首页|南海海表温度时空分布特征及其对不同厄尔尼诺事件的响应

南海海表温度时空分布特征及其对不同厄尔尼诺事件的响应

Temporal and Spatial Distribution Characteristics of Sea Surface Temperature in the South China Sea and Its Response to Different El NINO Events

扫码查看
基于1951-2017年空间分辨率为2°×2°的NOAA卫星全球月平均海表温度资料以及NINO 3.4指数,通过合成分析、相关分析和连续功率谱分析,探讨南海海表温度异常对厄尔尼诺事件的响应情况.结果表明,1951-2017年,南海海表温度出现显著的增温趋势,同时每隔3~4a出现异常情况;南海海表温度异常与NINO 3.4指数有一定的相关性,南海西南部海表温度异常与NINO 3.4指数的相关性最好;SP型厄尔尼诺事件中,南海海表温度在发生年的春季出现负异常,在冬季转为正异常后持续到衰退年的夏季;SU型厄尔尼诺事件,南海海表温度在发生年的春季出现负异常,持续到秋季,在衰退年的春季出现负异常,秋冬季亦持续出现负异常.
This article uses NOAA global monthly average sea surface temperature data with spatial resolution of 2° × 2°and NINO 3.4 index from 1951 to 2017 to further explore the response of the South China Sea temperature anomaly to El NINO's through synthetic analysis,correlation analysis and continuous power spectrum analysis.The study shows that:The sea surface temperature of the South China Sea has a significant warming trend from 1951 to 2017,and its sea temperature turns abnormal every 3 to 4 years;The SSTA in the South China Sea has a certain correlation with the NINO 3.4 index,and the best correlation with the NINO 3.4 index in the southwest of the South China Sea;SP-type El NINO sea surface temperature in the South China Sea firstly has a negative anomaly in the spring of the year of occurrence and then turns positive anomaly in the winter and continues into the summer of the year of recession;The SU type El NINO shows a negative anomaly in the spring of the year of occurrence,which lasts until the fall,and then another negative anomaly in the spring of the year of recession,which continues to show negative anomalies in the fall and winter of recession year.

SST in the South China SeaEl NINOtemporal and spatial distribution

薛佩珍、龙星玥、薛潇、马俊贵、牛宏宇

展开 >

中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室,宁夏银川 750002

宁夏气象防灾减灾重点实验室,宁夏银川 750002

宁夏石嘴山市气象局,宁夏石嘴山 753000

贵州省黔南布依族苗族自治州气象局,贵州 都匀 558000

南京信息工程大学滨江学院,江苏无锡 214000

展开 >

南海海温 厄尔尼诺 时空分布

中国气象局科技司公益性行业科研专项

RYSY201904

2023

宁夏大学学报(自然科学版)
宁夏大学

宁夏大学学报(自然科学版)

CSTPCD
影响因子:0.377
ISSN:0253-2328
年,卷(期):2023.44(4)
  • 1