Extreme weather events are on the rise, leading to increased frequency and severity.
Misconception: It is commonly thought that cold weather events will decrease with climate change.
Discussion Prompt: Analyze the impact of extreme weather, such as blizzards, in future scenarios and propose explanations.
The phenomenon is explored through videos and problem-based learning.
Online resources engage with real-world phenomena, focusing on California drought causes.
Reflection is required on how various factors increase drought likelihood.
Feedback mechanisms can either stabilize or destabilize climate systems and can result in extreme weather events like floods or droughts.
Two main factors affecting California’s climate stability are to be identified, along with their effects.
Processes in the earth's geologic system are driven by two main energy flows:
Electromagnetic Radiation from the Sun: Powers weather and ocean currents.
Heat from Earth’s Interior: Primarily from radioactive decay of isotopes, driving tectonic activity.
Energy from the sun powers water cycles and land erosion, stabilizing weather patterns.
Energy outflow and inflow directly affect overall temperature regulation.
Substantial differences in water storage across reservoirs:
Oceans: 1,370,000 km³, residence time of about 3100 years.
Glaciers: 29,000 km³, residence time of 16,000 years.
Atmosphere: Only 14 km³ with a short residence time of 9 days.
Vital elements such as carbon, nitrogen, and phosphorus cycle through various reservoirs, impacting ecological health.
Residence Time: Length of time an element remains in a particular reservoir, closely related to the size of the reservoir.
Processes initiated by energy from the sun dominate:
Evaporation, condensation, precipitation.
Gravity influences water flow back to the surface.
The carbon cycle includes reservoirs with various carbon storage levels:
Atmosphere: ~865 billion tons of carbon.
Ocean C sediments and Fossil Fuels: Long-term storage for millions of years.
Rock types interchange through:
Erosion: Breaks rocks into sediment.
Sedimentation: Compacts and cements sediments into rocks.
Metamorphism: Alters rocks chemically or physically under heat and pressure.
Reinforcing Feedback: Amplifies changes, possibly leading to extreme weather patterns.
Counterbalancing Feedback: Acts to stabilize the climate system, maintaining equilibrium.
As glaciers melt, land underneath gets exposed, absorbing more sunlight and exacerbating warming.
The feedback loop contributes to faster ice melt and increased sea level.
Human activities such as burning fossil fuels increase greenhouse gases, driving global warming trends.
Effective legislation has targeted pollution reduction but continued effort is needed to maintain atmospheric quality.
Understanding past climate events informs present conditions; historical correlations show links between weather fluctuations and human development.
Climate data collated highlights significant anthropogenic impacts, indicating urgent need for corrective measures to mitigate climate change.
Continuous investigation of climate impacts and feedback mechanisms fosters a deeper understanding of evolving environmental conditions.