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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

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

uk_monthly_climate_summary_201812.pdf

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

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_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

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

NCIC Monthly Summary

. The mild theme continued overnight into the 8 th with Colwyn Bay (Clwyd) not falling below 15.5 °C, then it was cloudy but mainly dry. The 9th was cloudy too, with a narrow band of light rain crossing parts of the west and north during the afternoon. 10th to 16th The 10th was mostly sunny, after some

NCIC Monthly Summary

and thunderstorms over the south-west spread north and east. The night of the 7th/8th was unusually warm with Langdon Bay (Kent) not falling below 22.3 °C. Between the 8th and 11th, it was widely hot and sunny but low cloud proved slow to clear at times in Midland and northern counties, especially

factsheet_15-weather-radar-2020_2023.pdf

002°35’43”W Titterstone Clee, near Ludlow, Shropshire Hameldon Hill 381060 428740 53°45’17”N 002°17’19”W Dunnockshaw, near Burnley, Lancashire Chenies 501642 199959 51°41’21”N 000°31’50”W Flauden, near Amersham, Hertfordshire Castor Bay 119112 520302 54°30’00”N 006°20’24”W Near Lurgan, Belfast

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