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chn24_1.15_wcssp_expression-of-interest.pdf
resilience of vulnerable communities around the world since 2014. Through the WCSSP programme, we are working collaboratively on projects that focus on the global challenges of weather and climate with partners in Brazil, China, India, South Africa and Southeast Asia. International collaboration
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marcia-zilli-jerry-samuel-neil-hart---future-changes-in-the-characteristics-of-the-dry-to-wet-transition-period-in-southern-africa-and-south-america-using-convection-permitting-simulations.pdf
and the Environment, University of Oxford, UK Dry-to-wet transition Two-tier approach: (1) climatologial envelope when the transition should occur (2) dry-to-wet transition in each year/season (1) Gradient (x100) Filtered precipitation Filtered Precipitation (60-points second order Butterworth filter
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marcia-zilli-jerry-samuel-neil-hart---future-changes-in-the-characteristics-of-the-dry-to-wet-transition-period-in-southern-africa-and-south-america-using-convection-permitting-simulationspdf
and the Environment, University of Oxford, UK Dry-to-wet transition Two-tier approach: (1) climatologial envelope when the transition should occur (2) dry-to-wet transition in each year/season (1) Gradient (x100) Filtered precipitation Filtered Precipitation (60-points second order Butterworth filter
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Microsoft Word - EAfrica2019
but probabilities of a wetter season than last year and of 10-year extremes are presented. A wetter season than 2018 is favoured in most boxes east of 30E and between 10N and 10S. Elsewhere a drier season than 2018 is likely in most grid boxes. Probabilities of a season drier than any in the past 10 years (2009
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Understanding convergence zones and the Intertropical Convergence Zone
continue to converge, wet conditions can persist, sometimes resulting in significant rainfall totals and even flooding. Convergence lines are not limited to a particular season and can occur at any time of year. During the summer months, local sea breezes can help form convergence lines
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centellaartola15caribbeanprecisdomainsizecompressedpdf
features in the Caribbean. Results are presented for the early wet season (May–July) and late wet season (August– October). There is a relative insensitivity to domain size for simulating some important features of the regional circulation and key rainfall characteristics e.g. the Caribbean low level
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centellaartola15caribbeanprecisdomainsize.compressed.pdf
features in the Caribbean. Results are presented for the early wet season (May–July) and late wet season (August– October). There is a relative insensitivity to domain size for simulating some important features of the regional circulation and key rainfall characteristics e.g. the Caribbean low level
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cssp_china_science__modelling.pdf
characteristics of the East Asian Summer Monsoon compared to regional scale models, including the daily cycle of rainfall across many regions of China. Li et al (2019) focussed on an event in 2016 where 600mm of rainfall fell over parts of eastern China in just 6 days leading to catastrophic flooding
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wiser0206_stakeholderengcxforum.pdf
start of the MAM 2020 season. The sub-region will experience warmer than normal temperatures through the season. Noting that there was abundant rainfall during October – December 2019 and considering that the coming MAM 2020 rainfall season is anticipated to be wet, all stakeholders are called upon
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southern-africa-climate-risk-report-final-pdf
of the region there is no clear consensus on whether the climate will be wetter or drier, although there is some evidence for a small delay to the start of the rainy season by mid-century in the north-east. The region has long coastlines with the Atlantic and Indian Oceans. The coastal regions bordering