Sentences with phrase «for dynamic equilibrium»

In her quest for dynamic equilibrium, it was Riley's introduction of greyscale effect — the mid-point between black and white — that had the greatest impact on the development of her oeuvre.

Not exact matches

ACC Accounting & Auditing, AFR Africa, AGE Economics of Ageing, AGR Agricultural Economics, ARA Arab World, BAN Banking, BEC Business Economics, CBA Central Banking, CBE Cognitive & Behavioural Economics, CDM Collective Decision - Making, CFN Corporate Finance, CIS Confederation of Independent States, CMP Computational Economics, CNA China, COM Industrial Competition, CSE Economics of Strategic Management, CTA Contract Theory & Applications, CUL Cultural Economics, CWA Central & Western Asia, DCM Discrete Choice Models, DEM Demographic Economics, DEV Development, DGE Dynamic General Equilibrium, ECM Econometrics, EDU Education, EEC European Economics, EFF Efficiency & Productivity, ENE Energy Economics, ENT Entrepreneurship, ENV Environmental Economics, ETS Econometric Time Series, EUR Microeconomics European Issues, EVO Evolutionary Economics, EXP Experimental Economics, FDG Financial Development & Growth, FIN Finance, FMK Financial Markets, FOR Forecasting, GEO Economic Geography, GRO Economic Growth, GTH Game Theory, HAP Economics of Happiness, HEA Health Economics, HIS Business, Economic & Financial History, HME Heterodox Microeconomics, HPE History & Philosophy of Economics, HRM Human Capital & Human Resource Management, IAS Insurance Economics, ICT Information & Communication Technologies, IFN International Finance, IND Industrial Organization, INO Innovation, INT International Trade, IPR Intellectual Property Rights, IUE Informal & Underground Economics, KNM Knowledge Management & Knowledge Economy, LAB Labour Economics, LAM Central & South America, LAW Law & Economics, LMA Labor Markets - Supply, Demand & Wages, LTV Unemployment, Inequality & Poverty, MAC Macroeconomics, MFD Microfinance, MIC Microeconomics, MIG Economics of Human Migration, MKT Marketing, MON Monetary Economics, MST Market Microstructure, NET Network Economics, NEU Neuroeconomics, OPM Open Macroeconomics, ORE Operations Research, PBE Public Economics, PKE Post Keynesian Economics, POL Positive Political Economics, PPM Project, Program & Portfolio Management, PUB Public Finance, REG Regulation, RES Resource Economics, RMG Risk Management, SBM Small Business Management, SEA South East Asia, SOC Social Norms & Social Capital, SOG Sociology of Economics, SPO Sports & Economics, TID Technology & Industrial Dynamics, TRA Transition Economics, TRE Transport Economics, TUR Tourism Economics, UPT Utility Models & Prospect Theory, URE Urban & Real Estate Economics.

ACC Accounting & Auditing, AFR Africa, AGE Economics of Ageing, AGR Agricultural Economics, ARA Arab World, BAN Banking, BEC Business Economics, CBA Central Banking, CBE Cognitive & Behavioural Economics, CDM Collective Decision - Making, CFN Corporate Finance, CIS Confederation of Independent States, CMP Computational Economics, CNA China, COM Industrial Competition, CSE Economics of Strategic Management, CTA Contract Theory & Applications, CUL Cultural Economics, CWA Central & Western Asia, DCM Discrete Choice Models, DEM Demographic Economics, DEV Development, DGE Dynamic General Equilibrium, ECM Econometrics, EDU Education, EEC European Economics, EFF Efficiency & Productivity, ENE Energy Economics, ENT Entrepreneurship, ENV Environmental Economics, ETS Econometric Time Series, EUR Microeconomic European Issues, EVO Evolutionary Economics, EXP Experimental Economics, FDG Financial Development & Growth, FIN Finance, FMK Financial Markets, FOR Forecasting, GEO Economic Geography, GRO Economic Growth, GTH Game Theory, HAP Economics of Happiness, HEA Health Economics, HIS Business, Economic & Financial History, HME Heterodox Microeconomics, HPE History & Philosophy of Economics, HRM Human Capital & Human Resource Management, IAS Insurance Economics, ICT Information & Communication Technologies, IFN International Finance, IND Industrial Organization, INO Innovation, INT International Trade, IPR Intellectual Property Rights, IUE Informal & Underground Economics, KNM Knowledge Management & Knowledge Economy, LAB Labour Economics, LAM Central & South America, LAW Law & Economics, LMA Labor Markets - Supply, Demand & Wages, LTV Unemployment, Inequality & Poverty, MAC Macroeconomics, MFD Microfinance, MIC Microeconomics, MIG Economics of Human Migration, MKT Marketing, MON Monetary Economics, MST Market Microstructure, NET Network Economics, NEU Neuroeconomics, OPM Open Macroeconomics, PBE Public Economics, PKE Post Keynesian Economics, POL Positive Political Economics, PPM Project, Program & Portfolio Management, PUB Public Finance, REG Regulation, RES Resource Economics, RMG Risk Management, SBM Small Business Management, SEA South East Asia, SOC Social Norms & Social Capital, SOG Sociology of Economics, SPO Sports & Economics, TID Technology & Industrial Dynamics, TRA Transition Economics, TRE Transport Economics, TUR Tourism Economics, UPT Utility Models & Prospect Theory, URE Urban & Real Estate Economics.

