chapter 2 Flashcards

1
Q

Why does the earth have seasons?

A

Due to the tilt of the earth’s axis. As the Earth revolves around the sun, this tilt means that different parts of the planet receive more direct sunlight at different times of the year, creating seasons

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2
Q

Explain why the Northern and Southern Hemispheres do not experience the same seasons at the same time.

A

Because when the Northern hemisphere is tilted towards the sun, the South hemisphere is tilted away from it and vice versa.

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3
Q

Explain why the equator generally has warmer temperatures than the poles.

A

Because the earth is a sphere, the sunlight hitting the equator is much more intense

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4
Q

Explain differences in length of day at different latitudes at different times of year. (Ex: Today, Bellevue will have 9 hours, 39 min of sunlight, but Phoenix, Arizona will have 10 hours, 40 min. of sunlight. Why is this so?)

A

Additionally, the days become a little longer at the higher latitudes (those at a distance from the equator) because it takes the sun longer to rise and set.

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5
Q

Explain why the amount of daylight changes throughout the year (shorter days in winter, longer in summer).

A

As the tilt of the earth towards the sun, the amount of sunlight received at a given point changes

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6
Q
  • Explain how and why the path of the Sun changes in the sky from one season to the next.
A

During summer in the northern hemisphere, the Sun rises north of east and sets north of west. It is high in the sky at noon. During winter in the northern hemisphere, sunrise and sunset appear farther south along the horizon.

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7
Q

Differences between weather and climate

A

Weather is short term, climate is more long term trends

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8
Q

How the tilt of the earth impacts climate on earth

A

Impacts seasons, causes more extreme seasonal variation closer to the poles

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9
Q

How wind patterns and the atmosphere influence climate

A

Redistribute heat and water

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10
Q

How ocean currents impact climate

A

Transporting warm water and precipitation from the equator toward the poles and cold water from the poles back to the tropics.

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11
Q

How does topography impact climate

A

Bodies of water – milder climates, absorb solar radiation and very slowly emit it
Mountainous – more extreme weather, block movement of air and moisture

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12
Q

Coriolis Effect and how it affects the movement of air currents on Earth

A

air moving in a straight path appears to curve to the right in the Northern Hemisphere and to the left in the Southern Hemisphere due to the earth’s rotation. causes large scale wind patterns that impact the formation of hurricanes

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13
Q

Convection currents in air (atmosphere) and water (oceans), considering changes in temperature, density, and pressure

A

Warmer, less dense air/water rises, and cooler, more dense air/water sinks, causing circular patterns.

In the air: cause large scale wind patterns (e.g. hadley cells, polar cells) and impact climate. There is a pressure diff between high pressure cold air and low pressure hot air zones, the stronger the pressure diff the stronger the winds

In the water: create cold currents in the deep ocean and warm surface currents

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14
Q

Hadley cells

A

Convection currents
Located between equator and 30 degree latitude
Hot air rises after gaining lots of heat from solar radiation, creating a low pressure zone at the equator. This air travels towards the poles and cools and sinks at lat. 30 degrees, creating low pressure zones.
This creates trade winds and contributes to the formation of rainforests at the equator

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15
Q

Ferrel cells

A

Mid-latitude atmospheric circulation cell (30-60) where air near the Earth’s surface flows poleward and eastward, while at higher altitudes it moves equatorward and westward. opposite of hadley cells.
responsible for the prevailing westerly winds in those regions.
unstable weather conditions like mid-latitude cyclones and fronts due to the mixing of warm and cold air masses.

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16
Q

Polar cells

A

Low intensity convection currents (60-70 lat)
Air rises at higher latitudes and travels towards the poles. Sinks and creates polar high pressure zones (polar highs)
Creates east-blowing surface winds. Low-pressure systems that bring rain to temperate regions.

17
Q

Types of weather seen with low pressure systems vs. high pressure systems

A

Low pressure systems are typically associated with cloudy, rainy, and sometimes stormy weather, while high pressure systems bring clear skies, dry conditions, and light winds

18
Q
  • Rain shadows- what they are, what to expect on windward vs. leeward side of the mountains
A

A “rain shadow” is a dry area on the leeward side of a mountain rang (side opposite the prevailing winds). Wetter windward side; essentially, the mountains “cast a shadow” of dryness on the leeward side.

