Sentences with phrase «in full equilibrium»

In full equilibrium, at any given level, there may be some net radiative heating at some frequencies compensated by some net radiative cooling at other frequencies, with convection balancing the full spectrum radiative cooling of the troposphere and heating of the surface.

In full equilibrium, I expect that the additional cash flows from corporate tax cuts will, directly or indirectly, be used to buy fresh Treasury debt.

Not exact matches

This required a model with a full representation of all the forces involved in ice flow applied specifically to PIG: «A more detailed understanding of PIG's departure from equilibrium flow will require an understanding of its particular stream mechanics» (Shepherd et al., 2001).

Hi Will, another amazing text like you, I believe too that healt (and hair) is do inside out Your program make sense to me, I avoid pharmacy drugs and have full respect for ancient cultures (and some contemporary, here in Brazil) that healing the body with nature I will purchase your program, and be the livin prove that nature equilibrium is enough You make a great job, congrats!

Included in the PowerPoint: Macroeconomic Objectives (AS Level) a) Aggregate Demand (AD) and Aggregate Supply (AS) analysis - the shape and determinants of AD and AS curves; AD = C+I+G + (X-M)- the distinction between a movement along and a shift in AD and AS - the interaction of AD and AS and the determination of the level of output, prices and employment b) Inflation - the definition of inflation; degrees of inflation and the measurement of inflation; deflation and disinflation - the distinction between money values and real data - the cause of inflation (cost - push and demand - pull inflation)- the consequences of inflation c) Balance of payments - the components of the balance of payments accounts (using the IMF / OECD definition): current account; capital and financial account; balancing item - meaning of balance of payments equilibrium and disequilibrium - causes of balance of payments disequilibrium in each component of the accounts - consequences of balance of payments disequilibrium on domestic and external economy d) Exchange rates - definitions and measurement of exchange rates - nominal, real, trade - weighted exchange rates - the determination of exchange rates - floating, fixed, managed float - the factors underlying changes in exchange rates - the effects of changing exchange rates on the domestic and external economy using AD, Marshall - Lerner and J curve analysis - depreciation / appreciation - devaluation / revaluation e) The Terms of Trade - the measurement of the terms of trade - causes of the changes in the terms of trade - the impact of changes in the terms of trade f) Principles of Absolute and comparative advantage - the distinction between absolute and comparative advantage - free trade area, customs union, monetary union, full economic union - trade creation and trade diversion - the benefits of free trade, including the trading possibility curve g) Protectionism - the meaning of protectionism in the context of international trade - different methods of protection and their impact, for example, tariffs, import duties and quotas, export subsidies, embargoes, voluntary export restraints (VERs) and excessive administrative burdens («red tape»)- the arguments in favor of protectionism This PowerPoint is best used when using worksheets and activities to help reinforce the ideas talked about.

Richard A. Goebel, DVM, Simmons Great Lakes For the full transcript visit: Mergers For Practices At Risk As An Exit Strategy Trends Affecting the Practice Market While the balance between buyers and sellers seems to be in equilibrium at the moment, the next decade may reveal a different trend.

Hofmann's floating rectangles of color are echoed in Equilibrium (1951), one of the few works in the show that does not swing those full - arm, stately and dignified curves.

It's unlikely that the greenhouse gas contribution in the period 1880 - 1940 was nearly 0.3 oC since that would be the full equilibrium response (under a 3 oC climate sensitivity).

Given the much more rapid respons time of the stratosphere to radiative forcings, there is (can be) some initial stratospheric cooling (or at least some cooling somewhere in the stratosphere), which consists of a transient component, and a component that remains at full equilibrium.

... interestingly in the grey gas case with no solar heating of the stratosphere, increasing the optical thickness of the atmosphere would result in an initial cooling of and in the vicinity of the skin layer (reduced OLR), and an initial radiative warming of the air just above the surface (increased backradiation)-- of course, the first of those dissappears at full equilibrium.

Adding more optical thickness to the same band reduces OLR in that band, cooling at least some portion of the upper atmosphere up to the TOA level, and increases in OLR outside that band results in some portion of that cooling remaining at full equilibrium (as expained by Andy Lacis).

But in full thermodynamic equilibrium, with equilibrium among all photons and non-photons, the rate of emission into a direction and absorption from that direction at some location, of each type of photon, will be equal.

But the added opacity will have its full effect in the stratosphere (which is in radiative equilibrium).

Refering to bands where optical thickness is constant over the interval of each band, if the atmospheric LW absorption is limited to some band (that doesn't cover all LW radiation), than increases in OLR in response to surface warming will occur outside that band, so OLR will drop within the band — there will still be some portion of stratospheric or near - TOA cooling that will be transient, but some will remain at full equilibrium.

(In full thermodynamic equilibrium, all photon - non-photon interactions, including Raman and Compton scattering, would sustain that equilibrium; all such interactions tend to eventually bring a system towards such equilibrium provided that photons (as well as other particles) are not entering or leaving the system from other systems with different conditions.)

(This is not a full thermodynamic equilibrium — it doesn't require chemical mixtures to be at equilibrium, or for the radiative intensities to be in equilibrium with the non-photon matter.

(PS don't mistake this dependence on solar heating in this context to equate to an argument that all full - equilibrium stratospheric cooling in the increase of a GHE requires stratospheric solar heating; also, this additional 10 W / m2 doesn't include any stratospheric adjustment effect.)

3 - proper weighing, with justifications, must be given to all (or most) of the internal and external forcings, with a clear understanding of how each affects the climate equilibrium 2 - this will naturally follow 3 and 4 - thorough model validation being a must 1 - predictions must be verified with full null hypothesis in place.

ECS does not refer to full thermodynamic equilibrium states but the states that have the partial equilibrium in Earth energy balance.

A full cylinder of compressed CO2 can not be distinguished from an empty CO2 cylinder if both are in thermal equilibrium with the surrounding environment — regardless of the mean free photon path distance in the respective cylinders.

Our results suggest that the atmosphere is actually in full thermodynamic equilibrium over distances of at least 20 - 30 km.

Spencer and Braswell freely admit that using their simple model is just the first step in a complicated diagnosis, but also point out that the results from simple models provide insight that should help guide the development of more complex models, and ultimately could help unravel some of the mystery as to why full climate models produce high estimates of the earth's equilibrium climate sensitivity, while estimates based in real - world observations are much lower.

The study didn't explore anything like full ranges of key climate parameters: equilibrium climate sensitivities below 2 K were not included in the ensemble, only a limited range of ocean heat uptake levels appears to have been considered, and it is unclear to me to what extent the possibility of aerosol forcing being small was represented.

If decay and photosynthesis are in equilibrium (after a full seasonal cycle of one year), then no oxygen is added or substracted to / from the atmosphere.

The difference between cycles and the emissions is that the latter is a one - way process, the former are two - way processes, which are more or less in equilibrium after a full cycle, except for temperature influences.

He says the success of any litigation practice, whether boutique or full - service, lies in the ability to «find the right equilibrium between the need for local and international expertise and sufficiently staffed teams to manage complex international litigation, while avoiding conflict hurdles and offering realistic rates».

... A preference for equilibrium and stability means that many shifts in the marketplace are met by business leaders denying that these shifts mean anything negative for them [until they're forced to deal with a full blown crisis].»

If the US produced in full (It won't happen) what they are capable of producing we would have $ 35 and lower oil for years even though the equilibrium price for oil is probably about $ 55.