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• 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

• 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

• 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

• 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

• 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

• PowerPoint Presentation

  -normal, though more mixed across DRC. 3-Month Outlook February to April - Rainfall The Short Rains season in East Africa brought wetter than normal conditions to many areas, most notably in November when most parts were very wet. In southern Africa during October, Zambia, Zimbabwe and Mozambique were wet

• PowerPoint Presentation

  of the Sahel and into Eastern Africa, and very likely to lead to dry conditions in Ethiopia, South Sudan and parts of Sudan. This time of year is the dry season for southern Africa. However, parts of South Africa, Zimbabwe and Madagascar are more likely to be wetter than normal, along with Somalia