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同位体比質量分析法×標準化降水量指数 (Standardized Precipitation Index)×
分野地球物理学地球物理学
系統Process / pipelineProcess / pipeline
提唱年19941993
提唱者Thomas Coplen and othersThomas McKee, Neil Doesken, and John Kleist
種類Measurement of stable and radiogenic isotope ratiosProbabilistic drought indicator
原典Coplen, T. B. (1994). Reporting of stable hydrogen, carbon, and oxygen isotopic abundances. Pure and Applied Chemistry, 66(2), 273-276. DOI ↗McKee, T. B., Doesken, N. J., & Kleist, J. (1993). The relationship of drought frequency and duration to time scales. Proceedings of the Eighth Conference on Applied Climatology, 179-184. link ↗
別名IRMSSPI
関連33
概要Isotope Ratio Mass Spectrometry (IRMS) is an analytical technique that measures the relative abundance of stable isotopes (H, C, N, O, S) and some radiogenic isotopes (e.g., ⁸⁷Sr/⁸⁶Sr) in samples with high precision. Standardized by Coplen and colleagues, IRMS enables paleoclimate reconstruction, source tracing (diet, water origin), geochemical fingerprinting, and age dating through radiogenic isotopes.The Standardized Precipitation Index (SPI) is a climate index that quantifies precipitation anomalies relative to historical norms, standardized to account for differences in precipitation climatology across regions. Introduced by McKee, Doesken, and Kleist in 1993, SPI has become a primary tool for drought detection and characterization, adopted by meteorological agencies worldwide for operational drought monitoring and early warning systems.
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ScholarGate手法を比較: Isotope Ratio Mass Spectrometry · Standardized Precipitation Index. 2026-06-20に以下より取得 https://scholargate.app/ja/compare