University of Washington Tacoma UW Tacoma Digital Commons SIAS Faculty Publications School of Interdisciplinary Arts and Sciences 6-4-2018 ‘Boundary’: Mapping and Visualizing Climatically Changed Landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon D. H. Shugar University of Washington Tacoma, [email protected] K. A. Colorado J. J. Clague M. J. Willis J. L. Best Follow this and additional works at: https://digitalcommons.tacoma.uw.edu/ias_pub Recommended Citation Shugar, D. H.; Colorado, K. A.; Clague, J. J.; Willis, M. J.; and Best, J. L., "‘Boundary’: Mapping and Visualizing Climatically Changed Landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon" (2018). SIAS Faculty Publications. 895. https://digitalcommons.tacoma.uw.edu/ias_pub/895 This Article is brought to you for free and open access by the School of Interdisciplinary Arts and Sciences at UW Tacoma Digital Commons. It has been accepted for inclusion in SIAS Faculty Publications by an authorized administrator of UW Tacoma Digital Commons. Journal of Maps ISSN: (Print) 1744-5647 (Online) Journal homepage: http://www.tandfonline.com/loi/tjom20 ‘Boundary’: mapping and visualizing climatically changed landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon D. H. Shugar, K. A. Colorado, J. J. Clague, M. J. Willis & J. L. Best To cite this article: D. H. Shugar, K. A. Colorado, J. J. Clague, M. J. Willis & J. L. Best (2018): ‘Boundary’: mapping and visualizing climatically changed landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon, Journal of Maps, DOI: 10.1080/17445647.2018.1467349 To link to this article: https://doi.org/10.1080/17445647.2018.1467349 © 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps Published online: 04 Jun 2018. Submit your article to this journal Article views: 448 View Crossmark data Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tjom20 JOURNAL OF MAPS, 2018 https://doi.org/10.1080/17445647.2018.1467349 ‘Boundary’: mapping and visualizing climatically changed landscapes at Kaskawulsh Glacier and Kluane Lake, Yukon D. H. Shugar a, K. A. Coloradob,c,d,e, J. J. Clague f, M. J. Willis g and J. L. Best h aWater, Sediment, Hazards and Earth-surface Dynamics (WaterSHED) Lab, School of Interdisciplinary Arts and Sciences, University of Washington Tacoma, Tacoma, WA, USA; bNational Oceanic and Atmospheric Administration (NOAA), Silver Spring, MD, USA; cDirección Nacional del Antártico (DNA); dVancouver Maritime Museum, Vancouver, BC, Canada; eUniversity of Northern British Columbia, Prince George, Canada; fCentre for Natural Hazards Research, Department of Earth Sciences, Simon Fraser University, Burnaby, BC, Canada; gCooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA; hDepartments of Geology, Geography and GIS, Mechanical Science and Engineering and Ven Te Chow Hydrosystems Laboratory, University of Illinois, Urbana, IL, USA ABSTRACT ARTICLE HISTORY This paper describes a collaboration between a visual artist and geoscientists, who together Received 5 July 2017 viewed the same rugged, high mountain landscape through different, yet complementary, Revised 4 December 2017 lenses. We pair scientific mapping and historic comparative photography with a series of Accepted 12 April 2018 site-specific sculptural installations to interpret the dramatic geological changes that KEYWORDS occurred at Kaskawulsh Glacier, Yukon, in the spring of 2016. In the summer of that year, Climate change; glacier; artist K.A. Colorado accompanied geoscientists D.H. Shugar, J.J. Clague, and J.L. Best to the sculpture; boundary; terminus of Kaskawulsh Glacier, as well as Kluane Lake downstream of the glacier, to mountain; river piracy document the landscape changes that occurred earlier in the year. The Boundary images were created as on-site, three-dimensional, artistic interpretations of the markedly changed boundaries that occurred as a result of climate-induced glacier retreat and the sudden subcontinental-scale reorganization of drainage. Both the scientific study conducted by the geomorphologists and the art installations created by the artist were performed simultaneously. The Boundary installation art project, together with satellite imagery and historical photographs, conveys the death of Slims River as a result of climate change. 