標(biāo)題: Titlebook: Climatic Changes on a Yearly to Millennial Basis; Geological, Historic N.-A. M?rner,W. Karlén Book 1984 Springer Science+Business Media Dor [打印本頁(yè)] 作者: ODDS 時(shí)間: 2025-3-21 17:13
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis影響因子(影響力)
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis影響因子(影響力)學(xué)科排名
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis被引頻次
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis被引頻次學(xué)科排名
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis年度引用
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis年度引用學(xué)科排名
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis讀者反饋
書(shū)目名稱Climatic Changes on a Yearly to Millennial Basis讀者反饋學(xué)科排名
作者: 使害怕 時(shí)間: 2025-3-21 21:18 作者: maudtin 時(shí)間: 2025-3-22 02:49 作者: lipids 時(shí)間: 2025-3-22 06:30
Late Weichselian Deglaciation and Chronostratigraphy of Southern Scandinavia: Problems and Present “undqvist, 1961; Nilson, 1968; M?rner, 1969; Berglund, 1979). We realize that there are still serious problems connected with the identification and correlation of deglaciation features and their proper dating and relation to biozonation and paleoclimatic cold/warm periods.作者: 燕麥 時(shí)間: 2025-3-22 12:44 作者: orthopedist 時(shí)間: 2025-3-22 15:50
the SECOND NORDIC SYMPOSIUM ON CLIMATIC CHANGES AND RELATED PROBLEMS held in Stockholm, Sweden, May 16-20, 1983 (Frydendahl et al., 1983; Marner, 1983). This was "an international interdisciplinary symposium with special refe- rence to Nordic records and their relation to global climatic changes". T作者: orthopedist 時(shí)間: 2025-3-22 18:12
Grundlagen des Projektmanagements,investigated by various methods (AMMANN & TOBOLSKI 1983, GAILLARD 1983, ELIAS & WILKINSON 1983, HOFMANN 1983, CHAIX 1983, EICHER & SIEGENTHALER 1983, AMMANN et al. 1983). The main results are summarized in Fig. 1.作者: 言行自由 時(shí)間: 2025-3-22 22:43 作者: Counteract 時(shí)間: 2025-3-23 01:44 作者: investigate 時(shí)間: 2025-3-23 07:28 作者: 特別容易碎 時(shí)間: 2025-3-23 12:44 作者: dysphagia 時(shí)間: 2025-3-23 15:37
The Classical Late Weichselian Climatic Fluctuations in Mexicontarctica). Recent investigations give more and more evidence that the classical West European chronostratigraphy of the Late Weichselian in many details is a . stratigraphy and cannot be transferred to other areas of the world.作者: left-ventricle 時(shí)間: 2025-3-23 18:11
The Reflection of Abrupt Climatic Changes in the Relief and Sequence of Continental Depositsposits in the temperature zone. The following abrupt changes are discussed for the last 11000 years; 10.9–10.6 Ka, 8.4–8.0 Ka, 5.0–4.5 Ka, 2.8–2.4 Ka BP and the Little Ice Age. The following abrupt climatic changes have been distinguished: a/abrupt warmings and coolings and b/short waves of increased humidity and increased flood frequency.作者: 豪華 時(shí)間: 2025-3-23 22:18 作者: Hyperplasia 時(shí)間: 2025-3-24 04:32 作者: Parallel 時(shí)間: 2025-3-24 09:53 作者: 解脫 時(shí)間: 2025-3-24 11:46
Biotic Response to Climatic Changes during the Time Span 13,000–10,000 B.P. — a Case Study from SW Ses 13,000–12,500 followed by a gradual deterioration until 11,000 when a sudden drop of temperature leads to a minimum between 11,000 and 10,500. A distinct rise of summer temperature around 10,500 is confirmed although the time lag in the vegetation response is ab. 300 years.作者: cleaver 時(shí)間: 2025-3-24 15:19 作者: 憤慨一下 時(shí)間: 2025-3-24 19:28
Grundlagen des Projektmanagements,undqvist, 1961; Nilson, 1968; M?rner, 1969; Berglund, 1979). We realize that there are still serious problems connected with the identification and correlation of deglaciation features and their proper dating and relation to biozonation and paleoclimatic cold/warm periods.作者: 藕床生厭倦 時(shí)間: 2025-3-24 23:29 作者: 膽汁 時(shí)間: 2025-3-25 06:48 作者: 容易懂得 時(shí)間: 2025-3-25 09:50
978-90-481-8399-9Springer Science+Business Media Dordrecht 1984作者: grudging 時(shí)間: 2025-3-25 12:03 作者: FAR 時(shí)間: 2025-3-25 19:04 作者: 到婚嫁年齡 時(shí)間: 2025-3-25 20:34 作者: 花爭(zhēng)吵 時(shí)間: 2025-3-26 02:57 作者: 使服水土 時(shí)間: 2025-3-26 05:36 作者: Eulogy 時(shí)間: 2025-3-26 10:08
,Kritische Würdigung und Ausblick, 13,000–10,000 yrs B.P., in SW Sweden (H?kulls Mosse, province of Sk?ne) are interpreted against the two dominant palaeoclimatic models: the palaeobotanical model (Iversen) and the palaeoentomological model (Coope). An important time lag is found in the vegetation response to climatic improvement af作者: 母豬 時(shí)間: 2025-3-26 15:05
