1932

Abstract

Glaciers offer the potential to reconstruct past climate over timescales from decades to millennia. They are found on nearly every continent, and at the Last Glacial Maximum, glaciers were larger in all regions on Earth. The physics of glacier-climate interaction are relatively well understood, and glacier models can be used to reconstruct past climate from geological evidence of past glacier extent. This can lead to significant insights regarding past, present, and future climate. For example, glacier modeling has demonstrated that the near-ubiquitous global pattern of glacier retreat during the last few centuries resulted from a global-scale climate warming of ∼1°C, consistent with instrumental data and climate proxy records. Climate reconstructions from glaciers have also demonstrated that the tropics were colder at the Last Glacial Maximum than was originally inferred from sea surface temperature reconstructions. Future efforts to reconstruct climate from glaciers may provide new constraints on climate sensitivity to CO forcing, polar amplification of climate change, and more.

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2017-08-30
2024-10-04
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Literature Cited

  1. Adhikari S, Marshall SJ. 2013. Influence of high-order mechanics on simulation of glacier response to climate change: insights from Haig Glacier, Canadian Rocky Mountains. Cryosphere 7:1527–41 [Google Scholar]
  2. Anderson BM, Lawson W, Owens I, Goodsell B. 2006. Past and future mass balance of ‘Ka Roimata o Hine Hukatere’ Franz Josef Glacier, New Zealand. J. Glaciol. 52:597–607 [Google Scholar]
  3. Anderson BM, Mackintosh AN. 2012. Controls on mass balance sensitivity of maritime glaciers in the Southern Alps, New Zealand: the role of debris cover. J. Geophys. Res. 117:F01003 [Google Scholar]
  4. Anderson BM, Mackintosh AN. 2006. Temperature change is the major driver of late-glacial and Holocene glacier fluctuations in New Zealand. Geology 34:121–34 [Google Scholar]
  5. Anderson LS, Roe GH, Anderson RS. 2014. The effects of interannual climate variability on the moraine record. Geology 42:55–58 [Google Scholar]
  6. Applegate PJ, Urban NM, Keller K, Lowell TV, Laabs BJC. et al. 2012. Improved moraine age interpretations through explicit matching of geomorphic process models to cosmogenic nuclide measurements from single landforms. Quat. Res. 77:293–304 [Google Scholar]
  7. Archer D, Pierrehumbert RT. 2011. The Warming Papers: The Scientific Foundation for the Climate Change Forecast Chichester, UK: Wiley-Blackwell [Google Scholar]
  8. Bahr DB, Pfeffer WT, Sassolas C, Meier MF. 1998. Response time of glaciers as a function of size and mass balance: 1. Theory. J. Geophys. Res. Solid Earth 103:9777–82 [Google Scholar]
  9. Balco G. 2011. Contributions and unrealized potential contributions of cosmogenic-nuclide exposure dating to glacier chronology, 1990–2010. Quat. Sci. Rev. 30:3–27 [Google Scholar]
  10. Barth C, Boyle DP, Hatchett BJ, Bassett SD, Garner CB, Adams KD. 2016. Late Pleistocene climate inferences from a water balance model of Jakes Valley, Nevada (USA). J. Paleolimnol. 56:109 [Google Scholar]
  11. Bartlein PJ, Harrison SP, Brewer S, Connor S, Davis BAS. et al. 2011. Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis. Clim. Dyn. 37:775–802 [Google Scholar]
  12. Benn DI, Evans DJA. 2010. Glaciers and Glaciation New York: Routledge., 2nd ed.. [Google Scholar]
