SIO 25 lectures 10-25 Flashcards
What are the primary ice sheets on Earth, and why are they significant?
The primary ice sheets are the Greenland and Antarctic ice sheets. They are significant because they store the majority of Earth’s freshwater and influence global sea levels and climate systems.
What is the positive feedback mechanism in ice sheet elevation-mass balance?
The positive feedback mechanism involves the reduction of ice sheet elevation due to melting, which exposes lower, warmer layers. This accelerates further melting due to higher temperatures at lower elevations.
What makes the West Antarctic Ice Sheet particularly vulnerable?
The West Antarctic Ice Sheet is vulnerable because much of it is grounded below sea level, making it susceptible to melting from warming ocean waters.
What is the potential impact of the melting Greenland ice sheet on the Atlantic Meridional Overturning Circulation (AMOC)?
The melting of the Greenland ice sheet releases large amounts of freshwater into the North Atlantic, which can disrupt the AMOC by reducing salinity and density, potentially weakening this critical climate-regulating current.
What are the key methods for measuring sea level, and what are their advantages and limitations?
Tide Gauges: Measure sea level relative to land. Advantage: Long historical record. Limitation: Affected by land movement (e.g., subsidence or uplift).
Satellite Altimetry: Measures sea level from space using radar. Advantage: Global coverage. Limitation: Requires advanced calibration and may not capture short-term, localized changes.
What factors contribute to global sea level rise?
- Thermal expansion of seawater due to warming.
- Melting of land ice (glaciers and ice sheets).
- Groundwater extraction and runoff into oceans.
How does isostatic rebound influence local sea level changes?
Isostatic rebound occurs when land previously compressed under the weight of glaciers rises after the ice melts. This can cause local sea levels to fall even as global sea levels rise.
Why is sea level rise a critical issue for coastal populations?
- Increased flooding and storm surges threaten infrastructure and homes.
- Saltwater intrusion can contaminate freshwater supplies.
- Coastal erosion leads to habitat loss and impacts agriculture and tourism.
Which areas of the United States are most vulnerable to sea level rise?
- Coastal areas like Florida, Louisiana, and the Eastern Seaboard (e.g., New - - — York, North Carolina).
Low-lying cities such as Miami and New Orleans. - Alaska, due to the rapid thawing of permafrost.
What strategies can mitigate the risks of sea level rise?
- Building sea walls and flood barriers.
- Restoring natural barriers like wetlands and mangroves.
- Implementing managed retreat (relocating communities).
- Reducing greenhouse gas emissions to slow global warming.
- Enhancing urban planning to make infrastructure more resilient.
How does atmospheric CO₂ contribute to ocean acidification?
Atmospheric CO₂ is absorbed by the ocean, where it reacts with water to form carbonic acid, which dissociates into hydrogen ions, lowering the ocean’s pH and making it more acidic.
What are the primary impacts of ocean acidification on marine organisms?
Ocean acidification affects marine organisms by reducing the availability of carbonate ions for shell and skeleton formation, weakening structures, and disrupting biological processes like growth, reproduction, and predator detection.
What is coral bleaching, and how is it linked to ocean acidification?
Coral bleaching is when corals expel their symbiotic algae due to stress. Ocean acidification weakens coral skeletons and makes them more vulnerable to thermal stress, increasing the likelihood of bleaching.
How does ocean acidification affect economically important marine species?
Ocean acidification makes it harder for species like oysters, clams, and certain fish to form shells, slowing growth and increasing mortality. This negatively impacts fisheries and aquaculture industries and disrupts food webs.
How does climate change impact global vegetation patterns?
Climate change alters temperature and precipitation patterns, which can shift the range of plant species. Some plants may thrive in new conditions, while others may decline, leading to changes in ecosystems and biodiversity.
What role do forests play in mitigating climate change, and how does deforestation contribute to it?
Forests act as carbon sinks, absorbing CO₂ from the atmosphere. Deforestation releases stored carbon back into the atmosphere, contributing to higher greenhouse gas concentrations and accelerating climate change.
What are the main challenges for agriculture due to climate change?
