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Climate data for Bengaluru (1991–2020, extremes 1901–present) Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year Record high °C (°F) 32.8 (91.0)
Rainfall and temperature. Due to its elevation, Bangalore enjoys a pleasant and equable climate throughout the year with occasional extreme weather events like heatwaves, coldwaves, floods and droughts. The highest temperature ever recorded in Bengaluru is 41.8°c in April 30, 2024 in Kengeri at Bengaluru.
From 1978 onward CRU began production of its gridded data set of land air temperature anomalies based on instrumental temperature records held by National Meteorological Organisations around the world. In 1986 sea temperatures were added to form a synthesis of data which was the first global temperature record, demonstrating unequivocally that ...
In its Biennial Update Report to the United Nations Framework Convention on Climate Change (UNFCCC) submitted in February, India said it has progressively continued decoupling of economic growth from greenhouse gas emissions. India's emission intensity of gross domestic product (GDP) has reduced by 24% between 2005 and 2016.
Heavy rains show the full might of Jog Falls in Shimoga district. The state of Karnataka in India experiences diverse rainfall quantities across its regions. While Malnad and Coastal Karnataka receive copious amount of rainfall; its north Bayaluseemae region in the Deccan Plateau is one of the most arid regions in the country.
Madikeri features a tropical highland climate as it has an elevation of 1,170 m (3,840 ft). Madikeri is located at 12°25′N 75°44′E / 12.42°N 75.73°E / 12.42; [ 14 ] [ 15 ] Madikeri lies in the Western Ghats and is a popular hill station.
Bengaluru (Kannada : Beṅgaḷūru ⓘ), formerly called Bangalore, is the capital and largest city of the southern Indian state of Karnataka.As per the 2011 census, the city had a population of more than 8.4 million, making it the third most populous city in India and the most populous in South India.
The Mahoney Tables (Evans, 1999; Evans, 2001) proposed a climate analysis sequence that starts with the basic and widely available monthly climatic data of temperature, humidity and rainfall, such as that found in HMSO (1958) and Pearce and Smith (1990), or data published by national meteorological services, for example SMN (1995).