Results 101 to 110 of about 50,383 (205)
Ocean heat uptake structure shapes future surface temperature change
Earth’s energy imbalance (EEI) is closely linked to global surface temperature changes over multidecadal timescales, yet this relationship weakens on shorter scales due to internal climate variability and ocean heat uptake.
Xuqian Li, Qingxiang Li
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Palaeoceanographic change during the Palaeocene/Eocene thermal maximum in Arctic Spitzbergen
The interaction of the ocean, atmosphere and ice in the Arctic region plays a critical role in modulating global climate. However, recent observations have illustrated the region is changing rapidly in response to anthropogenically-induced warming. Given
Charles, Adam J.
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In 2015, the Indian Ocean exhibits an exceptionally weakened CO2 uptake, highlighting strong interannual variability of ocean carbon sink. By utilizing multiple ocean CO2 partial pressure (pCO2) data and a state‐of‐the‐art ocean biogeochemical model, we ...
Enhui Liao +3 more
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Tropical ocean-atmosphere controls on inter-annual climate variability in the Cretaceous Arctic
The first annually resolved sedimentary record from the Cretaceous is used to develop time series of inter-annual and decadal scale climate variability from the Arctic Ocean.
Kemp, Alan E.S. +5 more
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Drivers of Future Indian Ocean Warming and Its Spatial Pattern in CMIP Models
Coupled Model Intercomparison Project phases 5 and 6 (CMIP5/6) projections display substantial inter‐model diversity in the future tropical Indian Ocean warming magnitude and spatial pattern.
S. Gopika +5 more
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On the community and ecosystem level consequences of warming
PhDThe carbon cycle modulates climate change, via the regulation of atmospheric CO2, and it represents one of the most important ecosystem services of value to humans.
Yvon-Durocher, Gabriel
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Site 1215 (26°01.77´N, 147°55.99´W, 5396 meters below sea level [mbsl]; Fig. F1) is the northernmost of seven sites drilled on the 56-Ma-crust transect during Ocean Drilling Program (ODP) Leg 199.
Lyle, M. +27 more
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Global warming and ocean acidification due to an increase in anthropogenic carbon dioxide can impact marine calcifying organisms. Shells of marine calcifying organisms protect their internal soft tissue and may be key in determining the susceptibility of
Emanuel, Martin Phillippe
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The impact of ocean acidification on the functional morphology of foraminifera
This work was supported by the NERC UK Ocean Acidification Research Programme grant NE/H017445/1. WENA acknowledges NERC support (NE/G018502/1). DMP received funding from the MASTS pooling initiative (The Marine Alliance for Science and Technology for ...
Austin, William E.N. +18 more
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Nitrogen Isotopes in the Global Ocean [PDF]
Nitrogen is an essential nutrient for life. Its low abundance throughout much of the sunlit surface ocean limits the growth of primary producers that form the base of ocean ecosystems.
Somes, Christopher J. +1 more
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