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Titlebook: Earth Surface Processes and Environmental Changes in East Asia; Records From Lake-ca Kenji Kashiwaya,Ji Shen,Ju Yong Kim Book 2015 Springer

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发表于 2025-3-21 17:54:31 | 显示全部楼层 |阅读模式
书目名称Earth Surface Processes and Environmental Changes in East Asia
副标题Records From Lake-ca
编辑Kenji Kashiwaya,Ji Shen,Ju Yong Kim
视频video
概述Presents information about climate-hydrological changes in the Holocene and recent past through the study of several lake-catchment systems in East Asia (from Mongolia to Taiwan).Illustrates how the l
图书封面Titlebook: Earth Surface Processes and Environmental Changes in East Asia; Records From Lake-ca Kenji Kashiwaya,Ji Shen,Ju Yong Kim Book 2015 Springer
描述.This book examines relationships between climate-hydrological changes and other phenomena including land use and natural disasters during the Holocene and recent past. In particular, periods of rapid climatic shifts such as global warming and global cooling are examined through paleohydrological and other studies of various lake-catchment systems in East Asia, from Mongolia in the north to Taiwan in the south. A number of different research techniques are used in the work presented here, including sediment analysis and optically stimulated luminescence dating and the reader learns how the lake-catchment system functions as a “proxy observatory” for past and present environmental monitoring. The lake catchments studied by the authors of this volume are under similar climatic conditions, i.e., under the East Asia monsoon, with some systematic difference in climatic factors. Both proxy and observation data are available for the surrounding countries’ provisions against natural disasters that are related to climate-hydrological events and readers will see how present instrumental observation data can be connected to past proxy data (sediment information) in the system..
出版日期Book 2015
关键词Climate Change and Hydrological Change; East Asia Monsoon; Lake-catchment System; Millennia Environment
版次1
doihttps://doi.org/10.1007/978-4-431-55540-7
isbn_softcover978-4-431-56254-2
isbn_ebook978-4-431-55540-7
copyrightSpringer Japan 2015
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Centennial-Scale Environmental Changes in Terhiin Tsagaan Lake, Mongolia Inferred from Lacustrine Se, can be used for the indicator for some hydro-climatic events and/or lake level changes. The gradual fluctuation of the averaged brightness was well correlated with the contents of biogenic silica plus organic matter. The profiles of the brightness can provide high resolution information regarding
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Palaeoenvironment and Palaeoclimate Evolution of Northeast China: Based on Multi-proxy Analysis of dry, and this period corresponded to the LGM (Last Glacial Maximum). During the period between 19,940 and 14,510 cal a BP, the precipitation increased compared to the previous period and temperature also increased to some extent. During the period between 14,510 and 11,500 cal a BP, the late glacia
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Paleovegetation and Paleoclimate Evolution of Past 27.7 cal ka BP Recorded by Pollen and Charcoal o climate condition. From 19.9 to 14.5 cal ka BP, there was broad-leaved forest steppe with . and . as the main component when . and Ferns increased greatly, which suggested a cold-wet climatic trend. During 14.5 ∼ 10.8 cal ka BP, the study region was occupied by sparse forest grassland with ., ., .
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Rapid Environmental Change of Jingpo Lake in Mid-Holocene: Inferred from Fluvial/Lacustrine Sedimen yr BP); (iii) Unite 3, lacustrine sedimentary facies (above 1,154 cm, after ∼5,060 cal. yr BP). Our results suggest that Unite 1 represents fluvial sedimentary facies, while the lacustrine sedimentary facies developed afterwards. Between 1,250 and 1,240 cm intervals, the highest MS values and high
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Palaeohydrological and Palaeoenvironmental Fluctuations of the Historic Eurimji Lake,ost artificial layers in Lake Eurimji, which vertically constitute the bottom of Eurimji bank or dyke at about 306.5 m.a.s.l. The height is about 15 m. The present study reconstructs the paleo-precipitation of Lake Eurimji by applying an age mode to core sediments in the ER3-1 borehole using the mea
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Late Quaternary Environmental Changes of the Hwajinpo and Songjiho Lagoons on the Eastern Coast of . Although the lithologic changes in the both lagoons do not show any temporal similarity, T-R (transgression and regression) trends based on the grain size variation shows simultaneity. T-R diagram presents three cycles clearly since 7,800 .C yr BP. Highstand sea levels (transgressions) are appeare
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