Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings
The magnitude of glacier advances generally increased in the Northern Hemisphere and decreased in the Southern Hemisphere over the Holocene. This trend can be explained be the orbital forcings. The exceptions are in some regions of the high Asia. 10–4 ka BP and during the 1th Century CE to the early...
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ftjias:oai:oai.ice.elpub.ru:article/58 |
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openpolar |
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Open Polar |
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Ice and Snow (E-Journal) |
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ftjias |
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Russian |
topic |
Аnthropogenic forcings;glacier fluctuations;Holocene;orbital forcing;solar activity;volcanic forcings Антропогенное воздействие на климат;вулканическая активность;голоцен;колебания ледников;орбитальный сигнал;солнечная активность |
spellingShingle |
Аnthropogenic forcings;glacier fluctuations;Holocene;orbital forcing;solar activity;volcanic forcings Антропогенное воздействие на климат;вулканическая активность;голоцен;колебания ледников;орбитальный сигнал;солнечная активность O. Solomina N. О. Соломина Н. Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
topic_facet |
Аnthropogenic forcings;glacier fluctuations;Holocene;orbital forcing;solar activity;volcanic forcings Антропогенное воздействие на климат;вулканическая активность;голоцен;колебания ледников;орбитальный сигнал;солнечная активность |
description |
The magnitude of glacier advances generally increased in the Northern Hemisphere and decreased in the Southern Hemisphere over the Holocene. This trend can be explained be the orbital forcings. The exceptions are in some regions of the high Asia. 10–4 ka BP and during the 1th Century CE to the early 13th century CE the glaciers were close by sizes to the modern ones or even smaller. The pattern is confirmed by the upper and Northern tree line advances in the Northern Hemisphere. The period with generally «small glaciers» (5–7 ka) coincides with the lack of the major volcanic eruptions, and with the low solar activity. The Early Holocene moraines cluster in seven groups (from 11.1 to 8.1 ka BP). They coincide with all Early Holocene Bond cycles (11.1, 10.3, 9.4, 8.1 ka) and all major volcanic eruptions (11.0, 9.5–9.7, 9.1–9.3, 8.0–8.1). Due to the coincidence of several eruptions with the Bond cycles (solar minima) it is difficult to distinguish between the solar and volcanic signals in the Early Holocene records. The coupling between the glacial and solar/volcanic forcings in the mid Holocene is less evident, but it become strong again in the last 2 ka (1.4 ka and LIA events). The modern glacier retreat disagrees with the actual orbital forcings and is due to both solar and anthropogenic influence. Glacier variations at the moment do not provide proofs for any cycles or global synchronism through the Holocene. However the lack of such evidences can be also explained by the limitations of these records (discontinuous, incomplete, of low accuracy, showing a mixture of advances triggered by both temperature and precipitation). Амплитуда наступаний ледников в голоцене в Северном полушарии в целом увеличивалась, а в Южном – уменьшалась. Этот тренд объясняется изменениями инсоляции, связанными с орбитальными параметрами Земли. Исключение из этого правила – некоторые районы Центральной Азии, где размеры ледников в голоцене уменьшались. 10–4 тыс. л.н. и в течение первого тысячелетия н.э. (примерно до начала XIII в.) ... |
format |
Article in Journal/Newspaper |
author |
O. Solomina N. О. Соломина Н. |
author_facet |
O. Solomina N. О. Соломина Н. |
author_sort |
O. Solomina N. |
title |
Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
title_short |
Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
title_full |
Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
title_fullStr |
Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
title_full_unstemmed |
Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
title_sort |
holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings |
publisher |
IGRAS |
publishDate |
2015 |
url |
https://ice-snow.igras.ru/jour/article/view/58 https://doi.org/10.15356/2076-6734-2014-3-81-90 |
genre |
Antarctic Science Arctic Arctic and Alpine Research |
genre_facet |
Antarctic Science Arctic Arctic and Alpine Research |
op_source |
Ice and Snow; Том 54, № 3 (2014); 81-90 Лёд и Снег; Том 54, № 3 (2014); 81-90 2412-3765 2076-6734 10.15356/2076-6734-2014-3 |
op_relation |
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A millennial perspective on Arctic warming from 14C in quartz and plants emerging beneath ice caps. Geophys. Research Letters. 2008, 35 (1): L01502. Antoniades D., Francusa P., Pienitza R., St-Ongec G., Vincenta W.F. Holocene dynamics of the Arctic’s largest ice. Proc. of the National Academy of Sciences of United States of America. 2011, 108 (47): 18899–18904. Bay R. C., Bramall N. E., Price P. B., Clow G. D., Hawley R. L., Udisti R., Castellano E. Globally synchronous ice core volcanic tracers and abrupt cooling during the last glacial period. Journ. of Geophys. Research: Atmospheres. 2006, 111: D11. doi:10.1029/2005JD006306 Bond G., Kromer B., Beer J., Muscheler R., Evans M.N., Showers W., Hoffmann S., Lotti-Bond R., Hajdas I., Bonani G. Persistent Solar Inßuence on North Atlantic Climate During the Holocene. Science. 2001, 294: 2130–2135. Bowerman N.D., Clark D.H. Holocene glaciation of the central Sierra Nevada, California. Quaternary Science Reviews. 2011, 30 (9–10): 1067–1085. Briner J.P., Davis P.T., Miller G.H. Latest Pleistocene and Holocene glaciation of Baffin Island, Arctic Canada: key patterns and chronologies. Quaternary Science Reviews. 2009, 28: 2075–2087. Broecker W.S., Kennett J.P., Flower B.P., Teller J.T., Trumboe S., Bonani G., Wölfli W. Routing of meltwater from the Laurentide ice sheet during the Younger Dryas cold episode. Nature. 1989, 341: 318– 321. Broecker W.S., Bond G., Klas M. A salt oscillator in the glacial North Atlantic? The concept. Paleoceanography. 1990, 5: 469–477. Clark P.U., Marshall S.J., Clarke G.K.C., Hostetler S.W., Licciardi J.M., Teller J.T. Freshwater forcing of abrupt climate change during the last glaciation. Science. 2001, 293: 283–287. Debret M., Bout-Roumazeilles V., Grousset F., Desmet M., McManus J. F. , Massei N., D. Sebag D., Petit J.-R., Copard Y., Trentesaux A. The origin of the 1500-year climate cycles in Holocene North-Atlantic records. Climate of the Past. 2007, 3: 569–575. Denton G.H., Karlen W. Lichenometry: its application to Holocene moraine studies in Southern Alaska and Swedish Lapland. Arctic and Alpine Research. 1973, 5 (4): 347–372. Domack E., Duran D., Leventer A., Ishman S., Doane S., McCallum S., Amblas D., Ring J., Gilbert R., Prentice M. Stability of the Larsen B ice shelf on the Antarctic Peninsula during the Holocene epoch. Nature. 2005, 436 (4): 681–685. Ferris D. G., Cole-Dai J., Reyes A. R., Budner D. M. South Pole ice core record of explosive volcanic eruptions in the first and second millennia A.D. and evidence of a large eruption in the tropics around 535 A.D. Journ. of Geophys. Research: Atmospheres. 2011, 116. № D17. doi:10.1029/2011JD015916 Geirsdóttir A., Miller G.H., Axford Y., Ólafsdóttir S. Holocene and latest Pleistocene 6climate and glacier fluctuations in Iceland. Quaternary Science Reviews. 2009, 28: 2107–2118. Glasser N.F., Clemmens S., Schnabel C., Fenton C.R., McHargue L. Tropical glacier fluctuations in the Cordillera Blanca, Peru between 12.5 and 7.6 ka from cosmogenic 10Be dating. Quaternary Science Reviews. 