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Spatio-temporal variability and predictability of summer monsoon onset over the Philippines

机译:菲律宾夏季风爆发的时空变化和可预测性

摘要

The spatio-temporal variability of boreal summer monsoon onset over the Philippines is studied through the analysis of daily rainfall data across a network of 76 gauges for the period 1977 to 2004 and the pentad Merged Analysis of Precipitation from the US Climate Prediction Center from 1979 to 2006. The onset date is defined using a local agronomic definition, namely the first wet day of a 5-day period receiving at least 40 mm without any 15-day dry spell receiving less than 5 mm in the 30 days following the start of that period. The onset is found to occur rather abruptly across the western Philippines around mid-May on average and is associated with the set-up of a "classical" monsoonal circulation with low-level easterlies subsequently veering to southerly, and then southwesterly. The onset manifests itself merely as a seasonal increase of rainfall over the eastern Philippines, where rainfall occurs throughout most of the year. Interannual variability of the onset date is shown to consist of a spatially coherent large-scale component, rather similar over the western and eastern Philippines, with a moderate to high amount of local-scale (i.e. station scale) noise. In consequence, the large-scale signal can be easily retrieved from any sample of at least 5–6 stations across the network although the local-scale coherence and fingerprint of the large-scale signal of the onset date are found to be stronger over the central Philippines, roughly from Southern Luzon to Northern Mindanao. The seasonal predictability of local onset is analyzed through a cross-validated canonical correlation analysis using tropical Pacific and Indian Ocean sea surface temperature in March and the 850 hPa May wind field from dynamical forecast models as predictors. The regional-scale onset, defined as the average of standardized local-scale anomalies in onset date, shows good predictive skill (r ≈ 0.8). Moreover, most of the stations show weak to moderate skill (median skill = 0.28-0.43 depending on the scheme) with spatial averaging across stations typically increasing skill to > 0.6.
机译:通过分析1977年至2004年期间76个测量仪网络的每日降雨量数据以及美国气候预测中心从1979年至2004年的五元合并降水分析,研究了菲律宾北半球夏季风发作的时空变化。 2006年。发病日期是根据当地的农艺学定义而定义的,即在开始的30天内,至少5天的第一湿日接收至少40毫米,而15天的干湿法接收不到5毫米。期。平均而言,发病时间在菲律宾西部平均在5月中旬左右突然发生,并且与“古典”季风环流有关,低水平的东风随后向南,然后向西南倾斜。发病仅表现为菲律宾东部降雨的季节性增加,菲律宾东部一年四季都在降雨。发病日期的年际变化显示为由空间上连贯的大尺度成分组成,在菲律宾西部和东部相当相似,具有中等到大量的局部尺度(即台站尺度)噪声。因此,尽管发现大范围信号在开始日期的本地一致性和指纹强度要强于网络,但可以轻松地从网络上至少5–6个站点的任何样本中检索大范围信号。菲律宾中部,大致从吕宋岛南部到棉兰老岛北部。通过交叉验证的典型相关分析,使用三月的热带太平洋和印度洋海面温度以及五月的850 hPa风场,通过动态预测模型作为预测因子,来分析局部发病的季节性可预测性。区域尺度的发作定义为发病日期标准化局部尺度异常的平均值,显示出良好的预测能力(r≈0.8)。而且,大多数工作站显示出弱到中等的技能(中位技能= 0.28-0.43,具体取决于方案),跨工作站的空间平均通常将技能提高到> 0.6。

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