Abstract
Future hydroclimate change is expected to generally follow a wet-get-wetter, dry-get-drier (WWDD) pattern, yet key uncertainties remain regionally and over land. It has been previously hypothesized that lake levels of the Last Glacial Maximum (LGM) could map a reverse analog to future hydroclimate changes due to reduction of CO2 levels at this time. Potential complications to this approach include, however, the confounding effects of factors such as the Laurentide Ice Sheet and lake evaporation changes. Using the ensemble output of six coupled climate models, lake energy and water balance models, an atmospheric moisture budget analysis, and additional CO2 sensitivity experiments, we assess the effectiveness of the LGM as a reverse analog for future hydroclimate changes for a transect from the drylands of North America to southern South America. The model ensemble successfully simulates the general pattern of lower tropical lake levels and higher extratropical lake levels at LGM, matching 82% of the lake proxy records. The greatest model-data mismatch occurs in tropical and extratropical South America, potentially as a result of underestimated changes in temperature and surface evaporation. Thermodynamic processes of the mean circulation best explain the direction of lake changes observed in the proxy record, particularly in the tropics and Pacific coasts of the extratropics, and produce a WWDD pattern. CO2 forcing alone cannot account for LGM lake level changes, however, as the enhanced cooling from the Laurentide ice sheet appears necessary to generate LGM dry anomalies in the tropics and to deepen anomalies in the extratropics. LGM performance as a reverse analog is regionally dependent as anti-correlation between LGM and future P − E is not uniformly observed across the study domain.
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References
Alkama R, Marchand L, Ribes A, Decharme B (2013) Detection of global runoff changes: results from observations and CMIP5 experiments. Hydrol Earth Syst Sci 17:2967–2979. https://doi.org/10.5194/hess-17-2967-2013
Allen BD, Anderson RY (2000) A continuous, high-resolution record of late Pleistocene climate variability from the Estancia basin, New Mexico. Geol Soc Am Bull 112:1444–1458
Allison IS (1982) Geology of Pluvial Lake Chewaucan, Lake County, Oregon. Oregon state monographs, studies in geology number eleven. Oregon State University Press, Oregon
Anderson DE, Wells SG (2003) Latest Pleistocene lake highstands in Death Valley, California. In: Enzel Y, Wells SG, Lancaster N (eds) Paleoenvironments and paleohydrology of the Mojave and southern Great Basin Deserts: Geological Society of America Special Paper, vol 368, pp 115–128
Antevs E (1948) The Great Basin, with emphasis on glacial and post-glacial times—climate changes and pre-white man. Bull Univ Utah Biol Ser 38:168–191
Argus DF, Peltier WR (2010) Constraining models of postglacial rebound using space geodesy: a detailed assessment of model ICE-5G (VM2) and its relatives. Geophys J Int 181:697–723
Bacon SN, Burke RM, Pezzopane SK, Jayko AS (2006) Last glacial maximum and Holocene lake levels of Owens Lake, eastern California, USA. Quat Sci Rev 25:1264–1282
Baker PA, Fritz SC (2015) Nature and causes of Quaternary climate variation of tropical South America. Quat Sci Rev 124:31–47
Baker PA, Rigsby CA, Seltzer GO, Fritz SC, Lowenstein TK, Bacher NP, Veliz C (2001) Tropical climate changes at millennial and orbital timescales on the Bolivian Altiplano. Nature 409:698–701
Barnosky CW (1985) Late Quaternary vegetation in the southwestern Columbia Basin, Washington. Quat Res 23:109–122
