{"id":8368,"date":"2024-05-25T16:36:46","date_gmt":"2024-05-25T08:36:46","guid":{"rendered":"https:\/\/tommykwan.com\/blog\/?p=8368"},"modified":"2024-09-07T11:33:21","modified_gmt":"2024-09-07T03:33:21","slug":"whats-sea-breeze-and-land-breeze","status":"publish","type":"post","link":"https:\/\/tommykwan.com\/blog\/aviation\/whats-sea-breeze-and-land-breeze\/","title":{"rendered":"What’s Sea Breeze and Land Breeze?"},"content":{"rendered":"

NWS JetStream – The Sea Breeze (weather.gov)<\/a><\/p>\n

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Sea breeze and Land breeze are kind of convective current<\/strong><\/span><\/p>\n

Day time \u5730\u7403\u5438\u71b1\u662fgreenhouse effect<\/strong><\/p>\n

Night time \u5730\u7403\u653e\u71b1\u662fradiation cooling<\/strong><\/p>\n

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The sea breeze circulation is composed of two opposing flows; one at the surface (called the sea breeze) and one aloft (which is a return flow). These two flows are a result of the\u00a0difference<\/i>\u00a0in air density between the land and sea caused by the sun’s heating.<\/p>\n

The sun warms both the ground and ocean<\/strong> at the same rate. However, since the ground’s heat<\/strong><\/span> remains confined to the top few inches of soil it radiates back <\/strong><\/span>into the atmosphere warming the air. As the air warms, its density decreases creating a weak low-pressure area called a “thermal low” (1).<\/strong><\/p>\n

Over the adjacent water<\/strong><\/span> the cooler<\/strong><\/span>, more dense air<\/strong><\/span>, being pull down by gravity, begins to spread inland (2).<\/strong><\/span><\/p>\n

This inland push of air from the ocean undercuts the less dense air over land forcing it to rise (3).<\/strong> A sharp boundary develops due to the large difference between the air temperature over land and over water. This boundary, called a sea breeze front, acts in the same manner as the cold front we typically experience.<\/p>\n

For example, the air temperature drops significantly after the sea breeze front passes a location, sometimes as much as 15-20\u00b0F<\/abbr>\u00a0(8-11\u00b0C<\/abbr>). The skies also clear after the sea breeze front pass by. Another change that takes place with the passage of the sea breeze front is an increase in humidity. Finally, there can be a significant change in wind direction and\/or speed.<\/p>\n

Over land, air forced up by the sea breeze front will begin to cool.<\/strong> This cooling means the density increases<\/strong> again forming<\/strong> a small area of high pressure (4).<\/strong> Typically, this occurs from 3,000 to 5,000 feet (1,000 to 1,500 meters) in elevation. At this level the air pressure and density, being greater than the same elevation over the water, causes air to flow back over water (5).<\/strong><\/p>\n

Once over water again, the air cools, increases in density and sinks toward the earth’s surface (6).<\/strong> This enhances high pressure near the ocean’s surface (7)<\/strong> and the whole process repeats as land flowing air pushes the sea breeze front further inland. While the sea breeze is generally associated with the ocean, they can occur along the shore of any large body of water such as the Great Lakes.<\/p>\n

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Land breezes can occur when the land’s nighttime temperature is less than the sea surface temperature. They are most common during the fall and winter seasons when water temperatures are still fairly warm and nights are cool. However, unlike the sea breeze, the land breeze is often much weaker.<\/p>\n

At night, the land temperature falls<\/strong> <\/span>to below that of the ocean resulting in an increase in the air’s density.<\/strong> <\/span>Gravity’s downward pull moves air downhill spilling it onto the water (1).<\/strong><\/span> This denser air undercuts the lighter, warmer air over the water (2) forcing it up into the atmosphere (3).<\/strong> <\/span>This rising air forms a weak low-pressure area (4).<\/strong><\/p>\n

The rising air accumulates aloft forming an area of higher pressure (5). Relative to the land at the same elevation, air flows back toward land from high pressure to low pressure (6). Once back over land, the air cools, increases in density and then sinks causing an increase in density and high pressure (7). Gravity pulls the dense air offshore again completing the circulation.<\/p>\n

Land breezes are weaker than sea breezes but not because of the difference in heating. Daytime heating and nighttime cooling occur at about the same rate so the potential for both land and sea breezes to be the same strength exists. But at night,<\/p>\n