Accelerating Thermokarst Transforms Ice‐Cored Terrain Triggering a Downstream Cascade to the Ocean

[1]  A. Dyke,et al.  Major end moraines of Younger Dryas age on Wollaston Peninsula, Victoria Island, Canadian Arctic: implications for paleoclimate and for formation of hummocky moraine , 2000 .

[2]  Robert H. Fraser,et al.  Increased precipitation drives mega slump development and destabilization of ice-rich permafrost terrain, northwestern Canada , 2015 .

[3]  Denis Lacelle,et al.  Climatic and geomorphic factors affecting contemporary (1950–2004) activity of retrogressive thaw slumps on the Aklavik Plateau, Richardson Mountains, NWT, Canada , 2010 .

[4]  Kenneth M. Hinkel,et al.  Patterns of soil temperature and moisture in the active layer and upper permafrost at Barrow, Alaska: 1993 1999 , 2001 .

[5]  Trevor C. Lantz,et al.  Climate-driven thaw of permafrost preserved glacial landscapes, northwestern Canada , 2017 .

[6]  Robert H. Fraser,et al.  Distribution and growth of thaw slumps in the Richardson Mountains-Peel Plateau region, northwestern Canada , 2015 .

[7]  T. F. Morris,et al.  Quaternary geology of Prince of Wales Island, Arctic Canada , 1992 .

[8]  Guido Grosse,et al.  Vulnerability and feedbacks of permafrost to climate change , 2011 .

[9]  Trevor C. Lantz,et al.  Acceleration of thaw slump activity in glaciated landscapes of the Western Canadian Arctic , 2016 .

[10]  Anna Liljedahl,et al.  Pan-Arctic ice-wedge degradation in warming permafrost and its influence on tundra hydrology , 2016 .

[11]  Trevor C. Lantz,et al.  Increasing rates of retrogressive thaw slump activity in the Mackenzie Delta region, N.W.T., Canada , 2008 .

[12]  P. Worsley.  Context of relict Wisconsinan glacial ice at Angus Lake, SW Banks Island, western Canadian Arctic and stratigraphic implications , 1999 .

[13]  S. Kokelj,et al.  The impacts of thawing permafrost on the chemistry of lakes across the subarctic boreal‐tundra transition, Mackenzie Delta region, Canada , 2009 .

[14]  Ian D. Clark,et al.  Thawing of massive ground ice in mega slumps drives increases in stream sediment and solute flux across a range of watershed scales , 2013 .

[15]  Hanno Meyer,et al.  Modern and Late Holocene Retrogressive Thaw Slump Activity on the Yukon Coastal Plain and Herschel Island, Yukon Territory, Canada , 2012 .

[16]  John H. Bradford,et al.  Sediment and nutrient delivery from thermokarst features in the foothills of the North Slope, Alaska: Potential impacts on headwater stream ecosystems , 2008 .

[17]  David J. A. Evans,et al.  Controlled moraines: origins, characteristics and palaeoglaciological implications , 2009 .

[18]  Ulrike Herzschuh,et al.  Terrain controls on the occurrence of coastal retrogressive thaw slumps along the Yukon Coast, Canada , 2017 .

[19]  Kenji Yoshikawa,et al.  Thermal state of permafrost in North America: a contribution to the international polar year , 2010 .

[20]  Scott F. Lamoureux,et al.  Erosion dynamics following localized permafrost slope disturbances , 2014 .

[21]  James P. McNamara,et al.  Arctic Landscapes in Transition: Responses to Thawing Permafrost , 2010 .

[22]  John England,et al.  Paleoglaciological insights from the age and morphology of the Jesse moraine belt, western Canadian Arctic , 2012 .

[23]  H. French,et al.  Nature and origin of ground ice, Sandhills Moraine, southwest Banks Island, Western Canadian Arctic , 1988 .

[24]  M. Leibman.  Cryogenic landslides on the Yamal Peninsula, Russia: Preliminary observations , 1995 .

[25]  A. Lewkowicz,et al.  Headwall retreat of ground-ice slumps, Banks Island, Northwest Territories , 1987 .

[26]  H. Craig.  Isotopic Variations in Meteoric Waters , 1961, Science.