Bartlein PJ et al (2011) Pollen-based continental climate reconstructions at 6 and 21 ka: a global synthesis. Clim Dyn 37:775–802
Benson LV, Lund SP, Burdett JW, Kashgarian M, Rose TP, Schwartz M (1998) Correlation of late Pleistocene lake level oscillations in Mono Lake, California, with North Atlantic climate events. Quat Res 49:1–10
Benson LV, Smoot JP, Lund SP, Mensing SA, Foit J, Rye FF RO (2013) Insights from a synthesis of old and new climate-proxy data from the Pyramid and Winnemucca lake basins for the period 48 to 11.5 cal ka. Quat Int 310:62–82
Berger AL (1978) Long-term variations of caloric insolation resulting from the Earth’s orbital elements. Quat Res 9:139–167
Berman AL, Silvestri GE, Tonello MS (2016) Differences between Last Glacial Maximum and present-day temperature and precipitation in southern South America. Quat Sci Rev 150:221–233
Berry RW, McCormick CW, Adam DP (1982) Pollen data from a 5-meter Upper Pleistocene Lacustrine Section from Walker Lake, Coconino County, Arizona US Geological Survey Open File Report 82–383
Blard P-H et al (2011) Lake highstands on the Altiplano (Tropical Andes) contemporaneous with Heinrich 1 and the Younger Dryas: new insights from 14C, U-Th dating and d18O of carbonates. Quat Sci Rev 30:3973–3989
Boos WR (2012) Thermodynamic scaling of the hydrological cycle of the Last Glacial Maximum. J Clim 25:992–1006
Braconnot P et al (2012) Evaluation of climate models using palaeoclimatic data. Nat Clim Change 2:417–424
Bradbury JP (2000) Limnologic history of Lago de Pátzcuaro, Michoacán, Mexico for the past 48,000 years: impacts of climate and man. Palaeogeogr Palaeoclimatol Palaeoecol 163:69–95
Bradbury JP, Colman SM, Dean WE (2004) Limnological and climatic environments at Upper Klamath Lake, Oregon during the past 45000 years. J Paleolimnol 31:167–188
Bradley RS, Yuretich RF, Salgado-Labouriau M, Weingarten B (1985) Late Quaternary paleoenvironmental reconstruction using lake sediments from the Venezuelan Andes: preliminary results. Z Gletsch Glazialgeol 21:97–106
Brady EC, Otto-Bliesner BL, Kay JE, Rosenbloom N (2013) Sensitivity to glacial forcing in the CCSM4. J Clim 26:1901–1925
Broccoli AJ (2000) Tropical cooling at the Last Glacial Maximum: an atmosphere-mixed layer ocean model simulation. J Clim 13:951–976
Broecker W (2010) Long-term water prospects in the western United States. J Clim 23:6669–6683
Burbridge RE, Mayle FE, Killeen TJ (2004) Fifty-thousand-year vegetation and climate history of Noel Kempff Mercado National Park. Boliv Amazon Quat Res 61:215–230
Bush MB, Hanselman JA, Hooghiemstra H (2007) Andean montane forests and climate change. In: Bush MB, Flenley JR (eds) Tropical rainforest responses to climate change. Praxis Springer, Chichester, pp 33–48
Byrne MP, O’Gorman PA (2015) The response of precipitation minus evapotranspiration to climate warming: why the “Wet-Get-Wetter, Dry-Get-Drier” scaling does not hold over land. J Clim 28:8078–8092. https://doi.org/10.1175/JCLI-D-15-0369.1
Caballero M, Ortega B, Valadez F, Metcalfe S, Macias JL, Suguira Y (2002) Sta. Cruz Atizapán: a 22-ka lake level record and climatic implications for the late Holocene human occupation in the Upper Lerma Basin, Central Mexico. Palaeogeogr Palaeoclimatol Palaeoecol 186:217–235
Cartwright A, Quade J, Stine S, Adams KD, Broecker W, Cheng H (2011) Chronostratigraphy and lake-level changes of Laguna Cari-Laufquén, Río Negro. Argent Quat Res 76:430–440
Chadwick R, Boutle I, Martin G (2013) Spatial patterns of precipitation change in CMIP5: why the rich do not get richer in the tropics. J Clim 26:3803–3822
