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The changing relationship between the December North Atlantic Oscillation and the following February East Asian trough before and after the late 1980s

机译:1980年代后期前后,12月北大西洋涛动与随后的2月东亚低谷之间的关系不断变化

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This study investigates the changing relationship between the December North Atlantic Oscillation (NAO) and the following February East Asian trough (EAT) throughout the past 60years. We found that the relationship between the December NAO and the following February EAT is significantly enhanced after the late 1980s compared with the period before the late 1980s. The changing relationship mainly results from the enhanced relationship between the December NAO and the following February North Atlantic mid-latitudes' sea surface temperature (SST) anomalies (NAMA) during the same period. During the period after the late 1980s, the persistent positive (negative) NAO pattern from December to the following January contributes to a positive (negative) NAMA, which reaches its maximum magnitude in the following February and excites an anomalous wave train along the North Atlantic and northern Eurasia, and significantly impacts the EAT. During the period before the late 1980s, the positive (negative) NAO pattern during December cannot persist into the following January, and the related positive (negative) NAMA is insignificant during the following February, causing the response of the simultaneous EAT to be insignificant as well. Moreover, there exists a significant impact of the December NAO on the December-January NAMA after the late 1980s, while the December-January NAMA is relatively less affected by the December NAO before the late 1980s. As a result, the simultaneous response of the atmospheric circulation anomalies to the December-January NAMA are evident before the late 1980s, and the positive (negative) NAMA can excite an anomalous wave train along the North Atlantic and northern Eurasia and significantly deepen (shallow) the downstream EAT. By contrast, after involving a feature of atmosphere forcing of SST, the simultaneous feedback of the December-January NAMA on EAT is significantly decreased after the 1980s.
机译:这项研究调查了过去60年中12月北大西洋涛动(NAO)与随后2月东亚海槽(EAT)之间变化的关系。我们发现,与1980年代后期之前的时期相比,12月份的NAO和随后的2月EAT之间的关系得到了显着增强。变化的关系主要是由于12月的NAO与随后的2月北大西洋中纬度的同期海表温度(SST)异常(NAMA)之间的关系增强。在1980年代后期之后,从12月到次年1月的NAO持续呈正(负)模式有助于NAMA呈正(负)值,并在随后的2月达到最大幅度,并激发了北大西洋沿岸的异常波列和北部的欧亚大陆,并极大地影响了EAT。在1980年代后期之前的12月,NAO的正(负)NAO模式不能持续到下一年的1月,而在随后的2月,相关的N(负)NAMA则微不足道,导致同时EAT的响应微不足道。好。此外,12月份的NAO对1980年代后期之后的12月至1月NAMA产生了重大影响,而12月份的1月NAMA受1980年代后期的12月NAO影响相对较小。结果,在1980年代末之前,大气环流异常同时响应了12月至1月的NAMA,并且正(负)NAMA可以激发北大西洋和欧亚大陆北部的异常波列并显着加深(浅)下游EAT。相比之下,在经历了SST强迫大气的特征之后,1980年代之后12月至1月NAMA对EAT的同时反馈显着降低。

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