Atoms and molecules, for example, are energy systems exhibiting more or less dynamic equilibrium.

And I'd venture to say that a tropical forest — any forest for that matter — is never at a «resting equilibrium» but is always dynamic, and always «productive»!

Koehler and Mishra (2008) argued that for effective technology integration all three knowledge elements (content, pedagogy, and technology) should exist in a dynamic equilibrium.

Mondrian has here moved on from Malevich's foundational square, yet his search for «dynamic equilibrium» similarly recognises the human hunger for the absolute and immutable, created by the relativity and mutability in things.

Set in context it is immediately clear what they mean with «decades to respond», the time it takes for the system to arrive at a new dynamic equilibrium, a lag caused by the thermal inertia mainly from the oceans.

# 192 «For example a strengthening of wind over some oceanic region http://web.science.unsw.edu.au/~matthew/nclimate2106-incl-SI.pdf then would increase the heat flow atmosphere - > ocean, leading to lower (dynamic) equilibrium temperature in the atmosphere which of course occurs very fast, as the thermal mass of the atmosphere is very low compared to the net energy throughput.»

First, the requirement is for thermodynamic equilibrium, not dynamic equilibrium.

We have a novel perturbation across the globe and each chaotic climate system on the globe; it is bigger and more persistent, and in nearly every measure a perturbation can generally be defined as more likely to upset a dynamic equilibrium or shift or radicalize attractors is larger than any perturbation for the past half million years.

Ah, bobdroege reappears, after being repeatedly shot down on the recent thread with his ludicrous «theory» that a static, closed, laboratory gas cylinder in equilibrium is somehow analogous to the dynamic, open, not - in - vertical - equilibrium 100 km atmosphere in a gravity - field, and his false claim that NASA used «circular reasoning» in deriving the «NASA Fact Sheet» physical values for Venus.

I spent 15 years working daily with dynamic and passive equilibriums, also designing various systems to alter the residual state of equilibriums for clients.

There is no such thing, in other words, as «gravitational heating» for a system in static equilibrium, nor is there any such thing as «gravitational heating» for a system in dynamic equilibrium.

If you want to prove that there is a non-GHG GE involving the dynamic motion of gases, play right on through, but realize that Jelbring's paper isn't about that and is incorrect because it ascribes the same effect to a completely static, completely dry ideal gas that has been left in place, isolated, for a billion years (or as long as equilibrium takes, which won't be anywhere near a billion years at a joule of conductive transport per meter of atmosphere per degree kelvin of temperature difference per 40 seconds).

QUOTE: «As shown on figure 17 - D the regions for absorption and out - gassing are separate; there is no «global» equilibrium between the atmosphere and the ocean; carbon absorbed tens of years ago at high latitudes is resurfacing in up - wellings; carbon absorbed by plants months to centuries ago is degassed by soils Sorry, there is a fundamental lack of knowledge of dynamic systems here: as long as the total of the CO2 influxes is the same as the total of the CO2 outfluxes, nothing happens in the atmosphere.

That is the «steady state» or dynamic equilibrium for the ocean — atmosphere system.

The above also is true for the opposite effect: if there were no other fast releases (like lots of volcanoes spewing lots of CO2 in short time), the ocean temperature will give more or less CO2, until a new dynamic equilibrium between ocean releases (mainly near the tropics) and sinks (mainly near the poles) and the biosphere releases and sinks is reached.

Which implies that the CO2 cycle was a simple dynamic equilibrium process in pre-industrial times... No problem at all for science.

The calculations by Kuang 2010 in which a dynamic model of radiative - convective equilibrium is perturbed systematically with different heat (and moisture) sources suggests that this is the path of least resistance for a convecting atmosphere, but that there are other possibilities as well — I need to understand this paper better.