Chávez-Lara CM, Roy PD, Pérez L, Muthu Sankar G, Lemus Neri V (2015) Ostracode and C/N based paleoecological record from Santiaguillo basin of subtropical Mexico over last 27 cal kyr BP. Revista Mexicana de Ciencias Geológicas 32:1–10
Chou C, Neelin JD, Chen C-A, Tu J-Y (2009) Evaluating the “Rich-Get-Richer” mechanism in tropical precipitation change under global warming. J Clim 22:1982–2005
Colinvaux PA, DeOliveira PE, Moreno JE, Miller MC, Bush MB (1996) A long pollen record from lowland Amazonia: forest and cooling in glacial times. Science 274:85–88
Colman SM, Bradbury JP, McGeehin JP, Holmes CW, Edginton D, Sarna-Wojcicki AM (2004) Chronology of sediment deposition in Upper Klamath Lake, Oregon. J Paleolimnol 31:139–149
Croft MG (1968) Geology and radiocarbon ages of Late Pleistocene lacustrine clay deposits, southern part of San Joaquin Valley, California. United States Geological Survey Professional Paper, vol 160B, pp 156–161
D’Apolito C, Absy ML, Latrubesse EM (2013) The Hill of Six Lakes revisited: new data and re-evaluation of a key Pleistocene Amazon site. Quat Sci Rev 76:140–155
Dallenbach A, Blunier T, Fluckiger J, Stauffer B, Chappellaz J, Raynaud D (2000) Changes in the atmospheric CH4 gradient between Greenland and Antarctica during the last glacial and the transition to the Holocene. Geophys Res Lett 27:1005–1008
Delcourt HR (1979) Late Quaternary vegetation history of the eastern Highland Rim and adjacent Cumberland Plateau of Tennessee. Ecol Monogr 49:255–280
Denton G, Lowell T, Moreno P, Andersen B, Schluchter B (1999) Interhemispheric linkage of paleoclimate during the last glaciation. Geogr Ann A 81A:167–229
Escobar J et al (2012) A ~ 43-ka record of paleoenvironmental change in the Central American lowlands inferred from stable isotopes of lacustrine ostracods. Quat Sci Rev 37:92–104
Flückiger J, Dallenbach A, Blunier T, Stauffer B, Stocker TF, Raynaud D, Barnola J-M (1999) Variations in atmospheric N2O concentration during abrupt climatic. Changes Sci 285:227–230
Freidel DE (1993) Chronology and climatic controls of late Quaternary lake-level fluctuations in Chewaucan, Fort Rock, and Alkali basins, south-central Oregon [Ph.D. Dissertation]. Ph.D. Dissertation, University of Oregon
Fritz SC et al (2004) Hydrologic variation during the last 170,000 years in the southern hemisphere tropics of South. Am Quat Res 61:95–104
Gonzalez MA, Maidana NI (1998) Post-Wisconsinian paleoenvironments at Salinas del Bebedero basin, San Luis, Argentina. J Paleolimnol 20:353–368
Greve P, Orlowsky B, Mueller B, Sheffield J, Reichstein M, Seneviratne SI (2014) Global assessment of trends in wetting and drying over land. Nat Geosci 7:716–721
Hargreaves JC, Abe-Ouchi A, Annan JD (2007) Linking glacial and future climates through an ensemble of GCM simulations. Clim Past 3:77–87
Held IM, Soden BJ (2006) Robust responses of the hydrological cycle to global warming. J Clim 19:5686–5699
Heusser CJ (1990) Ice age vegetation and climate of subtropical Chile. Palaeogeogr Palaeoclimatol Palaeoecol 80:107–127
Hevly RH (1985) A 50,000 year record of Quaternary environments, Walker Lake, Cocinino Co., Arizona. In: Jacobs BF, Fall PL, Davis OK (eds) Late quaternary vegetation and climates of the American Southwest, vol 16. American Association of Stratigraphic Palynologists Foundation, Dallas, pp 141–154
Hillyer R, Valencia BG, Bush MB, Silman MR, Steinitz-Kannan M (2009) A 24,700-yr paleolimnological history from the Peruvian. Andes Quat Res 71:71–82
Hodell DA et al (2008) An 85-ka record of climate change in lowland Central America. Quat Sci Rev 27:1152–1165
