首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Predominant modes of winter surface wind variability over the Gulf of Alaska
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Predominant modes of winter surface wind variability over the Gulf of Alaska

机译:阿拉斯加湾冬季表面风变率的主要模式

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摘要

Two distinct modes extracted from winter (Dec.-Mar.) monthly mean surface wind variability over the Gulf of Alaska (GOA) and part of the northeast Pacific Ocean have been identified along with their associations with sea surface temperature (SST), coastal downwelling, surface air temperature (SAT) and sea level Pressure (SLP). The leading mode of surface wind variability, accounting for 45% of the variance, is characterized by two distinct and alternating modes or their linear combination, and shows strong interannual and interdecadal variations with the transition years in the mid-1970s and the beginning and late of 1990s. One mode (M1) features a coherent cyclonic or anticyclonic surface wind anomaly in the GOA and pail of the northeast Pacific Ocean, and reflects wind field variability related to the intensity of large scale atmosphere-ocean interactions associated with the Aleutian Low, the Pacific/North American (PNA) pattern. the Pacific decadal oscillation (PDO), and the South Oscillation (SO). This mode significantly influences SAT over the GOA and the entire northeast Pacific and influences downwelling along the eastern and southeastern GOA. It does not significantly influence SST in the northern GOA. The other (M2) characterizes dominant southerly or northerly anomalies, and significantly influences coastal downwelling in the northern and Southeastern GOA. It is also correlated with SAT over the GOA, the Bering Sea shelf, and much of Alaska. The impact of M2 on SST is greater than that of M I in the GOA and the Bering Sea. M1 and M2, respectively, correspond to the PNA pattern and a dipole pattern. and the litter is characterized by the third mode of the empirical orthogonal function (EOF) analysis of winter SLP variability over the domain 20 degrees-70 degrees N and 160 degrees E-100 degrees W, accounting for 13% of the variance. The dipole pattern is a new mode of winter atmospheric variability, with opposite anomalous centres over the Southern Bering Sea and the west coast of the USA and part of the northeast Pacific Ocean.
机译:已经确定了从阿拉斯加湾(GOA)和东北太平洋部分地区冬季(12月至3月)的月平均地面风变率中提取的两种不同模式,以及它们与海表温度(SST),沿海下降的关系。 ,地表气温(SAT)和海平面压力(SLP)。地表风变异性的主导模式,占变异的45%,具有两种不同且交替的模式或它们的线性组合,并且在1970年代中期和始末期都表现出强烈的年际和年代际变化。 1990年代。一种模式(M1)在东北太平洋的GOA和桶中具有相干的气旋或反气旋地表风异常,并反映了与阿留申低地,太平洋/北美(PNA)模式。太平洋年代际振荡(PDO)和南方涛动(SO)。这种模式会极大地影响GOA和整个东北太平洋上的SAT,并影响沿GOA东部和东南部的下沉。它不会显着影响北部GOA的SST。另一个(M2)表征了主要的南北偏北异常,并且显着影响了北部和东南部GOA的沿海下降区。它还与GOA,白令海陆架和阿拉斯加大部分地区的SAT相关。 M2对海表温度的影响大于GOA和白令海中M I的影响。 M1和M2分别对应于PNA图案和偶极图案。凋落物的特征在于,经验性正交函数(EOF)分析的第三种模式在冬季20°-70°N和160°E-100°W范围内的冬季SLP变异性中占13%。偶极子模式是冬季大气变率的一种新模式,在白令海南部和美国西海岸以及东北太平洋的一部分上具有相反的异常中心。

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