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Modern rain-isotope data from Indian island and the mainland on the daily scale for the summer monsoon season

机译:夏季季风季节每日从印度岛屿和大陆获得的现代雨同位素数据

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摘要

The atmospheric stable isotopes in rainwater are measured as the ratio of heavy to the lighter (e.g., 18O/16O). This data article describes two datasets of daily rain isotopic variations during the Indian Summer Monsoon (ISM) season. Firstly, an island site (namely Port Blair) dataset for four years (2012–2015) and another dataset of Indian mainland sites (namely Nagpur, Tezpur, and Kolkata) for the year 2015. Port Blair is strategically situated in the Bay of Bengal (BoB), which is known to be a significant moisture source to ISM rainfall over the Indian landmass. On the other hand, sites in the mainland are receivers of the BoB moisture. This dataset includes 1030 isotopic analyses made on daily water samples as well as rainfall amount (24 hours) during ISM.The data is related to “Isotopic investigation of the moisture transport processes over the Bay of Bengal” [1].
机译:雨水中的大气稳定同位素以重与轻的比率(例如, 18 O / 16 O)进行测量。本数据文章介绍了印度夏季风(ISM)期间每日降雨同位素变化的两个数据集。首先,是四年(2012-2015年)的一个岛屿站点(即布莱尔港)数据集,以及2015年的另一个印度大陆站点(即那格浦尔,特兹普尔和加尔各答)的数据集。布莱尔港地理位置优越,位于孟加拉湾(BoB),这是印度陆地上ISM降雨的重要水分来源。另一方面,内地的站点是BoB湿气的接收者。该数据集包括对ISM期间的每日水样以及降雨量(24小时)进行的1030次同位素分析。该数据与“孟加拉湾水汽输送过程的同位素研究” [1]有关。

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