  13. Benn DI, Kirkbride MK, Owen LA, Brazier V. 2003. Glaciated valley landsystems. Glacial Landsystems DJA Evans 372–406 London: Arnold [Google Scholar]
  14. Benn DI, Warren CR, Mottram RH. 2007. Calving processes and the dynamics of calving glaciers. Earth-Sci. Rev. 82:143–79 [Google Scholar]
  15. Berger A, Loutre MF. 1991. Insolation values for the climate of the last 10 million years. Quat. Sci. Rev. 10:297–317 [Google Scholar]
  16. Betts AK, Ridgway W. 1992. Tropical boundary layer equilibrium in the last ice age. J. Geophys. Res. Atmos. 97:2529–34 [Google Scholar]
  17. Birkel SD, Putnam AE, Denton GH, Koons PO, Fastook JL. et al. 2012. Climate inferences from a glaciological reconstruction of the Late Pleistocene Wind River Ice Cap, Wind River Range, Wyoming. Arctic Antarct. Alp. Res. 44:265–76 [Google Scholar]
  18. Braconnot P, Harrison SP, Kageyama M, Bartlein PJ, Masson-Delmotte V. et al. 2012. Evaluation of climate models using palaeoclimatic data. Nat. Clim. Change 2:417–24 [Google Scholar]
  19. Bradley RS, Keimig FT, Diaz HF, Hardy DR. 2009. Recent changes in freezing level heights in the Tropics with implications for the deglacierization of high mountain regions. Geophys. Res. Lett. 36:LI7701 [Google Scholar]
  20. Braithwaite RJ. 1981. On glacier energy balance, ablation, and air temperature. J. Glaciol. 27:381–91 [Google Scholar]
  21. Braithwaite RJ. 1995. Positive degree-day factors for ablation on the Greenland ice sheet studied by energy-balance modelling. J. Glaciol. 41:153–60 [Google Scholar]
  22. Bravo C, Rojas M, Anderson BM, Mackintosh AN, Sagredo E, Moreno PI. 2015. Modelled glacier equilibrium line altitudes during the mid-Holocene in the southern mid-latitudes. Clim. Past 11:1575–86 [Google Scholar]
  23. Broecker WS, Denton GH. 1990. The role of ocean-atmosphere reorganizations in glacial cycles. Quat. Sci. Rev. 9:305–41 [Google Scholar]
  24. Budd WF, Jenssen D. 1975. Numerical modelling of glacier systems. In Snow and Ice Symposium—Neiges et Glaces,257–91 Wallingford, UK: IAHS [Google Scholar]
  25. Carey M. 2007. The history of ice: how glaciers became an endangered species. Environ. Hist. 12:3497–527 [Google Scholar]
  26. Clark PU, Dyke AS, Shakun JD, Carlson AE, Clark J. et al. 2009. The Last Glacial Maximum. Science 325:710–14 [Google Scholar]
  27. Clarke GKC, Jarosch AH, Anslow FS, Radic V, Menounos B. 2015. Projected deglaciation of western Canada in the twenty-first century. Nat. Geosci. 8:372–77 [Google Scholar]
  28. Clarke GKC, Schmok JP, Ommanney CSL, Collins SG. 1986. Characteristics of surge-type glaciers. J. Geophys. Res. Solid Earth 91:7165–80 [Google Scholar]
  29. Cogley JG, Hock R, Rasmussen LA, Arendt AA, Bauder A. et al. 2011. Glossary of Glacier Mass Balance and Related Terms Paris: UNESCO-IHP [Google Scholar]
  30. Collier E, Maussion F, Nicholson LI, Mölg T, Immerzeel WW, Bush ABG. 2015. Impact of debris cover on glacier ablation and atmosphere–glacier feedbacks in the Karakoram. Cryosphere 9:1617–32 [Google Scholar]
  31. Cruikshank J. 2001. Glaciers and climate change: perspectives from oral tradition. Arctic 54:377–93 [Google Scholar]
  32. Cuffey KM, Patterson WSB. 2010. The Physics of Glaciers Oxford, UK: Butterworth-Heinemann [Google Scholar]
  33. Cullen NJ, Conway JP. 2015. A 22 month record of surface meteorology and energy balance from the ablation zone of Brewster Glacier, New Zealand. J. Glaciol. 61:931–46 [Google Scholar]
