Sea breeze
Air over land is easily warmed —> cause reduction in pressure lapse rate eg pressure falls more slowly
Air over sea is colder —> pressure decreases more quickly
Transfer of air 1000ft above ground level outwards from land to sea = pressure increase over sea and pressure decrease over land
Air then flows back from sea to land due to PGF
Sea breeze deflection in northern hemisphere
Sea breeze initially blows at 90 degrees to the coastline.
as the PGF gradually increases the speed increases
As the Coriolis effect increases, (CF proportional to wind speed)the wind will veer in the N Hemisphere
In the S Hemisphere the wind will back
Land breeze
Air over sea is warm = reduction in pressure lapse rate eg pressure falls more slowly
Leading to higher pressure compared to pressure of cold land
Hence transfer of air from sea towards land - > surface pressure over sea decreases and increases over land
Air then moves back from land —> sea
Anabatic wind ‘valley breeze’
Wind which blows upwards in a mountainous area
Due to daytime heating of hillside slopes causing air to heat up and rise
‘Ana’ meaning rising
Katabatic wind ‘mountain breeze’
Develops during night with radiative cooling of hillside slopes causing air to cool and descend
‘Kata’ meaning descend
The bora
Katabatic wind
affecting the Adriatic Sea
Strongest in winter
Winds can exceed 100kts
The mistral
Valley wind
Blows from the north along the Rhone valley; often due to high pressure in the Bay of Biscay causing a northerly flow to affect central/southern France
Alps and Massif Central create a natural venturi which accelerates the air
Strongest in winter, a very cold wind with speeds up to 70kts
Föehn winds
STABLE AIR MASS REQUIRED
Cloud forms on the windward (upwind) side of mountain
Precipitation on the windward slope removes moisture from the airmass, causing the DP temp to be reduced = clouds are produced
Warm dry descending wind on the downwind side of a mountain
Eg chinook
Pampero
burst/advance of cold polar air from the south
Blows across the pampas of South America as a S/SW wind