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Get the Funchal, Madeira Islands local weather forecast by the hour and the next 10 days.
The floods and mudslides were the result of an extreme weather event that, in some places, dropped more than double the monthly average of rainfall in a very short period. Between 6 a.m. and 11 a.m. local time (and UTC ), 108 mm (4¼ inches) of rain was recorded at Funchal weather station and 165 mm (6½ inches) of rain at the weather station ...
Funchal (Portuguese pronunciation: ⓘ) is the capital, largest city and the municipal seat of Portugal's Autonomous Region of Madeira, bordered by the Atlantic Ocean. The city has a population of 105,795, [ 1 ] making it the sixth largest city in Portugal.
Strong mesocyclone on a thunderstorm near Tuscaloosa, Alabama, that was analyzed as fitting the characteristics of a TVS.It was associated with a tornado.. A tornadic vortex signature, abbreviated TVS, is a Pulse-Doppler radar weather radar detected rotation algorithm that indicates the likely presence of a strong mesocyclone that is in some stage of tornadogenesis. [1]
According to the Instituto de Meteorologia (IPMA), the average annual temperature at Funchal weather station is 19.6 °C (67.3 °F) for the 1981–2010 period. Relief is a determinant factor on precipitation levels; areas such as the Madeira Natural Park can get as much as 2,800 mm (110 in) of precipitation a year. [67]
Classic-style hook echo of the F5 1999 Bridge Creek-Moore tornado.. A hook echo is a pendant or hook-shaped weather radar signature as part of some supercell thunderstorms.It is found in the lower portions of a storm as air and precipitation flow into a mesocyclone, resulting in a curved feature of reflectivity.
Vertical cross-section through a supercell showing the BWER. The bounded weak echo region, also known as a BWER or a vault, is a radar signature within a thunderstorm characterized by a local minimum in radar reflectivity at low levels which extends upward into, and is surrounded by higher reflectivities aloft, forming a kind of dome of weak echoes.
Santa Luzia is boxed in by the Ribeira of João Gomes (whose origin is in the Serra do Poiso in the interior), in the east, and on the west by Ribeira de Santa Luzia (which springs from the area around the Pico do Areeiro and Pico do Escalvado, and is responsible for the volume of spring run-off that flows into the Ribeiro de Cideral, Ribeira dos Frades, Ribeira do Pisão an Ribeira do Til.