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Sea breeze

About: Sea breeze is a research topic. Over the lifetime, 2544 publications have been published within this topic receiving 55651 citations.


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Journal ArticleDOI
TL;DR: In this paper, the authors measured aerosols in the coastal zone and over the open sea in the Gdansk Basin (southern Baltic) during five campaigns at sea and 11 on land in 2001-2007.

27 citations

Journal ArticleDOI
01 Dec 2017
TL;DR: A field experiment was conducted on the northern Yucatan coast from April 1 to April 12, 2014 to investigate the role of intense wind events on coastal circulation from the inner shelf to the swash zone as discussed by the authors.
Abstract: A field experiment was conducted on the northern Yucatan coast from April 1 to April 12, 2014 to investigate the role of intense wind events on coastal circulation from the inner shelf to the swash zone. The study area is characterized by a micro-tidal environment, low-energy wave conditions, and a wide and shallow continental shelf. Furthermore, easterly trade winds, local breezes, and synoptic-scale events, associated with the passage of cold-fronts known as Nortes , are ubiquitous in this region. Currents were measured concurrently at different cross-shore locations during both local and synoptic-scale intense wind events to investigate the influence of different forcing mechanisms (i.e., large-scale currents, winds, tides, and waves) on the nearshore circulation. Field observations revealed that nearshore circulation across the shelf is predominantly alongshore-directed (westward) during intense winds. However, the mechanisms responsible for driving instantaneous spatial and temporal current variability depend on the weather conditions and the across-shelf location. During local strong sea breeze events ( W > 10 m s -1 from the NE) occurring during spring tide, westward circulation is controlled by the tides, wind, and waves at the inner-shelf, shallow waters, and inside the surf/swash zone, respectively. The nearshore circulation is relaxed during intense land breeze events ( W ≈ 9 m s -1 from the SE) associated with the low atmospheric pressure system that preceded a Norte event. During the Norte event ( W max ≈ 15 m s -1 from the NNW), westward circulation dominated outside the surf zone and was correlated to the Yucatan Current, whereas wave breaking forces eastward currents inside the surf/swash zone. The latter finding implies the existence of large alongshore velocity shear at the offshore edge of the surf zone during the Norte event, which enhances mixing between the surf zone and the inner shelf. These findings suggest that both sea breezes and Nortes play an important role in sediment and pollutant transport along/across the nearshore of the Yucatan shelf.

27 citations

Journal ArticleDOI
TL;DR: In this paper, two kinds of field observation are carried out to examine the cooling effects of a river and a sea breeze on the thermal environment in a built-up area in summer.

27 citations

Journal ArticleDOI
TL;DR: In this paper, the characteristics of the sea breeze circulation involved with circular and slab elongated-symmetric midlatitude islands were modeled and evaluated through a scale analysis, showing that the circulation characteristics of both types of islands become similar when the half-width of an island is about the same as the distance of inland penetration of a nonisland case.
Abstract: Model scaling of the characteristics of the sea breeze circulation involved with circular and slab elongated-symmetric midlatitude islands was performed. Larger horizontal and vertical velocities were indicated over the small circular islands as compared to those over corresponding elongated islands. The circulation characteristics of both types of islands become similar when the half-width of the island is about the same as the distance of inland penetration of the sea breeze in a nonisland case. Evaluation of the results through a scale analysis is presented.

27 citations


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Performance
Metrics
No. of papers in the topic in previous years
YearPapers
202383
2022192
2021101
202087
201978
201877