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评估 CMIP5 模式中红海温度在当前和未来气候下的表现。

Assessment of Red Sea temperatures in CMIP5 models for present and future climate.

机构信息

Centre Oceanogràfic de Balears, Instituto Español de Oceanografía, Palma, Spain.

King Abdullah University of Science and Technology (KAUST), Red Sea Research Center (RSRC), Thuwal, Saudi Arabia.

出版信息

PLoS One. 2021 Jul 30;16(7):e0255505. doi: 10.1371/journal.pone.0255505. eCollection 2021.

Abstract

The increase of the temperature in the Red Sea basin due to global warming could have a large negative effect on its marine ecosystem. Consequently, there is a growing interest, from the scientific community and public organizations, in obtaining reliable projections of the Red Sea temperatures throughout the 21st century. However, the main tool used to do climate projections, the global climate models (GCM), may not be well suited for that relatively small region. In this work we assess the skills of the CMIP5 ensemble of GCMs in reproducing different aspects of the Red Sea 3D temperature variability. The results suggest that some of the GCMs are able to reproduce the present variability at large spatial scales with accuracy comparable to medium and high-resolution hindcasts. In general, the skills of the GCMs are better inside the Red Sea than outside, in the Gulf of Aden. Based on their performance, 8 of the original ensemble of 43 GCMs have been selected to project the temperature evolution of the basin. Bearing in mind the GCM limitations, this can be an useful benchmark once the high resolution projections are available. Those models project an averaged warming at the end of the century (2080-2100) of 3.3 ±> 0.6°C and 1.6 ±> 0.4°C at the surface under the scenarios RCP8.5 and RCP4.5, respectively. In the deeper layers the warming is projected to be smaller, reaching 2.2 ±> 0.5°C and 1.5 ±> 0.3°C at 300 m. The projected warming will largely overcome the natural multidecadal variability, which could induce temporary and moderate decrease of the temperatures but not enough to fully counteract it. We have also estimated how the rise of the mean temperature could modify the characteristics of the marine heatwaves in the region. The results show that the average length of the heatwaves would increase ~15 times and the intensity of the heatwaves ~4 times with respect to the present conditions under the scenario RCP8.5 (10 time and 3.6 times, respectively, under scenario RCP4.5).

摘要

由于全球变暖,红海盆地的温度升高可能会对其海洋生态系统产生很大的负面影响。因此,科学界和公共组织越来越有兴趣获得整个 21 世纪红海温度的可靠预测。然而,用于进行气候预测的主要工具——全球气候模式(GCM),可能并不完全适合该相对较小的地区。在这项工作中,我们评估了 CMIP5 集合中的 GCM 在再现红海 3D 温度变化的不同方面的能力。结果表明,一些 GCM 能够以与中高分辨率回溯相当的精度在大空间尺度上再现当前的可变性。一般来说,GCM 在红海内部的表现优于外部,在亚丁湾。根据它们的表现,从最初的 43 个 GCM 集合中选择了 8 个来预测该盆地的温度演变。考虑到 GCM 的局限性,一旦获得高分辨率预测,这可以作为一个有用的基准。这些模型预测,在 RCP8.5 和 RCP4.5 情景下,到本世纪末(2080-2100 年),表面平均升温分别为 3.3±>0.6°C 和 1.6±>0.4°C。在更深的层次上,预计升温较小,在 300 米处达到 2.2±>0.5°C 和 1.5±>0.3°C。预计升温将大大超过自然的多年代际可变性,这可能导致温度暂时适度下降,但不足以完全抵消它。我们还估计了平均温度的上升将如何改变该地区海洋热浪的特征。结果表明,与当前条件相比,在 RCP8.5 情景下(在 RCP4.5 情景下分别为 10 倍和 3.6 倍),热浪的平均长度将增加约 15 倍,强度将增加约 4 倍。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/39b8/8323894/1ff7e7dc6359/pone.0255505.g001.jpg

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