Hostetler SW (1991) Simulation of lake ice and its effect on the late-Pleistocene evaporation rate of Lake Lahontan. Clim Dyn 6:43–48
Hostetler SW, Bartlein PJ (1990) Simulation of lake evaporation with application to modeling lake level variations of Harney-Malheur Lake, Oregon. Water Resour Res 26:2603–2612
Hostetler S, Benson LV (1990) Paleoclimatic implications of the high stand of Lake Lahontan derived from models of evaporation and lake level. Clim Dyn 4:207–217
Ibarra DE, Egger AE, Weaver KL, Harris CR, Maher K (2014) Rise and fall of late Pleistocene pluvial lakes in response to reduced evaporation and precipitation: evidence from Lake Surprise, California. Geol Soc Am Bull 126:1387–1415
Ives PC, Levin B, Oman CL, Rubin M (1967) U.S. Geological Survey radiocarbon dates IX. Radiocarbon 9:505–529
Jacob J, Disnar J-R, Boussafir M, Sifeddine A, Turcq B, Albuquerque ALS (2004) Major environmental changes recorded by lacustrine sedimentary organic matter since the last glacial maximum near the equator (Lagoa do Caçó, NE Brazil). Palaeogeogr Palaeoclimatol Palaeoecol 205:183–197
Kageyama M et al (2013) Mid-Holocene and Last Glacial Maximum climate simulations with the IPSL model—part I: comparing IPSL_CM5A to IPSL_CM4. Clim Dyn 40:2447–2468
Khodri M, Kageyama M, Roche DM (2009) Sensitivity of South American tropical climate to Last Glacial Maximum boundary conditions: focus on teleconnections with tropics and extratropics. In: Vimeux F, Sylvestre F, Khodri M (eds) Past climate variability in South America and surrounding regions. Springer, Berlin, pp 213–238
Kliem P et al (2013) Magnitude, geomorphic response and climate links of lake level oscillations at Laguna Potrok Aike, Patagonian steppe (Argentina). Quat Sci Rev 71:131–146
Kohfeld KE, Graham RM, de Boer AM, Sime LC, Wolff EW, Le Quéré C, Bopp L (2013) Southern hemisphere westerly wind changes during the Last Glacial Maximum: paleo-data synthesis. Quat Sci Rev 68:76–95
Krider PR (1998) Paleoclimatic significance of late Quaternary lacustrine and alluvial stratigraphy, Animas Valley, New Mexico. Quat Res 50:283–289
Kumar S, Allan RP, Zwiers FW, Lawrence DM, Dirmeyer PA (2015) Revisiting trends in wetness and dryness in the presence of internal climate variability and water limitations over land. Geophys Res Lett 42:10867–10875. https://doi.org/10.1002/2015GL066858
Laîné A et al (2009) Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle precipitation. Clim Dyn 32:593–614
Lambeck K, Purcell A, Zhao J, Svensson N-O (2010) The Scandinavian Ice Sheet: From MIS4 to the end of the Last. Glac Maximum Boreas 39:410–435
Lamy F, Kaiser J, Arz HW, Hebbeln D, Ninnemann U, Timm O, Timmermann A, Toggweiler JR (2007) Modulation of the bipolar seesaw in the southeast pacific during termination 1. Earth Planet Sci Lett 259:400–413
Li Y, Morrill C (2010) Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments. Clim Dyn 35:1119–1132
Li G, Harrison SP, Bartlein PJ, Izumi K, Prentice IC (2013) Precipitation scaling with temperature in warm and cold climates: an analysis of CMIP5 simulations. Geophys Res Lett 40:4018–4024. https://doi.org/10.1002/grl.50730
Licciardi JM, Clark PU, Jenson JW, Macayeal DR (1998) Deglaciation of a soft-bedded Laurentide ice sheet. Quat Sci Rev 17:427–448
Lin JC et al (1998) A reassessment of U-Th and 14C ages for Late-Glacial high-frequency hydrological events at Searles Lake, California. Quat Res 49:11–23
Liu Y, Andersen JJ, Williams JW, Jackson ST (2013) Vegetation history in central Kentucky and Tennessee (USA) during the last glacial and deglacial periods. Quat Res 79:189–198
