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• Tropical cyclone names

  North Pacific (east of 140 °W) L : North Atlantic A : Arabian sea B : Bay of Bengal S : South Indian Ocean (west of 135 °E) P : South Pacific Ocean (east of 135 °E) Q : South Atlantic NHC Miami and CPHC Hawaii also use the "ATCF" identifier for Eastern & Central North Pacific and Atlantic depressions

• 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

• west-africa-climate-risk-report-final.pdf

  rise will impact coastal settlements through loss of beaches, shoreline retreat and inundation of low-lying areas posing a considerable risk for the third of West Africa’s population that live in coastal regions. Low-lying villages and settlements along the coast are vulnerable to inundation

• west-africa-climate-risk-report-finalpdf

  rise will impact coastal settlements through loss of beaches, shoreline retreat and inundation of low-lying areas posing a considerable risk for the third of West Africa’s population that live in coastal regions. Low-lying villages and settlements along the coast are vulnerable to inundation

• 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-april-2026.pdf

  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

• 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

• 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

• scipsa_gcm_verification_finalpdf

  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_finalpdf

  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