Intro (The Climatic Influence of Ocean Currents) Flashcards
The water of the oceans is in perpetual state of circulatory motion driven by ______.
convection
Has a large effect on climate, particularly in Europe
oceanic conveyor belt
- This motion is partly initiated by subsidence of water in _______.
- Water ____ because of its _______ (low temperature, high salinity)
- North Atlantic
- sinks, high density
When water freezes, it contains about____________ of a percent salt. It leaves behind a _____ amount of salt in the water. When this ______ the salinity of the surrounding ocean water and thus ______ its density.
- five tenths
- considerable
- increases (same answer)
Great Ocean Conveyor Belt
- North Atlantic: ______ because of its relatively high density (due to ____ and ______)
- water sinks, low temperature and high salinity
Great Ocean Conveyor Belt
- Indian and Pacific Oceans: water is warmed by the ___ –> becomes ____ –> ______ to the surface
- The return to the ____ (at the surface, as “surface currents”) and bring warm water into otherwise ______.
- sun, becomes warmer, rises
- North, cold seas
Winds blowing across the _______ transfer a significant degree of warmth to the surrounding countries.
- Annual amount of heat absorbed from the conveyor belt is almost ____ as much as the heat received from the sun in this location.
- The counties in this location is ____ than they would be without the ____.
- North Atlantic
- one-third
- 8C warmer, conveyor belt.
As prevailing winds blow across the oceans some of their kinetic energy is transferred to the water, producing the great surface currents of the world.
Wind-blown surface currents
- Rotation of the earth influences the paths of the currents: _____
- North of equator: ______
- South: _____
- circular flows
- clockwise
- anti-clockwise
Tropospheric airflow
- primary circulation, _______ movements
- ___ and ___ are also recognized; e.g. smaller-scale phenomena covering distance < ______
- large-scale
- 2° and 3°, 160 km
Tropospheric airflow
- three forces influencing circulation
1. (main driving force)
2. (decreases speed)
3. (deflects direction)
- The pressure gradient
- The frictional force
- The Coriolis force
________
- A force generated by a difference in pressure
- A fluid tends to move from ________ region to ______ region
Pressure gradient force
- high pressure, low pressure
Deflection, depending on
which hemisphere you are:
north, right; south, left
The Coriolis force
The direction of _______ as a consequence of Coriolis force
airflow deflection
________
- a force that tends to dissipate the energy of a moving body (moving surface air transfers some of its energy to the Earth’s surface -> velocity of air is reduced)
- it acts in the direction _____ the direction of surface air movement
Frictional Forces
- opposite
The result of the forces causing airflow
Tropospheric airflow
Three cell model of primary air circulation
- The Hadley Cell
- Polar Cell
- Ferrel cell
_______
- Cold air at the pole sinks -> high
pressure areas at the north and
south poles.
- -> divergent flow at the surface
(to balance the incoming flow of
sinking cold air); air moves equatorwards (becoming easterly
because of Coiolis force)
Polar Cell
_______
- At the divergent zone: the
equatorwards surface air
(easterlies) is part of hadley cell.
- The poleward surface air
(westerlies) meets the
equatorwards surface air
(easterlies) of the polar cell. ->
______.
Ferrel cell
- low pressure 60° convergence
Average surface wind directions
Tropospheric airflow
- Three-cell model: Within each cell, the flow ____(upper air flow) must be in the opposite direction to
that in the ground (surface air flow). - Within the ___ (mid-latitude) cell in the north, the upper air flow must be ___, opposite to the westerly poleward surface air flow.
- But the predominant upper air flow is westerly. -> ____ (very high speeds)
- This is know to be present in both the ___ and ____ hemisphere.
- aloft
- Ferrel, easterly
- jet streams
- north, south
Two essentially circumpolar jet streams within the mid-latitude region
- subtropical jet stream
- polar front jet stream
Not truly circular about either pole: wave-like -> ____
Rossby waves
A _____ is an area of strong winds ranging from ____
mph that can be thousands of miles long, a couple of hundred
miles across and a few miles deep.
- jet stream
- 120-250
Jet streams usually sit at
the boundary between the troposphere and the stratosphere at a level called the ____ about____ off the ground.
- tropopause
- 6-9 miles
A jet stream forms directly over the _____of the strongest area of horizontal temperature difference, or the ____.
- center, front
As a general rule, a ____ has a jet stream directly above it that is ___ to it.
- strong front, parallel
- The ___ sits at roughly 60°N latitude because this is generally where the ____ sits.
- The _____ is at roughly 30°N latitude. The _____ is located at 30°N because of the temperature differences between ____ at mid-latitudes and the______.
- polar jet, polar front
- subtropical jet (same answer for two blanks), air, warmer equatorial air.