ze fine sea breeze and land breez?
Answers
Answer:
Land breeze blows during the night from land to sea and the land becomes cooler faster than the sea. The air above the sea becomes less dense (i.e. warmer) and rises. The cooler air from the land moves in to take its place. Sea breeze: Sea breeze blows during the day and the land heats up faster than the sea.
Explanation:
Answer:
A sea breeze is a coastal wind generated by the differential heating of the land and the water (Estoque, 1961; Rotunno, 1983). When the land is at a higher temperature than the neighbouring water, the air above it is heated and rises. The air at lower levels is replaced by cooler air advected from the adjacent ocean areas. Coastal temperatures are regularly impacted by sea breezes. If an offshore flow exists when a sea breeze forms, then there will be a region where the two opposing surface winds meet and are forced to ascend; this region is called a sea breeze front (Simpson et al., 1977). If there is enough moisture in the atmosphere, clouds and precipitation can form.
Sea breezes typically impact the land within some tens of kilometres of the coastline, a scale much too small to be resolved in today’s global models. They are consistently occurring phenomena that can result in the coastal climate being several degrees cooler in summer than nearby inland areas, as well as having higher levels of precipitation. While sea breezes affect all coastlines to some degree, there are locations where the effect is larger, often because of the geometry of the coastline. Long, relatively thin peninsulas and islands can form sea breezes from opposing sides that will converge, greatly enhancing the potential for precipitation (Figure 9.4). The inter-relationships between sea breezes, the boundary layer, and larger-scale convection were studied during MCTEX in 1995 (Keenan et al., 2000; Schafer et al., 2001).
Explanation:
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