Is a third scale of motion admissible in a boundary-current region?

2017 ◽  
Vol 132 (2) ◽  
Author(s):  
Fulvio Crisciani ◽  
Fabio Cavallini ◽  
Renzo Mosetti
1996 ◽  
Vol 54 (6) ◽  
pp. 1097-1122 ◽  
Author(s):  
M. A. Pena ◽  
K. L. Denman ◽  
J. R. Forbes ◽  
S. E. Calvert ◽  
R. E. Thomson

2021 ◽  
Author(s):  
Dmitry Stepanov ◽  
Alexander Ostrovskii ◽  
Dmitry Kaplunenko ◽  
Jae-Hun Park ◽  
Young-Gyu Park ◽  
...  

2021 ◽  
Author(s):  
Christopher Chapman ◽  
Bernadette Sloyan ◽  
Madeleine Cahill

<p>We investigate Marine Heat Waves and Marine Cold Spells (MHWs/MCSs) along the east coast of the Australian continent, a western boundary current region with exceedingly complex dynamics. We provide evidence that episodic MWHs/MCSs along the south-east of the Australian continent are driven by upstream variations in the position, but not necessarily the strength, of the East Australian Current, and that these variations are, in turn, controlled by small-scale (100s of kilometers) eddies that propagate into the region from the east. These eddies are able to alternately 'shut-off' and `turn-on' the poleward transport of warm water by the boundary current in a manner analogous to atmospheric blocking. Precursors to these `blocks' are detectable as much as 60 days prior to the onset of an event. We will discuss the implications of our results for the early prediction of MHW/MCS events.</p>


2021 ◽  
pp. 103619
Author(s):  
Alexander Ostrovskii ◽  
Dmitry Stepanov ◽  
Dmitry Kaplunenko ◽  
Jae-Hun Park ◽  
Young-Gyu Park ◽  
...  

2016 ◽  
Vol 33 (12) ◽  
pp. 2717-2733 ◽  
Author(s):  
Wenjing Jia ◽  
Dong Wang ◽  
Nadia Pinardi ◽  
Simona Simoncelli ◽  
Andrea Storto ◽  
...  

AbstractA quality control (QC) procedure is developed to estimate monthly mean climatologies from the large Argo dataset (2005–12) over the North Pacific western boundary current region. In addition to the individual QC procedure, which checks for instrumental, transmission, and gross errors, the paper describes and shows the impact of climatological checks (collective QC) on the quality of both processed profiles and resultant climatological distributions. Objective analysis (OA) is applied progressively to produce the gridded climatological fields. The method uses horizontal regional climatological averages defined in five regime-oriented subregions in the Kuroshio area and the Japan Sea. Performing the QC procedure on specific coherent subregions produces improved profiling data and climatological fields because more details about the local hydrodynamics are taken into consideration. Nonrepresentative data and random noises are more effectively rejected by this method, which has value both in defining a climatological mean and identifying outlier data. Assessing with both profiling and coordinated datasets, the agreement is reasonably good (particularly for those areas with abundant observations), but the results (although already smoothed) can capture more detailed or mesoscale features for further regional studies. The method described has the potential to meet future challenges in processing accumulating Argo observations in the coming decades.


2020 ◽  
Vol 54 (6) ◽  
pp. 1703-1722 ◽  
Author(s):  
Narges Soltani ◽  
Sebastián Lozano

In this paper, a new interactive multiobjective target setting approach based on lexicographic directional distance function (DDF) method is proposed. Lexicographic DDF computes efficient targets along a specified directional vector. The interactive multiobjective optimization approach consists in several iteration cycles in each of which the Decision Making Unit (DMU) is presented a fixed number of efficient targets computed corresponding to different directional vectors. If the DMU finds one of them promising, the directional vectors tried in the next iteration are generated close to the promising one, thus focusing the exploration of the efficient frontier on the promising area. In any iteration the DMU may choose to finish the exploration of the current region and restart the process to probe a new region. The interactive process ends when the DMU finds its most preferred solution (MPS).


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