Koha e akullit

Nj? p?rshtypje artistike e epok?s s? akullit t? Tok?s n? maksimumet akullnajore. Bazuar n?: Crowley, T. J. (1995). "Ice age terrestrial carbon changes revisited". *Global Biogeochemical Cycles*. 9 (3): 377–389. Bibcode:1995GBioC...9..377C. doi:10.1029/95GB01107. Arkivuar nga origjinali m? 1 n?ntor 2012. Marr? m? 4 qershor 2016. `{{cite journal}}`: Mungon ose ?sht? bosh parametri `|language=` (Ndihm?!)"Ice age terrestrial carbon changes revisited" Arkivuar 1 n?ntor 2012 tek Wayback Machine. *Global Biogeochemical Cycles* 9 (3): 377–389. Bibcode:1995GBioC...9..377C. doi:10.1029/95GB01107.

Shtresat e akullit n? Antarktik. Shtresat akullnajore zgjerohen gjat? nj? *"epoke t? akullit"*.

百度数据显示，近年来车险业务同比增速逐年下滑，由2013年的18%逐步下降至2016年的%，而最新数据显示，2017年财产险公司车险业务原保费收入亿元，同比增速进一步降至%。

Koha e akullit ose nj? epok? e akullit ?sht? nj? periudh? afat-gjate e uljes s? temperatur?s t? sip?rfaqes dhe atmosfer?s s? Tok?s, duke rezultuar n? pranin? ose zgjerimin e flet?ve kontinentale dhe polare akullit dhe akullnajat alpine. Brenda nj? kohe t? akullit afatgjate, impulset individuale t? klim? t? ftoht? quhen si "periudha akullnajore" (ose ndryshe "glaciale" ose "t? ngrira"), dhe periudha e p?rhershme e ngroht? quhet "interglaciale". Glaciologjikisht, koha e akullit n?nkupton pranin? e gjer? t? shtresave akullnajore n? hemisfer?n veriore dhe n? jugore.^[1] Nga ky p?rkufizim, ne jemi n? nj? periudh? interglaciale— Holocene— e koh?s s? akullit e cila filloi 2.6 milion vjet m? par?, n? fillim t? epok?s Pleistocene, p?r shkak se shtresat akullnajore t? Groenland?s, Arktik, dhe Antarktiku ende ekzistojn?.^[2]

Origjina e teoris? s? koh?s s? akullit

N? vitin 1742 Pierre Martel (1706–1767), nj? inxhinier dhe gjeograf q? jetonte n? Gjenev?, vizitoi lugin?n e Chamonix n? Alpet e Savoy-s?.^[3]^[4] Dy vite m? von? ai botoi nj? pasqyr? t? udh?timit t? tij. Ai raportoi se banor?t e k?saj lugine shp?rndarjen e gur?ve t? ?rregullt ja atribuojn? akullnajave, duke th?n? se nj? her? ato kan? qen? t? zgjeruara m? larg.^[5]^[6] M? von? shpjegime t? ngjashme jan? raportuar nga rajonet e tjera t? Alpeve. N? vitin 1815, marangozi dhe gjuetari i dhive t? egra, Jean-Pierre Perraudin (1767–1858) shpjegoi gur?t e m?dhenj t? ?rregullt n? Val de Bagnes n? kantonin zviceran t? Valaisit se ishin p?r shkak se akullnajat m? par? shtriheshin m? tej.^[7] Nj? dru-prer?s i panjohur nga Meiringen n? Bernese Oberland mbrojti iden? e ngjashme n? nj? diskutim me gjeologjistin gjermano-zviceran Jean de Charpentier (1786–1855) n? vitin 1834.^[8]Shpjegime t? krahasueshme jan? t? njohura edhe nga Val de Ferret n? Valais dhe Seeland n? Zvicr?n per?ndimore^[9] dhe n? pun?n shkencore t? Goethes.^[10] Shpjegime t? tilla mund t? gjenden edhe n? pjes? t? tjera t? bot?s. Kur natyralisti bavarez Ernst von Bibra (1806-1878) vizitoi Andet kilian n? 1849-1850, vendasit i atribuan fosilet e moraineve, veprimeve t? m?parsh?m t? akullnajave.^[11]

