scholarly journals Оn the role of eddies in the global ocean meridional heat transport

2019 ◽  
Vol 486 (2) ◽  
pp. 243-246
Author(s):  
K. V. Ushakov ◽  
R. A. Ibrayev
Keyword(s):  
Model Calculation ◽  
Heat Transport ◽  
World Ocean ◽  
Explicit Description ◽  
Global Ocean ◽  
Meridional Heat Transport ◽  
The World ◽  
Correct Reproduction ◽  
Eddy Dynamics

By means of an eddy-resolving model, calculation of the eddy meridional heat transport (EMHT) in the World Ocean has been performed. Its distribution is associated with intense currents and forms several characteristic types of structures. Comparison with results of other models shows that for the correct reproduction of EMHT, an explicit description of the eddy dynamics is preferable.

Part V Regional Perspectives on Global Ocean Governance, 16 The Role of the World Ocean Council and the Ocean Business Community in Global Ocean Governance

2018 ◽  
Author(s):  
Holthus Paul
Keyword(s):  
Sustainable Development Goals ◽  
World Ocean ◽  
Institutional Development ◽  
Business Community ◽  
Global Ocean ◽  
The Sustainable Development ◽  
Ocean Governance ◽  
The World ◽  
Development Goals

This chapter discusses the role of the World Ocean Council (WOC) and the international ocean business community in global ocean governance (GOG). It first provides an overview of the institutional development and profile of the WOC before considering the work and role and work of the WOC on ocean governance with and for the ocean business community. It then examines the Sustainable Development Goals (SDGs) in relation to ocean business and the WOC, as well as the size, complexity trends in the ocean economy and ocean business community, which are fundamental to understanding their importance to GOG. It also analyses GOG issues relevant to the ocean business community and WOC that the United Nations and its associated bodies must address and concludes with an assessment of the role of the ocean business community and WOC in the future of the GOG agenda.

scholarly journals Air-to-sea flux of soluble iron: is it driven more by HNO<sub>3</sub> or SO<sub>2</sub>? – an examination in the light of dust aging

2007 ◽  
Vol 7 (4) ◽  
pp. 10043-10063 ◽  
Author(s):  
H. Yang ◽  
Y. Gao
Keyword(s):  
Atmospheric Chemistry ◽  
Transport Model ◽  
World Ocean ◽  
Global Ocean ◽  
Relative Role ◽  
Chemistry Transport Model ◽  
Acidic Gases ◽  
Relative Contribution ◽  
The World

Abstract. Aeolian dust provides the major micronutrient of soluble Fe to organisms in certain regions of the global ocean. In this study, we conduct numerical experiments using the MOZART-2 atmospheric chemistry transport model to simulate the global distribution of soluble Fe flux and Fe solubility. One of the mechanisms behind the hypothesis of acid mobilization of Fe in the atmosphere is that the coating of acidic gases changes dust from hydrophobic to hydrophilic, a prerequisite of Fe mobilization. We therefore include HNO3, SO2 and sulfate (SO42−) as dust transformation agents in the model. General agreement in Fe solubility within a factor of 2 is achieved between model and observations. The total flux of soluble Fe to the world ocean is estimated to be 731–924×109 g yr−1, and the average Fe solubility is 6.4–8.0%. Wet deposition contributes over 80% to total soluble Fe flux to most of the world oceans. Special attention is paid to the relative role of HNO3 versus SO2 and sulfate. We demonstrate that coating by HNO3 produces over 36% of soluble Fe fluxes compared to that by SO2 and sulfate combined in every major oceanic basin. Given present trends in the emissions of NOx and SO2, the relative contribution of HNO3 to Fe mobilization may get even larger in the future.

scholarly journals The regulatory role of GABAA receptor in Actinia equina nervous system and the possible effect of global ocean acidification

2021 ◽  
Author(s):  
Sergii Snigirov ◽  
Sergiy Sylantyev
Keyword(s):  
Ocean Acidification ◽  
Startle Response ◽  
World Ocean ◽  
Global Ocean ◽  
Cell Excitability ◽  
Time Modulation ◽  
The World ◽  
Behavioural Reaction ◽  
First Time

AbstractGlobal warming and connected acidification of the world ocean attract a substantial amount of research efforts, in particular in a context of their impact on behaviour and metabolism of marine organisms, such as Cnidaria. Nevertheless, mechanisms underlying Cnidarians’ neural signalling and behaviour and their (possible) alterations due to the world ocean acidification remain poorly understood. Here we researched for the first time modulation of GABAA receptors (GABAARs) in Actinia equina (Cnidaria: Anthozoa) by pH fluctuations within a range predicted by the world ocean acidification scenarios for the next 80–100 years and by selective pharmacological activation. We found that in line with earlier studies on vertebrates, both changes of pH and activation of GABAARs with a selective allosteric agonist (diazepam) modulate electrical charge transfer through GABAAR and the whole-cell excitability. On top of that, diazepam modifies the animal behavioural reaction on startle response. However, despite behavioural reactions displayed by living animals are controlled by GABAARs, changes of pH do not alter them significantly. Possible mechanisms underlying the species resistance to acidification impact are discussed.

