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of a particular place is often described in seasonal periods (e.g. summer/ winter or rainy/ dry season) over the cycle of the year.   The climate can also naturally vary between different years due to the process of Earth system cycles, especially those associated with large circulations of the oceans

Systems (CREWS).    Since COP26, CLARE has become one of the most prominent research programmes in Climate Adaptation and Resilience globally. So far, 24 research projects are underway involving 136 organisations in 38 countries, three quarters of which in Africa and Asia. CLARE is developing

All tropical cyclones in the northern hemisphere season in 2015 are listed below including details of their start and end dates, lowest central pressure and maximum sustained wind (MSW).

Click on the name of the tropical cyclone to see a chart of the observed track and forecast tracks from the Met Office global model. Verification statistics on each tropical cyclone are available upon request from [email protected]. At the end of the season a verification report on the performance

the SSP5-RCP8.5 scenario (Gutiérrez et al., 2021; Figure 2). In general, decreases in precipitation and increases in temperature and evaporation are expected to intensify drought severity and duration over the region. Wet season rain storms are also projected to become more intense, as a warmer

and rainfall, with the southerly coastal regions being cooler and wetter and the northern areas being hotter and drier as they get closer to the Sahel. Observations from 1981-2010 show a moderate increasing trend in temperature compared to other regions of the world, but as the region has a narrow climatic

general trends of climate changes in the 21 st century are similar to UKCP09, with a move towards warmer, wetter winters and hotter, drier summers. However, natural variations mean that some cold winters, some dry winters, some cool summers and some wet summers will still occur. • At 2°C of global mean

and WP-MIP Machine Learning Emulation of Climate Change Projections for Southeast Asia 12:00 Discussion groups 13:00 Group photo 13:05 Lunch + Poster Session 2&3 14:00 Plenary debrief Ron McTaggart- Cowan Chen Chen ECCC CCRS Session 2b: AI/ML models and integration with seamless physical model

and WP-MIP Machine Learning Emulation of Climate Change Projections for Southeast Asia 12:00 Discussion groups 13:00 Group photo 13:05 Lunch + Poster Session 2&3 14:00 Plenary debrief Ron McTaggart- Cowan Chen Chen ECCC CCRS Session 2b: AI/ML models and integration with seamless physical model

) was the second storm of the 2017-2018 winter season, following Storm Aileen on 12 to 13 September. The strongest winds were around Irish Sea coasts, particularly west Wales, with gusts of 60 to 70 Kt or higher in exposed coastal locations. Impacts The most severe impacts were across the Republic of Ireland

for understanding climate variability in East Asia on timescales of seasons to decades and to assist in collaborative attribution studies of extreme events. Model development is at the core of CSSP China. Longer-term goals include joint development of high-resolution models for the East Asian