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Books > Earth & environment > Earth sciences > Geology & the lithosphere > Geological surface processes (geomorphology)

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High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems - Past Climatic Changes Using Cave Structures (Paperback, Softcover reprint of the original 1st ed. 2018) Loot Price: R2,957
Discovery Miles 29 570
High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems - Past Climatic Changes...

High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems - Past Climatic Changes Using Cave Structures (Paperback, Softcover reprint of the original 1st ed. 2018)

Anoop Kumar Singh

Series: Springer Theses

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Loot Price R2,957 Discovery Miles 29 570 | Repayment Terms: R277 pm x 12*

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This thesis encompasses a study of past precipitation patterns based on six cave stalagmites from different parts of the Indian Himalaya. This is the first speleothem study in the Indian Himalaya that shows a direct relationship between past precipitation and the collapse of civilization. The stalagmites examined were KL-3 from Jammu and Kashmir; TCS and BR-1 from Himachal Pradesh; and DH-1, SA-1 and CH-1 from Uttarakhand. Based on the high-resolution palaeoclimatic reconstruction (35 U/th dates, 5 AMS dates, 1,500 samples for 18O and 13C values) obtained for the duration of the Pleistocene-Holocene transition (16.2-9.5 ka BP) and Mid-Holocene-Present (ca. 4.0 ka BP-Present), three major events were identified, namely the Older Dryas (OD), Bolling-Allerod (BA) period and Younger Dryas (YD) at ca. 14.3-13.9, 13.9-12.7 and 12.7-12.2 ka BP, respectively. The study showed a gradual reduction in the precipitation from 4 ka BP onwards for about a millennium with a peak arid period between 3.2 and 3.1 ka BP. According to the findings, the LIA (Little Ice Age) covers a time span from 1622-1820 AD, during which the climate was wetter than that in the post-LIA period (1820-1950 AD). In addition, this thesis supports the assumption that the WDs (Western Disturbances) contribute significantly to the total rainfall in the Himalaya region.

General

Imprint: Springer International Publishing AG
Country of origin: Switzerland
Series: Springer Theses
Release date: June 2019
First published: 2018
Authors: Anoop Kumar Singh
Dimensions: 235 x 155mm (L x W)
Format: Paperback
Pages: 146
Edition: Softcover reprint of the original 1st ed. 2018
ISBN-13: 978-3-319-89252-8
Categories: Books > Earth & environment > Earth sciences > Palaeontology > General
Books > Earth & environment > Earth sciences > Geology & the lithosphere > Geological surface processes (geomorphology) > General
Books > Earth & environment > Geography > Physical geography > Topography > Mountains
LSN: 3-319-89252-5
Barcode: 9783319892528

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