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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >An updated assessment of trends and variability in total and extreme rainfall in the western Pacific
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An updated assessment of trends and variability in total and extreme rainfall in the western Pacific

机译:西太平洋地区总和极端降雨趋势和变化的最新评估

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摘要

Rainfall records for 23 countries and territories in the western Pacific have been collated for the purpose of examining trends in total and extreme rainfall since 1951. For some countries this is the first time that their data have been included in this type of analysis and for others the number of stations examined is more than twice that available in the current literature. Station trends in annual total and extreme rainfall for 1961–2011 are spatially heterogeneous and largely not statistically significant. This differs with the results of earlier studies that show spatially coherent trends that tended to reverse in the vicinity of the South Pacific Convergence Zone (SPCZ). We infer that the difference is due to the Interdecadal Pacific Oscillation switching to a negative phase from about 1999, largely reversing earlier rainfall changes. Trend analyses for 1981–2011 show wetter conditions in the West Pacific Monsoon (WPM) region and southwest of the mean SPCZ position. In the tropical North Pacific it has become wetter west of 160°E with the Intertropical Convergence Zone/WPM expanding northwards west of 140°E. Northeast of the SPCZ and in the central tropical Pacific east of about 160°E it has become drier. Our findings for the South Pacific subtropics are consistent with broader trends seen in parts of southern and eastern Australia towards reduced rainfall. The relationship between total and extreme rainfall and Pacific basin sea surface temperatures (SSTs) has been investigated with a focus on the influence of the El Ni?o-Southern Oscillation (ENSO). We substantiate a strong relationship between ENSO and total rainfall and establish similar relationships for the threshold extreme indices. The percentile-based and absolute extreme indices are influenced by ENSO to a lesser extent and in some cases the influence is marginal. Undoubtedly, larger-scale SST variability is not the only influence on these indices.
机译:自1951年以来,已整理了西太平洋23个国家和地区的降雨记录,以检查总降雨和极端降雨的趋势。对于某些国家来说,这是首次将其数据纳入这种类型的分析中,而对于其他国家,这是首次检查站的数量是当前文献中数量的两倍以上。 1961-2011年全年和极端降雨的台站趋势在空间上是非均质的,并且在统计上没有显着意义。这与早期研究的结果不同,后者的研究表明在南太平洋收敛带(SPCZ)附近空间趋势趋于相反。我们推断,差异是由于年代际太平洋涛动从大约1999年开始转为负相,很大程度上逆转了先前的降雨变化。 1981-2011年的趋势分析显示,西太平洋季风(WPM)地区和SPCZ平均位置西南的湿润状况。在北太平洋热带地区,热带湿润区/ WPM向北扩展至140°E以西,在160°E以西变得较湿。 SPCZ的东北部和东经约160°E的中部热带太平洋已变得干燥。我们对南太平洋亚热带地区的发现与澳大利亚南部和东部部分地区降雨减少的大趋势一致。已经研究了总和极端降雨与太平洋盆地海表温度(SSTs)之间的关系,重点是厄尔尼诺-南方涛动(ENSO)的影响。我们证实了ENSO与总降雨量之间的密切关系,并为阈值极端指数建立了相似的关系。基于百分位数的指数和绝对极端指数受ENSO的影响较小,在某些情况下影响很小。无疑,更大范围的SST变异性不是唯一影响这些指标的因素。

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