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臧恒范等在研究冬季渤海海冰的长期预报时发现,前一年7月北太平洋西风漂流区的海水温度是一个较好的指标,为了能进一步对这个指标进行检查,除在日常业务预报中试用外,逐步探讨这个指标与预报对象之间联系的物理过程也是很重要的。本文即是这方面的一个初步尝试。
When studying the long-term forecast of winter sea ice in the Bohai Sea, Zang et al. Found that the seawater temperature in the westerly drift over the North Pacific in July of the previous year was a good indicator. In order to further examine this indicator, in addition to its trial in daily business forecast In addition, it is also important to gradually explore the physical process of the link between this indicator and the forecasted object. This article is an initial attempt in this area.