  34. Davies BJ, Golledge NR, Glasser NF, Carrivick JL, Ligtenberg SRM. et al. 2014. Modelled glacier response to centennial temperature and precipitation trends on the Antarctic Peninsula. Nat. Clim. Change 4:993–98 [Google Scholar]
  35. Denton GH, Anderson RF, Toggweiler JR, Edwards RL, Schaefer JM, Putnam AE. 2010. The last glacial termination. Science 328:1652–56 [Google Scholar]
  36. Denton GH, Hendy CH. 1994. Younger Dryas age advance of Franz Josef Glacier in the Southern Alps of New Zealand. Science 264:1434–37 [Google Scholar]
  37. Denton GH, Karlén W. 1973. Holocene climatic variations—their pattern and possible cause. Quat. Res. 3:155–205 [Google Scholar]
  38. Doughty AM, Anderson BM, Mackintosh AN, Kaplan MR, Vandergoes MJ. et al. 2013. Evaluation of Late Glacial temperatures in the Southern Alps of New Zealand based on glacier modelling at Irishman Stream, Ben Ohau Range. Quat. Sci. Rev. 74:160–69 [Google Scholar]
  39. Doughty AM, Mackintosh AN, Anderson BM, Dadic R, Putnam AE. et al. 2017. An exercise in glacier length modeling: Interannual climatic variability alone cannot explain Holocene glacier fluctuations in New Zealand. Earth Planet. Sci. Lett. 470:48–53 [Google Scholar]
  40. Dowdeswell JA, Hagen JO, Björnsson H, Glazovsky AF, Harrison WD. et al. 1997. The mass balance of Circum-Arctic glaciers and recent climate change. Quat. Res. 48:1–14 [Google Scholar]
  41. Eaves SR, Mackintosh AN, Anderson BM, Doughty AM, Townsend DB. et al. 2016. The Last Glacial Maximum in the central North Island, New Zealand: palaeoclimate inferences from glacier modelling. Clim. Past 12:943–60 [Google Scholar]
  42. Egholm DL, Knudsen MF, Clark CD, Lesemann JE. 2011. Modeling the flow of glaciers in steep terrains: the integrated second-order shallow ice approximation (iSOSIA). J. Geophys. Res. 116:F02012 [Google Scholar]
  43. Eisenman I, Huybers P. 2006. Integrated summer insolation calculations IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series # 2006-079, updated Aug Paleoclimatology Program Boulder, CO: [Google Scholar]
  44. Fitzharris BB, Clare GR, Renwick J. 2007. Teleconnections between Andean and New Zealand glaciers. Glob. Planet. Change 59:159–74 [Google Scholar]
  45. Fountain AG, Dana GL, Lewis KJ, Vaughn BH, McKnight DH. 1998. Glaciers of the McMurdo Dry Valleys, Southern Victoria Land, Antarctica. Ecosystem Dynamics in a Polar Desert: The McMurdo Dry Valleys, Antarctica JC Priscu 65–75 Washington, DC: Amer. Geophys. Union [Google Scholar]
  46. Frierson DMW. 2008. Midlatitude static stability in simple and comprehensive general circulation models. J. Atmos. Sci. 65:1049–62 [Google Scholar]
  47. Goehring BM, Schaefer JM, Schluechter C, Lifton NA, Finkel RC. et al. 2011. The Rhone Glacier was smaller than today for most of the Holocene. Geology 39:679–82 [Google Scholar]
  48. Golledge NR, Mackintosh AN, Anderson BM, Buckley KM, Doughty AM. et al. 2012. Last Glacial Maximum climate in New Zealand inferred from a modelled Southern Alps icefield. Quat. Sci. Rev. 46:30–45 [Google Scholar]
  49. Gosse JC, Phillips FM. 2001. Terrestrial in situ cosmogenic nuclides: theory and application. Quat. Sci. Rev. 20:1475–560 [Google Scholar]
  50. Greuell W. 1992. Hintereisferner, Austria: mass-balance reconstruction and numerical modelling of the historical length variations. J. Glaciol. 38:233–44 [Google Scholar]
  51. Haeberli W, Brandova D, Burga C, Egli M, Frauenfelder R. et al. 2003. Methods for absolute and relative age dating of rock-glacier surface in alpine permafrost. Proceedings of the Eight International Conference on Permafrost M Philips, SM Springman, LU Arenson 343–48 Lisse, Neth.: Balkema [Google Scholar]