Nd?rkoh?, studiuesit evropian? kishin filluar t? pyesin veten se ?far? kishte shkaktuar shp?rndarja e materialit t? ?rregullt. Nga mesi i shekullit t? 18-t?, disa diskutuan akullin si nj? mjet transporti. Eksperti suedez i minierave Daniel Tilas (1712–1772), n? vitin 1742, ishte personi i par? q? sugjeroj copat e akullit q? lundrojn? n? det p?r t? shpjeguar pranin? e gur?ve t? ?rregullt n? rajonet skandinave dhe baltike.^[12] N? 1795, shkenc?tari dhe filozofi skocez, James Hutton (1726-1797), shpjegoi gur?t e ?rregullt n? Alpe si pajoj? e akullnajave.^[13] Dy dekada m? von?, n? vitin 1818, botanisti suedez G?ran Wahlenberg (1780-1851) botoi teorin? e tij p?r nj? akullnaj? t? gadishullit skandinav. Ai e konsideronte akullnaj?n si nj? fenomen rajonal.^[14]

Referime

^ Imbrie, J.; Imbrie, K.P (1979). Ice ages: solving the mystery. Short Hills NJ: Enslow Publishers. ISBN 978-0-89490-015-0. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!)
^ Gribbin, J.R. (1982). Future Weather: Carbon Dioxide, Climate and the Greenhouse Effect. Penguin. ISBN 0140224599. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!)
^ Rémis, F.; Testus, L.; Testut (2006). "Mais comment s'écoule donc un glacier ? Aper?u historique" (PDF). C. R. Geoscience (n? fr?ngjisht). 338 (5): 368–385. Bibcode:2006CRGeo.338..368R. doi:10.1016/j.crte.2006.02.004.{{cite journal}}: Mir?mbajtja CS1: Emra t? shum?fisht?: lista e autor?ve (lidhja) Note: p. 374
^ Montgomery 2010
^ Martel, Pierre (1898). "Appendix: Martel, P. (1744) An account of the glacieres or ice alps in Savoy, in two letters, one from an English gentleman to his friend at Geneva ; the other from Pierre Martel , engineer, to the said English gentleman". p?rmbledhur nga Mathews, C.E. (red.). The annals of Mont Blanc. Lond?r: Unwin. fq. 327. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!) See (Montgomery 2010) for a full bibliography
^ Krüger, Tobias (2013). Discovering the Ice Ages. International Reception and Consequences for a Historical Understanding of Climate (German edition: Basel 2008). Leiden. fq. 47. ISBN 978-90-04-24169-5. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!)Mir?mbajtja CS1: Mungon sht?pia botuese te vendodhja (lidhja)
^ Krüger 2013, fq. 78–83
^ Krüger 2013, f. 150
^ Krüger 2013, fq. 83, 151
^ Goethe, Johann Wolfgang von: Geologische Probleme und Versuch ihrer Aufl?sung, Mineralogie und Geologie in Goethes Werke, Weimar 1892, ISBN 3-423-05946-X, book 73 (WA II,9), p. 253, 254.
^ Krüger 2013, f. 83
^ Krüger 2013, f. 38
^ Krüger 2013, fq. 61–2
^ Krüger 2013, fq. 88–90

[1] Imbrie, J.; Imbrie, K.P (1979). Ice ages: solving the mystery. Short Hills NJ: Enslow Publishers. ISBN 978-0-89490-015-0. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!)

[2] Gribbin, J.R. (1982). Future Weather: Carbon Dioxide, Climate and the Greenhouse Effect. Penguin. ISBN 0140224599. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!)

