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• PowerPoint Presentation

  are expected across parts of Indochina and the South China Sea. Conversely warmer than normal conditions are very likely across Indonesia, Malaysia, the Philippines, and across the Bay of Bengal and much of the Indian Ocean where Sea Surface Temperatures (SSTs) are above normal. Also warmer-than-normal

• uk_monthly_climate_summary_201907pdf

  the west coast, but the east remained very warm with some sunshine. The 25th was hot and sunny in most areas with a high of 32.5 °C at Colwyn Bay (Clwyd), and the heat sparked off some thunderstorms in the east during the afternoon. The night of the 25th/26th was unusually warm with the temperature

• uk_monthly_climate_summary_201812pdf

  pressure close by, but a generally westerly airflow maintained mild cloudy weather. The 24th was a sunny day in the north-east with 5.0 hours recorded at Colwyn Bay (Clwyd), but it was cloudy and drizzly in the south and south-west. The cloudy drizzly weather spread across the country for the 25th

• mwr_2025_05_for_printpdf

  . Weather diary • High pressure dominates, wet and windy end to the month The UK got an early taste of summer during May with high pressure dominating the scene for most of the month, with frontal systems weakened or kept at bay, and many places seeing no measurable rain for the better part of 3 weeks

• PowerPoint Presentation

  activity is signalled, however, there are signals that storm track may be displaced slightly further west compared to normal, with more storms affecting regions surrounding the South China Sea. For the Bay of Bengal, activity tends to peak in October and November. Near normal levels of activity

• wcssp_impact_brochure_final.pdf

  for rip currents in South Africa. Rip currents are strong hazardous currents that run out to sea and cause hundreds of coastal drownings each year around the world. They are one of the biggest dangers facing beach users in South Africa. Research has shown that rip currents are strongly related

• scipsa_gcm_verification_final.pdf

  the JJAS season, mainly driven by weak tropical depressions that originate in the Bay of Bengal (Shahid, 2010). Rainfall distribution varies considerably, with the lowest amounts in central-western parts and highest in eastern parts (Figure 2). Floods are a common occurrence in Bangladesh

• scipsa_review_seasonal_forecasting_south_asia_final.pdf

  areas, the strongest of which are known as monsoon depressions. The depressions usually originate over the north of the Bay of Bengal from June to September, then propagate westnorthwestward along the axis of the monsoon trough to the Indian subcontinent, lasting 3 to 5 days on average (Godbole, 1977

• trd---climate-risk-report-for-csa---v4-final.pdf

  South West monsoon. ENSO interacts with the variability and intensity of IOD on an interannual timescale, with positive phases of IOD correlating with warmer seasonal temperatures and above average precipitation (Wang et al., 2016). Tropical cyclones also impact countries surrounding the Bay

• trd---climate-risk-report-for-csa---v4-final-april-2026pdf

  surrounding the Bay of Bengal and the Arabian Sea. In Central Asia, the NAO and ENSO are the main drivers of climate variability. The NAO varies interannually and is driven by atmospheric pressure differences between the Azores High and Icelandic low in the Atlantic. When NAO is positive, it leads