Results 251 to 260 of about 116,641 (323)
Decreased Deep Water Oxygenation in the Western North Pacific During the Plio‐Pleistocene Transition
Abstract The deep North Pacific, a vast respired carbon reservoir, likely plays a key role in the Plio‐Pleistocene CO2 decline and global cooling, but evidence for this is lacking. Here, oxygenation change in the upper deep western North Pacific between 5.3 and 1.0 million years ago (Ma) is reconstructed using multiple organic and inorganic proxies ...
Man Zhao, Guodong Jia
wiley +1 more source
The return of stagnant slab recorded by intraplate volcanism. [PDF]
Zhou ZB+7 more
europepmc +1 more source
Atmospheric Response to Antarctic Coastal Polynyas
Abstract The lack of sea ice in Antarctic coastal polynyas enables strong ocean‐to‐atmosphere heat fluxes and intense sea‐ice production. Although these features are primarily driven by intense offshore winds, their impact on local atmospheric conditions remains poorly understood.
M. Noel, S. Masson, C. Rousset
wiley +1 more source
Strength and timing of austral winter Angolan coastal upwelling. [PDF]
Körner M, Brandt P, Dengler M.
europepmc +1 more source
Abstract Arctic amplification, the accelerated warming of the Arctic compared to lower latitude, remains poorly understood, particularly regarding the role of clouds. In this study, we analyze 26 years of downwelling longwave radiation (DLR) measurements from an Extended‐range Atmospheric Emitted Radiance Interferometer (E‐AERI) at the US Department of
B. Riot‐Bretêcher+3 more
wiley +1 more source
Reduced N2 fixation in the Atlantic Ocean during the Warm Late Pliocene
Yehudai M+12 more
europepmc +1 more source
A slab window in the south rim of the Parece-Vela Basin. [PDF]
Zhen Z, Dong X, Lintao Z.
europepmc +1 more source
Coastal Upwelling Gradient during the Late Pleistocene
David M. Anderson, Warren L Prell
openalex +1 more source
Timing of the Recent Migration and Intensification of the Southern Hemisphere Westerly Winds
Abstract In recent decades, the Southern Hemisphere westerly winds have strengthened and migrated south, attributed to greenhouse gas emissions and stratospheric ozone depletion. However, the onset and acceleration of these drivers is coincident with the start of the instrumental record, thus, hindering our ability to determine the significance of the ...
Dieter R. Tetzner+4 more
wiley +1 more source