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• New global dataset shines a light on humidity extremes

  this is more difficult, increasing health risk to humans. Analysis of the new data has shown that global annual / seasonal mean of maximum daily wet bulb temperature, a measure of humidity, has increased by around 0.2°C each decade between 1973-2022. This rate of change is even higher when looking

• africa-climate-outlook---november-2024pdf

  the month (dry season). Additional Information: (1) Note: Normal or cold in the north, hot in the south (2) Note: Normal in the northeast (3) Note: Large variations across the country (4) Note: Warm or hot in the southwest, cool to normal in the northeast (5) Note: Normal in the west, very wet

• africa-climate-outlook---november-2024.pdf

  the month (dry season). Additional Information: (1) Note: Normal or cold in the north, hot in the south (2) Note: Normal in the northeast (3) Note: Large variations across the country (4) Note: Warm or hot in the southwest, cool to normal in the northeast (5) Note: Normal in the west, very wet

• PowerPoint Presentation

  Kenya, western Tanzania and parts of Malawi and Zambia were wetter than normal, with more mixed conditions in December. 3-Month Outlook February to April - Rainfall Outlook: The development of La Niña usually increases slightly the chance of a wetter than normal season across parts of southern Africa

• Climate change drives increase in storm rainfall

  1991/92 to 2020/21. Source: Met Office HadUK-Grid and Met Éireann’s gridded precipitation datasets. Climate change also had a strong influence on autumn and winter total rainfall. In a pre-industrial climate, wet periods such as the 2023-24 October-March season had an estimated return period of 1

• cop_1.5_report_3.pdf

  decrease is about 15%. However, some basins in south and east Asia are projected to see increased flow in all simulations. Flows in the Ganges increase by up to 90% at 1.5°C and by up to 130% at 2°C. Figure 2. Range of projected changes in flow in major river basins at 2°C and 1.5°C global warming

• cop_15_report_3pdf

  decrease is about 15%. However, some basins in south and east Asia are projected to see increased flow in all simulations. Flows in the Ganges increase by up to 90% at 1.5°C and by up to 130% at 2°C. Figure 2. Range of projected changes in flow in major river basins at 2°C and 1.5°C global warming

• cop_15_report_3pdf-1.cop_15_report_3pdf

  decrease is about 15%. However, some basins in south and east Asia are projected to see increased flow in all simulations. Flows in the Ganges increase by up to 90% at 1.5°C and by up to 130% at 2°C. Figure 2. Range of projected changes in flow in major river basins at 2°C and 1.5°C global warming

• review-of-sea-level-rise-literature-for-pakistan---arrcc-report---external.pdf

  ) and Special Report on the Ocean and Cryosphere in a Changing Climate (SROCC) as one of the most important risks facing coastal nations and communities. The lowlying islands and densely populated coastal areas of South Asia are vulnerable to the impacts of sea level rise, such as coastal erosion

• central-africa-climate-risk-report-finalpdf

  compared to the rest of the region. There has been no significant trend In average precipitation in recent decades. By 2050 there is some indication for wetter conditions in the rainy season and a delay to the onset of the rainy season. Flood and drought events are likely to be more frequent