[OANNES Foro] Deep-reaching acceleration of global mean ocean circulation over the past two decades

Mario Cabrejos casal en infotex.com.pe
Lun Feb 10 09:35:27 PST 2020


Science Advances  

05 Feb 2020 Vol. 6, no. 6 
DOI: 10.1126/sciadv.aax7727 

Deep-reaching acceleration of global mean ocean circulation over the past
two decades

Shijian Hu <https://advances.sciencemag.org/content/6/6/eaax7727#aff-1> 1,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-2> 2,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-3> 3,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-4> 4,
<https://advances.sciencemag.org/content/6/6/eaax7727#corresp-1> *, Janet
Sprintall <https://advances.sciencemag.org/content/6/6/eaax7727#aff-5> 5,
Cong Guan <https://advances.sciencemag.org/content/6/6/eaax7727#aff-1> 1,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-2> 2,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-3> 3,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-4> 4, Michael J.
McPhaden <https://advances.sciencemag.org/content/6/6/eaax7727#aff-6> 6, Fan
Wang <https://advances.sciencemag.org/content/6/6/eaax7727#aff-1> 1,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-2> 2,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-3> 3,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-4> 4,
<https://advances.sciencemag.org/content/6/6/eaax7727#corresp-1> *, Dunxin
Hu <https://advances.sciencemag.org/content/6/6/eaax7727#aff-1> 1,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-2> 2,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-3> 3,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-4> 4 and Wenju Cai
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-3> 3,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-7> 7,
<https://advances.sciencemag.org/content/6/6/eaax7727#aff-8> 8

Abstract

Ocean circulation redistributes Earth's energy and water masses and
influences global climate. Under historical greenhouse warming, regional
ocean currents show diverse tendencies, but whether there is an emerging
trend of the global mean ocean circulation system is not yet clear. Here, we
show a statistically significant increasing trend in the globally integrated
oceanic kinetic energy since the early 1990s, indicating a substantial
acceleration of global mean ocean circulation. The increasing trend in
kinetic energy is particularly prominent in the global tropical oceans,
reaching depths of thousands of meters. The deep-reaching acceleration of
the ocean circulation is mainly induced by a planetary intensification of
surface winds since the early 1990s. Although possibly influenced by wind
changes associated with the onset of a negative Pacific decadal oscillation
since the late 1990s, the recent acceleration is far larger than that
associated with natural variability, suggesting that it is principally part
of a long-term trend.

 

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