114:
17:
71:, cooler summers in higher latitudes of North America, which would cease to completely melt the annual snowfall, were masked at first by the presence of the slowly disappearing continental ice sheets, which persisted long after the astronomically calculated
312:
Osborn, Gerald; Menounos, Brian; Ryane, Chanone; Riedel, Jon; Clague, John J.; Koch, Johannes; Clark, Douglas; Scott, Kevin; Davis, P. Thompson (2012). "Latest
Pleistocene and Holocene glacier fluctuations on Mount Baker, Washington".
214:
have advanced and receded twice more recently, with advances peaking about 2800 BP and 300 BP (noting G.H. Denton and W. Karlen, ""Holocene climatic variations— their pattern and possible cause",
221:
1973:155-205), and J.M. Ryder and B. Thomson, "Neoglaciation in the southern Coast
Mountains of British Columbia: chronology prior to the Late Neoglacial Maximum",
358:
242:; Walker, Ian R.; Leng, Melanie J.; Hu, Feng Sheng (2011). "Abrupt Holocene climate change and potential response to solar forcing in western Canada".
277:
Menounos, Brian; Osborn, Gerald; Clague, John J.; Luckman, Brian H. (2009). "Latest
Pleistocene and Holocene glacier fluctuations in western Canada".
60:-induced temperature increase starting in the 20th century. The neoglaciation has no well-marked universal beginning: local conditions and
193:(Chicago: University of Chicago Press) 1991:15 note 13. Pielou discusses the neoglaciation in ch. 14 "The Neoglaciation" pp 291-310.
113:
61:
83:" (mid-14th to late 19th centuries), neoglaciation appears to have been reversed in the late 20th century, evidently caused by
106:. The most severe part of the best documented neoglacial period, especially in Europe and the North Atlantic, is termed the "
182:
E.C. Pielou 1991:291; S.C. Porter and G.H. Denton, "Chronology of the neo-glaciation in the North
American cordillera",
117:
Holocene climate reconstructions and glacial-advance records from western Canada. Data compiled from published studies
102:. In the mountains of western North America, montane glaciers that had completely melted reformed shortly before 5000
84:
138:
20:
Greenland ice sheet temperatures interpreted with 18O isotope from 6 ice cores (Vinther, B., et al., 2009)
75:: "the neoglaciation can be said to have begun when the cooling caught up with the warming", remarked
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lowlands, in the retreat of grassland before an advancing forest border in the
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90:. Neoglaciation had been marked by a retreat from the warm conditions of the
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In North
America, neoglaciation had ecological effects in the spread of
154:
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29:
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on flat, poorly drained land, such as the bed of recently drained
64:
affected the onset of detectably cooler (and wetter) conditions.
99:
95:
191:
After the Ice Age: The Return of Life to
Glaciated North America
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Gavin, Daniel G.; Henderson, Andrew C.G.; Westover, Karlyn S.;
122:
52:, the warmest point in the Earth's climate during the current
276:
237:
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48:. Neoglaciation has followed the hypsithermal or
32:") describes the documented cooling trend in the
345:
137:, and in shifting ranges of forest trees and
359:History of climate variability and change
112:
15:
346:
189:(1967:177-210), noted in E.C. Pielou,
98:that had not existed since the last
13:
223:Canadian Journal of Earth Sciences
210:suggest that mountain glaciers in
94:and the advance or reformation of
14:
370:
335:10.1016/j.quascirev.2012.06.004
299:10.1016/j.quascirev.2008.10.018
264:10.1016/j.quascirev.2011.03.003
73:moment of maximum summer warmth
40:, following the retreat of the
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176:
1:
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184:American Journal of Science
148:
10:
375:
315:Quaternary Science Reviews
279:Quaternary Science Reviews
244:Quaternary Science Reviews
46:most recent glacial period
79:. With the close of the "
67:Driven inexorably by the
50:Holocene Climatic Optimum
170:
139:diagnostic plant species
118:
21:
116:
56:stage, excluding the
19:
285:(21–22): 2049–2074.
141:(identified through
42:Wisconsin glaciation
327:2012QSRv...49...33O
291:2009QSRv...28.2049M
256:2011QSRv...30.1243G
250:(9–10): 1243–1255.
216:Quaternary Research
240:Fritz, Sherilyn C.
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69:Milankovitch cycle
62:ecological inertia
22:
202:Pielou 1991:291;
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208:glacial moraines
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108:Little Ice Age
88:global warming
81:Little Ice Age
58:global warming
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26:neoglaciation
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135:Great Plains
127:Lake Agassiz
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77:E. C. Pielou
66:
54:interglacial
25:
23:
129:and in the
36:during the
348:Categories
155:Neopluvial
143:palynology
131:Hudson Bay
30:glaciation
28:("renewed
321:: 33–51.
165:Subboreal
354:Holocene
160:Holocene
149:See also
96:glaciers
38:Holocene
323:Bibcode
287:Bibcode
252:Bibcode
100:ice age
123:muskeg
44:, the
171:Notes
24:The
331:doi
295:doi
260:doi
206:of
187:265
145:).
110:".
350::
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319:49
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283:28
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226:23
104:BP
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219:3
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