  52. Hansen J, Sato M, Russell G, Kharecha P. 2013. Climate sensitivity, sea level and atmospheric carbon dioxide. Philos. Trans. R. Soc. A 371:20120294 [Google Scholar]
  53. He F, Shakun JD, Clark PU, Carlson AE, Liu Z. et al. 2013. Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation. Nature 494:81–85 [Google Scholar]
  54. Herman F, Beyssac O, Brughelli M, Lane SN, Leprince S. et al. 2015. Erosion by an Alpine glacier. Science 350:193–95 [Google Scholar]
  55. Hock R. 1999. A distributed temperature-index ice- and snowmelt model including potential direct solar radiation. J. Glaciol. 45:101–11 [Google Scholar]
  56. Hock R. 2005. Glacier melt: a review of processes and their modelling. Prog. Phys. Geogr. 29:362–91 [Google Scholar]
  57. Hubbard A. 1999. High-resolution modeling of the advance of the Younger Dryas Ice Sheet and its climate in Scotland. Quat. Res. 52:27–43 [Google Scholar]
  58. Hubbard A, Blatter H, Nienow P, Mair D, Hubbard B. 1998. Comparison of a three-dimensional model for glacier flow with field data from Haut Glacier d'Arolla, Switzerland. J. Glaciol. 44:368–78 [Google Scholar]
  59. Huss M, Hock R, Bauder A, Funk M. 2010. 100-year mass changes in the Swiss Alps linked to the Atlantic Multidecadal Oscillation. Geophys. Res. Lett. 37:L10501 [Google Scholar]
  60. IPCC (Intergov. Panel Clim. Change). 2013. Climate Change 2013: The Physical Science Basis Cambridge, UK: Cambridge Univ. Press [Google Scholar]
  61. Jarosch AH, Anslow FS, Clarke GKC. 2012. High-resolution precipitation and temperature downscaling for glacier models. Clim. Dyn. 38:391–409 [Google Scholar]
  62. Jóhannesson T, Raymond C, Waddington E. 1989. Timescale for adjustment of glaciers to changes in mass balance. J. Glaciol. 35:355–69 [Google Scholar]
  63. Jomelli V, Favier V, Vuille M, Braucher R, Martin L. et al. 2014. A major advance of tropical Andean glaciers during the Antarctic cold reversal. Nature 513:224–28 [Google Scholar]
  64. Kamb B. 1987. Glacier surge mechanism based on linked cavity configuration of the basal water conduit system. J. Geophys. Res. Solid Earth 92:9083–100 [Google Scholar]
  65. Kaplan MR, Schaefer JM, Denton GH, Barrell DJA, Chinn TJH. et al. 2010. Glacier retreat in New Zealand during the Younger Dryas stadial. Nature 467:194–97 [Google Scholar]
  66. Kaplan MR, Schaefer JM, Denton GH, Doughty AM, Barrell DJA. et al. 2013. The anatomy of long-term warming since 15 ka in New Zealand based on net glacier snowline rise. Geology 41:8887 [Google Scholar]
  67. Kessler MA, Anderson RS, Stock GM. 2006. Modeling topographic and climatic control of east-west asymmetry in Sierra Nevada glacier length during the Last Glacial Maximum. J. Geophys. Res. Earth Surf. 111:F02002 [Google Scholar]
  68. Le Meur E, Gagliardini O, Zwinger T, Ruokolainen J. 2004. Glacier flow modelling: a comparison of the Shallow Ice Approximation and the full-Stokes solution. Comptes Rendus Physique 5:709–22 [Google Scholar]
  69. Leclercq P, Oerlemans J. 2012. Global and hemispheric temperature reconstruction from glacier length fluctuations. Clim. Dyn. 38:1065–79 [Google Scholar]
  70. Lüthi MP. 2009. Transient response of idealized glaciers to climate variations. J. Glaciol. 55:918–30 [Google Scholar]
  71. Machguth H, Purves RS, Oerlemans J, Hoelzle M, Paul F. 2008. Exploring uncertainty in glacier mass balance modelling with Monte Carlo simulation. Cryosphere 2:191–204 [Google Scholar]
