Arctic circulation from a Lagrangian perspective

[EN] In the context of rapid increase of temperature in the polar regions, inducing a dramatic ice melting, Lagrangian transport in the Arctic Ocean becomes an area of key interest. There exists evidence of changes in the circulation of water masses at different depths such as a notable decrease in...

Full description

Bibliographic Details
Main Authors: Balibrea Iniesta, Francisco, García Garrido, Víctor José, Mancho, Ana María, Wiggins, Stephen
Other Authors: Rodríguez Archilla, Juan Francisco, Didactica de la Matematica, Escuela de Ingenierias Industrial, Informática y Aeroespacial
Format: Review
Language:English
Published: Universidad de Sevilla 2016
Subjects:
Online Access:https://hdl.handle.net/10612/20489
https://idus.us.es/bitstream/handle/11441/79571/9788409056545-NoLineal2016-bookofabstracts.pdf?sequence=1&isAllowed=y
Description
Summary:[EN] In the context of rapid increase of temperature in the polar regions, inducing a dramatic ice melting, Lagrangian transport in the Arctic Ocean becomes an area of key interest. There exists evidence of changes in the circulation of water masses at different depths such as a notable decrease in intensity of the so-called Beaufort Gyre and the discharge of a great amount of fresh water into the North-West Atlantic Ocean. These facts may have a direct impact on the global circulation of water and heat. The aim of this talk is to show the phase portrait of the sea currents throughout the Arctic Ocean, which allows us to study aspects of their dynamics. This is done by means of the numerical method known as Lagrangian descriptors, which computes and graphically displays flow structures over a given domain of the ocean, highlighting coherent jet circulation patterns in red color. The research of FB-I, VG-G and AMM is supported by the MINECO under grant MTM2014-56392-R. We acknowledge support from MINECO: ICMAT Severo Ochoa project SEV-2011-0087.