Park. (a) Photo collected during field validation. Photo credit: NPS/ Chris Lauver (2011). (b) Pre-disturbance 1998 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2013 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of thirty six pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Bright red color in (e) the last image chip corresponds to clouds.
Figure A5.
A 2003 Progressive Defoliation patch generated by LandTrendr at North Cascades National Park. (a) Photo collected during field validation. Photo credit: NPS/ Chris Lauver (2011). (b) Pre-disturbance 1998 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2013 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of thirty six pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Bright red color in (e) the last image chip corresponds to clouds.
6. Riparian
Riparian patches are restricted to the valley floor where the gradient is much lower and the valley floor is wider. Typical riparian patches show areas where either conifer or broadleaf vegetation previously existed and have been converted to either active river channel, with water, or river bank, with gravel and sediment.
Figure A6 shows a 2006 Riparian landscape patch from Mount Rainier National Park with evident tree mortality and gravel and sediment depositions. The spectral trajectories of these changes show either sudden increase in wetness or brightness, depending on the resulting cover type. These changes are usually easily identified on aerial photos and Landsat image chips (
Figure A6b–d).
Figure A6.
A 2007 Riparian patch generated by LandTrendr at Mount Rainier National Park. (a) Photo collected during field validation. Photo credit: NPS/ Natalya Antonova (2016). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines.
Figure A6.
A 2007 Riparian patch generated by LandTrendr at Mount Rainier National Park. (a) Photo collected during field validation. Photo credit: NPS/ Natalya Antonova (2016). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines.
7. Tree Toppling
The Tree Toppling category primarily includes forest areas where the trees have been both broken off and toppled to the ground in major wind events. This category is rare at NOCA and MORA. It is more common at OLYM, especially in the Quinault, Hoh, and Queets River valleys on the west side of the park and also in the northeast corner of the park.
Figure A7 shows a large 2008 Tree Toppling patch that resulted from the December 2007 Great Coastal Gale [
19]. This category also includes areas where the Tree Toppling is due to root rot - the structural outcome is similar and the agent is typically hard to determine just from the imagery. Large Tree Toppling events can build on themselves, with subsequent events occurring in the vicinity of the original patch. TimeSync trajectory of these events often shows some green vegetation remaining after the toppling, either because some of the trees are still standing or the foliage of the downed trees is not completely dead (
Figure A7d). Down tree trunks are often visible on the aerial photograph. Windthrow events usually occur in areas on the landscape that are exposed to wind, either on top of ridges and knolls or along rivers.
Figure A7.
A 2008 Tree Toppling patch generated by LandTrendr at Olympic National Park. (a) Photo collected during field validation. Photo credit: NPS (2008). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines and bright red color corresponds to clouds.
Figure A7.
A 2008 Tree Toppling patch generated by LandTrendr at Olympic National Park. (a) Photo collected during field validation. Photo credit: NPS (2008). (b) Pre-disturbance 2006 aerial photo as viewed in Google Earth™. (c) Post-disturbance 2009 aerial photo as viewed in Google Earth™. (d) TimeSync spectral trajectory of nine pixels around patch centroid. (e) Part of the series of tasseled-cap image chips covering pre- and post-disturbance years as viewed in TimeSync. Dark blue streaks in (e) correspond to Landsat 7 missing scan lines and bright red color corresponds to clouds.