2009, 28: 3448–3458. Goehring B.M., Vacco D.A., Alley R.B., Schaefer J.M. Holocene dynamics of the Rhone Glacier, Switzerland, deduced from ice flow models and cosmogenic nuclides.Earth and Planetary Science Letters. 2012, 351–352: 27–35. Grove J. M. Little ice ages: ancient and modern. New York, Routledge, 2004: 402 p. Hall B.L, Denton G.H. Holocene history of the Wilson Piedmont Glacier along the southern Scott Coast, Antarctica. The Holocene. 2002, 12 (5): 619–627. Hjort C., Bently M.J., Ingolfsson О. Holocene and pre-Holocene temporary disappearance of the George VI Ice Shelf, Antarctic Peninsula Antarctic. Science. 2001, 13 (3): 296–301. Hodgson D.A. First synchronous retreat of ice shelves marks a new phase of polar deglaciation. Proc. of the National Academy of Sciences of United States of America. 2011, 108 (47): 18859–18860. 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ftjias:oai:oai.ice.elpub.ru:article/58 2023-05-15T14:14:53+02:00 Holocene glacier variations and their potential orbital, solar, volcanic and anthropogenic forcings Колебания ледников в голоцене и возможное влияние на них орбитального сигнала, солнечной и вулканической активности и антропогенного воздействия O. Solomina N. О. Соломина Н. 2015-03-27 application/pdf https://ice-snow.igras.ru/jour/article/view/58 https://doi.org/10.15356/2076-6734-2014-3-81-90 rus rus IGRAS https://ice-snow.igras.ru/jour/article/view/58/32 Ganyushkin D.A. Sovremennoe i drevnee oledenenie gornogo massiva Mongun-Tayga. Modern and ancient glaciation of Mongun-Tayga Mounatin region. LAP, 2012: 278 p. [In Russian]. Nazarov A.N., Solomina O.N., Myglan V.S. Variations of the Tree Line and Glaciers in the Central and Eastern Altai Regions in the Holocene Doklady Akademii Nauk. Proc. of the Academy of Sciences. 2012, 444 (2): 787–790. [In Russian]. Abbott M.B., Wolfe B.B., Wolfe A.P., Seltzer G.O., Aravena R., Mark B.G., Polissar P.J., Rodbell D.T., Rowe H.D., Vuille M. Holocene paleohydrology and glacial history of the central Andes using multiproxy lake sediment studies. Palaeogeography, Palaeoclimatology, Palaeoecology. 2003, 194: 123–138. Alley R.B., Agustsdottir A.M. The 8k event: cause and consequences of a major Holocene abrupt climate change. Quaternary Science Reviews. 2005, 24: 1123–1149. Anderson R.K., Miller G.H., Briner J.P., Lifton N.A., De Vogel S.B. A millennial perspective on Arctic warming from 14C in quartz and plants emerging beneath ice caps. Geophys. Research Letters. 2008, 35 (1): L01502. Antoniades D., Francusa P., Pienitza R., St-Ongec G., Vincenta W.F. Holocene dynamics of the Arctic’s largest ice. Proc. of the National Academy of Sciences of United States of America. 2011, 108 (47): 18899–18904. Bay R. C., Bramall N. E., Price P. B., Clow G. D., Hawley R. L., Udisti R., Castellano E. Globally synchronous ice core volcanic tracers and abrupt cooling during the last glacial period. Journ. of Geophys. Research: Atmospheres. 2006, 111: D11. doi:10.1029/2005JD006306 Bond G., Kromer B., Beer J., Muscheler R., Evans M.N., Showers W., Hoffmann S., Lotti-Bond R., Hajdas I., Bonani G. Persistent Solar Inßuence on North Atlantic Climate During the Holocene. Science. 2001, 294: 2130–2135. Bowerman N.D., Clark D.H. Holocene glaciation of the central Sierra Nevada, California. Quaternary Science Reviews. 2011, 30 (9–10): 1067–1085. Briner J.P., Davis P.T., Miller G.H. Latest Pleistocene and Holocene glaciation of Baffin Island, Arctic Canada: key patterns and chronologies. Quaternary Science Reviews. 2009, 28: 2075–2087. Broecker W.S., Kennett J.P., Flower B.P., Teller J.T., Trumboe S., Bonani G., Wölfli W. Routing of meltwater from the Laurentide ice sheet during the Younger Dryas cold episode. Nature. 