@article{PAR00000638,
  title = {{S}pectral characteristics of the response of the meridional overturning circulation to deep-water formation},
  author = {{D}eshayes, {J}. and {F}rankignoul, {C}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}he response of the upper limb of the meridional overturning circulation to the variability of deep-water formation is investigated analytically with a linear, reduced-gravity model in basins of simple geometry. {T}he spectral characteristics of the model response are first derived by prescribing white-noise fluctuations in the meridional transport at the northern boundary. {A}lthough low-frequency basin modes are solutions to the eigenproblem, they are too dissipative to be significantly excited by the boundary forcing, and the thermocline depth response has a red spectrum with no prevailing time scale other than that of a high-frequency equatorial mode, only flattening at the millennial time scale because of vertical diffusivity. {T}he meridional transport is asymmetric about the equator because the northern part of the basin is directly influenced by the boundary forcing while the southern part is mostly set in motion by long {R}ossby waves. {T}his results in the equator acting as a low-pass filter for the {S}outhern {H}emisphere, which clarifies the so-called buffering effect of the equator. {I}n a basin connected by a southern circumpolar channel, the thermocline depth and the transport spectra are redder than in the forced basin and, when a somewhat more realistic stochastic forcing derived from general circulation model simulations is considered, the variability is strongly reduced at high frequency. {T}he linear model qualitatively explains several features of the low-frequency variability of the meridional overturning circulation in climate models, such as its red spectrum and its larger intensity in the {N}orth {A}tlantic {O}cean.},
  keywords = {},
  booktitle = {},
  journal = {{J}ournal of {P}hysical {O}ceanography},
  volume = {35},
  numero = {10},
  pages = {1813--1825},
  ISSN = {0022-3670},
  year = {2005},
  DOI = {10.1175/{JPO}2793.1},
  URL = {https://www.documentation.ird.fr/hor/{PAR}00000638},
}