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The role of sea-land air thermal difference, shape of the coastline and sea surface temperature in the nocturnal offshore convection

Autor
Mazon, J.; Pino, D.
Tipus d'activitat
Article en revista
Revista
Tellus. Series A, dynamic meteorology and oceanography
Data de publicació
2013-01-31
Volum
65
Número
20027
Projecte finançador
REGIMENES DE TRANSICION Y VARIABILIDAD EN LA DINAMICA Y LA QUIMICA DE LA BAJA TROPOSFERA
Repositori
http://hdl.handle.net/2117/17977 Obrir en finestra nova
URL
http://dx.doi.org/10.3402/tellusa.v65i0.20027 Obrir en finestra nova
Resum
Nocturnal precipitation cells and lines occur near the coastline in the whole Mediterranean basin in all seasons. The precipitation events are mainly located in areas where coastal mountain ranges and rivers enhance convergence though the interaction of nocturnal mesoscale and local flows (land breeze, katabatic and drainages winds) with prevailing synoptic wind or with other mesoscale and local flows. The methodology used here to study this phenomenon consists of three stages. First, the Tropic...
Citació
Mazon, J.; Pino, D. The role of sea-land air thermal difference, shape of the coastline and sea surface temperature in the nocturnal offshore convection. "Tellus. Series A, dynamic meteorology and oceanography", 31 Gener 2013, vol. 65, núm. 20027.
Grup de recerca
DF - Dinàmica de Fluids: formació d'estructures i aplicacions geofísiques

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