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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Diagnosing warm-season rainfall variability in Mexico: A classification tree approach
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Diagnosing warm-season rainfall variability in Mexico: A classification tree approach

机译:诊断墨西哥暖季降水变化:分类树方法

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摘要

Many observational studies provide evidence that connects seasonal rainfall variations over parts of the subtropical and tropical Americas with the behaviour of large-scale climate modes. This paper extends these claims based on analysis of a fairly extensive historical rainfall data set (1943-2006) from several locations in Mexico. The paper applies classification tree (CT) analysis to link warm-season rainfall variability to climate indices, which characterize ENSO state, the NAO, and sea-level pressure in the eastern North Pacific. While the results generally indicate that a significant part of the variability in warm-season rainfall over Mexico is conditioned by large-scale climate modes, there is only limited evidence of simple lag relationships involving Mexican rainfall and antecedent climate behaviour. The main implication here is that advances in warm seasonal rainfall prediction are likely to depend partially on improved capabilities to foreshadow the behaviour of large-scale climate modes a season or more in advance. Copyright (C) 2009 Royal Meteorological Society
机译:许多观测研究提供了证据,将亚热带和热带美洲部分地区的季节性降雨变化与大规模气候模式的行为联系起来。本文基于对墨西哥多个地点的相当广泛的历史降雨数据集(1943-2006年)的分析来扩展这些主张。本文应用分类树(CT)分析将暖季降雨的可变性与气候指数联系起来,以表征ENSO状态,NAO和北太平洋东部海平面压力。虽然这些结果通常表明,墨西哥暖季降雨的很大一部分变化是由大规模气候模式决定的,但只有有限的证据表明,简单的滞后关系涉及墨西哥的降雨和先前的气候行为。这里的主要含义是,温暖的季节性降雨预报的进展可能部分取决于提高的能力,以便提前一个季节或更早地预示大规模气候模式的行为。皇家气象学会(C)2009

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