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  • sur-sharmila-oscar-alves-harry-hendon-antje-weisheimer-magdalena-balmaseda-matthew-wheeler-wendy-sharples-andrew-marshall---predicting-enso-events-and-their-regional-impacts-beyond-a-year.pdf

    series of Niño3.4 indices for all initialised forecasts relative to ERSST IV. Prediction of Regional Impacts Based on Nov0 initialised forecasts: Model predicts overall dry conditions across Australia during 1 st (Y0) and 2 nd (Y+1) wet-season of multi-year El Nino events but underestimates the rainfall

  • sur-sharmila-oscar-alves-harry-hendon-antje-weisheimer-magdalena-balmaseda-matthew-wheeler-wendy-sharples-andrew-marshall---predicting-enso-events-and-their-regional-impacts-beyond-a-yearpdf

    series of Niño3.4 indices for all initialised forecasts relative to ERSST IV. Prediction of Regional Impacts Based on Nov0 initialised forecasts: Model predicts overall dry conditions across Australia during 1 st (Y0) and 2 nd (Y+1) wet-season of multi-year El Nino events but underestimates the rainfall

  • 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

  • PowerPoint Presentation

    balanced (Climatological Odds). This wet signal extends into northern Mozambique. Otherwise, much of southern Africa is more likely to be drier than normal, although in absolute terms the potential rainfall deficit is likely to be small as this is towards the end of the dry season. Tropical cyclones

  • PowerPoint Presentation

    and Burkina Faso were wet or very wet. Uganda was also very wet in July and August with Cameroon wet in July and very dry in August. Ghana was very dry in July. 3-Month Outlook November to January - Rainfall Outlook: In East Africa, the ‘Short Rains’ season takes place for many parts during this period

  • 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

  • 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

  • PowerPoint Presentation

    /maproom/. Additional Information: ^Note: In March western Nigeria had normal rainfall but it was Very Wet in the east, whilst the dry season continued in the north. ^^Note: In April, northern Nigeria was Very Wet and western Cameroon Very Dry. * Region usually experiences less than 10mm/month

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