APES Test 4 Part 2 Flashcards
What is wind??
Vertical movement of air along surface
Pressure gradient!
Uneven Heating of Earth
Incoming solar radiation (insolation) is the Earth’s main source of energy
The angle of the sun’s rays determines the intensity of the solar radiation. Due to the shape of the Earth, the latitude that is directly horizontal to the solar radiation receives the most intensity.
The highest solar radiation per unit area is received at the equator and decreases toward the poles.
The solar radiation received at a location on the Earth’s surface varies seasonally, with the most radiation received during the location’s longest summer day and the least on the shortest winter day.
The tilt of Earth’s axis of rotation causes the Earth’s seasons and the number of hours of daylight in a particular location on the Earth’s surface.
High and Low Pressure
High and Dry!
High pressure is formed by cold air- this air is heavy- dense- and sinks down to the surface.
Low pressure is formed by warm air- warm air rises, carries moisture with it, usually leads to precipitation events- but this less dense warm air leads to lower pressure
We move from H to L
High pressure wants to fill in those lower density areas left in low pressure systems- so high pressure air masses move toward low pressure air masses- leading to wind!
Globally, winds want to move away from the poles
Why is this the general trend?
We will do a demo….
But- it is much, much more complicated than this- forming several bands on the earth with different prevailing winds
STUDY CONVECTION CELLS LOOK AT DIAGRAM AND LOOK AT VIDEO ABOUT WIND TRENDS AND CELLS
Coriolis Effect
We will do a demo and play with some inflatable globes
Remember that earth is rotating counterclockwise (eg- to the right when north is up)
This will have implications for how winds move across the earth
Hadley Cells
These are convection cells that are located between the equator, and 30 degrees north and 30 degrees south (there are two cells).
Warm air from equator rises, moves away from equator, as cold dense air from closer to the poles rushes in to fill its place
Polar Cells
Cold air moves away from the poles, warms up, rises, moves back toward the pole, cools, and sinks
Occurs at NP and SP to 60 degrees
Ferrel Cells- Indirect Circulation Cell
These are kind of confusing- but on a model of the earth with polar and hadley cells filled in, Ferrel cells essentially fill in the gaps and match the arrows up.
At 30 degrees north, Hadley cells are pulling down cold air- some of this cold air rushes to fill in the low pressure zone at the equator (forming the rest of the Hadley cell), but some other air rushes to fill in the low pressure zone that forms at 60 degree north, where low pressure is forming from polar air after it warms up
GLOBAL WIND PATTERNS
KNOW/MEMORIZE AND UNDERSTAND THIS LOOK AT DIAGRAM AND VIDEOS
Weather and climate are affected not only by the sun’s energy but by geologic and geographic factors, such as mountains and ocean temperature
Oceans-
Any large body of water is going to have a moderating effect on climate- that is, because water has a high specific heat, it is resistant to changes in temperature.
Ocean currents can have a large impact on ocean temperatures, too
Ocean currents (which we will not go over in detail) bring warm and cool water around the globe
There is some risk to oceanic current collapse in the future
Rain Shadow Effect
a patch of land that has been forced to become a desert because mountain ranges blocked all plant-growing, rainy weather. On one side of the mountain, wet weather systems drop rain and snow. On the other side of the mountain—the rain shadow side—all that precipitation is blocked.
windward vs. leeward sides
Watersheds
‘Watershed’ is an area of land where all precipitation will flow to a single body of water (river, basin, sea/ocean, etc.)
Watersheds are defined by what happens to precipitation.
What happens to precipitation?
In many ‘natural’ forest ecosystems, most rainwater is absorbed by soil and taken up by plants….
Rain is first captured by the forest canopy, where it slowly drips to the forest floor and is absorbed by soil.
In the absence of a canopy or vegetation to capture rainfall, the ground will quickly become too saturated and water will ‘run off’
Three Things happen to precipitation:
1) Canopy Interception and Evapotranspiration
Tree canopy and other vegetation intercepts rainfall. Much of this rainfall collects on leaves, where it slowly drips down or evaporates.
2) Soil Infiltration
Water, once it gets through the canopy, will infiltrate, or absorb into the soil
Shallow infiltration saturates the soil, providing plant life and soil organisms with moisture
3) Runoff
The remaining water will runoff, meaning it will move across the surface, to bodies of water