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Geography flashcards
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Card 1
Why does the monsoon and trade-wind coastal climate experience a strong wet season when the ITCZ is nearby?
The Intertropical Convergence Zone (ITCZ) is a belt of low pressure where the trade winds from the Northern and Southern Hemispheres converge. When the ITCZ is nearby, it brings warm, moist air masses, leading to significant uplift and condensation, which results in abundant rainfall characteristic of the wet season in these regions.
Card 2
Distinguish between the causes of wet periods in equatorial east coasts and tropical south/west coasts within the monsoon and trade-wind coastal climate.
Equatorial east coasts receive warm, moist air masses primarily from easterly trade winds, which bring consistent moisture. In contrast, tropical south and west coasts experience wet periods due to moist air from southwesterly monsoon winds, which are driven by seasonal shifts in temperature differences between land and ocean.
Card 3
How does the dry tropical climate sustain its characteristic lack of rainfall and high temperatures during the high-sun season?
The dry tropical climate is situated in the belt of persistent subtropical high pressure, which is characterized by sinking air that inhibits cloud formation and precipitation. During the high-sun season, the intense solar insulation, combined with the lack of cloud cover, leads to very high surface temperatures and minimal rainfall.
Card 4
Explain the primary difference in temperature cycles between the wet equatorial climate and the dry tropical climate, and the reasons behind it.
The wet equatorial climate exhibits very little temperature difference throughout the year due to consistent cloud cover and abundant rainfall, which moderate daily and annual temperature fluctuations. Conversely, the dry tropical climate shows a strong annual temperature cycle with very high temperatures during the high-sun season and cooler temperatures during the low-sun season, largely due to clear skies allowing maximum solar heating and radiation loss.
Card 5
Why do Midlatitude climates exhibit a strong variation in temperature and/or precipitation throughout the year?
Midlatitude climates are characterized by the interaction of tropical and polar air masses, which gives rise to traveling cyclones, anticyclones, and frontal boundaries. This dynamic atmospheric activity, along with seasonal shifts in solar radiation, results in significant variability in both temperature and precipitation patterns over the course of a year.
Card 6
Describe how the dry subtropical climate differs from the dry tropical climate, specifically regarding low-sun season temperatures.
While both are dry, the dry subtropical climate experiences cooler temperatures during its low-sun season compared to the dry tropical climate. This cooling is primarily due to the invasion of continental polar air masses into the subtropical region, which do not typically reach the more equatorial dry tropical zones.
Card 7
Explain the dual mechanisms that provide abundant precipitation to the moist subtropical climate during both summer and winter.
In summer, warm, moist maritime tropical air masses provide convective showers to the moist subtropical climate. In winter, midlatitude cyclones are the primary source of precipitation, bringing rain and occasional snow. This combination ensures abundant rainfall throughout the year.
Card 8
Why does the Mediterranean climate experience a dry summer despite being along midlatitude west coasts, which typically receive oceanic moisture?
During summer, the Mediterranean climate is dominated by dry subtropical high pressure, which moves poleward and blocks rainfall. This high-pressure system suppresses convection and prevents the formation of precipitation, leading to characteristically dry summers.
Card 9
How does the orographic effect enhance precipitation in the marine west-coast climate?
The orographic effect enhances precipitation in the marine west-coast climate as moist air masses from the ocean are forced to rise over coastal mountain ranges. As the air ascends, it cools, condenses, and leads to increased cloud formation and rainfall on the windward slopes.
Card 10
What factors contribute to the low precipitation and large annual temperature variation characteristic of the dry Midlatitude climate?
The dry Midlatitude climate is found in continental interiors, often in rain shadows of mountain ranges or far from oceanic moisture sources. These geographical factors limit access to moist air, resulting in low precipitation. The continental location also leads to a large annual temperature variation due to the absence of moderating oceanic influence.
Card 11
Why does the moist continental climate exhibit highly variable weather, particularly in the polar-front zone?
The moist continental climate is situated in the polar-front zone, where cold polar air masses frequently clash with warm tropical air masses. This constant interaction generates numerous frontal systems, traveling cyclones, and anticyclones, leading to highly variable and often rapidly changing weather conditions.
Card 12
Describe the primary difference in winter conditions between the boreal forest climate and the tundra climate, despite both being high-latitude climates.
The boreal forest climate experiences long, bitterly cold winters dominated by cold, dry continental arctic and polar air masses. In contrast, the tundra climate, while also very cold, has its winter temperatures moderated by maritime influence, preventing them from falling to the extreme levels seen in the boreal forest climate.
