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The cold prevailing northwesterly wind from Greece continuously blows over the northern coast without the interposition of an eventual mountain range and thus, greatly moderates temperatures throughout the year. Because of the effect, average low temperatures vary from 15 °C (59 °F) in wintertime to 27–35 °C (80.6–95.0 °F) in summertime ...
This is a list of countries and sovereign states by temperature.. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group, derived from raw gridded climatologies from the Climatic Research Unit.
Other lake ecosystems throughout Egypt are also negatively affected by climate change. Lake Qarun and Lake Manzallah have experienced higher levels of water evaporation and increases in salinity. Climate change has also caused changes in the chemical properties of the rivers, making them more vulnerable to invasive species such as the red swamp ...
4.2-kiloyear event dry, lasted most of the 22nd century BC, linked to the end of the Old Kingdom in Egypt, and the Akkadian Empire in Mesopotamia, various archaeological cultures in Persia and China 1800–1500: Middle Bronze Age Cold Epoch, a period of unusually cold climate in the North Atlantic region Bond Event 2
Christopher C. Burt, a weather historian writing for Weather Underground, believes that the 1913 Death Valley reading is "a myth", and is at least 2.2 or 2.8 °C (4 or 5 °F) too high. [13] Burt proposes that the highest reliably recorded temperature on Earth could still be at Death Valley, but is instead 54.0 °C (129.2 °F) recorded on 30 ...
Cairo, the capital of Egypt, is a bustling metropolis that sits on the banks of the River Nile. Home to an estimated 22 million people, the city has more recently expanded into a sprawling jumble ...
Khamsin, [1] chamsin or hamsin (Arabic: خمسين ḫamsīn, meaning "fifty"), more commonly known in Egypt and Israel as khamaseen (Egyptian Arabic: خماسين ḫamāsīn, IPA: [xɑmæˈsiːn] ⓘ), is a dry, hot, sandy local wind affecting Egypt and the Levant; similar winds, blowing in other parts of North Africa, the Arabian Peninsula [citation needed] and the entire Mediterranean ...
The Sannai-Maruyama site in Japan declined during the same period; [76] the growing population of the Jomon culture gradually turned to decline after that. [ 77 ] Rebun Island experienced an abrupt, intense cooling around 4,130 BP believed to be associated with the 4.2 ka event.