Long A (1966) Late Pleistocene and Recent Chronologies of Playa Lakes in Arizona and New Mexico. University of Arizona
Lora JM, Mitchell JL, Risi C, Tripati AE (2017) North Pacific atmospheric rivers and their influence on western North America at the Last Glacial Maximum. Geophys Res Lett 44:1051–1059
Lozano-García S, Sosa-Nájera S, Sugiura Y, Caballero M (2005) 23,000 year of vegetation history of the Upper Lerma, a tropical high-altitude basin in Central. Mex Quat Res 64:70–82
Lyle M et al (2012) Out of the Tropics: The Pacific, Great Basin Lakes, and Late Pleistocene Water Cycle in the Western United States. Science 337:1629–1633
Markgraf V, Bradbury JP, Forester RM, Singh G, Sternberg RS (1984) San Agustin Plains, New Mexico: age and paleoenvironmental potential reassessed. Quat Res 22:336–343
Markgraf V et al (2000) Paleoclimate reconstruction along the Pole-Equator-Pole transect of the Americas (PEP 1). Quat Sci Rev 19:125–140
Massaferro JI, Moreno PI, Denton GH, Vandergoes M, Dieffenbacher-Krall A (2009) Chironomid and pollen evidence for climate fluctuations during the Last Glacial Termination in NW Patagonia. Quat Sci Rev 28:517–525
Mayle FE, Burbridge R, Killeen TJ (2000) Millennial-scale dynamics of southern Amazonian rain forests. Science 290:2291–2294
McGlue MM, Cohen AS, Ellis GS, Kowler AL (2013) Late Quaternary stratigraphy, sedimentology and geochemistry of an underfilled lake basin in the Puna plateau (northwest Argentina). Basin Res 25:638–658
Metcalfe S, Say A, Black S, McCulloch R, O’Hara S (2002) Wet conditions during the last glaciation in the Chihuahuan Desert, Alta Babicora Basin. Mex Quat Res 57:91–101
Metcalfe SE, Davies SJ, Braisby JD, Leng MJ, Newton AJ, Terrett NL, O’Hara SL (2007) Long and short-term change in the Pátzcuaro Basin, central Mexico. Palaeogeogr Palaeoclimatol Palaeoecol 247:272–295
Metcalfe SE, Whitney BS, Fitzpatrick KA, Mayle FE, Loader NJ, Street-Perrott FA, Mann DG (2014) Hydrology and climatology at Laguna La Gaiba, lowland Bolivia: complex responses to climatic forcings over the last 25,000 years. J Quat Sci 29:289–300
Monnin E et al (2001) Atmospheric CO2 concentrations over the last glacial termination. Science 291:112–114
Moreno PI, León AL (2003) Abrupt vegetation changes during the last glacial to Holocene transition in mid-latitude South America. J Quat Sci 18:787–800
Morrill C, Small EE, Sloan LC (2001) Modeling orbital forcing of lake level change: Lake Gosiute (Eocene). N Am Glob Planet Change 29:57–76
Morrill C, Lowry DP, Hoell A (2018) Thermodynamic and dynamic causes of pluvial conditions during the last glacial maximum in Western North America. Geophys Res Lett 45(1):335–345
Munroe JS, Laabs BJC (2013) Temporal correspondence between pluvial lake highstands in the southwestern US and Heinrich Event 1. J Quat Sci 28:49–58
Orme AJ (1998) Lake Thompson, Mojave Desert, California: The late Pleistocene lake system and its Holocene desiccation. In: Reheis MC, Hershler R, Miller DM (eds) Late Cenozoic Drainage History of the Southwestern Great Basin and Lower Colorado River Region: Geologic and Biotic Perspectives: Geological Society of America Special Paper 439. pp 261–278. https://doi.org/10.1130/2008.2439(11)
Orme AR, Orme AJ (2008) Late Pleistocene shorelines of Owens Lake, California, and their hydroclimatic and tectonic implications. In: Reheis MC, Hershler R, Miller DM (eds) Late Cenozoic Drainage History of the Southwestern Great Basin and Lower Colorado River Region: Geologic and Biotic Perspectives: Geological Society of America Special Paper 439. pp 207–225. https://doi.org/10.1130/2008.2439(09)