Climate change leads to more extreme weather events, such as droughts, floods, and heatwaves, which negatively affect crop yields, disrupt growing seasons, and increase pests and diseases, threatening food security.
How does agriculture contribute to global greenhouse gas emissions?
Agriculture contributes to greenhouse gas emissions through livestock digestion (methane), fertilizer use (nitrous oxide), and land-use changes (carbon dioxide). These emissions come from farming practices and deforestation for agricultural expansion.
How do livestock contribute to climate change, and what strategies exist to reduce this?
Livestock produce methane during digestion (enteric fermentation), a potent greenhouse gas. Strategies to reduce emissions include improving feed quality, implementing better manure management, and adopting more sustainable farming practices.
What is permafrost, and why is its thawing a potential tipping point for climate change?
Permafrost is permanently frozen ground found in polar regions. Thawing releases stored greenhouse gases, such as methane and CO₂, into the atmosphere, potentially accelerating climate change in a feedback loop.
What are the Earth’s major reservoirs of carbon?
The major reservoirs of carbon on Earth include the atmosphere, oceans, terrestrial biosphere (plants and soils), and fossil fuels (coal, oil, natural gas).
How does the ocean act as a carbon sink, and what is the role of the biological pump?
The ocean absorbs CO₂ from the atmosphere, acting as a carbon sink. The biological pump involves marine organisms, such as plankton, absorbing CO₂ for photosynthesis, and when they die, the carbon is transported to the ocean depths, effectively sequestering it.
How does the weathering of silicate rocks remove CO₂ from the atmosphere?
When silicate rocks weather, they chemically react with CO₂ and water to form bicarbonate ions, which are carried by rivers to the ocean. This process reduces atmospheric CO₂ over long periods, contributing to Earth’s carbon balance.
What are the turnover times for carbon in various reservoirs, such as the atmosphere, plants, soil, and oceans?
- Atmosphere: Around 3-5 years (carbon stays in the atmosphere before being absorbed or removed).
- Plants: A few months to a decade (carbon in plant biomass is cycled quickly).
- Soil: A few years to thousands of years, depending on the type of carbon and soil conditions.
- Oceans: The surface ocean exchanges carbon with the atmosphere in a few years, but deep ocean carbon can stay for centuries.
How have human activities perturbed the carbon cycle?
Human activities, such as burning fossil fuels, deforestation, and agriculture, have added excess CO₂ and methane to the atmosphere, disrupting the natural carbon cycle, leading to higher concentrations of greenhouse gases and contributing to global warming.
What are the primary sources of methane emissions, both natural and anthropogenic?
- Natural sources: Wetlands, termites, and oceanic processes.
- Anthropogenic sources: Livestock digestion (enteric fermentation), landfills, fossil fuel extraction, and rice paddies.
What is radiative forcing, and how does it affect the Earth’s climate system?
Radiative forcing is the change in energy balance caused by factors like greenhouse gases or aerosols. It affects Earth’s climate system by altering the amount of incoming or outgoing energy, influencing global temperatures. Positive forcing leads to warming, while negative forcing leads to cooling.
What role do aerosols play in radiative forcing, and how do they contribute to cooling?
Aerosols can reflect sunlight back into space, creating a negative radiative forcing that leads to cooling. They also influence cloud formation, which can increase cloud reflectivity and further cool the atmosphere.
What are the main positive feedback mechanisms in the climate system?
Main positive feedback mechanisms include:
- Water vapor feedback: Warmer temperatures increase evaporation, raising water vapor (a potent greenhouse gas), which further warms the atmosphere.
- Ice-albedo feedback: Melting ice reduces the Earth’s reflectivity, causing more solar radiation to be absorbed, which accelerates warming.
Cloud feedback: Some clouds trap heat, further warming the planet.
How does the ice/snow albedo feedback accelerate warming?
As ice and snow melt due to warming temperatures, the Earth’s surface becomes darker (e.g., exposed ocean or land), causing more solar radiation to be absorbed instead of reflected. This accelerates warming and leads to further ice melt, creating a self-reinforcing cycle.