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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. [1] Theophrastus (371 – c. 287 BC) wrote that date trees could grow in Greece if they were planted but that they could not set fruit there.
Allerød oscillation warm & moist (B-S) 11,400–9,500: Huelmo–Mascardi Cold Reversal cold in Southern Hemisphere: 10,800–9,500: Younger Dryas sudden cold and dry period in Northern Hemisphere (B-S) 9,500–5,500: Holocene climatic optimum A warm period about 4.9 °C warmer than the LGM
Unusually high precipitation levels were in Roman Spain during the so-called Iberian–Roman Humid Period. Roman Spain experienced three major phases: the most humid interval in 550–190 BC, an arid interval in 190 BC–150 AD and another humid period in 150–350. [ 16 ]
The Late Antique Little Ice Age is seen between the middle of the 6th century and the start of the 7th century, and preceded by the Roman Warm Period. [1]The Late Antique Little Ice Age (LALIA) was a long-lasting Northern Hemispheric cooling period in the 6th and 7th centuries AD, during the period known as Late Antiquity.
It is the period in which Greek and Roman society flourished and wielded great influence throughout Europe, North Africa and the Middle East. Post-classical history – Period of time that immediately followed ancient history. Depending on the continent, the era generally falls between the years AD 200–600 and AD 1200–1500.
At about the same time the Byzantine Empire reached its first acme and Christianity established itself in Europe as the leading monotheistic religion. After this relatively short cool interlude the climate ameliorated again and reached between 800 and 1200 almost the values of the Roman Warm Period (used temperature proxies are sediments in the ...
5. Crete, Greece. The largest of the Greek islands, Crete is another fantastic warm winter destination in Europe, enjoying mild temperatures during the winter months, with an average temperature ...
It has also been known by many other names, such as Altithermal, Climatic Optimum, Holocene Megathermal, Holocene Optimum, Holocene Thermal Maximum, Holocene global thermal maximum, Hypsithermal, and Mid-Holocene Warm Period. The warm period was followed by a gradual decline, of about 0.1 to 0.3 °C per millennium, until about two centuries ago ...