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% and -36% by 2100. This more intense cycle is also visible in the Sub-Andean mountain range with strongest precipitation decreases around August. In the highlands, this pattern reverses by 2100 with strongest relative precipitation in-and decrease during the dry- and wet season respectively. Because

and the IRI Map Room: http://iridl.ldeo.columbia.edu/maproom/. * Region usually experiences less than 10mm/month rainfall during the month (dry season). (1) Note: Large variations across the country. (2) Note: Hot in the north, cold in the south. (3) Note: Hot in north and west. (4) Note: Very wet

and August’s respective average temperatures were generally closer to average. However, despite above average temperatures for the season, it has also been a wetter than average summer, with July leading the way in terms of rainfall; which was provisionally the UK’s sixth wettest July on record

season in Nepal. Model evaluation criteria: How well do the climate models capture the large-scale processes in the atmosphere that cause extreme precipitation events? Model assessment criteria: In a south Asian monsoon, how well does the model capture wind speed and direction over the monsoon period

. December average temperatures 6 o C above the long-term mean in England from the Midlands southwards, and 5 o C above the long-term mean elsewhere. Average seasonal temperatures 3 o C above the long-term mean across the UK. Compound months and seasons November to April Wet (rainfall 2.5 times

Asia-Pac. J. Atmos. Sci., 52(4), 353-369, 2016 pISSN 1976-7633 / eISSN 1976-7951 DOI:10.1007/s13143-016-0004-1 Climate Change Projections over India by a Downscaling Approach Using PRECIS Prasanta Kumar Bal 1,2 , Andimuthu Ramachandran 1 , Kandasamy Palanivelu 1 , Perumal Thirumurugan 1 , Rajadurai

‘Wet’ days: greater than the 1981-2010 90 th percentile daily precipitation ‘Windy’ days: greater than the 1981-2010 90 th percentile daily mean windspeed The thresholds are calculated separately by month and region, and the frequencies of exceedance averaged by nation and season. Based on UKCP18

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

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

Forecasts for the north-east part of Brazil between 0° S to 10° S and east of 50° W for the February to May wet season.

The wet season is between February and May with considerable year-to-year and decade-to-decade variability. The forecasts are produced using a combination of dynamical forecast models and statistical predictions and include predictions of the most likely of five rainfall categories (very wet, wet