  72. Mackintosh AN, Dugmore AJ, Hubbard AL. 2002. Holocene climatic changes in Iceland: evidence from modelling glacier length fluctuations at Sólheimajökull. Quat. Int. 91:139–52 [Google Scholar]
  73. Mackintosh AN, Anderson BM, Lorrey A, Renwick JA, Frei P, Dean SM. 2017. Regional cooling caused recent New Zealand glacier advances in a period of global warming. Nature Commun 8:14202 [Google Scholar]
  74. Malone AGO, Pierrehumbert RT, Lowell TV, Kelly MA, Stroup JS. 2015. Constraints on southern hemisphere tropical climate change during the Little Ice Age and Younger Dryas based on glacier modeling of the Quelccaya Ice Cap, Peru. Quat. Sci. Rev. 125:106–16 [Google Scholar]
  75. MARGO (Multiproxy Approach Reconstr. Glacial Ocean Surf.). 2009. Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum. Nat. Geosci. 2:127–32 [Google Scholar]
  76. Marzeion B, Cogley JG, Richter K, Parkes D. 2014. Attribution of global glacier mass loss to anthropogenic and natural causes. Science 345:919–21 [Google Scholar]
  77. McKinnon KA, Mackintosh AN, Anderson BM, Barrell DJA. 2012. The influence of sub-glacial bed evolution on ice extent: a model-based evaluation of the Last Glacial Maximum Pukaki glacier, New Zealand. Quat. Sci. Rev. 57:46–57 [Google Scholar]
  78. McNabb RW, Hock R. 2014. Alaska tidewater glacier terminus positions, 1948–2012. J. Geophys. Res. Earth Surf. 119:153–67 [Google Scholar]
  79. Meier MF, Post A. 1987. Fast tidewater glaciers. J. Geophys. Res. Solid Earth 92:9051–58 [Google Scholar]
  80. Mercer J. 1961. The response of fjord glaciers to changes in the firn limit. J. Glaciol. 3:850–58 [Google Scholar]
  81. Milankovitch M. 1941. Canon of Insolation and the Ice Age Problem Belgrade, Serbia: Textbook Publishing [Google Scholar]
  82. Mölg T, Cullen NJ, Hardy DR, Winkler M, Kaser G. 2009. Quantifying climate change in the tropical midtroposphere over East Africa from glacier shrinkage on Kilimanjaro. J. Clim. 22:4162–81 [Google Scholar]
  83. Mölg T, Kaser G. 2011. A new approach to resolving climate-cryosphere relations: downscaling climate dynamics to glacier-scale mass and energy balance without statistical scale linking. J. Geophys. Res. Atmos. 116:D16101 [Google Scholar]
  84. Mölg T, Kaser G, Cullen NJ. 2010. Glacier loss on Kilimanjaro is an exceptional case. PNAS 107:E68 [Google Scholar]
  85. New M, Lister D, Hulme M, Makin I. 2002. A high-resolution data set of surface climate over global land areas. Clim. Res. 21:1–25 [Google Scholar]
  86. Nye JF. 1951. The flow of glaciers and ice-sheets as a problem in plasticity. Proc. R. Soc. A 207:554–72 [Google Scholar]
  87. Nye JF. 1960. The response of glaciers and ice-sheets to seasonal and climatic changes. Proc. R. Soc. A 256:559–84 [Google Scholar]
  88. Nye JF. 1965. A numerical method of inferring the budget history of a glacier from its advance and retreat. J. Glaciol. 35:355–69 [Google Scholar]
  89. Oerlemans J. 1986. An attempt to simulate historic front variations of Nigardsbreen, Norway. Theor. Appl. Climatol. 37:126–35 [Google Scholar]
  90. Oerlemans J. 1992. Climate sensitivity of glaciers in southern Norway: application of an energy-balance model to Nigardsbreen, Hellstugubreen and Alfotbreen. J. Glaciol. 38:223–44 [Google Scholar]
  91. Oerlemans J. 1997. A flowline model for Nigardsbreen, Norway: projection of future glacier length based on dynamic calibration with the historic record. J. Glaciol. 24:382–89 [Google Scholar]
