Results 21 to 30 of about 50,383 (205)

Is the Arctic Ocean warming? [PDF]

open access: yesJournal of Geophysical Research: Oceans, 1998
Recent high‐quality hydrographic measurements in the Arctic Ocean have revealed a warming of up to 1 K of the Atlantic Layer when compared with Russian climatologies of the 1940s to 1970s. About half of this warming can be attributed to the different methods by which the two data sets were obtained: the climatologies are based on discrete bottle data ...
Quadfasel, Detlef Rudolf   +3 more
openaire   +3 more sources

Change of Global Ocean Temperature and Decadal Variability under 1.5 °C Warming in FOAM

open access: yesJournal of Marine Science and Engineering, 2022
The rise in atmospheric CO2 concentration is regarded as the dominant reason for observed warming since the mid-20th century. Based on the Paris Agreement target, this research designs three conceptual pathways to achieve the warming target of 1.5 °C ...
Sheng Wu   +3 more
doaj   +1 more source

Isolating the signal of ocean global warming [PDF]

open access: yes, 2007
Identifying the signature of global warming in the world's oceans is challenging because low frequency circulation changes can dominate local temperature changes.
Tett, S.   +7 more
core   +1 more source

Climate model and proxy data constraints on ocean warming across the Paleocene-Eocene Thermal Maximum [PDF]

open access: yes, 2013
Constraining the greenhouse gas forcing, climatic warming and estimates of climate sensitivity across ancient large transient warming events is a major challenge to the palaeoclimate research community.
Lunt, Daniel J.   +16 more
core   +1 more source

Pantropical Response to Global Warming and the Emergence of a La Niña‐Like Mean State Trend

open access: yesGeophysical Research Letters, 2020
A recent study by Zhang et al. (2019, https://doi.org/10.1029/2019GL084088) proposes “an interbasin ocean thermostat mechanism” to support the hypothesis that enhanced Indian Ocean warming during the past century has reduced the Pacific warming response ...
Sang‐Ki Lee   +3 more
doaj   +1 more source

Recent acceleration in global ocean heat accumulation by mode and intermediate waters

open access: yesNature Communications, 2023
The ocean absorbs >90% of anthropogenic heat in the Earth system, moderating global atmospheric warming. However, it remains unclear how this heat uptake is distributed by basin and across water masses.
Zhi Li   +2 more
doaj   +1 more source

Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary? [PDF]

open access: yes, 2002
During the Paleocene-Eocene Thermal Maximum (PETM, ~55 Ma), marine and terrestrial carbon isotope values exhibit a negative shift of at least 2.5‰, indicative of massive destabilization of marine methane hydrates, releasing ~1100 gigatonnes of methane ...
Marotzke, J. ; https://orcid.org/   +3 more
core   +1 more source

Indian Ocean Warming [PDF]

open access: yes, 2020
AbstractSea surface temperature (SST) and upper ocean heat content (OHC, upper 700 m) in the tropical Indian Ocean underwent rapid warming during 1950–2015, with the SSTs showing an average warming of about 1 °C. The SST and OHC trends are very likely to continue in the future, under different emission scenarios.
M. K. Roxy   +10 more
openaire   +1 more source

Ocean acidification and warming in the Norwegian and Barents Seas: impacts on marine ecosystems and human uses [PDF]

open access: yes, 2014
This report synthesizes the results from interviews and a workshop with stakeholders in Norway about the impacts of climate change and ocean acidification on marine ecosystems and ecosystem ...
Koenigstein, Stefan   +3 more
core   +1 more source

Biomass changes and trophic amplification of plankton in a warmer ocean [PDF]

open access: yes, 2014
Ocean warming can modify the ecophysiology and distribution of marine organisms, and relationships between species, with nonlinear interactions between ecosystem components potentially resulting in trophic amplification.
Icarus Allen, J.   +134 more
core   +1 more source

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