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A concise overview of local winds, focusing on sea breezes and land breezes. It explains the differential heating of land and sea, the timing and strength of sea breezes, and the effects of land breezes. Additionally, it touches on terrain channeling and its impact on wind patterns. This information is useful for understanding basic meteorological phenomena and their effects on local weather conditions. Structured as a series of key points, making it easy to review and understand the main concepts related to local winds and their behavior. It is a good resource for students studying meteorology or geography, as well as anyone interested in learning more about weather patterns.
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Sea Breezes - correct answer ✔✔Develop due to differential heating of land and sea Land Breezes - correct answer ✔✔Reverse of sea breeze, occur as land loses heat. Less powerful Specific Heat - correct answer ✔✔Land heats faster due to lower specific heat than water Sea Breeze Timing - correct answer ✔✔Starts mid-morning, peaks mid-afternoon Sea Breeze Strength - correct answer ✔✔Usually 10-15 knots, stronger in Spring Sea Breeze Extent - correct answer ✔✔Travels inland 25-50 km, up to 3000' vertically Sea Breeze Cloud Formation - correct answer ✔✔Cumulus clouds inland, clear skies towards coast Sea Breeze Precipitation - correct answer ✔✔Associated with cumulus clouds Sea Breeze Turbulence - correct answer ✔✔Dependent on circulation, off-shore air smooth Land Breeze Principle - correct answer ✔✔Occurs as land cools faster than sea at night Land Breeze Effects - correct answer ✔✔Creates localized down-draught and turbulence
Terrain Channelling - correct answer ✔✔Air forced through constriction by high ground