1989, 341: 318– 321. Broecker W.S., Bond G., Klas M. A salt oscillator in the glacial North Atlantic? The concept. Paleoceanography. 1990, 5: 469–477. Clark P.U., Marshall S.J., Clarke G.K.C., Hostetler S.W., Licciardi J.M., Teller J.T. Freshwater forcing of abrupt climate change during the last glaciation. Science. 2001, 293: 283–287. Debret M., Bout-Roumazeilles V., Grousset F., Desmet M., McManus J. F. , Massei N., D. Sebag D., Petit J.-R., Copard Y., Trentesaux A. The origin of the 1500-year climate cycles in Holocene North-Atlantic records. Climate of the Past. 2007, 3: 569–575. Denton G.H., Karlen W. Lichenometry: its application to Holocene moraine studies in Southern Alaska and Swedish Lapland. Arctic and Alpine Research. 1973, 5 (4): 347–372. Domack E., Duran D., Leventer A., Ishman S., Doane S., McCallum S., Amblas D., Ring J., Gilbert R., Prentice M. Stability of the Larsen B ice shelf on the Antarctic Peninsula during the Holocene epoch. Nature. 2005, 436 (4): 681–685. Ferris D. G., Cole-Dai J., Reyes A. R., Budner D. M. South Pole ice core record of explosive volcanic eruptions in the first and second millennia A.D. and evidence of a large eruption in the tropics around 535 A.D. Journ. of Geophys. Research: Atmospheres. 2011, 116. № D17. doi:10.1029/2011JD015916 Geirsdóttir A., Miller G.H., Axford Y., Ólafsdóttir S. Holocene and latest Pleistocene 6climate and glacier fluctuations in Iceland. Quaternary Science Reviews. 2009, 28: 2107–2118. Glasser N.F., Clemmens S., Schnabel C., Fenton C.R., McHargue L. Tropical glacier fluctuations in the Cordillera Blanca, Peru between 12.5 and 7.6 ka from cosmogenic 10Be dating. Quaternary Science Reviews. 2009, 28: 3448–3458. Goehring B.M., Vacco D.A., Alley R.B., Schaefer J.M. Holocene dynamics of the Rhone Glacier, Switzerland, deduced from ice flow models and cosmogenic nuclides.Earth and Planetary Science Letters. 2012, 351–352: 27–35. Grove J. M. Little ice ages: ancient and modern. New York, Routledge, 2004: 402 p. Hall B.L, Denton G.H. Holocene history of the Wilson Piedmont Glacier along the southern Scott Coast, Antarctica. The Holocene. 2002, 12 (5): 619–627. Hjort C., Bently M.J., Ingolfsson О. Holocene and pre-Holocene temporary disappearance of the George VI Ice Shelf, Antarctic Peninsula Antarctic. Science. 2001, 13 (3): 296–301. Hodgson D.A. First synchronous retreat of ice shelves marks a new phase of polar deglaciation. Proc. of the National Academy of Sciences of United States of America. 2011, 108 (47): 18859–18860. Holzhauser H., Magny M., Zumbuehl H.J. Glacier and lake-level variations in west-central Europe over the last 3500 . The Holocene. 2005, 15: 789–801. Hormes A., Muller B.U. The Alps with little ice: evidence for eight Holocene phases of reduced glacier extent in the Central Swiss Alps. The Holocene. 2001, 11 (3): 255–265. Ivy-Ochs S., Kerschner H., Maisch M., Christl M., Kubik P.W., Schluechter C. Latest Pleistocene and Holocene glacier variations in the European Alps. Quaternary Science Reviews. 2009, 28: 2137–2149. Joerin U.E., Nicolussi K., Fischer A., Stocker T.F., Schlüchter C. Holocene optimum events inferred from subglacial sediments at Tschierva Glacier, Eastern Swiss Alps. Quaternary Science Reviews. 2008, 27: 337–350. Jomelli V., Khodri M., Favier V., Brunstein D., Ledru M.-P., Wagnon P., Blard P.-H., Sicart J.-E., Braucher R., Grancher D., Bourlès D., Braconnot P., Vuille M. Irregular tropical glacier retreat over the Holocene epoch driven by progressive warming. Nature. 2011, 474: 196–199. Kelly M.A., Lowell T.V. Fluctuations of local glaciers in Greenland during latest Pleistocene and Holocene time. Quaternary Science Reviews. 2009, 28: 2088–2106. Kirkbride M.P., Dugmore A.J. Responses of mountain ice caps in central Iceland to Holocene climate change. Quaternary Science Reviews. 