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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Atmospheric centres of action associated with the Atlantic ITCZ position
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Atmospheric centres of action associated with the Atlantic ITCZ position

机译:与大西洋ITCZ位置相关的大气作用中心

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Relationships between Atlantic extra-tropical features and Intertropical Convergence Zone (ITCZ) position close to Northeast Brazil are discussed, on the basis of atmosphere and ocean patterns in DJF and April. Composites for three situations were analysed. In the first composite, years with extreme positive North Atlantic Oscillation Index (NAOI) in DJF and the ITCZ displaced southward in April were selected. The other two composites were related only to anomalous ITCZ positions - either south or north of the equator - in April. The physical mechanism for the relation between the NAOI and the ITCZ is the influence of the southern North Atlantic Oscillation (NAO) centre on the North Atlantic subtropical high, the sea surface temperature (SST) and the intensity of the trade winds; however, this situation occurred in only a few years. Analysis of the other situations indicated the influence of a dominant mode of variability over the North and South Atlantic Oceans that affects the ITCZ position. Over the North Atlantic, this mode was related to a shifting of the NAO pattern, which modified the position of the North Atlantic subtropical high. Over the South Atlantic, this mode indicated an extra-tropical centre of action associated with displacement of the South Atlantic subtropical high. A proposed index for monitoring ITCZ position, named the North Atlantic Index (NAI), was calculated from sea level pressure (SLP) anomalies in the two centres of action of the North Atlantic in DJF, which are related to the shifting of the NAO. Although the NAO index is related to atmospheric/oceanic features associated with ITCZ displacement, the new index presented higher and more organized correlations with atmospheric and oceanic conditions linked to ITCZ behaviour and can be useful even when the NAO is not extreme.
机译:根据DJF和4月的大气和海洋模式,讨论了大西洋热带外地貌特征与靠近巴西东北部的热带收敛区(ITCZ)位置之间的关系。分析了三种情况的复合材料。在第一个综合报告中,选择了DJF和ITCZ在四月向南移位的北大西洋涛动指数(NAOI)极高的年份。其他两个组合仅与4月份ITCZ异常位置有关-赤道以南或以北。 NAOI和ITCZ之间关系的物理机制是北大西洋涛动中心(NAO)对北大西洋副热带高压,海表温度(SST)和信风强度的影响;但是,这种情况仅在短短几年内就发生了。对其他情况的分析表明,北大西洋和南大西洋的主要变化模式影响了ITCZ的位置。在北大西洋上空,这种模式与NAO模式的转变有关,这改变了北大西洋副热带高压的位置。在南大西洋上空,这种模式表明与南大西洋副热带高压的位移有关的热带外作用中心。从北大西洋在DJF的两个行动中心的海平面压力(SLP)异常计算出一个建议的用于监视ITCZ位置的指数,即北大西洋指数(NAI),这与NAO的移动有关。尽管NAO指数与与ITCZ位移相关的大气/海洋特征有关,但新指数与与ITCZ行为相关的大气和海洋条件呈现出越来越高的组织相关性,即使NAO并不极端,它也很有用。

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