globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00382-016-3242-0
Scopus记录号: 2-s2.0-84976292951
论文题名:
Heat and salt redistribution within the Mediterranean Sea in the Med-CORDEX model ensemble
作者: Llasses J.; Jordà G.; Gomis D.; Adloff F.; Macías D.; Harzallah A.; Arsouze T.; Akthar N.; Li L.; Elizalde A.; Sannino G.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2018
卷: 51, 期:3
起始页码: 1119
结束页码: 1143
语种: 英语
英文关键词: Heat fluxes ; Med-CORDEX ; Mediterranean Sea ; Ocean regional climate models ; Salt fluxes
Scopus关键词: climate modeling ; climate prediction ; data assimilation ; ensemble forecasting ; heat flux ; heat transfer ; regional climate ; Mediterranean Sea
英文摘要: Characterizing and understanding the basic functioning of the Mediterranean Sea in terms of heat and salt redistribution within the basin is a crucial issue to predict its evolution. Here we quantify and analyze the heat and salt transfers using a simple box model consisting of four layers in the vertical for each of the two (western and eastern) basins. Namely, we box-average 14 regional simulations of the Med-CORDEX ensemble plus a regional and a global reanalysis, computing for each of them the heat and salt exchanges between layers. First, we analyze in detail the mechanisms behind heat and salt redistribution at different time scales from the outputs of a single simulation (NEMOMED8). We show that in the western basin the transfer between layer 1 (0–150 m) and layer 2 (150–600 m) is upwards for most models both for heat and salt, while in the eastern basin both transfers are downwards. A feature common to both basins is that the transports are smaller in summer than in winter due to the enhanced stratification, which dampen the mixing between layers. From the comparison of the 16 simulations we observe that the spread between models is much larger than the ensemble average for the salt transfer and for the heat transfer between layer 1 and layer 2. At lower layers (below 600 m) there is a set of models showing a good agreement between them, while others are not correlated with any other. The mechanisms behind the ensemble spread are not straightforward. First, to have a coarse resolution prevents the model to correctly represent the heat and salt redistribution in the basin. Second, those models with a very different initial stratification also show a very different redistribution, especially at intermediate and deep layers. Finally, the assimilation of data seems to perturb the heat and salt redistribution. Besides this, the differences among regional models that share similar spatial resolution and initial conditions are induced by more subtle mechanisms which depend on the variable and process analyzed. In order to reduce the uncertainties in the Mediterranean regional climate projections further modelling studies and better observational datasets are needed to constrain the main sources of discrepancies among models. In the absence of those, an ensemble modelling approach as the one followed in the Med-CORDEX initiative seems to be the best solution to evaluate model uncertainties into the future climate projections. © 2016, Springer-Verlag Berlin Heidelberg.
Citation statistics:
被引频次[WOS]:19   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109180
Appears in Collections:影响、适应和脆弱性
气候变化事实与影响

Files in This Item:

There are no files associated with this item.


作者单位: Mediterranean Institute for Advanced Studies (IMEDEA, UIB-CSIC), Miquel Marquès 21, Esporles, 0719, Spain; CNRM Météo-France/CNRS, UMR 3589, Toulouse, France; Water Research Unit, Institute for Environment and Sustainability, European Commission, Joint Research Center, Via Enrico Fermi 2749, Ispra, 21027, Italy; Institut National des Sciences et Technologies de la Mer, 28, rue du 2 mars 1934 2025 Salammbô, Tunis, Tunisia; Laboratoire de Météorologie Dynamique, CNRS/Ecole Polytechnique/ENS/UPMC, Palaiseau Cedex, Paris, 91128, France; Institute for Atmospheric and Environmental Sciences, Goethe University, Altenhöferallee 1, Frankfurt/Main, 60438, Germany; Max Planck Institute for Meteorology, Bundestrasse 53, Hamburg, 20146, Germany; ENEA Centro Ricerche Casaccia, Via Anguillarese, 301, Rome, 00123, Italy

Recommended Citation:
Llasses J.,Jordà G.,Gomis D.,et al. Heat and salt redistribution within the Mediterranean Sea in the Med-CORDEX model ensemble[J]. Climate Dynamics,2018-01-01,51(3)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Llasses J.]'s Articles
[Jordà G.]'s Articles
[Gomis D.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Llasses J.]'s Articles
[Jordà G.]'s Articles
[Gomis D.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Llasses J.]‘s Articles
[Jordà G.]‘s Articles
[Gomis D.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.