2006, 25 (13–14): 1692–1707. Koch J., Clague J.J. Are insolation and sunspot activity the primary drivers of global Holocene glacier fluctuations? Pages Newsletter. 2006, 14 (3): 20–21. Larsen N.K., Kjær K.H., Olsen J., Funder S., Kjeldsen K.K., Nørgaard-Pedersen N. Restricted impact of Holocene climate variations on the southern Greenland Ice Sheet. Quaternary Science Reviews. 2011, 30 (21–22): 3171–3180. Larsen D.J., Miller G.H., Geirsdóttir A., Ólafsdóttir S. Non-linear Holocene climate evolution in the North Atlantic: a high-resolution, multi-proxy record of glacier activity and environmental change from Hvítárvatn, central Iceland. Quaternary Science Reviews. 2012, 39: 14–25. Licciardi J.M., Schaefer J.M., Taggart J.R., Lund D.C. Holocene Glacier Fluctuations in the Peruvian Andes Indicate Northern Climate Linkages. Science. 2009, 325: 1677–1679. doi:10.1126/science.1175010 Luckman B.H., Wilson R.J.S. Summer temperature in the Canadian Rockies during the last millennium – a revised record. Climate Dynamics. 2005, 24: 131–144. 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CC-BY Ice and Snow; Том 54, № 3 (2014); 81-90 Лёд и Снег; Том 54, № 3 (2014); 81-90 2412-3765 2076-6734 10.15356/2076-6734-2014-3 Аnthropogenic forcings;glacier fluctuations;Holocene;orbital forcing;solar activity;volcanic forcings Антропогенное воздействие на климат;вулканическая активность;голоцен;колебания ледников;орбитальный сигнал;солнечная активность info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2015 ftjias https://doi.org/10.15356/2076-6734-2014-3-81-90 https://doi.org/10.15356/2076-6734-2014-3 https://doi.org/10.1029/2005JD006306 https://doi.org/10.1029/2011JD015916 https://doi.org/10.1126/science.1175010 https://doi.org/10.1029/2011GL050168 ht 2022-12-20T13:30:26Z The magnitude of glacier advances generally increased in the Northern Hemisphere and decreased in the Southern Hemisphere over the Holocene. This trend can be explained be the orbital forcings. The exceptions are in some regions of the high Asia. 10–4 ka BP and during the 1th Century CE to the early 13th century CE the glaciers were close by sizes to the modern ones or even smaller. The pattern is confirmed by the upper and Northern tree line advances in the Northern Hemisphere. The period with generally «small glaciers» (5–7 ka) coincides with the lack of the major volcanic eruptions, and with the low solar activity. The Early Holocene moraines cluster in seven groups (from 11.1 to 8.1 ka BP). They coincide with all Early Holocene Bond cycles (11.1, 10.3, 9.4, 8.1 ka) and all major volcanic eruptions (11.0, 9.5–9.7, 9.1–9.3, 8.0–8.1). Due to the coincidence of several eruptions with the Bond cycles (solar minima) it is difficult to distinguish between the solar and volcanic signals in the Early Holocene records. The coupling between the glacial and solar/volcanic forcings in the mid Holocene is less evident, but it become strong again in the last 2 ka (1.4 ka and LIA events). The modern glacier retreat disagrees with the actual orbital forcings and is due to both solar and anthropogenic influence. Glacier variations at the moment do not provide proofs for any cycles or global synchronism through the Holocene. However the lack of such evidences can be also explained by the limitations of these records (discontinuous, incomplete, of low accuracy, showing a mixture of advances triggered by both temperature and precipitation). Амплитуда наступаний ледников в голоцене в Северном полушарии в целом увеличивалась, а в Южном – уменьшалась. Этот тренд объясняется изменениями инсоляции, связанными с орбитальными параметрами Земли. Исключение из этого правила – некоторые районы Центральной Азии, где размеры ледников в голоцене уменьшались. 10–4 тыс. л.н. и в течение первого тысячелетия н.э. 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