Sea Surface Temperature Changes Over the Twentieth and Twenty-First Centuries in East Vietnam Sea Simulated by Multi CMIP5 Models

L. Thien
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Abstract

The East ​​Vietnam Sea plays important roles in the Pacific Northwest region. The projection of changes in sea surface temperature (SST) in these regions is an important research topic in marine science. However, this is a very difficult problem due to the lack of available long-term projection data. Recently, with the development of numerical modeling technology, it has become an important way to help us understand climate change. This paper focuses on studying the SST changes in the East Vietnam Sea during the history of the 20th century and the change under 3 emission scenarios in the 21st century based on a combination of 20 global models (GCM) from Phase 5 of the the Climate Model Intercomparison Project (CMIP5) and together with the observed data set. Compared with the observed data, most of the global GCMs models can simulate well the spatial and seasonal changes of the SST over the East Vietnam Sea regions. The spatial and annual SST trends over the the 20th century based on both observations and multimodel ensemble averages show that the warming trend of SST over most of the East Vietnam Sea with the largest warming trend occurred in the center and southern regions of the East Vietnam Sea. However, compared with the observation, CMIP5 underestimated SST trends over most regions of East Vietnam Sea. In addition, there is a consistency between the CMIP5 and the spatial and seasonal observations of the SST trend in the East Vietnam Sea areas. The future SST projections for East Vietnam Sea indicate that RCP 4.5 and RCP 8.5 exhibit a gradual increase in annual SST during the 21st century at a rate of 0.1 °C and 0.3 °C per 10 years respectively. The lowest emission mitigation scenario, RCP 2.6, produces the lowest rate of warming. By the end of the 21st century, the annual SST is projected to increase by 0.5-2.0 °C in 3 emission scenarios of typical representative concentration pathways (RCP) 8.5, 4.5 and 2.6.  
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多个CMIP5模式模拟的20世纪和21世纪东越南海海面温度变化
东越海在太平洋西北地区占有重要地位。这些地区海温变化的预估是海洋科学的一个重要研究课题。然而,由于缺乏现有的长期预测数据,这是一个非常困难的问题。近年来,随着数值模拟技术的发展,它已成为帮助我们了解气候变化的重要途径。本文基于气候模式比对项目(CMIP5)第5阶段的20个全球模式(GCM),结合观测资料,重点研究了20世纪东越南海海温的历史变化和21世纪3种排放情景下的海温变化。与观测资料相比,大多数全球GCMs模式都能较好地模拟东越南海区海温的空间和季节变化。基于观测资料和多模式综合平均的20世纪海温空间和年变化趋势表明,东越南海大部分地区的海温呈现增温趋势,增温趋势最大的是东越南海中部和南部地区。然而,与观测结果相比,CMIP5低估了东越南海大部分地区的海温趋势。此外,CMIP5模式与东越南海温趋势的空间和季节观测结果具有一致性。对东越南海未来海温的预估表明,在21世纪,RCP 4.5和RCP 8.5的年海温分别以每10年0.1°C和0.3°C的速率逐渐增加。最低排放减缓情景,即RCP 2.6,产生的升温速度最低。预计到21世纪末,在典型代表性浓度路径(RCP) 8.5、4.5和2.6的3种排放情景下,年海表温度将增加0.5 ~ 2.0°C。
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