Oster JL, Ibarra DE, Winnick MJ, Maher K (2015) Steering of westerly storms over western North America at the Last Glacial Maximum. Nat Geosci 8:201–205
Oviatt CG (2015) Chronology of Lake Bonneville, 30,000 to 10,000 year B.P. Quat Sci Rev 110:166–171
Pausata FSR, Li C, Wettstein JJ, Kageyama M, Nisancioglu KH (2011) The key role of topography in altering North Atlantic atmospheric circulation during the last glacial period. Clim Past 7:1089–1101. https://doi.org/10.5194/cp-7-1089-2011
Pérez L, Curtis J, Brenner M, Hodell D, Escobar J, Lozano S, Schwalb A (2013) Stable isotope values (d18O & d13C) of multiple ostracode species in a large Neotropical lake as indicators of past changes in hydrology. Quat Sci Rev 66:96–111
Placzek C, Quade J, Patchett PJ (2006) Geochronology and stratigraphy of late Pleistocene lake cycles on the southern Bolivian Altiplano: Implications for causes of tropical climate change. Geol Soc Am Bull 118:515–532
Polson D, Hegerl GC (2017) Strengthening contrast between precipitation in tropical wet and dry regions. Geophys Res Lett 44:365–373. https://doi.org/10.1002/2016GL071194
Quade J, Broecker WS (2009) Dryland hydrology in a warmer world: lessons from the Last Glacial period European Physical. J Spec Topics 176:21–36
Reeves CC Jr, Parry WT (1965) Geology of west Texas pluvial lake carbonates. Am J Sci 263:606–615
Roderick ML, Sun F, Lim WH, Farquhar GD (2014) A general framework for understanding the response of the water cycle to global warming over land and ocean. Hydrol Earth Syst Sci 18:1575–1589. https://doi.org/10.5194/hess-18-1575-2014
Rowe HD, Dunbar RB, Mucciarone DA, Seltzer GO, Baker PA, Fritz S (2002) Insolation, moisture balance and climatic change on the South American Altiplano since the last glacial maximum. Clim Change 52:175–199
Scheff J, Frierson D (2012) Twenty-first-century multimodel subtropical precipitation declines are mostly midlatitude shifts. J Clim 25:4330–4347
Scheff J, Seager R, Liu H, Coats S (2017) Are glacials dry? Consequences for paleoclimatology and for greenhouse warming. J Clim 30:6593–6609
Seager R, Henderson N (2013) Diagnostic computation of moisture budgets in the ERA-Interim Reanalysis with reference to analysis CMIP-archived atmospheric model data. J Clim 26:7876–7901
Seager R, Naik N, Vecchi GA (2010) Thermodynamic and dynamic mechanisms for large-scale changes in the hydrologic cycle in response to global warming. J Clim 23:4651–4668
Sifeddine A et al (2003) A 21000 cal years paleoclimate record from Caco Lake, northern Brazil: Evidence from sedimentary and pollen analyses Palaeogeography. Palaeoclimatology Palaeoecology 189:25–34
Sime LC, Kohfeld KE, Le Quéré C, Wolff EW, De Boer AM, Graham RM, Bopp L (2013) Southern Hemisphere westerly wind changes during the Last Glacial Maximum: model-data comparison. Quat Sci Rev 64:104–120. https://doi.org/10.1016/j.quascirev.2012.12.008
Street FA, Grove AT (1979) Global maps of lake-level fluctuations since 30 000 year B. P. Quat Res 12:83–118
Sylvestre F (2009) Moisture pattern during the Last Glacial Maximum in South America. In: Vimeux F, Sylvestre F, Khodri M (eds) Past climate variability in South America and surrounding regions: from the Last Glacial Maximum to the Holocene. Springer, Berlin, pp 3–28
Tarasov L, Peltier WR (2004) A geophysically constrained large ensemble analysis of the deglacial history of the North American ice-sheet complex. Quat Sci Rev 23:359–388
Ullman DJ, LeGrande AN, Carlson AE, Anslow FS, Licciardi JM (2013) Assessing the impact of Laurentide Ice-Sheet topography on glacial climate. Clim Past Discuss 9:3239–3306
