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Sea Breeze - an overview | ScienceDirect Topics The sea breeze fronts are evident in (a) along the north and south coasts of the island, and the convergence of the fronts prompts the development of more intense convection in the east, which develops, drifts in the environmental flow, and intensifies, forming an intense storm by 0515, which continues west and then dissipates
Sea Breeze - an overview | ScienceDirect Topics The sea breeze is an example of a flow generated by the relatively rapid generation of a baroclinic zone (density gradient) Warming of the land surface after sunrise is rapid, while the sea surface temperature remains almost constant, so the boundary layer inland becomes relatively warm over the space of a few hours This leads to a baroclinic overturning (Figure 3A) and the development of a
Segregation of sea breezes and cooling effects on land-surface . . . The cooling effect on land surface temperature decreases as the sea breeze wind direction shifts from northeast to south in Shanghai With urbanization, thermal environmental problems in coastal cities are becoming increasingly prominent Utilizing the cooling effects of sea breezes is an effective means of solving this problem
Cooling power of sea breezes and its inland penetration in dry-summer . . . In this study, we analyze sea breeze cooling capacity (SBCC) and propose a new method in estimating the penetration distance of sea breeze cooling in metropolitan Adelaide during summer using data from the Adelaide urban heat island monitoring network
Idealized large-eddy simulation study of interaction between urban heat . . . The sea breeze horizontally injects relatively colder air over the inland region and interaction between the sea-breeze flow and the co-occurring UHI convergent flow forms a severe stagnation region on the leeside of the UHI (Cenedese and Monti, 2003; Ooi et al , 2017; Wang et al , 2020)
Assessment of cooling effect of sea breeze under future climate based . . . As climate change continues, the heat balance mechanism of the urban space is expected to change as the sea breeze becomes hotter and more humid because of higher sea surface temperatures In addition, the amount of anthropogenic heat released is expected to increase because of increased cooling loads for air conditioning systems [28]
Long-term trend in the sea-land breeze in Hong Kong The average wind speeds of both the land and sea breezes declined rapidly The annual average decline rate for sea breeze wind speed is 2 30%, while for wind speed of land breeze, it is 1 37% The observed reduction in SLB energy in Hong Kong over the past 50 years may be associated with urbanisation