scholarly journals A new perspective of the Alboran Upwelling System reconstruction during the Marine Isotope Stage 11: A high-resolution coccolithophore record

2020 ◽  
Vol 245 ◽  
pp. 106520
Author(s):  
Alba González-Lanchas ◽  
José-Abel Flores ◽  
Francisco J. Sierro ◽  
María Ángeles Bárcena ◽  
Andrés S. Rigual-Hernández ◽  
...  
2017 ◽  
Vol 114 (38) ◽  
pp. 10047-10052 ◽  
Author(s):  
Carlos Pérez-Mejías ◽  
Ana Moreno ◽  
Carlos Sancho ◽  
Miguel Bartolomé ◽  
Heather Stoll ◽  
...  

The Late Quaternary glacial–interglacial transitions represent the highest amplitude climate changes over the last million years. Unraveling the sequence of events and feedbacks at Termination III (T-III), including potential abrupt climate reversals similar to those of the last Termination, has been particularly challenging due to the scarcity of well-dated records worldwide. Here, we present speleothem data from southern Europe covering the interval from 262.7 to 217.9 kyBP, including the transition from marine isotope stage (MIS) 8 to MIS 7e. High-resolution δ13C, δ18O, and Mg/Ca profiles reveal major millennial-scale changes in aridity manifested in changing water availability and vegetation productivity. uranium–thorium dates provide a solid chronology for two millennial-scale events (S8.1 and S8.2) which, compared with the last two terminations, has some common features with Heinrich 1 and Heinrich 2 in Termination I (T-I).


2018 ◽  
Vol 123 (12) ◽  
pp. 9416-9428 ◽  
Author(s):  
Nele Tim ◽  
Eduardo Zorita ◽  
Franziska U. Schwarzkopf ◽  
Siren Rühs ◽  
Kay‐Christian Emeis ◽  
...  

Author(s):  
Ruben Vazquez ◽  
Ivan Parras-Berrocal ◽  
William Cabos ◽  
Dmitry V. Sein ◽  
Rafael Mañanes ◽  
...  

2021 ◽  
Vol 126 (3) ◽  
Author(s):  
Norbert R. Nowaczyk ◽  
Jiabo Liu ◽  
Birgit Plessen ◽  
Antje Wegwerth ◽  
Helge W. Arz

Urban Climate ◽  
2021 ◽  
Vol 38 ◽  
pp. 100919
Author(s):  
Miao Yu ◽  
Xuan Chen ◽  
Jiachuan Yang ◽  
Shiguang Miao

2013 ◽  
Vol 43 (5) ◽  
pp. 1004-1014 ◽  
Author(s):  
Julien Jouanno ◽  
Julio Sheinbaum

Abstract The upper-ocean heat budget of the Caribbean upwelling system is investigated during the onset of the Atlantic warm pool (June–September) using high-resolution observations of sea surface temperature and a high-resolution (°) regional model. Vertical mixing is found to be the major cooling contribution to the mixed layer heat budget in the nearshore and offshore Colombia Basin. Numerical results show that intense mesoscale eddies in the Colombia Basin significantly shape the turbulent cooling and may participate in the maintenance of cooler temperature in this region compared to surrounding areas. Indeed, increased mixing at the base of the mixed layer occurs below energetic surface jets that form on the downstream side of the eddies. These jets generally flow offshore and may arise from the deformation of the surface mesoscale field. It is shown that significant contribution of horizontal advection to the mixed layer heat budget is limited to a radius of 300 km around the Guajira and Margarita upwelling zones.


2016 ◽  
Vol 35 (11) ◽  
pp. 977-985 ◽  
Author(s):  
Daniele Colombo ◽  
Gary McNeice ◽  
Diego Rovetta ◽  
Ernesto Sandoval-Curiel ◽  
Ersan Turkoglu ◽  
...  

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