| contributor author | Pinardi, N. | |
| contributor author | Bonaduce, A. | |
| contributor author | Navarra, A. | |
| contributor author | Dobricic, S. | |
| contributor author | Oddo, P. | |
| date accessioned | 2017-06-09T17:08:23Z | |
| date available | 2017-06-09T17:08:23Z | |
| date copyright | 2014/01/01 | |
| date issued | 2013 | |
| identifier issn | 0894-8755 | |
| identifier other | ams-79991.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4222831 | |
| description abstract | formalism 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 stochastic-like 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. | |
| publisher | American Meteorological Society | |
| title | The Mean Sea Level Equation and Its Application to the Mediterranean Sea | |
| type | Journal Paper | |
| journal volume | 27 | |
| journal issue | 1 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/JCLI-D-13-00139.1 | |
| journal fristpage | 442 | |
| journal lastpage | 447 | |
| tree | Journal of Climate:;2013:;volume( 027 ):;issue: 001 | |
| contenttype | Fulltext | |
