globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-13-00139.1
Scopus记录号: 2-s2.0-84892467183
论文题名:
The mean sea level equation and its application to the mediterranean sea
作者: Pinardi N.; Bonaduce A.; Navarra A.; Dobricic S.; Oddo P.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2014
卷: 27, 期:1
起始页码: 442
结束页码: 447
语种: 英语
Scopus关键词: Almost periodic ; Buoyancy fluxes ; Equation of state ; ITS applications ; Mass conservation equations ; Mean sea level ; Mediterranean sea ; Volume transport ; Equations of state ; Surface waters ; Sea level ; equation of state ; mass balance ; sea level ; stochasticity ; surface water ; Mediterranean Sea
英文摘要: Aformalism to obtain a mean sea level equation (MSLE) is constructed for any limited ocean region and/or the global ocean by considering the mass conservation equation with compressible effects and a linear equation of state. The MSLE contains buoyancy fluxes terms representing the steric effects and the mass flux is represented by surface water fluxes and volume transport terms. The MSLE is studied for the Mediterranean Sea case using a simulation experiment for the decade 1999-2008. It is found that the Mediterranean MSL tendency is made of a steric contribution that is almost periodic in time superimposed on a stochasticlike signal due to the mass balance, dominating the MSL tendency. The MSL tendency stochastic-like term is a result of the imbalance between the volume flux at Gibraltar and the area average surface water flux. © 2014 American Meteorological Society.
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被引频次[WOS]:25   [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/51387
Appears in Collections:气候变化事实与影响

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作者单位: Department of Physics and Astronomy, Bologna University, Bologna, Italy; Centro EuroMediterraneo sui Cambiamenti Cimatici, Bologna, Italy; Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna, Bologna, Italy

Recommended Citation:
Pinardi N.,Bonaduce A.,Navarra A.,et al. The mean sea level equation and its application to the mediterranean sea[J]. Journal of Climate,2014-01-01,27(1)
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