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The climate of Indonesia is almost entirely tropical. The uniformly warm waters that make up 81% of Indonesia's area ensure that temperatures on land remain fairly constant, with the coastal plains averaging 28 °C (82 °F), the inland and mountain areas averaging 26 °C (79 °F), and the higher mountain regions, 23 °C (73 °F).
Cozumel has a tropical savanna climate under the Köppen climate classification that closely borders on a tropical monsoon climate. [31] The dry season is short, from February to April, but even in these months precipitation averages about 45 millimeters (1.8 in) of rain per month.
The month of October was the warmest October ever recorded. [208] October 4 – Monthly record highs were set in Burlington, Vermont, and Syracuse, New York, with temperatures of 86 °F (30 °C) and 89 °F (32 °C). [209] [210]
Get the Cozumel, QR local weather forecast by the hour and the next 10 days.
The hottest months are April and August, in which the average high is 33 °C (91.4 °F), while January is the coldest month with an average low of 17 °C (62.6 °F). [16] Extreme temperatures can range from a low of 10 °C (50.0 °F) in the coldest months to 36 °C (96.8 °F) in the hottest months. [ 15 ]
1816 is known as the Year Without a Summer because of severe climate abnormalities that caused average global temperatures to decrease by 0.4–0.7 °C (0.7–1 °F). [1] Summer temperatures in Europe were the coldest of any on record between 1766 and 2000, [2] resulting in crop failures and major food shortages across the Northern Hemisphere. [3]
Weakening sea surface temperature anomalies in the tropical Pacific in early 2023 associated with the end of the La Niña event. The 2020–2023 La Niña event was unusual in that it featured three consecutive years of La Niña conditions (also called a "triple-dip" La Niña) in contrast to the typical 9–12 month cycles of the El Niño–Southern Oscillation (ENSO), [3] though the magnitude ...
The climate of Asia is dry across its southwestern region. Some of the largest daily temperature ranges on Earth occur in the western part of Asia . The monsoon circulation dominates across the southern and eastern regions, due to the Himalayas forcing the formation of a thermal low which draws in moisture during the summer.