Card 13
What is the fundamental difference between ecological biogeography and historical biogeography?
Ecological biogeography examines how the current distribution patterns of organisms are affected by their physiological needs and interactions with the present environment. Historical biogeography, on the other hand, investigates how these spatial distribution patterns have evolved and arisen over geological time and space, considering factors like continental drift and past climate changes.
Card 14
Explain how human activity specifically impacts the carbon cycle, leading to climate change.
Human activities, primarily the burning of fossil fuels and deforestation, release large amounts of carbon dioxide into the atmosphere. This increases the concentration of CO2 in the atmospheric storage pool, enhancing the greenhouse effect and trapping more heat, which is a significant driver of current climate change.
Card 15
Why is nitrogen, despite being abundant in the atmosphere, not directly assimilable by most plants and animals, and what process addresses this?
Nitrogen in the atmosphere (N2) is in a stable diatomic form that most organisms cannot directly utilize. The process of nitrogen fixation, primarily carried out by certain soil bacteria and blue-green algae, converts atmospheric nitrogen into usable forms like ammonia, making it accessible to plants and subsequently to animals.
Card 16
Distinguish between the concepts of a species' 'habitat' and its 'ecological niche'.
A species' habitat refers to the specific physical environment where it lives and carries out its activities, such as a forest, desert, or aquatic ecosystem. Its ecological niche, however, describes the species' role and position within that ecosystem, encompassing how it uses resources, its interactions with other organisms, and its impact on the environment.
Card 17
How do xerophytes adapt to cope with the scarcity of water in dry and hot environments?
Xerophytes employ various adaptations to survive in arid conditions. Phreatophytes develop deep roots to reach groundwater, succulents store water internally in spongy tissues, and sclerophylls have hard, leathery leaves to reduce water loss through transpiration.
Card 18
Define and differentiate between the concepts of 'resistance' and 'resilience' in an ecosystem.
Resistance is the ability of an ecosystem to remain largely unchanged or withstand disturbances without significant alteration. Resilience, conversely, is the capacity of an ecosystem to recover and return to its original state or a similar stable state after a disturbance has occurred.
Card 19
Why is high biodiversity often associated with greater ecosystem stability?
High biodiversity contributes to greater ecosystem stability because a diverse array of species often means a wider range of functional roles and redundancies within the ecosystem. If one species is affected by a disturbance, others can often compensate, making the overall system more robust and less prone to collapse.
Card 20
What is desertification, and in what specific types of areas does it primarily occur?
Desertification is the degradation of land, leading to reduced biological productivity and loss of fertile soil. It primarily occurs in arid, semi-arid, and dry sub-humid areas, often exacerbated by human activities such as overgrazing, deforestation, and unsustainable agricultural practices.
Card 21
Explain why the wet-dry tropical climate is characterized by savanna woodland vegetation.
The wet-dry tropical climate features a very dry season alternating with a very wet season. This seasonal precipitation pattern supports savanna woodland, a sparse cover of trees over grassland, as the trees can survive the wet season but are too widely spaced to form a dense forest due to the stress of the prolonged dry season.
Card 22
How do midlatitude wave cyclones contribute to rainfall in the dry subtropical climate, particularly during certain months?
In the dry subtropical climate, midlatitude wave cyclones, especially those on a southerly path, can bring significant rainfall during December through March. These cyclones transport moist air from oceanic sources inland, providing a distinct wet period despite the overall aridity of the climate.
Card 23
What role do maritime tropical air masses play in the summer precipitation of the moist continental climate?
In the moist continental climate, maritime tropical air masses enhance summer precipitation. These warm, moist air masses, when interacting with moving cold fronts and squall lines, provide the necessary moisture and instability for the formation of thunderstorms, leading to a summer maximum in rainfall.
Card 24
Why does the ice sheet climate record the lowest temperatures on Earth, and what is its defining temperature characteristic?
The ice sheet climate records the lowest temperatures on Earth due to its extreme high latitude, high elevation, and the presence of vast, reflective ice sheets that minimize solar absorption. Its defining temperature characteristic is that no month has a mean temperature above freezing, with winter mean monthly temperatures often around -40 degrees Celsius.
Card 25
How does the annual temperature range of Madison, Wisconsin, reflect the characteristics of a moist continental climate?
Madison, Wisconsin, located in a moist continental climate, exhibits a large annual temperature range with cold winters (three consecutive months below freezing) and warm summers. This range is a direct result of its continental interior location, which lacks the moderating influence of large bodies of water, allowing for significant seasonal temperature extremes.
