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Near - surface winds blow toward the oceancausingland breeze
the heating of the islandsmight createan onshore sea breeze
lower pressure ... in turncausesan onshore sea breeze
During the day , land heats to a much greater extent than does the oceancausingan onshore sea breeze
the air moving from the high pressure area over land to the low pressure area over the seacreatesland breeze
Thus the cool air from the land blows from the land towards the seacausingland breeze
Since wind blow from high to low pressure area , the wind blow from the land to the seacreatingland breeze
temperature differences between land and water(passive) caused byA land / sea breeze
Continue reading → Posted in Case study | Tagged doppler , fireworks , hurricane , swell tracking | Recent Posts Envisat services interrupted Swell wave products from ENVISAT Wide swath complex now available on SOPRANO Cold wave over Adriatic coastcausesland breeze
air circulation between the sea and landmass in the PRD estuary(passive) created bythe land - sea breeze
because land cools down more quicklycreatingland breeze
Enhanced convergence from several colliding outflow boundarieshas leadandthe sea - breeze
the temperature difference when the sea surface is warmer than the adjacent land(passive) caused byland breeze
ozone concentrations at coastal sitesalso influenceozone concentrations at coastal sites
These wind systems like(passive) are createdThese wind systems like
showers or even thunderstormscan causeshowers or even thunderstorms
during the night by cool air sinking over the land and warm aircreatedduring the night by cool air sinking over the land and warm air
air quality(passive) often influenced byair quality
convergence over convex coastline and divergence zone over a concave coastlinecreatesconvergence over convex coastline and divergence zone over a concave coastline
radiative cooling and advection(passive) caused byradiative cooling and advection
-cool denser air from H2O moves in -sea breeze(passive) is created-cool denser air from H2O moves in -sea breeze
a 10 to 15 °creatinga 10 to 15 °
the occurrence of nocturnal O3 maxima trough the transport of O3 from places where its concentrations were higherinfluencedthe occurrence of nocturnal O3 maxima trough the transport of O3 from places where its concentrations were higher
to the entrainment of burning plumes into the traveling air mass , which would explain the enrichmentmay leadto the entrainment of burning plumes into the traveling air mass , which would explain the enrichment
The manner in which temperature , humidity , and wind should behave(passive) is influenced byThe manner in which temperature , humidity , and wind should behave
The dispersion mechanism of pollutants in coastal zones(passive) is mainly influenced byThe dispersion mechanism of pollutants in coastal zones
severe atmospheric pollutioncan causesevere atmospheric pollution
reservoirs of pollutants that are brought back the following day ( Millán et al .creatingreservoirs of pollutants that are brought back the following day ( Millán et al .
as the land cools much faster than the seais createdas the land cools much faster than the sea
a vertical circulation(passive) solely caused bya vertical circulation