125:
28:
82:, 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
323:
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".
225:
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",
232:
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",
369:
253:; Walker, Ian R.; Leng, Melanie J.; Hu, Feng Sheng (2011). "Abrupt Holocene climate change and potential response to solar forcing in western Canada".
288:
Menounos, Brian; Osborn, Gerald; Clague, John J.; Luckman, Brian H. (2009). "Latest
Pleistocene and Holocene glacier fluctuations in western Canada".
71:-induced temperature increase starting in the 20th century. The neoglaciation has no well-marked universal beginning: local conditions and
204:(Chicago: University of Chicago Press) 1991:15 note 13. Pielou discusses the neoglaciation in ch. 14 "The Neoglaciation" pp 291-310.
124:
72:
94:" (mid-14th to late 19th centuries), neoglaciation appears to have been reversed in the late 20th century, evidently caused by
117:. The most severe part of the best documented neoglacial period, especially in Europe and the North Atlantic, is termed the "
193:
E.C. Pielou 1991:291; S.C. Porter and G.H. Denton, "Chronology of the neo-glaciation in the North
American cordillera",
128:
Holocene climate reconstructions and glacial-advance records from western Canada. Data compiled from published studies
113:. In the mountains of western North America, montane glaciers that had completely melted reformed shortly before 5000
95:
149:
31:
Greenland ice sheet temperatures interpreted with 18O isotope from 6 ice cores (Vinther, B., et al., 2009)
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86:: "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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101:. 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
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on flat, poorly drained land, such as the bed of recently drained
75:
affected the onset of detectably cooler (and wetter) conditions.
110:
106:
202:
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.;
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63:, the warmest point in the Earth's climate during the current
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248:
322:
59:. Neoglaciation has followed the hypsithermal or
43:") describes the documented cooling trend in the
356:
148:, and in shifting ranges of forest trees and
370:History of climate variability and change
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26:
14:
357:
200:(1967:177-210), noted in E.C. Pielou,
109:that had not existed since the last
24:
234:Canadian Journal of Earth Sciences
221:suggest that mountain glaciers in
105:and the advance or reformation of
25:
381:
346:10.1016/j.quascirev.2012.06.004
310:10.1016/j.quascirev.2008.10.018
275:10.1016/j.quascirev.2011.03.003
84:moment of maximum summer warmth
51:, following the retreat of the
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13:
1:
7:
195:American Journal of Science
159:
10:
386:
326:Quaternary Science Reviews
290:Quaternary Science Reviews
255:Quaternary Science Reviews
57:most recent glacial period
90:. With the close of the "
78:Driven inexorably by the
61:Holocene Climatic Optimum
181:
150:diagnostic plant species
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32:
127:
67:stage, excluding the
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296:(21–22): 2049–2074.
152:(identified through
53:Wisconsin glaciation
338:2012QSRv...49...33O
302:2009QSRv...28.2049M
267:2011QSRv...30.1243G
261:(9–10): 1243–1255.
227:Quaternary Research
251:Fritz, Sherilyn C.
130:
80:Milankovitch cycle
73:ecological inertia
33:
213:Pielou 1991:291;
16:(Redirected from
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119:Little Ice Age
99:global warming
92:Little Ice Age
69:global warming
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37:neoglaciation
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146:Great Plains
138:Lake Agassiz
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88:E. C. Pielou
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65:interglacial
36:
34:
140:and in the
47:during the
359:Categories
166:Neopluvial
154:palynology
142:Hudson Bay
41:glaciation
39:("renewed
18:Neoglacial
332:: 33–51.
176:Subboreal
365:Holocene
171:Holocene
160:See also
107:glaciers
49:Holocene
334:Bibcode
298:Bibcode
263:Bibcode
111:ice age
134:muskeg
55:, the
182:Notes
35:The
342:doi
306:doi
271:doi
217:of
198:265
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121:".
361::
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237:23
115:BP
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20:)
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