  92. Oerlemans J. 2001. Glaciers and Climate Change Rotterdam: A.A. Balkema [Google Scholar]
  93. Oerlemans J. 2005. Extracting a climate signal from 169 glacier records. Science 308:675–77 [Google Scholar]
  94. Oerlemans J, Knap WH. 1998. A 1 year record of global radiation and albedo in the ablation zone of Morteratschgletscher, Switzerland. J. Glaciol. 44:231–38 [Google Scholar]
  95. Ohmura A. 2001. Physical basis for the temperature-based melt-index method. J. Appl. Meteorol. 40:4753–61 [Google Scholar]
  96. Ohmura A, Kasser P, Funk M. 1992. Climate at the equilibrium line of glaciers. J. Glaciol. 38:397–409 [Google Scholar]
  97. Oreskes N, Shrader-Frechette K, Belitz K. 1994. Verification, validation, and confirmation of numerical models in the Earth sciences. Science 263:641–46 [Google Scholar]
  98. Painter TH, Flanner MG, Kaser G, Marzeion B, VanCuren RA, Abdalati W. 2013. End of the Little Ice Age in the Alps forced by industrial black carbon. PNAS 110:15216–21 [Google Scholar]
  99. Pellicciotti F, Carenzo M, Bordoy R, Stoffel M. 2014. Changes in glaciers in the Swiss Alps and impact on basin hydrology: current state of the art and future research. Sci. Total Environ. 493:1152–70 [Google Scholar]
  100. Pfeffer WT, Arendt AA, Bliss A, Bolch T, Cogley JG. et al. 2014. The Randolph Glacier Inventory: a globally complete inventory of glaciers. J. Glaciol. 60:537–52 [Google Scholar]
  101. Pierrehumbert RT. 2011. Principles of Planetary Climate Cambridge, UK: Cambridge Univ. Press [Google Scholar]
  102. Plummer MA, Phillips FM. 2003. A 2-D numerical model of snow/ice energy balance and ice flow for paleoclimatic interpretation of glacial geomorphic features. Quat. Sci. Rev. 22:1389–406 [Google Scholar]
  103. Pollard D, DeConto RM. 2009. Modelling West Antarctic ice sheet growth and collapse through the past five million years. Nature 458:329–32 [Google Scholar]
  104. Porter SC. 1975. Equilibrium-line altitudes of late Quaternary glaciers in the Southern Alps, New Zealand. Quat. Res. 5:27–47 [Google Scholar]
  105. Purdie H, Anderson B, Chinn T, Owens I, Mackintosh A, Lawson W. 2014. Franz Josef and Fox Glaciers, New Zealand: historic length records. Glob. Planet. Change 121:41–52 [Google Scholar]
  106. Putkonen J, Swanson T. 2003. Accuracy of cosmogenic ages for moraines. Quat. Res. 59:255–61 [Google Scholar]
  107. Putnam AE, Schaefer JM, Denton GH, Barrell DJA, Andersen BG. et al. 2013a. Warming and glacier recession in the Rakaia valley, Southern Alps of New Zealand, during Heinrich Stadial 1. Earth Planet. Sci. Lett. 382:98–110 [Google Scholar]
  108. Putnam AE, Schaefer JM, Denton GH, Barrell DJA, Birkel SD. et al. 2013b. The Last Glacial Maximum at 44°S documented by a 10Be moraine chronology at Lake Ohau, Southern Alps of New Zealand. Quat. Sci. Rev. 62:114–41 [Google Scholar]
  109. Putnam AE, Schaefer JM, Denton GH, Barrell DJA, Finkel RC. et al. 2012. Regional climate control of glaciers in New Zealand and Europe during the pre-industrial Holocene. Nat. Geosci. 5:627–30 [Google Scholar]
  110. Reichert BK, Bengtsson L, Oerlemans J. 2002. Recent glacier retreat exceeds internal variability. J. Clim. 15:3069–81 [Google Scholar]
  111. Réveillet M, Rabatel A, Gillet-Chaulet F, Soruco A. 2015. Simulations of changes to Glaciar Zongo, Bolivia (16°S), over the 21st century using a 3-D full-Stokes model and CMIP5 climate projections. Ann. Glaciol. 56:89–97 [Google Scholar]
