There are integrated meteorological observation IMO stations operated by SKTechX, that are used for observation of the horizontal distribution of surface meteorology. However, if there are larger scale atmospheric conditions also affecting the weather, then the sea breeze and sea breeze front can have a much larger impact on the type and intensity of weather one observes. To investigate the characteristics of surface meteorological variables when the sea-breeze front passes, an enhanced time series and a 1-min horizontal distribution were analyzed, respectively Figs. At night, the land temperature falls to below that of the ocean resulting in an increase in the air's density. This is a result of the Coriolis force having impact on the air flow. On two of these days, the inland penetration of the sea breeze front could be clearly traced.
Features of sea–land-breeze circulation over the Seoul Metropolitan Area
The contours were roughly parallel with the shoreline. J Meteorol Soc Jpn 73 6 — As such, sea breezes are more localised than prevailing winds. Availability of data and materials Data used in this study can be provided upon request. Through time—height cross-section wind analysis, the temporal and vertical regimes of sea- and land-breeze circulation could be checked. They play an important role on the local weather and air quality in a number of ways. Because land absorbs solar radiation far more quickly than water, a sea breeze is a common occurrence along coasts after sunrise.
Sea breeze - Wikipedia
To find the overall local circulation features, the period from 17 to 22 May , consecutively weak synoptic winds and less-cloudy conditions, was selected. The most inland area Station 7 showed the largest maximum and lowest minimum pressures, and, subsequently, the maximum daily sea-level pressure range. The offshore island Station 1 showed the lowest maximum sea-level PA and the highest minimum sea-level PA. Meanwhile, the eastern land regions exhibited a relatively high temperature, whereas the western sea regions exhibited a relatively low temperature between and LST Fig.
Description: This is mainly because the strength of the land breeze is weaker than the sea breeze. These were the major forces driving the sea—land circulation. Simpson JE Sea breeze and local winds, vol Categories : Marine meteorology and sailing Wind.