塔那那利佛-马达加斯加两站降水水稳定同位素组成的比较研究

V. Ramaroson, J. Rajaobelison, L. P. Fareze, F. A. Razafitsalama, Mamiseheno Rasolofonirina, C. Rakotomalala
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引用次数: 0

摘要

在“全球降水同位素网络”数据库中,塔那那利佛有来自两个站点的两个不同的数据集。这两个数据集相隔34年。本研究一方面旨在描述两站降水水稳定同位素组成的变化,并了解其来源,主要与气象因素有关。另一方面,将塔那那利佛数据与区域和国际数据进行比较,以确定降水中同位素组成变率的其他来源。同位素记录表明,经过34年的间隔,夏季和冬季(两个主要季节)降水中重同位素的富集程度更高。降水量的波动是造成这种时间变化的主要原因。与夏季和冬季降水相反,季间降水在34年后具有相似的同位素值。这两个站在地理上很近,因此空间方面可以忽略不计,因为纬度和海拔对降水的同位素组成没有影响。二阶参数d-excess的月平均值均大于100/00,表明水汽再循环。与区域/国际资料的比较表明,降水同位素变异主要受降水量效应、不同水汽源、与水汽源的站距以及水汽轨迹沿线气象因子的变化等因素的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Water Stable Isotope Composition of Precipitations at Two Stations in Antananarivo-Madagascar: A Comparative Study
In the “Global Network of Isotopes in Precipitation” database, Antananarivo has two distinct datasets from two stations. Thirty-four years separate the two datasets. This study aims on the one hand to depict the variations of the water stable isotopes composition of precipitations from the two stations and understand their origins, mainly in relation to meteorological factors. On the other hand, the Antananarivo data are compared with regional and international data to identify other sources of isotope composition variability in precipitation. Isotope records showed that after thirty-four-year gap, summer and winter (the two main seasons) precipitations are more enriched in heavy isotopes. The precipitation amount fluctuation would mostly contribute to this temporal variation. Opposite to summer and winter precipitations, inter-season rainfalls have similar isotope values after thirty-four years. The two stations are geographically close and the spatial aspect is therefore negligible since there are no latitude nor altitude effects on the isotope composition of precipitations. Regarding the second order parameter d-excess, the monthly mean values from both stations are higher than 100/00 and could indicate moisture recycling. The comparison with regional/international data showed that the isotope variability in precipitation is primarily due to precipitation amount effect, different moisture source, the stations distance from it and the change of meteorological factors along the moisture trajectory.
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