1. Introduction such change and reach people in different ways. Here, we marry maps and photographs used to explain the Landscapes undergo change over a wide range of tem- science of such landscape change with new and different poral and spatial scales and in response to many auto- portrayals of boundaries within the changed landscape genic and allogenic drivers. Such change can be slow revealed by art. We seek to support a view that art can and imperceptible but also, when a threshold or tipping lie at the center of an ‘eARTh science’ representation, point is reached, can be sudden and catastrophic. Slow here illustrated by collaboration between geomorpholo- hillside creep and catastrophic landslides are examples gists and an artist and their observations of rapid land- of such scale changes acting on one geomorphic scapechangeviewedthroughtwodifferentlenses. element. Climate change also ushers in new conditions and environmental change, and anthropogenically induced change is currently reshaping processes and 2. Late Holocene evolution of Kaskawulsh landscape response in many parts of the world. Such Glacier changes also frequently yield boundaries between new and old, between changed and static, and between Our physical science team approached the phenom- one geomorphic state and another. In this paper, we enon of boundary change at Kaskawulsh Glacier describe one such sudden change – to a river drainage using a series of new and historical maps of the glacier network – that is the product of climate change within terminus and its associated glacial lakes. Kaskawulsh the industrial era. Although the scientific publication Glacier is one of the largest valley glaciers flowing east- arising from our work (Shugar et al., 2017) reached a ward from the St. Elias Mountains (Figure 1), and wide audience through press coverage in print (e.g. scientists have shown that this glacier achieved its Devlin, 2017; Schwartz, 2017), radio (e.g. BBC World maximum Little Ice Age (LIA) extent between ∼AD Service, 2017; CBC The Current, 2017), and online 1717 and the 1750s (Borns & Goldthwait, 1966; Den- (e.g. Frostenson, 2017; Kingdon, 2017; Struzik, 2017), ton & Stuiver, 1966; Reyes, Luckman, Smith, Clague, art can provide another medium by which to portray & Van Dorp, 2006). During this LIA ice advance, a CONTACT D. H. Shugar [email protected] Water, Sediment, Hazards and Earth-surface Dynamics (WaterSHED) Lab, School of Interdisciplinary Arts and Sciences, University of Washington Tacoma, Tacoma, WA 98402, USA © 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. 2 D. SHUGAR ET AL. Figure 1. Location map of study area in southwest Yukon. Numbered dots refer to locations of historic photos (Figure 3) and Bound- ary installation photos (Figures 4–11). sediment fan was built by meltwater flowing from the catchments that discharged into different oceans. Ice nearby terminus of Kaskawulsh Glacier, raising the retreat did not begin until the late nineteenth century, level of a river that formerly drained south from Kluane and by 1972 (the first Landsat satellite scene), the eastern Lake. At the LIA maximum, the glacier extended across and western lobes had retreated ∼1.5 and 1.9 km, respect- the valley occupied by the Slims and Kaskawulsh rivers, ively, from the LIA terminal moraine. Between 1972 and and its terminus split into two lobes around a promi- 2016, the glacier retreated a further 0.1–1.1 km. The nent bedrock hill (Figures 1–3). Some of the meltwater width-averaged retreat of Kaskawulsh Glacier between from the glacier discharged north via Slims River into 1899 and 2016 was 1.9 km (Shugar et al., 2017). Kluane Lake, and eventually into the Bering Sea, As Kaskawulsh Glacier retreated, proglacial lakes while the remainder discharged via Kaskawulsh River formed at its terminus and fed large braided rivers. into Alsek River and from there to the North Pacific The lakes –‘Slims Lake’ on the west side of the glacier Ocean. Kaskawulsh Glacier thus fed water across a terminus and ‘Kaskawulsh Lake’ on the east – drainage divide and a border between two river expanded dramatically toward the end of the twentieth JOURNAL OF MAPS 3 Figure 2. Maps showing changes in the terminus of Kaskawulsh Glacier since the LIA and lake growth since 1972. (A) Contour map (interval 100 m) overlain by dashed lines indicating the glacier terminus positions in ∼1717, 1972, and 2016, with gray polygons indicating the extent of proglacial lakes in 1972, 2000, and 2016. (B) The same terminus positions and lake extents as in (A), except with a 2-m satellite-derived DEM as a background. Note that contour lines in (A) were produced from the same DEM as shown in (B), but with 100 m intervals. The 2-m DEM was derived from along-track stereo WorldView-1 imagery (29 November 2012) provided by the DigitalGlobe Foundation, and constructed using the SETSM algorithm (Noh & Howat, 2015). Outlines of the Slims and Kaska- wulsh rivers were digitized from a SPOT5 satellite image from 18 June 2016. The camera icon in (B) shows the approximate location and orientation of the photo stations used to acquire the images in Figure 3. century (Figure 2, Main Map). In the spring of 2016, and lake extents were digitized manually in ArcGIS. Slims Lake suddenly drained into Kaskawulsh Lake, Figure 2(B) is underpinned by a hillshaded digital thereby beheading Slims River (Shugar et al., 2017).