2.4/6.1 Flashcards

1
Q

How does Precipitation, light, temperature influence biomes?

A

Precipitation, light and temperature are influenced by latitude and longtitude which create distinct biomes.

Eg. Tropical rainforest have high temperatures and high precipitation
Deserts have high temperature but low precipitation
Tundra occurs where temperatures are low regardless of precipitation levels

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Catagory of biomes

A

Freshwater, marine, forest, grassland, desert and tundra. These characteritics all have abiotic limiting factors, productivity and diversity.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Limiting factor of rainforest

A

-Nutrient locked in biomass instead of soil
-Thin soil
-High productivty due to warm temperatures
-Highest biodiversity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

Limiting factor of Desert

A

-Little precipitation
-High evaporation
-Low productivity because H2O is needed for photosynthesis
-Low biodiversity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Limiting factor of tundra

A

-Slow nutrient cycle
-Photosynthesis is limited from frozen water
-Limited biodiversity because too cold for cold blooded species.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Longtitude

A

Vertical lines measuring distance east or west of the Prime Meridian (0°).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

latitude

A

Horizontal lines measuring distance north or south of the Equator (0°)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Seasonality of isolation

A

Changes in the amount of solar energy received at different times of the year due to Earth’s tilt.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Relationship between Seasonality of isolation and latitude

A

Higher latitude = Greater seasonal variation (more extreme summers and winters).
Lower latitude = Less seasonal variation (consistent temperatures year-round).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Natural greenhouse effect

A

Gases that trap heat naturally, maintaining Earth’s temperature (e.g., CO₂, CH₄, H₂O vapor, N₂O).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Anthropogenic greenhouse effect

A

Human-made gases increasing global warming (e.g., CO₂ from fossil fuels, CH₄ from livestock, CFCs from industry).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Tri-cellular Model

A

Global atmospheric circulation through three major convection cells in each hemisphere, driven by the uneven heating of Earth’s surface:

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Polar cells

A

Cold air sinks at the poles, moves toward 60°, rises again (creates polar easterlies).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Hardley Cells

A

Warm air rises at the equator, moves poleward, sinks at 30° (creates deserts & trade winds).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Feral cells

A

Acts like a conveyor belt, moving air between Hadley & Polar cells (creates westerly winds).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

How does wind affect ocean currents?

A

Trade Winds (0°–30°): Push warm water west (create Equatorial Currents).
💨 Westerlies (30°–60°): Push water east (help warm places like Europe).
💨 Polar Easterlies (60°–90°): Move cold water toward the equator (create cold currents).

17
Q

Nomal conditions without el nino

A

Trade winds blow from east to west across the Pacific Ocean.
These winds push warm surface water toward Australia and Southeast Asia, causing heavy rainfall there.
In the eastern Pacific (near South America), cold water rises from the deep ocean through upwelling, supporting marine life and fisheries.

18
Q

El nino

A

Trade winds weaken or reverse, so warm water stays in the central and eastern Pacific instead of moving west.
Without strong trade winds, upwelling stops, meaning less cold, nutrient-rich water reaches the surface near South America.
The Pacific Ocean becomes warmer than usual, disrupting global weather patterns.

19
Q

Impact of el nino

A

South America (Eastern Pacific):

Warmer ocean temperatures lead to heavy rainfall and flooding.
Fisheries decline due to reduced upwelling, affecting marine life.
Australia & Southeast Asia (Western Pacific):

Less warm water leads to droughts and wildfires.
Other Global Impacts:

Warmer global temperatures due to increased heat in the ocean.
Stronger hurricanes in the Pacific Ocean, but fewer hurricanes in the Atlantic Ocean

20
Q

Case Study

A

During El nino in New Zealand, there an frequency of wind from the west in summer, promoting dryness in eastern areas and more rain in the west. During winter, the winds blow more from the south, causing colder temperature across the country. Particularly in the east, the drier-than normal conditions in regions like Hawke’s bay and Canterbury reduces soil moisture and water availability.

21
Q

Climagraph: Trophic zones

A

regions between the tropics and polar zones (30°–60° latitude). They experience moderate temperatures and distinct seasons (winter, spring, summer, fall).

Example: United States (e.g., California, New York) and Europe (e.g., Germany).
Climate: Moderate rainfall and temperature ranges, suitable for agriculture.

22
Q

Climagraph: polar zones

A

located near the North and South Poles (60°–90° latitude). These areas are cold year-round, with very little sunlight in winter.

Example: Arctic and Antarctic regions.
Climate: Low temperatures, minimal precipitation (mostly snow), and long winters.

23
Q

Climagraph: Temperate zone

A

refer to the layers in an ecosystem, often related to how energy flows through food webs. I