登录    注册    忘记密码    使用帮助

详细信息

楚科奇陆架海域夏季温度年际变化特征     被引量:1

Interannual Variation of SummerTemperature of SeaAreas on the Chukchi Shelf

文献类型:期刊文献

中文题名:楚科奇陆架海域夏季温度年际变化特征

英文题名:Interannual Variation of SummerTemperature of SeaAreas on the Chukchi Shelf

作者:王贵圆[1,2,3];李敏[1,2,3];于婷[4];李丙瑞[5];施旭东[1,2,3];谢玲玲[1,2,3]

机构:[1]陆架及深远海气候、资源与环境广东省高等学校重点实验室,广东湛江524088;[2]自然资源部空间海洋遥感与应用重点实验室,北京100081;[3]广东海洋大学海洋与气象学院,广东湛江524088;[4]国家海洋信息中心,天津300171;[5]中国极地研究中心,上海200136

年份:2023

卷号:43

期号:4

起止页码:112

中文期刊名:广东海洋大学学报

外文期刊名:Journal of Guangdong Ocean University

收录:CSTPCD、、CSCD_E2023_2024、北大核心、CSCD、北大核心2020

基金: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)。

语种:中文

中文关键词:楚科奇海;温度;年际变化;海表热通量;侧向热通量

外文关键词:Chukchi sea;temperature;interannual variation;surface heat flux;lateral heat flux

中文摘要:【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50 m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。

外文摘要:【Objective】To study the interannual variation of the temperature on the Chukchi shelf in August-October.【Method】The temperature reanalysis data(GLORYS12V1),surface heat flux,and lateral heat flux were used to analyze the interannual variation of temperature and its relationship with surface and lateral heat fluxes.【Result and Conclusion】The results show that the temperature in the southeast is higher than that in the west and east,and the highest temperature is 8℃,and the temperature in the northern and western area is mostly below 3℃.The temperatures at the depths of 5 m,29 m,47 m and above 50 m increase by 0.03-0.07℃/a for the linear trend with obvious interannual variation during 1993—2020.The first mode of the EOF analysis shows that the temperature in the entire domain varies in phase,with maximum difference between the warm year and cold year present in different regions for the different depth layers.The heat budget analysis shows that the short wave heat flux and the heat from Bering Strait are two main inputs which affect the interannual variation of temperature,and the long wave heat flux,the latent heat flux,and the heat flux through the eastern and northern sections are the output.The quantitative relation between the heat flux and temperature variation can provide a reference for the manifestation and forecast of the characteristics and variations of the temperature in the Chukchi Sea.

参考文献:

正在载入数据...

版权所有©广东海洋大学 重庆维普资讯有限公司 渝B2-20050021-8 
渝公网安备 50019002500408号 违法和不良信息举报中心