2000-2020 年春季北太平洋海冰浓度的主要模式和特征区

LI Xu, M. J. C. Crabbe
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摘要

在北极放大效应的影响下,北太平洋海冰变化正在成为全球气候变化的一个重要指标。由于北太平洋海冰变化影响广泛而复杂,了解其动态变化,特别是其时空演变规律具有重要意义。本研究利用旋转经验正交分解法,将整个北太平洋划分为近期全球变暖下海冰浓度演变的六个特征区,突出了近海海域海冰变化的复杂性和多样性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
LEADING MODES AND FEATURE ZONES OF SEA ICE CONCENTRATION IN NORTH PACIFIC DURING SPRING SEASONS OF 2000–2020
Under the influence of the Arctic amplification, sea ice variability in North Pacific is becoming a key indicator of global climate changes. Due to the widespread and complex impacts of North Pacific sea ice variations, the understanding of its dynamic changes, especially its spatial and temporal evolution patterns, has great significance. In this study, we used the rotated empirical orthogonal decomposition to divide the whole North Pacific into six feature zones on the evolution sea ice concentration under the recent global warming and highlighted the complexity and diversity of sea ice variations in the offshore waters.
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