Sentence examples for breeze circulation from inspiring English sources

Exact(9)

The so-called sea and land breeze circulation is a local wind system typically encountered along coastlines adjacent to large bodies of water and is induced by differences that occur between the heating or cooling of the water surface and the adjacent land surface.

Circles in d, f indicate rough locations of the contour line around which the mountain valley breeze circulation occurs.

In a simulation of a sea breeze circulation, the new scheme gives a sharper sea breeze front.

We analyzed the impact on two distinct groups of convective cells triggered by the sea breeze circulation on August 24 2000 and compared the model simulated precipitation to RADAR data.

The typical values are observationally less than 102 km in the extratropics and theoretically given as the half horizontal wavelength using the gravity-wave dispersion relation, substituting the height of the sea land breeze circulation cell as the half vertical wavelength (internal case, latitude < 30°) (e.g., Rotunno 1983; Niino 1987).

Occurrences of brown clouds over the Himalayan foothills and Northern Indo Gangetic Plains have been identified by high aerosol optical depth (AOD) values >0.4 and are associated with high concentrations of pollutants measured at PYR, as characterized by an up-valley breeze circulation (Bonasoni et al. 2010).

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Similar(51)

Exactly how the MJO interacts with local processes, such as sea and land breeze circulations, to influence precipitation over the region is not well understood.

Further studies based on numerical experiments with the aid of atmospheric circulation models are needed to reveal the detailed physical mechanism by which the MJO interacts with local processes, such as the sea and land breeze circulations, to influence precipitation over the region.

Much higher resolution models (7 and 3.5 km grids) have simulated local clouds activated by an MJO causing a flood in the Malay Peninsula (Miura et al. 2007) and rainfall coupled with convergence of sea−land breeze circulations over the IMC (Sato et al. 2009).

From the dynamical characteristics of the area, sea-breeze circulation and channeling effects due to terrain features highly influence the location of the pollutant plumes.

This finding is related to the smaller frictional elements of the altered land cover located upon the axis of the seabreeze flow, which enhances the local sea-breeze circulation and its inland extent.

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