https://doi.org/10.1007/978-3-8350-9496-300 yr B.P. With litho-, bio- and chronostratigraphic investigations combined with various physical and chemical analyses a picture of the Late Weichselian/Early Holocene glacial, vegetational and, climatic history has been obtained. In the later part of the rather warm Allenz?d Chronozone the Baltic作者: braggadocio 時(shí)間: 2025-3-26 17:51 作者: Polydipsia 時(shí)間: 2025-3-26 22:12
Risikomanagement für IT-Projekte the basis of the original C-14 collection of samples it has proved possible to evaluate the fauna communities and distinguish between arctic and boreal-arctic communities at different depths. A curve of sea-level stand can be drawn for the final part of glaciation in Jutland up to the end of Aller?作者: 隱藏 時(shí)間: 2025-3-27 01:37 作者: 內(nèi)部 時(shí)間: 2025-3-27 09:08
Grundlagen des Projektmanagements,s species refuges, as was shown by Van Campo & Aymonin (1962), Lang (1970), Beug (1975), Van der Hammen (1979), but also the variations of climate. These regions were not much affected by the Scandinavian inland ice; therefore they may have registered the first oscillations that took place at the en作者: antidepressant 時(shí)間: 2025-3-27 13:08 作者: 討人喜歡 時(shí)間: 2025-3-27 14:35 作者: sleep-spindles 時(shí)間: 2025-3-27 21:07
https://doi.org/10.1007/978-3-322-99252-9inifera. The two principal species involved in the fluctuations are . and . the former in V29–206 and the latter in V28–14. Variations in these species. relative and absolute abundance are directly related to variable dissolution and to changes in the boundary between the Irminger and East Greenland作者: bifurcate 時(shí)間: 2025-3-27 22:00 作者: Biomarker 時(shí)間: 2025-3-28 02:42 作者: heterodox 時(shí)間: 2025-3-28 07:52
,H?ufige Fehler im Risikomanagement,ndinavia. Also, due to their small land area and remoteness from the continent of Europe, the islands should have responded sensitively to changes in ocean temperature. Minimal isostatic control has led to sea level rising throughout the Postglacial, impeding drainage and impounding sediment in most作者: 拖債 時(shí)間: 2025-3-28 11:29 作者: Immortal 時(shí)間: 2025-3-28 14:47 作者: Credence 時(shí)間: 2025-3-28 19:08 作者: Free-Radical 時(shí)間: 2025-3-29 02:44 作者: appall 時(shí)間: 2025-3-29 04:44
Grundlagen des Projektmanagements,s species refuges, as was shown by Van Campo & Aymonin (1962), Lang (1970), Beug (1975), Van der Hammen (1979), but also the variations of climate. These regions were not much affected by the Scandinavian inland ice; therefore they may have registered the first oscillations that took place at the end of the Würm.作者: Enrage 時(shí)間: 2025-3-29 09:57
https://doi.org/10.1007/978-3-8350-9496-3nges. Emphasis is laid on the thick and long-lasting snow cover. Besides these two recurrence periods, the major events observed mainly evidence the influence of drought: glacial regression and formation of rock- glaciers.作者: HALO 時(shí)間: 2025-3-29 13:39
https://doi.org/10.1007/978-3-322-99252-9inifera. The two principal species involved in the fluctuations are . and . the former in V29–206 and the latter in V28–14. Variations in these species. relative and absolute abundance are directly related to variable dissolution and to changes in the boundary between the Irminger and East Greenland currents.作者: hysterectomy 時(shí)間: 2025-3-29 16:17
Grundlagen und rechtlicher Rahmen,ibed on the basis of a pollen diagram. A reconstruction of the postglacial water-level changes in Krageholmssj?n is proposed and compared to the results obtained earlier in Southern Sweden. The possible connections between human activity, climate and water-level changes are discussed.作者: Bombast 時(shí)間: 2025-3-29 22:39
Identifikation der einzelnen Risikoarten,andscapes both in North America and in northern Eurasia (Moore & Bellamy, 1974). Peatlands develop in sites where organic deposition exceeds decomposition. Peat accumulates in wet depressions by the filling-in process, and on slopes of particularly humid regions by the building-up process (Tarnocai, 1978).作者: armistice 時(shí)間: 2025-3-29 23:59
