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The climate of Agra features a semi-arid climate that borders on a humid subtropical climate. The city features mild winters, hot and dry summers and a monsoon season. The monsoon, though substantial in Agra, is not quite as heavy as the monsoon in other parts of India. The mean annual rainfall of Agra district is 671 mm (26.4 in). [1]
South Africa is a sunny country, averaging 8–10 daily sunshine hours in most regions. [2] The average annual rainfall for South Africa is about 464 mm (compared to a global average of 950 mm [3]) but large and unpredictable variations are common. Overall, rainfall is greatest in the east and gradually decreases westward, with some semi-desert ...
Annually, the rain belt across the continent moves northward into Sub-Saharan Africa by August, then passes back southward into south-central Africa by March. [22] Areas with a savannah climate in Sub-Saharan Africa, such as Ghana, Burkina Faso, [23] [24] Darfur, [25] Eritrea, [26] Ethiopia, [27] and Botswana have a distinct rainy season. [28]
On 13 January 2013, Kanpur recorded its all-time low temperature when the temperature plunged to −1.1 °C or 30.0 °F and on the same day, Agra recorded −0.7 °C or 30.7 °F. In January, in Lucknow, the temperature can plunge below freezing; Lucknow recorded 0.0 °C or 32.0 °F on 18 January 2017.
Sunshine hours for selected cities in Africa Country City Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Ref. Ivory Coast: Gagnoa: 183.0 180.0
The Zulu calendar is the traditional lunisolar calendar used by the Zulu people of South Africa. [1] Its new year begins at the new moon of uMandulo(September) in the Gregorian calendar . The Zulu calendar is divided into two seasons, the summer iHlobo and Winter ubuSika . [ 2 ]
The Noongar people of South-West Western Australia recognise maar-keyen bonar, [41] or six seasons. Each season's arrival is heralded not by a calendar date, but by environmental factors [42] such as changing winds, flowering plants, temperature and migration patterns and lasts approximately two standard calendar months. The seasons also ...
However, as the obliquity changes, the overall wandering path of the thermal equator shifts between 22.2° and 24.5° north and south. This wandering may affect the positioning of the North African Summer Monsoon Front and thus impact the perceived strength of the North African Monsoon.