ON EVALUATION OF THE ROLE OF THERMAL AND WIND FACTORS FOR A PHYSICAL MODEL OF THE WORLD OCEAN GENERAL CIRCULATION SYSTEM

2019 ◽  
Vol 47 (3) ◽  
pp. 80-91
Author(s):  
V. G. Neiman
Keyword(s):  
Physical Model ◽  
Ocean Circulation ◽  
General Circulation ◽  
World Ocean ◽  
Circulation System ◽  
The Public ◽  
The World ◽  
Almost All ◽  
Conceptual Foundations

The main content of the work consists of certain systematization and addition of longexisting, but eventually deformed and partly lost qualitative ideas about the role of thermal and wind factors that determine the physical mechanism of the World Ocean’s General Circulation System (OGCS). It is noted that the conceptual foundations of the theory of the OGCS in one form or another are contained in the works of many well-known hydrophysicists of the last century, but the aggregate, logically coherent description of the key factors determining the physical model of the OGCS in the public literature is not so easy to find. An attempt is made to clarify and concretize some general ideas about the two key blocks that form the basis of an adequate physical model of the system of oceanic water masses motion in a climatic scale. Attention is drawn to the fact that when analyzing the OGCS it is necessary to take into account not only immediate but also indirect effects of thermal and wind factors on the ocean surface. In conclusion, it is noted that, in the end, by the uneven flow of heat to the surface of the ocean can be explained the nature of both external and almost all internal factors, in one way or another contributing to the excitation of the general, or climatic, ocean circulation.

Trends in phytoplankton communities within large marine ecosystems diverge from the global ocean

2021 ◽  
pp. 1-12
Author(s):  
Kevin D. Friedland ◽  
John R. Moisan ◽  
Aurore A. Maureaud ◽  
Damian C. Brady ◽  
Andrew J. Davies ◽  
...  
Keyword(s):  
Chlorophyll Concentration ◽  
World Ocean ◽  
Marine Ecosystems ◽  
Fishing Effort ◽  
Global Ocean ◽  
Human Populations ◽  
Anthropogenic Pressures ◽  
Large Marine Ecosystems ◽  
Phytoplankton Communities ◽  
The World

Large marine ecosystems (LMEs) are highly productive regions of the world ocean under anthropogenic pressures; we analyzed trends in sea surface temperature (SST), cloud fraction (CF), and chlorophyll concentration (CHL) over the period 1998–2019. Trends in these parameters within LMEs diverged from the world ocean. SST and CF inside LMEs increased at greater rates inside LMEs, whereas CHL decreased at a greater rates. CHL declined in 86% of all LMEs and of those trends, 70% were statistically significant. Complementary analyses suggest phytoplankton functional types within LMEs have also diverged from those characteristic of the world ocean, most notably, the contribution of diatoms and dinoflagellates, which have declined within LMEs. LMEs appear to be warming rapidly and receiving less solar radiation than the world ocean, which may be contributing to changes at the base of the food chain. Despite increased fishing effort, fishery yields in LMEs have not increased, pointing to limitations related to productivity. These changes raise concerns over the stability of these ecosystems and their continued ability to support services to human populations.

scholarly journals Oceanic Overturning and Heat Transport: The Role of Background Diffusivity

2019 ◽  
Vol 32 (3) ◽  
pp. 701-716 ◽  
Author(s):  
Magnus Hieronymus ◽  
Jonas Nycander ◽  
Johan Nilsson ◽  
Kristofer Döös ◽  
Robert Hallberg
Keyword(s):  
Heat Transport ◽  
Large Scale ◽  
Energy Transport ◽  
Climate Model ◽  
Potential Temperature ◽  
Meridional Heat Transport ◽  
Sea Ice Extent ◽  
Antarctic Sea Ice ◽  
Meridional Overturning

The role of oceanic background diapycnal diffusion for the equilibrium climate state is investigated in the global coupled climate model CM2G. Special emphasis is put on the oceanic meridional overturning and heat transport. Six runs with the model, differing only by their value of the background diffusivity, are run to steady state and the statistically steady integrations are compared. The diffusivity changes have large-scale impacts on many aspects of the climate system. Two examples are the volume-mean potential temperature, which increases by 3.6°C between the least and most diffusive runs, and the Antarctic sea ice extent, which decreases rapidly as the diffusivity increases. The overturning scaling with diffusivity is found to agree rather well with classical theoretical results for the upper but not for the lower cell. An alternative empirical scaling with the mixing energy is found to give good results for both cells. The oceanic meridional heat transport increases strongly with the diffusivity, an increase that can only partly be explained by increases in the meridional overturning. The increasing poleward oceanic heat transport is accompanied by a decrease in its atmospheric counterpart, which keeps the increase in the planetary energy transport small compared to that in the ocean.

The Time-varying Characteristics of the Meridional Ekman Heat Transport for the World Ocean

1993 ◽  
Vol 23 (12) ◽  
pp. 2704-2716 ◽  
Author(s):  
David Adamec ◽  
Michele M. Rienecker ◽  
Jeffrey M. Yukovich
Keyword(s):  
Heat Transport ◽  
World Ocean ◽  
Time Varying ◽  
The World

scholarly journals ON THE ROLE AND TASKS OF DOMESTIC FISHERY SCIENCE IN OCEANIC FISHERIES DEVELOPMENT

Fisheries ◽  
2020 ◽  
Vol 2020 (2) ◽  
pp. 18-23 ◽  
Author(s):  
Vladimir Sauskan ◽  
Viktor Osadchii ◽  
Aleksandr Arkhipov
Keyword(s):  
Sustainable Development ◽  
World Ocean ◽  
International Level ◽  
Russian Science ◽  
Bilateral Agreements ◽  
Fishery Science ◽  
The World ◽  
International Regulations

A role of Russian science is increasing along with domestic fisheries development in the world Ocean. One of the main tasks of researchers is to protect the interests of Russian fisheries on the international level. Such protection is based on living resources investigation and formulation of recommendations on their sustainable development, taking into account the international regulations’ and bilateral agreements’ demands.

The Role of Salinity in the Global Distribution of Surface Density Fluxes in the World Ocean Based on the Example of 2014

Oceanology ◽  
2021 ◽  
Vol 61 (4) ◽  
pp. 450-458
Author(s):  
V. M. Kukushkin ◽  
M. Yu. Markina ◽  
S. K. Gulev ◽  
S. A. Dobrolyubov
Keyword(s):  
Surface Density ◽  
World Ocean ◽  
Global Distribution ◽  
The World

scholarly journals Optimal Surface Salinity Perturbations of the Meridional Overturning and Heat Transport in a Global Ocean General Circulation Model

2008 ◽  
Vol 38 (12) ◽  
pp. 2739-2754 ◽  
Author(s):  
Florian Sévellec ◽  
Thierry Huck ◽  
Mahdi Ben Jelloul ◽  
Nicolas Grima ◽  
Jérôme Vialard ◽  
...  
Keyword(s):  
Heat Transport ◽  
General Circulation ◽  
Meridional Overturning Circulation ◽  
Global Ocean ◽  
Transient Growth ◽  
Surface Salinity ◽  
Meridional Heat Transport ◽  
Overturning Circulation ◽  
Optimal Surface ◽  
Meridional Overturning

Abstract Recent observations and modeling studies have stressed the influence of surface salinity perturbations on the North Atlantic circulation over the past few decades. As a step toward the estimation of the sensitivity of the thermohaline circulation to salinity anomalies, optimal initial surface salinity perturbations are computed and described for a realistic mean state of a global ocean general circulation model [Océan Parallélisé (OPA)]; optimality is defined successively with respect to the meridional overturning circulation intensity and the meridional heat transport maximum. Although the system is asymptotically stable, the nonnormality of the dynamics is able to produce a transient growth through an initial stimulation. Optimal perturbations are calculated subject to three constraints: the perturbation applies to surface salinity; the perturbation conserves the global salt content; and the perturbation is normalized, to remove the degeneracy in the linear maximization problem. Maximization using Lagrangian multipliers leads to explicit solutions (rather than eigenvalue problems), involving the integration of the model adjoint for each value to maximize. The most efficient transient growth for the intensity of the meridional overturning circulation appears for a delay of 10.5 yr after the perturbation by the optimal surface salinity anomaly. This optimal growth is induced by an initial anomaly located north of 50°N. In the same way, the most efficient transient growth for the intensity of the meridional heat transport appears for a shorter delay of 2.2 yr after the perturbation by the optimal surface salinity anomaly. This initial optimal perturbation corresponds to a zonal salinity gradient around 24°N. The optimal surface salinity perturbations studied herein yield upper bounds on the intensity of the response in meridional overturning circulation and meridional heat transport. Using typical amplitudes of the Great Salinity Anomalies, the upper bounds for the associated variability are 0.8 Sv (1 Sv ≡ 106 m3 s−1) (11% of the mean circulation) and 0.03 PW (5% of the mean circulation), respectively.

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