19
Q

Ocean currents are driven by wind, Coriolis effect, gravity, temperature, salinity, and topography (shape and location of the land/continents)

A

Wind directly pushes the surface layer of the ocean, creating initial movement and setting the direction of surface currents.
This force, caused by Earth’s rotation, deflects moving water to the right in the Northern Hemisphere and to the left in the Southern Hemisphere, influencing the overall path of ocean currents.
Gravity plays a role in density differences within the ocean, causing denser water to sink and less dense water to rise, which contributes to vertical circulation.
Differences in temperature and salinity create density variations in the water, further impacting vertical movement and influencing the direction of surface currents.
The shape and location of the ocean floor and landmasses can obstruct or redirect ocean currents, creating gyres and other large-scale circulation patterns.

20
Q

Gyres, connection to garbage patches

A

Large, circular ocean currents. Act as whirlwinds to pull garbage in

21
Q

Upwelling- how it occurs and why it is an important phenomenon

A

Upwelling is an oceanographic process where deep, cold water rises to the surface, typically driven by winds pushing surface water away from the coast, which then gets replaced by nutrient-rich water from below, creating a vital food source for marine life and making upwelling regions highly productive fishing grounds; this is considered an important phenomenon because it significantly contributes to the base of the marine food chain by bringing essential nutrients to the surface layer

22
Q

How terrestrial biomes are defined (which factors are used to categorize the biomes)

A

Temp, precipitation, vegetation

23
Q

Tundra

A

Extremely cold temperatures, low precipitation + productivity, short growing season, permafrost, a lack of trees, and simple vegetation consisting mainly of low-lying shrubs, grasses, mosses, and lichens. Found at high lats and arctic regions

24
Q

Taiga (Boreal forest)

A

Very cold winters with significant snowfall
Short, mild summers. Moderate precipitation. Mostly coniferous evergreen trees like spruce, fir, and pine. Poor soil conditions – thus low productivity relative to other forests. High lats

25
Q

Temperate rainforests

A

Mild temperatures, heavy rainfall, and a long growing season. Mid latitudes. High productivity

26
Q

Temperate seasonal forest

A

Experiences distinct seasons and is characterized by broadleaf trees that lose their leaves in the fall. Moderate temps and rainfall

27
Q

woodland/shrubland

A

Small trees and shrubs, and is found in areas with a variety of climates and soil types. Hot dry summers and mild/wet winters. Moderate precipitation (more than deserts but less than forested areas). Poor productivity.

28
Q

Temperate grassland/cold desert

A

Cold winters, hot summers, and some rain (moderate to low) that supports grasses and nonwoody flowering plants. Large temp fluctuations. More productive than deserts but not great.

29
Q

Tropical rainforest

A

A hot, wet biome with dense vegetation and heavy rainfall that occurs near the equator. Highest productivity.

30
Q

Tropical seasonal forest/savanna

A

Grasslands with scattered trees that develop in areas where seasonal forests or woodlands would normally grow, but certain factors prevent the establishment of those trees. Savannas are characterized by a hot, tropical climate with a long dry season and a short wet season. Some precipitation in wet season. Variable productivity

31
Q

Subtropical desert

A

A subtropical desert is a hot, dry biome with low annual rainfall, high winds, and warm soil. Low productivity

32
Q

How aquatic biomes are defined, which factors are used to categorize them

A

Sunlight availability, water depth, salinity levels, water flow, temperature, and dissolved oxygen concentration

33
Q

Streams and rivers

A

Flowing bodies of water that move in one direction, originating at a high point and traveling downhill. Typically starting from a source like a spring or snowmelt, and carrying sediment as they erode the land, shaping their channels as they flow towards a larger body of water like a lake or ocean.

34
Q

Ponds and Lakes

A

Ponds and lakes are both bodies of freshwater, but ponds are generally smaller and shallower than lakes. Both are surrounded by land. Lakes are usually too deep for plants to grow on the bottom, while ponds are shallow enough for sunlight to reach the bottom and plants to grow.

35
Q

Freshwater wetlands

A

Characterized by water-saturated soil, shallow water bodies, and vegetation specifically adapted to moist conditions. High productivity and nutrient dense – high biodiversity.

36
Q

Salt marshes, including estuaries

A

Salt marshes are spongy areas with water that ranges from freshwater to salt-saturated. They are dominated by salt-tolerant plants An estuary is a partially enclosed body of water where freshwater from rivers mixes with salt water from the ocean

37
Q

Mangrove swamps

A

Coastal wetlands that are home to a variety of specialized plants and animals that can survive in the brackish to saline waters and extreme conditions of these environments

38
Q
A