Valero-Garcés BL, Jenny B, Rondanelli M, Delgado-Huertas A, Burns SJ, Veit H, Moreno A (2005) Palaeohydrology of Laguna de Tagua Tagua (34° 30’S) and moisture fluctuations in Central Chile for the last 46000 year. J Quat Sci 20:625–641
Vélez MI, Hooghiemstra H, Metcalfe S, Martínez I, Mommersteeg H (2003) Pollen- and diatom based environmental history since the Last Glacial Maximum from the Andean core Fúquene-7, Colombia. J Quat Sci 18:17–30
Voldoire A et al (2013) The CNRM-CM5.1 global climate model: description and basic evaluation. Clim Dyn 40:2091–2121
Wainer I, Clauzet G, Ledru M-P (2005) Last Glacial Maximum in South America: Paleoclimate proxies and model results. Geophys Res Lett 32:L08702. https://doi.org/10.1029/2004GL021244
Watanabe S et al (2011) MIROC-ESM 2010: model description and basic results of CMIP5-20c3m experiments. Geosci Model Dev 4:845–872
Waters MR (1989) Late Quaternary lacustrine history and paleoclimatic significance of pluvial Lake Cochise, southeastern Arizona. Quat Res 32:1–11
Watts WA (1980) Late-Quaternary vegetation history at White Pond on the inner coastal plain of South Carolina. Quat Res 13:187–199
Weingarten B, Yuretich R, Bradley R, Salgado-Labouriau ML (1990) Environmentally controlled variations in clay mineral assemblages from lake sediments in the Venezuelan Andes Proceedings of the 9th International Clay Conference 88:53–61
Wells SG, Brown WJ, Enzel Y, Anderson RY, McFadden LD (2003) Late Quaternary geology and paleohydrology of pluvial Lake Mojave, southern California. In: Enzel Y, Wells SG, Lancaster N (eds) Paleoenvironments and paleohydrology of the Mojave and southern Great Basin Deserts: Geological Society of America Special Paper 368. pp 79–114
Whitlock C, Bartlein PJ (1997) Vegetation and climate change in northwest America during the past 125 kyr. Nature 388:57–61
Whitney BS et al (2011) A 45 kyr paleoclimate record from the lowland interior of tropical South America. Palaeogeogr Palaeoclimatol Palaeoecol 307:177–192
Wilkins DE, Currey DR (1997) Timing and extent of late Quaternary paleolakes in the Trans-Pecos closed basin, west Texas and south-central New. Mexico Quat Res 47:306–315
Wilkins GR, Delcourt PA, Delcourt HR, Harrison FW, Turner MR (1991) Paleoecology of central Kentucky since the last glacial. Maximum Quat Res 36:224–239
Wills RC, Byrne MP, Schneider T (2016) Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle. Geophys Res Lett 43:4640–4649. https://doi.org/10.1002/2016GL068418
Yoshimori M, Yokohata T, Abe-Ouchi A (2009) A comparison of climate feedback strength between CO2 doubling and LGM experiments. J Clim 22:3374–3395
Yukimoto S et al (2012) A new global climate model of the Meteorological Research Institute: MRI-CGCM3. J Meteorol Soc Jpn 90A:23–64
Acknowledgements
We acknowledge the World Climate Research Programme’s Working Group on Coupled Modeling and the modeling groups participating in CMIP/PMIP for producing and sharing model output. We thank E. Brady and B.L. Otto-Bliesner for sharing output from the LGM-CO2 experiment, and A.L. Steiner and J.M. Russell for their constructive feedback. DPL acknowledges support from the NOAA Hollings Scholarship Program and CM received funding from the NOAA Climate Program Office. All CMIP/PMIP data supporting the conclusions can be obtained from the World Data Center for Climate.
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Lowry, D.P., Morrill, C. Is the Last Glacial Maximum a reverse analog for future hydroclimate changes in the Americas?. Clim Dyn 52, 4407–4427 (2019). https://doi.org/10.1007/s00382-018-4385-y
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DOI: https://doi.org/10.1007/s00382-018-4385-y