Results 211 to 220 of about 13,090 (264)

Contrasting evolution of the Arabian Sea and Pacific Ocean oxygen minimum zones during the Miocene. [PDF]

Commun Earth Environ
Hess AV, Auderset A, Rosenthal Y, Sigman DM, Martínez-García A.   +4 more
europepmc   +1 more source

Connections and causes of inter-model spread in boreal summer precipitation across monsoon regions in AMIP6 simulations. [PDF]

Sci Rep
Wen N, Huan K.
europepmc   +1 more source

The Global Deep Sea Exploration Goals: A representative approach to visually observing the deep seafloor. [PDF]

Sci Adv
Johannes KN, Poulton SE, Kennedy BRC, Bell KLC.   +3 more
europepmc   +1 more source

Poster Sessions

HemaSphere, Volume 10, Issue S1, June 2026.
wiley   +1 more source

Publication Only

HemaSphere, Volume 10, Issue S1, June 2026.
wiley   +1 more source

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A dipole mode in the tropical Indian Ocean

Nature, 1999
For the tropical Pacific and Atlantic oceans, internal modes of variability that lead to climatic oscillations have been recognized, but in the Indian Ocean region a similar ocean-atmosphere interaction causing interannual climate variability has not yet been found.
Saji, NH, Goswami, BN, Vinayachandran, PN, Yamagata, T   +3 more
openaire   +2 more sources

Bioluminescence of the tropical Indian Ocean: a multiple‐scale variation

Luminescence, 2022
AbstractLarge‐scale surveys represented by 5800 bathymetric casts in the western Indian Ocean (0–22oN, 54–58oE), elucidated the 10‐fold variation of the bioluminescent potential (BP) in the upper mixed layer, during the winter (north‐east) monsoon season. The mesoscale survey in February 2017 consisted of 26 drift stations (4oN–3oS, 65–68oE) on which 5–
Sergey A. Piontkovski, Alexandr V. Melnik, Irina M. Serikova, Vladislav P. Evstigneev, Sergey Dobretsov   +4 more
openaire   +2 more sources

Coupled Ocean-Atmosphere Variability in the Tropical Indian Ocean

2013
The Indian Ocean Dipole (IOD) is a natural ocean-atmosphere coupled mode that plays important roles in seasonal and interannual climate variations. The coupled mode locked to boreal summer and fall is distinguished as a dipole in the SST anomalies that are coupled to zonal winds.
Yamagata, Toshio, K. Behera, Swadhin, Luo, Jing-Jia, Masson, Sébastien, R. Jury, Mark, A. Rao, Suryachandra   +5 more
openaire   +2 more sources

Intraseasonal oscillation in the tropical Indian Ocean

Advances in Atmospheric Sciences, 2005
The features of the intraseasonal oscillation (ISO) of the tropical Indian Ocean are studied using several sources of observational data. It is shown that there are intraseasonal oscillations in the tropical Indian Ocean, but their periods vary with latitude: the major period is about 20–30 days in the equatorial region, about 30–50 days at 10°N/10°S ...
Li Chongyin, Hu Ruijin, Yang Hui
openaire   +1 more source