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  • scipsa_gcm_verification_final.pdf

    An assessment of 12 dynamical seasonal prediction systems is conducted, assessing their ability to predict South Asian seasonal precipitation during the two key monsoon seasons; southwest (June to September (JJAS)) and northeast (October to November (OND)). This research has been conducted as part

  • scipsa_gcm_verification_finalpdf

    An assessment of 12 dynamical seasonal prediction systems is conducted, assessing their ability to predict South Asian seasonal precipitation during the two key monsoon seasons; southwest (June to September (JJAS)) and northeast (October to November (OND)). This research has been conducted as part

  • 20220502-scipsa-final-regional-report---sascof-csuf-_-final_clean.pdf

    , for example through including additional variables, such as temperature which has been routinely included in the SASCOF forecast process since 2021. Consideration could also be made for additional key seasons for specific regions in South Asia, such as the peak wet season in Afghanistan and Pakistan during

  • 20220502-scipsa-final-regional-report---sascof-csuf-_-final_cleanpdf

    , for example through including additional variables, such as temperature which has been routinely included in the SASCOF forecast process since 2021. Consideration could also be made for additional key seasons for specific regions in South Asia, such as the peak wet season in Afghanistan and Pakistan during

  • video_script_finalpdf

    and September. So, if we already know the “typical” weather in a season – that is, the “climate”, then why do we need a forecast? Well a season’s characteristics naturally vary from one year to another; for example, a mild and wet winter one year may be followed by a cold and dry winter the next

  • video_script_final.pdf

    and September. So, if we already know the “typical” weather in a season – that is, the “climate”, then why do we need a forecast? Well a season’s characteristics naturally vary from one year to another; for example, a mild and wet winter one year may be followed by a cold and dry winter the next

  • arrcc_carissa_ws4_observational_datasets-v2.pdf

    Report Understanding and quantifying extreme precipitation events in South Asia Part III – Observational datasets for the assessment of present day monsoon-season rainfall extremes in Nepal CARISSA Activity 4: Climate services for the water and hydropower sectors in South Asia March 2022 Delivery

  • PowerPoint Presentation

    the eastern Caribbean was drier than normal, despite an active tropical cyclone season. The only area that were wetter than normal was the far west of Cuba, where tropical cyclone impacts did occur. Outlook: Below normal rainfall is likely across the Middle East and North Africa during the next 3-6

  • PowerPoint Presentation

    (dry season). Climate Outlook Africa: July to April Current Status 10 Current Status – Central Africa Current Status: Temperature Current Status: Rainfall July August September July August September Niger Warm Normal Normal Wet^^ Wet^^ Wet^^ Chad Normal Normal Normal Wet^^ Wet^^ Wet^^ DRC Warm^ Warm

  • southeast_asia_climate_framework.pdf

    to increase across the whole of Southeast Asia (see figure 5.). The strongest annual warming is likely to occur in mainland Southeast Asia, with fairly uniform warming throughout the seasons. Regional surface air temperature is typically expected to rise by 2 °C by mid-century and by 4 °C by the end

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