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Syeda Rafiq, Charitha Pattiaratchi and Ivica Janekovic
The land?sea breeze (LSB) system, driven by the thermal contrast between the land and the adjacent ocean is a widely known atmospheric phenomenon, which occurs in coastal regions globally. South-west Australia experiences a persistent and one of the stro...
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Shangfei Hai, Yucong Miao, Lifang Sheng, Linbo Wei and Qing Chen
During the past few decades, rapid economic development occurred in Qingdao. Inevitably, human activities have caused great changes to the underlying surface, including urbanization and coastal change. Coastal change mainly refers to the expansion of the...
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Riccardo Martellucci, Alberto Pierattini, Francesco Paladini De Mendoza, Cristiano Melchiorri, Viviana Piermattei and Marco Marcelli
Coupling between sea/land breeze and coastal circulation and the influence of wind-driven dynamics are substantially relevant for understanding coastal Mediterranean ecosystems. These coastal areas are particularly dynamic and are characterized by high-v...
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N. S. PANCHAL
This study discusses the climatological characteristics of sea/land breeze systems and their influence on meteorological parameters at Kalpakkam, Madras Atomic Power Project site on the east coast of India. Continuous data recorded at the meteorologi...
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Ascario Pérez,Juan Carlos Ortiz,Luis F. Bejarano,Luis Otero D.,Juan C. Restrepo L.,Andrés Franco H.
Pág. 389 - 406
Circulation of sea breeze is a well-known and important mesoscale system, boosted by different properties of reception and storage of solar heat between land and sea during one day, and its effect on waves, currents, and transport of atmospheric contamin...
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Abigail Dah, Boualem Khouider and Courtney Schumacher
Coastal convection is often organized into multiple mesoscale systems that propagate in either direction across the coastline (i.e., landward and oceanward). These systems interact non-trivially with synoptic and intraseasonal disturbances such as convec...
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Miho Kiriya, Tomoaki Okuda, Hana Yamazaki, Kazuki Hatoya, Naoki Kaneyasu, Itsushi Uno, Chiharu Nishita, Keiichiro Hara, Masahiko Hayashi, Koji Funato, Kozo Inoue, Shigekazu Yamamoto, Ayako Yoshino and Akinori Takami
Observation of the ambient aerosol surface area concentrations is important to understand the aerosol toxicity because an increased surface area may be able to act as an enhanced reaction interface for certain reactions between aerosol particles and biol...
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Jordi Mazon and David Pino
Using the Weather Research and Forecasting (WRF) ? Advanced Research WRF (ARW) mesoscale model (WRF?ARW), we investigate how two nocturnal offshore rainbands occurring in the Mediterranean basin are modified in a warmer sea surface temperature (SST). Aft...
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Miguel A. Cahuich-López,Ismael Mariño-Tapia,Alejandro José Souza,Gerardo Gold-Bouchot,Mark Cohen,David Valdés-Lozano
Pág. 123 - 142
The balance between synoptic and sea breeze atmospheric phenomena can profoundly influence atmospheric circulation in coastal regions. In this paper, a comprehensive study to understand the quasi-permanent patterns of such variability over the surface wi...
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C. FERNÁNDEZ,M. CASTRO
A two-dimesional hydrostatic mesometeorological model has been applied to analyze a typical atmospheric local circulation observed in anorthern zone of the iberian peninsula during the summer. by means of two model simulation with different land-use type...
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Hyun-Goo Kim, Jin-Young Kim and Yong-Heack Kang
This study evaluated the applicability of long-term datasets among third-generation reanalysis data CFSR, ERA-Interim, MERRA, and MERRA-2 to determine which dataset is more suitable when performing wind resource assessment for the ?Southwest 2.5 GW Offsh...
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C. AZORIN MOLINA,J. MARTÍN VIDE
This study examines the degree of persistence in the sea-breeze in Alicante. This research is based upon the sequence of semi-hourly data for wind direction and speed for the five-year period from 1999 to 2003 (database of sea b...
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C. AZORIN MOLINA,S. SÁNCHEZ LORENZO,J. CALBO
Sea breezes blow under anticyclonic weather types, weak surface pressure gradients, intense solar radiation and relatively cloud-free skies. Generally, total cloud cover must be less than 4/8 in order to cause a thermal and pressure difference betwee...
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