Card 26
Define the concept of 'ecological niche' and explain how it differs from a species' 'habitat'.
The ecological niche describes the role and position of a species within an ecosystem, encompassing how it utilizes resources, interacts with other organisms, and influences its environment. In contrast, a species' habitat refers specifically to the physical environment where it lives and carries out its activities. While habitat is 'where they live,' the niche is 'how they live'.
Card 27
Explain the fundamental difference between C3 and C4 plants in terms of their photosynthetic pathways and adaptation to environmental conditions.
C3 plants form a three-carbon compound as the first product of carbon fixation, with CO2 fixed directly into the Calvin cycle. They exhibit strong photorespiration and lower photosynthetic efficiency, adapting to cool and moist environments. C4 plants, however, form a four-carbon compound first, fixing CO2 in mesophyll cells before transporting it to bundle sheath cells. They have weak photorespiration, higher efficiency, and are adapted to hot and sunny environments.
Card 28
How do xerophytes adapt to dry and hot environments, and what are three distinct examples of such adaptations?
Xerophytes are plants specifically adapted to survive in dry and hot environments by minimizing water loss and maximizing water uptake or storage. Three examples of adaptations include phreatophytes, which possess deep roots to access groundwater; succulents, which store water internally in spongy tissues; and sclerophylls, characterized by hard-leaved evergreen trees and woody shrubs that reduce transpiration.
Card 29
Distinguish between the concepts of 'resistance' and 'resilience' in the context of ecosystem stability.
Resistance refers to an ecosystem's ability to remain unchanged or largely unaffected when a disturbance occurs. Resilience, on the other hand, is the capacity of an ecosystem to recover and return to its original state or function after being subjected to a disturbance. A highly resistant ecosystem might not change much, while a highly resilient one can bounce back quickly.
Card 30
Explain the significance of the carbon cycle in relation to climate change and how human activities impact this cycle.
The carbon cycle is crucial for climate change because carbon flows among storage pools in the atmosphere, ocean, and land, with carbon dioxide being a major greenhouse gas. Human activities, particularly the burning of fossil fuels and deforestation, significantly increase carbon dioxide concentrations in the atmospheric storage pool, leading to enhanced greenhouse effect and global warming.
Card 31
Describe the concept of net primary production (NPP) and identify the ecosystems with the highest and lowest NPP, along with the key climatic factors influencing it.
Net primary production (NPP) is the rate at which primary producers accumulate carbohydrate, representing the energy available to higher trophic levels. Equatorial rainforests and freshwater swamps/marshes are among the most productive ecosystems, while deserts are the least productive. The most important climatic factors controlling NPP are day length, air and soil temperature, and water availability.
Card 32
Compare and contrast Lamarck's inheritance of acquired traits with Darwin's theory of natural selection.
Lamarck's theory proposed that organisms could pass on traits acquired during their lifetime to their offspring, suggesting a direct inheritance of characteristics developed through use or disuse. In contrast, Darwin's theory of natural selection posits that species evolve through 'survival of the fittest,' where individuals with advantageous, heritable traits are more likely to survive and reproduce, passing those traits to the next generation without individuals acquiring new traits during their lifetime.
Card 33
Why are terrestrial ecosystems considered to be closely woven into the fabric of physical geography?
Terrestrial ecosystems are directly influenced by climate, which is a fundamental component of physical geography. Factors like precipitation, temperature, and evaporation dictate the types of plants and animals that can thrive in a region, leading to distinct biome distributions. Therefore, understanding terrestrial ecosystems requires a deep appreciation of the underlying physical geographical conditions that shape them.
Card 34
Define 'biogeography' and differentiate between its two main branches: ecological biogeography and historical biogeography.
Biogeography is the study of the distribution of plants and animals (biota) over the Earth. Ecological biogeography focuses on how current environmental factors, such as physiological needs and climate, affect the distribution patterns of organisms. Historical biogeography, on the other hand, examines how the spatial distribution patterns of organisms have arisen and changed over long periods of time and across geographical space.
Card 35
Explain the photosynthetic strategy of CAM plants and describe how it benefits them in their typical environments.
CAM (Crassulacean Acid Metabolism) plants utilize a special photosynthetic pathway where their stomata open at night to absorb CO2, which is then stored as organic acids. During the daytime, when stomata are closed to conserve water, the stored CO2 is released for use in the Calvin cycle. This adaptation significantly helps reduce water loss, making CAM plants well-suited for arid environments like those inhabited by cacti and pineapples.
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