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• 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

• prasanta_kumar_bal_2014_india.pdf

  as the major driver of the timing, magnitude, and variability of wet-season rainfall and its extremes to access the impact on the water resources. Here, our focus is to look for models that demonstrate reasonable skills in simulating rainfall patterns over the study region as well as the wider Indian

• prasanta_kumar_bal_2014_indiapdf

  as the major driver of the timing, magnitude, and variability of wet-season rainfall and its extremes to access the impact on the water resources. Here, our focus is to look for models that demonstrate reasonable skills in simulating rainfall patterns over the study region as well as the wider Indian

• theor_appl_clim_tamil_nadu_india_precispdf

  of the timing, magnitude, and variability of wet-season rainfall and its extremes to access the impact on the water resources. Here, our focus is to look for models that demonstrate reasonable skills in simulating rainfall patterns over the study region as well as the wider Indian subcontinent. We assessed

• theor_appl_clim_tamil_nadu_india_precis.pdf

  of the timing, magnitude, and variability of wet-season rainfall and its extremes to access the impact on the water resources. Here, our focus is to look for models that demonstrate reasonable skills in simulating rainfall patterns over the study region as well as the wider Indian subcontinent. We assessed

• 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

• africa-climate-outlook---june-2025.pdf

  in the northeast (2) Note: Wet in the far west and dry in parts of the east, else normal (3) Note: Normal, but dry in the west * Region usually experiences less than 10mm/month rainfall during the month (dry season). Climate Outlook Africa: March to December Current Status 12 Current Status – Central Africa

• africa-climate-outlook---june-2025pdf

  in the northeast (2) Note: Wet in the far west and dry in parts of the east, else normal (3) Note: Normal, but dry in the west * Region usually experiences less than 10mm/month rainfall during the month (dry season). Climate Outlook Africa: March to December Current Status 12 Current Status – Central Africa