王贵圆,李敏,于婷,李丙瑞,施旭东,谢玲玲

• 1:陆架及深远海气候
• 2:资源与环境广东省高等学校重点实验室
• 3:自然资源部空间海洋遥感与应用重点实验室
• 4:广东海洋大学海洋与气象学院

摘要(Abstract)：

【目的】研究楚科奇海陆架区夏季（8—10月）温度年际变化。【方法】利用GLORYS12V1再分析数据，并结合海表热通量及断面侧向热通量数据，分析楚科奇海温度年际变化及其与海表热通量和侧向热通量的关系。【结果与结论】楚科奇海东南海域温度最高，约8℃；北部和西部海域多低于3℃；1993—2020年5、29、47 m以及50m以浅温度的线性增加趋势为0.03～0.07℃/a，且表现出年际变化特征；经验正交函数分解结果显示，各层第一模态均表现出整个研究区域为同位相变化，且各层温度变化具有较大的区域不同；热收支分析结果显示，该时期短波辐射和白令海峡热输送是两个主要热量输入量，影响温度年际变化，而长波辐射、潜热通量以及通过东侧和北侧断面的热量为主要的热量输出量。线性回归分析得出楚科奇海热通量的变化与8—10月平均温度之间的定量关系，可为更好地表征和预测楚科奇海温度变化特征提供参考。

关键词(KeyWords)： 楚科奇海;温度;年际变化;海表热通量;侧向热通量

Abstract:

Keywords:

基金项目(Foundation): 国家重点研发计划（2022YFC3104805）;; 广东海洋大学博士科研启动经费（R20022）;; 自然资源部海洋环境信息保障技术重点实验室开放基金课题（B22209）;; 工业与信息化部高技术船舶科研项目（MC-201919-C11）;; 广东省冲一流专项资金（080503032101,231420003）

作者(Author): 王贵圆,李敏,于婷,李丙瑞,施旭东,谢玲玲

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