[PDF] Top 20 Global ocean salinity : a climate change diagnostic?
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Global ocean salinity : a climate change diagnostic?
... the global oceans mass ...upper ocean (0-200m), and following the calculation presented in ...regional salinity change of ...considering ocean circulation timescales much greater than ... See full document
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Climate change: what is happening in the ocean?
... Atlantic Ocean surface layer circulation is part of a global ocean circulation which is primarily wind driven, but it also forms the upper branch of a global ocean thermohaline ...a ... See full document
29
Climate Change and China as a Global Emerging Regulatory Sea Power in the Arctic Ocean: Is China a Threat for Arctic Ocean Security?
... of climate change, in particular the risk of adaptation since possible assertive behaviors in term of conflict could not only galvanize one approach or the other 12 and increase insecurity but also delay ... See full document
9
Modeling geologically abrupt climate changes in the Miocene: Potential effects of high latitudinal salinity changes
... The middle Miocene experiment (Exp. m14-3) shows that surface salinizing in this run does indeed cause deep-ocean temperatures to cool by approximately 1 to 1.5˚C (Figures 4(e) and (f)). Counter-intuitively, the ... See full document
10
Global Climate Change
... Earth’s climate changes ...of climate change include variations in ocean currents (which can alter the distribution of heat and precipitation) and large eruptions of volcanoes (which can ... See full document
9
Climate change impedes scleractinian corals as primary reef ecosystem engineers
... to global climate change. Ocean warming can cause extensive mass coral bleaching, which triggers dysfunction of major engineering ...with ocean acidification, further lead to long-term ... See full document
11
Did COVID-19 lockdown brew “Amphan” into a super cyclone?
... oceans. Climate change and associated global warming have enabled significant accumulation of ocean heat content (OHC) across the globe increasing the frequency of intense tropical ... See full document
5
Characteristics of the seasonal cycle of surface layer salinity in the global ocean
... whereas ocean circula- tion processes can have time scales of years to ...and climate is the seasonal, where intra-year changes in solar input cause changes in such fea- tures as the position of the ... See full document
15
The impact of desalination and climate change on salinity in the Arabian Gulf
... of climate change on Gulf-averaged ...of climate change and desalination capacity increase on salinities at a local scale is of a higher order (>1 PSU) than projected salt accumulation Gulf ... See full document
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Climate Change and the Great Plague Pandemics of History: Causal Link between Global Climate Fluctuations and Yersinia Pestis Contagion?
... of ocean currents and the atmospheric wind patterns. Both the global conveyer of ocean currents and the circulating atmospheric winds are responsible for bringing heat and moisture to the higher ... See full document
42
The “Ocean Stabilization Machine” May Represent a Primary Factor Underlying the Effect of “Global Warming on Climate Change”
... Figure 4 illustrates the geographic distribution of the correlation coefficients between the GLST monthly anomalies and SST anomalies at all grid-points worldwide. We can see that the monthly anomaly of SST in six ... See full document
11
Report of the CLIVAR/OOPC/IAI Workshop on the South Atlantic Climate Observing System (SACOS), February 6 8, 2003, Hotel Portogalo, Angra dos Reis Brazil
... to climate variability studies for several ...could change the shape and heat content of the southern subtropical ...measure climate change over longer time periods. In the Pacific ... See full document
123
Formulation of an ocean model for global climate simulations
... the climate model simulation, and in particular what time scales are ...resting ocean) to dry 27 ...mean salinity av- eraged over 800–1200 m became quite salty (roughly ...World Ocean Atlas of ... See full document
35
The Road to Copenhagen 2009 - The European Union and Climate Change Action. EU Centre, Singapore Background Brief No. 1, 10 November 2009
... within the Union. According to the package, the EU is now committed to cutting overall greenhouse gas emissions to at least 20% below 1990 levels by 2020, a commitment that will rise to 30% if other industrialised ... See full document
20
The timescale and extent of thermal expansion of the global ocean due to climate change
... The steady upward drift in the Munk model is balanced by the downwelling flows, which may have varied in heat con- tent during the analysis period. The abyssal heat budget is dominated by flows at the boundaries rather ... See full document
6
Effects of the World’s Oceans on Global Climate Change
... of change in clarity is change of organic matter ...of climate the main effect of plankton and accompanying organic matter is to shade subsurface waters from solar energy ...deep ocean ... See full document
8
Ocean temperature and salinity responses to 50 year changes in surface conditions
... the global ocean’s temperature and salinity in the last decades are evidence of the Earth’s warming ...interior ocean changes are driven by changes in ocean surface fluxes of heat, freshwater ... See full document
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How well can we derive Global Ocean Indicators from Argo data?
... the ocean salinity field due to the large-scale balance between the surface freshwater flux (evaporation minus precipitation and continental run- off), salinity variations and the ocean’s advective ... See full document
9
IMPACTS OF GLOBAL CLIMATE CHANGE ON INDONESIA OCEAN ENVIRONMENT.
... of global climate change to Indonesian ocean ...of climate change to sea level, significant wave height and sea water ...to climate change. Increasing trend of sea ... See full document
7
Ocean circulation drifts in multi-millennial climate simulations: the role of salinity corrections and climate feedbacks
... The MOC responses are not limited to changes in strength; there are also structural changes (Figs. 3, 4). In the Atlantic basin, NADW initially extends across all latitudes to depths of 3 km, with maximum strengths of ≈ ... See full document
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