[3] Rémis, F.; Testus, L.; Testut (2006). "Mais comment s'écoule donc un glacier ? Aper?u historique" (PDF). C. R. Geoscience (n? fr?ngjisht). 338 (5): 368–385. Bibcode:2006CRGeo.338..368R. doi:10.1016/j.crte.2006.02.004.{{cite journal}}: Mir?mbajtja CS1: Emra t? shum?fisht?: lista e autor?ve (lidhja) Note: p. 374

[4] Montgomery 2010

[5] Martel, Pierre (1898). "Appendix: Martel, P. (1744) An account of the glacieres or ice alps in Savoy, in two letters, one from an English gentleman to his friend at Geneva ; the other from Pierre Martel , engineer, to the said English gentleman". p?rmbledhur nga Mathews, C.E. (red.). The annals of Mont Blanc. Lond?r: Unwin. fq. 327. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!) See (Montgomery 2010) for a full bibliography

[6] Krüger, Tobias (2013). Discovering the Ice Ages. International Reception and Consequences for a Historical Understanding of Climate (German edition: Basel 2008). Leiden. fq. 47. ISBN 978-90-04-24169-5. {{cite book}}: Mungon ose ?sht? bosh parametri |language= (Ndihm?!)Mir?mbajtja CS1: Mungon sht?pia botuese te vendodhja (lidhja)

[7] Krüger 2013, fq. 78–83

[8] Krüger 2013, f. 150

[9] Krüger 2013, fq. 83, 151

[10] Goethe, Johann Wolfgang von: Geologische Probleme und Versuch ihrer Aufl?sung, Mineralogie und Geologie in Goethes Werke, Weimar 1892, ISBN 3-423-05946-X, book 73 (WA II,9), p. 253, 254.

[11] Krüger 2013, f. 83

[12] Krüger 2013, f. 38

[13] Krüger 2013, fq. 61–2

[14] Krüger 2013, fq. 88–90

[1]

[2]

[3]

[4]

[5]

[6]

[7]

[8]

[9]

[10]

[11]

[12]

[13]

[14]

输卵管堵塞吃什么药能打通	一姐是什么意思	征候是什么意思	热水器什么牌子好	一个火一个同念什么
为什么一喝酒就拉肚子	马飞是什么药	肝右叶钙化灶是什么意思	什么大河	北京佑安医院擅长什么
大三阳吃什么药好	作死是什么意思	博物馆里有什么	布洛芬是什么药	孔雀男是什么意思
大学院长是什么级别	斐乐什么档次	diss是什么意思	见到黑猫代表什么预兆	鹭鸶是什么动物

广州有什么美食hcv9jop6ns0r.cn	尿黄尿臭是什么原因hcv7jop9ns6r.cn	宫腔镜是什么手术hcv9jop1ns5r.cn	保育员是什么bjcbxg.com	腮腺炎吃什么药好hcv8jop2ns2r.cn
taco是什么hcv8jop4ns7r.cn	胎儿右侧脉络丛囊肿是什么意思hcv9jop4ns7r.cn	最近天气为什么这么热hcv7jop6ns4r.cn	飞花令是什么hcv8jop8ns0r.cn	梦见生娃娃是什么意思hcv8jop8ns9r.cn
惊涛骇浪是什么意思hcv9jop6ns4r.cn	鸽子拉绿稀便是什么病hcv8jop5ns2r.cn	no.是什么意思hcv8jop0ns2r.cn	火疖子是什么hcv8jop6ns2r.cn	郭麒麟什么学历hcv9jop5ns1r.cn
杀马特是什么hcv9jop0ns2r.cn	眼睛充血用什么药hcv9jop0ns3r.cn	癫痫是什么病onlinewuye.com	一直吐口水是什么原因hcv8jop7ns4r.cn	昙花一现什么意思youbangsi.com