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A thunderstorm in Sydney. The climate of Sydney, Australia is humid subtropical (Köppen: Cfa), [1] shifting from mild [2] [3] [4] and cool [5] in winter to warm and occasionally hot [5] in the summer, with no extreme seasonal differences since the weather has some maritime influence (as it is moderated by proximity to the Pacific Ocean). [3]
The highest maximum temperature was recorded as 50.7 °C (123.3 °F) at Oodnadatta on 2 January 1960, which is the highest official temperature recorded in Australia. The lowest minimum temperature was −8.0 °C (17.6 °F) at Yongala on 20 July 1976. [12] Labelled map of South Australia showing where the places mentioned in the table are located
Sydney has a humid subtropical climate (Cfa) with warm and sometimes hot summers, and winters shifting from mild to cool. Although Sydney is predominantly humid subtropical, the hilly areas of the Forest District, such as Terrey Hills, among others, have a borderline oceanic climate (Cfb). The weather is moderated by proximity to the ocean, and ...
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 .
Climate charts provide an overview of the climate in a particular place. The letters in the top row stand for months: January, February, etc. The bars and numbers convey the following information: The blue bars represent the average amount of precipitation (rain, snow etc.) that falls in each month.
A Köppen–Geiger climate map showing temperate climates for 1991–2020 The different geographical zones of the world. The temperate zones, in the sense of geographical regions defined by latitude, span from either north or south of the subtropics (north or south of the orange dotted lines, at 35 degrees north or south) to the polar circles.
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The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar).