optimum$55409$ - ορισμός. Τι είναι το optimum$55409$
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Τι (ποιος) είναι optimum$55409$ - ορισμός

GEOGRAPHICAL REGION WHICH EFFICIENTLY SHARES A SINGLE CURRENCY
Optimal currency; Optimal Currency Area; Optimal currency area; Optimum currency region; Optimal currency region; Optimal Currency Region; Optimum Currency Region; Optimum Currency Area; Optimum Currency; Optimum currency; Optimal Currency; Optimum currency areas; Optimum currency form; Optimum currency forms

Roman Warm Period         
WARM WEATHER PERIOD, 250 BC TO AD 400
Roman Climatic Optimum
The Roman Warm Period, or Roman Climatic Optimum, was a period of unusually-warm weather in Europe and the North Atlantic that ran from approximately 250 BC to AD 400. Theophrastus (371 – c.
Optimum currency area         
In economics, an optimum currency area (OCA) or optimal currency region (OCR) is a geographical region in which it would maximize economic efficiency to have the entire region share a single currency.
Holocene climatic optimum         
  • Vegetation and water bodies in northern and central Africa in the [[Eemian]] (bottom) and [[Holocene]] (top)
WARM PERIOD DURING ROUGHLY THE INTERVAL 9,000 TO 5,000 YEARS BP
Holocene Climatic Optimum; Holocene thermal maximum; Holocene optimum; Holocene maximum; Hypsithermal; Climatic optimum; Altithermal; Holocene Climate Optimum; Holocene Maximum; Holocene thermal optimum; The Holocene Thermal Optimum; Holocene Thermal Maximum; Mid-Holocene Warm Period; Mid Holocene Warm Period; Holocene Megathermal
The Holocene Climate Optimum (HCO) was a warm period that occurred in the interval roughly 9,000 to 5,000 years ago BP, with a thermal maximum around 8000 years BP. It has also been known by many other names, such as Altithermal, Climatic Optimum, Holocene Megathermal, Holocene Optimum, Holocene Thermal Maximum, Hypsithermal, and Mid-Holocene Warm Period.

Βικιπαίδεια

Optimum currency area

In economics, an optimum currency area (OCA) or optimal currency region (OCR) is a geographical region in which it would maximize economic efficiency to have the entire region share a single currency.

The underlying theory describes the optimal characteristics for the merger of currencies or the creation of a new currency. The theory is used often to argue whether or not a certain region is ready to become a currency union, one of the final stages in economic integration.

An optimal currency area is often larger than a country. For instance, part of the rationale behind the creation of the euro is that the individual countries of Europe do not each form an optimal currency area, but that Europe as a whole does. The creation of the euro is often cited because it provides the most modern and largest-scale case study of an attempt to identify an optimum currency area, and provides a comparative before-and-after model by which to test the principles of the theory.

In theory, an optimal currency area could also be smaller than a country. Some economists have argued that the United States, for example, has some regions that do not fit into an optimal currency area with the rest of the country.

The theory of the optimal currency area was pioneered in the 1960s by economist Robert Mundell. Credit often goes to Mundell as the originator of the idea, but others point to earlier work done in the area by Abba Lerner. Kenen (1969) and McKinnon (1963) were further developers of this idea.