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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 .
This is a list of cities by average temperature (monthly and yearly). The temperatures listed are averages of the daily highs and lows. Thus, the actual daytime temperature in a given month may be considerably higher than the temperature listed here, depending on how large the difference between daily highs and lows is.
A humid tropical climate with an average temperature of 30 °C (86 °F). The Southwestern Bands of the Amazon rainforest for the central and northwestern areas of Bolivia, where temperatures are hot for a majority of the year, with slightly milder winters. Precipitation in these areas ranges from 2,000mm to 4,000mm per year, with some areas ...
The whole city has rainy summers and dry winters. The city has a relatively dry climate, with rainfall occurring mainly in the slightly warmer months of November to March. Heavy precipitation typically occurs throughout summer, and often causes destructive mudslides. The wettest month is January with a monthly average of 100–140 mm (3.9–5.5 ...
Bolivia, [c] officially the Plurinational State of Bolivia, [d] is a landlocked country located in central South America.The country features diverse geography, including vast Amazonian plains, tropical lowlands, mountains, the Gran Chaco Province, warm valleys, high-altitude Andean plateaus, and snow-capped peaks, encompassing a wide range of climates and biomes across its regions and cities.
Bolivia, officially the Plurinational State of Bolivia, is a landlocked country located in central South America.The country features diverse geography, including vast Amazonian plains, tropical lowlands, mountains, the Gran Chaco Province, warm valleys, high-altitude Andean plateaus, and snow-capped peaks, encompassing a wide range of climates and biomes across its regions and cities.
Seasonal lag is the phenomenon whereby the date of maximum average air temperature at a geographical location on a planet is delayed until some time after the date of maximum daylight (i.e. the summer solstice). This also applies to the minimum temperature being delayed until some time after the date of minimum insolation.
The Austrian locality of Stetten had a mean winter temperature of 9.6–13.3 °C and a mean summer temperature of 24.7–27.9 °C, contrasting with −1.4 °C and 19.9 °C respectively in the present; precipitation amounts at this site were 9–24 mm in winter and 204–236 mm in summer. [15]