Long wave dynamics for a liquid CO2 lake in the deep ocean

2019 ◽  
Vol 141 ◽  
pp. 144-157
Author(s):  
Krister J. Trandal ◽  
Henrik Kalisch
Keyword(s):  
Deep Ocean ◽  
Wave Dynamics ◽  
Long Wave ◽  
Liquid Co2

scholarly journals Physical modeling of resonance phenomena in the long wave dynamics

2016 ◽  
pp. 57-64 ◽  
Author(s):  
Nizar Abcha ◽  
Alexander Ezersky ◽  
Efim Pelinovsky
Keyword(s):  
Physical Modeling ◽  
Wave Dynamics ◽  
Long Wave ◽  
Resonance Phenomena

scholarly journals Long-Wave Dynamics of Sea Level Variations during Indian Ocean Dipole Events

2009 ◽  
Vol 39 (5) ◽  
pp. 1115-1132 ◽  
Author(s):  
Dongliang Yuan ◽  
Hailong Liu
Keyword(s):  
Indian Ocean ◽  
Sea Level ◽  
Indian Ocean Dipole ◽  
Rossby Waves ◽  
Western Boundary ◽  
Kelvin Wave ◽  
Wave Pulse ◽  
Wave Dynamics ◽  
Long Wave ◽  
Equatorial Rossby Waves

Abstract Long-wave dynamics of the interannual variations of the equatorial Indian Ocean circulation are studied using an ocean general circulation model forced by the assimilated surface winds and heat flux of the European Centre for Medium-Range Weather Forecasts. The simulation has reproduced the sea level anomalies of the Ocean Topography Experiment (TOPEX)/Poseidon altimeter observations well. The equatorial Kelvin and Rossby waves decomposed from the model simulation show that western boundary reflections provide important negative feedbacks to the evolution of the upwelling currents off the Java coast during Indian Ocean dipole (IOD) events. Two downwelling Kelvin wave pulses are generated at the western boundary during IOD events: the first is reflected from the equatorial Rossby waves and the second from the off-equatorial Rossby waves in the southern Indian Ocean. The upwelling in the eastern basin during the 1997–98 IOD event is weakened by the first Kelvin wave pulse and terminated by the second. In comparison, the upwelling during the 1994 IOD event is terminated by the first Kelvin wave pulse because the southeasterly winds off the Java coast are weak at the end of 1994. The atmospheric intraseasonal forcing, which plays an important role in inducing Java upwelling during the early stage of an IOD event, is found to play a minor role in terminating the upwelling off the Java coast because the intraseasonal winds are either weak or absent during the IOD mature phase. The equatorial wave analyses suggest that the upwelling off the Java coast during IOD events is terminated primarily by western boundary reflections.

Open boundary conditions for horizontal 2-D curvilinear-grid long-wave dynamics of a strait

1995 ◽  
Vol 18 (5) ◽  
pp. 267-276 ◽  
Author(s):  
A.A. Androsov ◽  
K.A. Klevanny ◽  
E.S. Salusti ◽  
N.E. Voltzinger
Keyword(s):  
Boundary Conditions ◽  
Open Boundary ◽  
Open Boundary Conditions ◽  
Wave Dynamics ◽  
Long Wave ◽  
Curvilinear Grid

scholarly journals Review of Long Wave Dynamics over Reefs and into Ports with Implication for Port Operations

2016 ◽  
Vol 4 (1) ◽  
pp. 12 ◽  
Author(s):  
Ap van Dongeren ◽  
Martijn de Jong ◽  
Cock van der Lem ◽  
Alex van Deyzen ◽  
Joost den Bieman
Keyword(s):  
Wave Dynamics ◽  
Port Operations ◽  
Long Wave

scholarly journals Dissolution from a liquid CO2 lake disposed in the deep ocean

2003 ◽  
Vol 48 (2) ◽  
pp. 872-883 ◽  
Author(s):  
Ilker Fer ◽  
Peter M. Haugan
Keyword(s):  
Deep Ocean ◽  
Liquid Co2

Direct disposal of liquified fossil fuel carbon dioxide in the ocean

1999 ◽  
Author(s):  
Keith A. Hunter
Keyword(s):  
Fossil Fuel ◽  
Control Strategies ◽  
Scientific Evidence ◽  
Deep Ocean ◽  
Global Carbon Cycle ◽  
Global Engineering ◽  
Liquid Co2 ◽  
Wide Debate ◽  
Global Carbon ◽  
Co2 Addition

Growing awareness of the impending effects on climate of increasing levels of CO2 in the atmosphere has generated wide debate at an international level that is directed towards a variety of CO2 control strategies. Of these, direct disposal of liquid CO2 into the deep ocean offers a number of potential advantages: the oceanic reservoir is very large, and has the ability to buffer chemical changes caused by CO2 addition. In addition, time scales of mixing in the ocean are very long. This paper reviews some of the scientific evidence associated with this emerging form of global engineering, and discusses some of the important concepts in terms of the global carbon cycle.

scholarly journals LONG-WAVE DYNAMICS IN THE CONTEXT OF THE DEVELOPMENT OF INSTITUTIONAL ECONOMIC THEORY

2020 ◽  
pp. 120-125
Author(s):  
B. A. Yerznkyan
Keyword(s):  
World Wide ◽  
Institutional Economics ◽  
Executive Power ◽  
Economic Systems ◽  
Wave Dynamics ◽  
Institutional Economic ◽  
Long Wave ◽  
The Subject ◽  
The Impact ◽  
Selection Of

The subject of the study is the long-wave dynamics due to the impact of scientific and technological progress and examined from the standpoint of institutional economics. The goal of the paper is identification of the features of the long-wave dynamics phases from the standpoint of technological, institutional and world-wide structures. Analytical and logical methods of institutional analysis have been used. The need of correcting the long-wave dynamics notions, caused as by objective changes of economic development as well as by the evolving nature of institutional theory has been identified. The results can be used by executive power authorities relating to strategic management of the development and connecting with the design of social and economic institutions that support self-organization and sustainable functioning of ecosystems. It has been proved that the development of economic systems depends on the relevant selection of technological, institutional and world-wide economic structures and ways of managing them. It has been shown that intra-firm transactions are based on the implicit ternary contracts, market with the mediators on the explicit ternary contracts, market without mediators on the explicit binary contracts, and the network transactions in ecosystems are based on the implicit binary contracts.

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