Lecture 1 Flashcards
energy source that drives the circulation
the Sun! And the unbalanced distribution of the suns energy on the Earth.
Long term energy source of earth circulation
radioactive decay and its production of heat
wehy does wind occur?
horizontal movement and vertical movement caused by differences in pressure and mechanical reasons, vertica
Coriolis Effect
the apparent tendency for a fluid , moving across earths surface to be deflected from its straight-line path. North -South moving object would curve East or west- however, if we were to see this from space, it would appear to be travelling on a straight path (it depends on your frame of reference).
Distribution of surface winds
-Polar HIgh
-Polar Easterlies
-Subpolar low
-Westerlies
-Subtropical High
-Northeast Trades
-Intertropical Convergence zone
- Southeast Trades
Subtropical HIgh
- Westerlies
-Subpolar Low
-Polar Easterlies
-Polar HIgh
what is an ‘Easterly’ wind
wind that blows FROM the East to the west
Doldrums
Where winds are light and Frequently change direction, this happens at the equator
Cyclones
small areas of low pressure form due to pressure gradients and sue to higher processes in the troposphere. Air blow into the region and curves right, (In the north). Local circular flow - Cyclone.
Anticyclone
air flowing out of a high pressure region curveig to the right and causing a circular flow
Extra tropical cylones
Low pressure systems that form outside the tropics.
Warm and cold air attemt to mix- but there is extensive uplift of the warmer air as they do not mix easily. Results in formation of rain or snow
Geostropic Wind
BAlance of the Pressure GRadient Force and the force ue to the Coriolis Effect. Pressure gradient acts perpendicular to isobars in the direction of low pressure. . Coriolis effect is opposite to the is and the Geostrophic wind (Vg) is then parallel to Isobars.
Time when Earth is closest to the sun:
Perihelion
Time when Earth is furthest from the Sun
Aphelion
Obliquity
Angle of Earths spin axis relative to a line drawn perpendicular to the plane of the planets orbit around the sun. Earth = 23.5 degrees
Movement of ITCZ due to seasos
MAximum northwards position late in northern Hemisphere summer, and move down to South in the north hemisphere winter.