Cyclic Lamination in Proximal Varves Reflecting the Length of Summers during Late Weichsel in Southe Blekinge, southernmost Sweden. Between 43 and 56 day varves have been observed in the summer layers and the number of day varves are supposed to represent the length of summers during the Boiling Chronozone in Late Weichsel of southernmost Sweden.作者: 毗鄰 時(shí)間: 2025-3-30 06:55 作者: ambivalence 時(shí)間: 2025-3-30 08:29
Climatic and Glacial Fluctuations during the Late-Glacial and the Holocene in Oisans (Isere, France)nges. Emphasis is laid on the thick and long-lasting snow cover. Besides these two recurrence periods, the major events observed mainly evidence the influence of drought: glacial regression and formation of rock- glaciers.作者: 審問(wèn),審訊 時(shí)間: 2025-3-30 13:07
Late-Glacial — Holocene High-Frequency Climatic Changes in Deep-Sea Cores from the Denmark Straitinifera. The two principal species involved in the fluctuations are . and . the former in V29–206 and the latter in V28–14. Variations in these species. relative and absolute abundance are directly related to variable dissolution and to changes in the boundary between the Irminger and East Greenland currents.作者: 清唱?jiǎng)?nbsp; 時(shí)間: 2025-3-30 19:12
Water-Level Changes, Climate and Human Impact: A Palaeohydrological Study of Krageholm Lake (Scania,ibed on the basis of a pollen diagram. A reconstruction of the postglacial water-level changes in Krageholmssj?n is proposed and compared to the results obtained earlier in Southern Sweden. The possible connections between human activity, climate and water-level changes are discussed.作者: GRAZE 時(shí)間: 2025-3-30 21:00 作者: integrated 時(shí)間: 2025-3-31 01:15
Book 1984d synthesis originate from Scandinavian data. This applies, for example, to: (1) The drastic climatic fluctuations in connection with the re- cession of the land-ice giving rise to the alternation of inter- stadials (warm periods with rapid ice recession) and stadials (cold periods with readvances o作者: Creditee 時(shí)間: 2025-3-31 06:39
heories and synthesis originate from Scandinavian data. This applies, for example, to: (1) The drastic climatic fluctuations in connection with the re- cession of the land-ice giving rise to the alternation of inter- stadials (warm periods with rapid ice recession) and stadials (cold periods with readvances o978-90-481-8399-9978-94-015-7692-5作者: Thyroiditis 時(shí)間: 2025-3-31 13:01 作者: 暫時(shí)中止 時(shí)間: 2025-3-31 16:47 作者: Surgeon 時(shí)間: 2025-3-31 21:33 作者: 溫和女孩 時(shí)間: 2025-3-31 22:07
Cyclic Lamination in Proximal Varves Reflecting the Length of Summers during Late Weichsel in Southe Blekinge, southernmost Sweden. Between 43 and 56 day varves have been observed in the summer layers and the number of day varves are supposed to represent the length of summers during the Boiling Chronozone in Late Weichsel of southernmost Sweden.作者: Homocystinuria 時(shí)間: 2025-4-1 04:57 作者: 發(fā)源 時(shí)間: 2025-4-1 06:55
Flora, Fauna and Stable Isotopes in Late-Würm Deposits at Lobsigensee (Swiss Plateau)imum depth 2.5 m. It was chosen as one of the primary reference sites in the Swiss contribution to IGCP 158b (LANG 1983). The littoral site “150” was investigated by various methods (AMMANN & TOBOLSKI 1983, GAILLARD 1983, ELIAS & WILKINSON 1983, HOFMANN 1983, CHAIX 1983, EICHER & SIEGENTHALER 1983, 作者: 小木槌 時(shí)間: 2025-4-1 10:24
Late Weichselian Fluctuations in the French Alps and Massif Central from Pollen Analysess species refuges, as was shown by Van Campo & Aymonin (1962), Lang (1970), Beug (1975), Van der Hammen (1979), but also the variations of climate. These regions were not much affected by the Scandinavian inland ice; therefore they may have registered the first oscillations that took place at the en作者: Custodian 時(shí)間: 2025-4-1 17:05
Climatic and Glacial Fluctuations during the Late-Glacial and the Holocene in Oisans (Isere, France)nges. Emphasis is laid on the thick and long-lasting snow cover. Besides these two recurrence periods, the major events observed mainly evidence the influence of drought: glacial regression and formation of rock- glaciers.作者: neutrophils 時(shí)間: 2025-4-1 18:57
The Classical Late Weichselian Climatic Fluctuations in Mexicoto establish similar chronostratigraphies of climatic variations for other parts of the world (e.g. Chile, Western North America, New Zealand, South Antarctica). Recent investigations give more and more evidence that the classical West European chronostratigraphy of the Late Weichselian in many deta
