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从印度三个地貌区域采集的日降雨样本的三年稳定水同位素数据

Three Years of Stable Water Isotope Data of Daily Rain Samples Collected from Three Geomorphic Regions of India.

作者信息

Rajaveni Sundara Pandian, Nimya S S, Sengupta Saikat, Datye Amey, Sarma Dipankar

机构信息

Centre for Climate Change Research, Indian Institute of Tropical Meteorology, Ministry of Earth Sciences, Pune, India.

Department of Earth, Atmospheric and Planetary Sciences, Purdue University, West Lafayette, IN, USA.

出版信息

Sci Data. 2024 Dec 28;11(1):1445. doi: 10.1038/s41597-024-04308-7.

DOI:10.1038/s41597-024-04308-7
PMID:39732720
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11682116/
Abstract

High-frequency precipitation (solid/liquid) isotope datasets are useful for identification of moisture sources and various dynamical and thermodynamical processes controlling precipitation formation. Here, we report three-year (2019-2021) daily rain isotope (both oxygen, δO hereafter, and hydrogen, δH, hereafter) datasets from three unique locations in India during the Indian Summer Monsoon (ISM). The locations are- (1) Port Blair- an island situated in the Bay of Bengal (BoB); (2) Mahabaleshwar, located at the crest of the Western Ghats Mountain; and (3) Tezpur, in northeast India, situated close to a dense forest. These stations receive moisture from different sources and experience different rain mechanisms during ISM. Therefore, the isotope datasets presented here would be useful for envisaging the impact of diverse rain formation processes on isotope values during the ISM.

摘要

高频降水(固态/液态)同位素数据集有助于识别水汽来源以及控制降水形成的各种动力和热力过程。在此,我们报告了印度夏季风(ISM)期间,来自印度三个独特地点的为期三年(2019 - 2021年)的每日降雨同位素(以下简称氧同位素δO和氢同位素δH)数据集。这些地点分别是:(1)位于孟加拉湾(BoB)的岛屿布莱尔港;(2)位于西高止山脉山顶的马哈巴利普兰;(3)位于印度东北部、靠近茂密森林的提斯普尔。这些站点在ISM期间接收来自不同来源的水汽,并经历不同的降雨机制。因此,本文呈现的同位素数据集将有助于设想ISM期间不同降雨形成过程对同位素值的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/4ab561519100/41597_2024_4308_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/124ee9189a76/41597_2024_4308_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/10e2a8d4feee/41597_2024_4308_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/4ab561519100/41597_2024_4308_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/124ee9189a76/41597_2024_4308_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/10e2a8d4feee/41597_2024_4308_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e32e/11682116/4ab561519100/41597_2024_4308_Fig3_HTML.jpg

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本文引用的文献

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Extreme local recycling of moisture via wetlands and forests in North-East Indian subcontinent: a Mini-Amazon.通过印度东北部次大陆的湿地和森林实现水分的极端局地再循环:迷你亚马逊。
Sci Rep. 2023 Jan 10;13(1):521. doi: 10.1038/s41598-023-27577-5.
2
Four years of daily stable water isotope data in stream water and precipitation from three Swiss catchments.来自瑞士三个流域的溪流和降水的四年稳定日水位同位素数据。
Sci Data. 2022 Feb 10;9(1):46. doi: 10.1038/s41597-022-01148-1.
3
Temperature and precipitation effects on the isotopic composition of global precipitation reveal long-term climate dynamics.
温度和降水对全球降水同位素组成的影响揭示了长期气候动态。
Sci Rep. 2021 Sep 16;11(1):18503. doi: 10.1038/s41598-021-98094-6.
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Stable isotopes in water vapor and rainwater over Indian sector of Southern Ocean and estimation of fraction of recycled moisture.南大洋印度海域水汽和雨水中的稳定同位素以及再循环水汽比例的估算
Sci Rep. 2018 May 15;8(1):7552. doi: 10.1038/s41598-018-25522-5.
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Role of Oceanic and Terrestrial Atmospheric Moisture Sources in Intraseasonal Variability of Indian Summer Monsoon Rainfall.海洋和陆地大气水分源在印度夏季风降雨季节内变化中的作用。
Sci Rep. 2017 Oct 6;7(1):12729. doi: 10.1038/s41598-017-13115-7.
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Sci Rep. 2016 Jan 25;6:19555. doi: 10.1038/srep19555.
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18O depletion in monsoon rain relates to large scale organized convection rather than the amount of rainfall.季风雨水中的18O亏损与大规模有组织的对流有关,而非与降雨量有关。
Sci Rep. 2014 Jul 11;4:5661. doi: 10.1038/srep05661.