Large‐scale air‐sea interactions over the North Pacific from summer 1962 through the subsequent winter
Large‐scale air‐sea interactions over the North Pacific from summer 1962 through the subsequent winter
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DOI：
10.1029/jz068i022p06171
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发表时间：
1963-11
影响因子：
--
通讯作者：
J. Namias
中科院分区：
文献类型：
--
作者：
J. Namias
本文描述了1962年下半年和1963年上半年北太平洋中部和东部沃茨广泛而持续的温暖，并将其归因于盛行的异常风和天气系统。证据表明，大尺度盛行的大气系统的演变部分是由异常水温以及强迫的影响，由于季节性变化的太阳高度。证据部分是南极天气学的，部分是物理的，包括计算感热和湍流热交换以及辐射平衡。其中比较突出的异常天气是台风弗里达的奇怪行为和1962-1963年北方大部分地区的极端异常冬季。
The extensive and persistent warmth of central and eastern North Pacific waters during the last half of 1962 and early 1963 is described and attributed to prevailing abnormal wind and weather systems. Evidence is presented to indicate that the evolution of the large-scale prevailing atmospheric systems was partly determined by the anomalous water temperatures as well as forcing influences due to a seasonal change in the elevation of the sun. The evidence is partly statistic-synoptic and partly physical, involving computations of sensible and turbulent heat exchange as well as radiation balance. Among the more outstanding weather abnormalities treated are the strange behavior of typhoon Freda and the extremely abnormal winter of 1962–1963 over much of the northern hemisphere.