Ocean Circulation and Climate: Observing and Modelling the Global Ocean

By G. Siedler, J. Church, J. Gould. 2001

445 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Ocean Engineering, Oceanography

View Paper: https://www.semanticscholar.org/paper/772308aa2f154d30e8b3ddaa59e9247551d15ed7

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Citations in the corpus

Parameterization of Eddy Fluxes near Oceanic Boundaries (2008, background): “This is at odds with the observational evidence that eddy fluxes have a strong impact both on the material composition and exchange rate between the surface BL and pycnocline and on the air–sea fluxes of heat (Robbins et al. 2000; Price 2001; Weller 2003).”
Dynamically and Kinematically Consistent Global Ocean Circulation and Ice State Estimates (2013, methodology): “Discussion 575 Acknowledgments 575 References 576”
Fundamentals of Ocean Climate Models (2004, methodology): “• The book edited by Siedler et al. (2001) is noteworthy for its many lucid contributions by leading experts.”
Description and validation of a two-step analogue/regression downscaling method (2013, background): “This limitation may be associated with the insufficient spatial and temporal resolution used (i.e. that offered by GCMs), as they cannot resolve atmospheric structures which are small in size and/or have a short life cycle, such as the convective structures responsible for heavy precipitations in Sp”
Evaluation of the GECCO2 ocean synthesis: transports of volume, heat and freshwater in the Atlantic (2015, background): “3 PW (Bryden and Imawaki, 2001; Lumpkin and Speer, 2007), which is consistent with a maximum of 1.”
The presence of the ctenophore Mnemiopsis leidyi in the Oslofjorden and considerations on the initial invasion pathways to the North and Baltic Seas (2007, background): “The drifting from the northern Gulf Stream to the North Sea, through NAC, can least 15 to 60 days, depending on the season and wind oscillations (cf. Siedler et al. 2001).”
VERTICAL MIXING, ENERGY, AND THE GENERAL CIRCULATION OF THE OCEANS (2004, background): “THE STRATIFICATION Observations In a few narrow, sporadic oceanic regions at high latitudes (see Warren 1981) near-surface fluid sometimes becomes sufficiently dense to be vertically unstable, sinking to the sea floor (see several chapters in Siedler et al. 2001).”