  112. Rind D, Peteet D. 1985. Terrestrial conditions at the Last Glacial Maximum and CLIMAP sea-surface temperature estimates: Are they consistent?. Quat. Res. 24:1–22 [Google Scholar]
  113. Roe GH. 2005. Orographic precipitation. Annu. Rev. Earth Planet. Sci. 33:645–71 [Google Scholar]
  114. Roe GH. 2011. What do glaciers tell us about climate variability and climate change?. J. Glaciol. 57:567–78 [Google Scholar]
  115. Roe GH, Baker MB. 2014. Glacier response to climate perturbations: an accurate linear geometric model. J. Glaciol. 60:670–84 [Google Scholar]
  116. Roe GH, Baker MB, Herla F. 2017. Centennial glacier retreat as categorical evidence of regional climate change. Nat. Geosci. 10:95–99 [Google Scholar]
  117. Roethlisberger F, Schneebeli W. 1979. Genesis of lateral moraine complexes, demonstrated by fossil soils and tree trunks; indicators of postglacial climatic fluctuations. Moraines and Varves C Schlüchter 387–419 Rotterdam: AA Balkema [Google Scholar]
  118. Rojas M, Moreno P, Kageyama M, Crucifix M, Hewitt C. et al. 2009. The Southern Westerlies during the last glacial maximum in PMIP2 simulations. Clim. Dyn. 32:525–48 [Google Scholar]
  119. Rowan AV, Brocklehurst SH, Schultz DM, Plummer MA, Anderson LS, Glasser NF. 2014. Late Quaternary glacier sensitivity to temperature and precipitation distribution in the Southern Alps of New Zealand. J. Geophys. Res. Earth Surf. 119:1064–81 [Google Scholar]
  120. Schaefer JM, Denton GH, Barrell DJA, Ivy-Ochs S, Kubik PW. et al. 2006. Near-synchronous interhemispheric termination of the Last Glacial Maximum in mid-latitudes. Science 312:1510–13 [Google Scholar]
  121. Schaefer JM, Denton GH, Kaplan M, Putnam A, Finkel RC. et al. 2009. High-frequency Holocene glacier fluctuations in New Zealand differ from the northern signature. Science 324:622–25 [Google Scholar]
  122. Schmittner A, Urban NM, Shakun JD, Mahowald NM, Clark PU. et al. 2011. Climate sensitivity estimated from temperature reconstructions of the Last Glacial Maximum. Science 334:1385–88 [Google Scholar]
  123. Shakun JD, Clark PU, He F, Lifton NA, Liu Z, Otto-Bliesner BL. 2015. Regional and global forcing of glacier retreat during the last deglaciation. Nat. Commun. 6:8059 [Google Scholar]
  124. Shelley M. 1831. Frankenstein; or, The Modern Prometheus London: Henry Colburn and Richard Bentley. , 3rd ed.. [Google Scholar]
  125. Shulmeister J, Davies TR, Evans DJA, Hyatt OM, Tovar DS. 2009. Catastrophic landslides, glacier behaviour and moraine formation—a view from an active plate margin. Quat. Sci. Rev. 28:1085–96 [Google Scholar]
  126. Sigurdsson O, Jonsson T. 1995. Relation of glacier variations to climate changes in Iceland. Ann. Glaciol. 21:263–70 [Google Scholar]
  127. Smith RB. 2006. Progress on the theory of orographic precipitation. Geol. Soc. Am. Spec. Pap. 398:1–16 [Google Scholar]
  128. Stone PH, Carlson JH. 1979. Atmospheric Lapse rate regimes and their parameterization. J. Atmos. Sci. 36:415–23 [Google Scholar]
  129. Thompson LG, Brecher HH, Mosley-Thompson E, Hardy DR, Mark BG. 2009. Glacier loss on Kilimanjaro continues unabated. PNAS 106:19770–75 [Google Scholar]
  130. Williams IN, Pierrehumbert RT, Huber M. 2009. Global warming, convective threshold and false thermostats. Geophys. Res. Lett. 36:L21805 [Google Scholar]
  131. Zemp M, Frey H, Gärtner-Roer I, Nussbaumer SU, Hoelzle M. et al. 2015. Historically unprecedented global glacier decline in the early 21st century. J. Glaciol. 61:745–62 [Google Scholar]
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