Climate Change Flashcards
(31 cards)
What is paleoclimatology?
the study of the Earth’s past climates through proxy methods
What are the three methods for long-term climate reconstruction?
- isotope analysis
- ice cores
- ocean sediment core
What is significant about the climate of the past 70 million years (3)?
- scientists have been able to reliably recreate climate
- continents have been stable throughout this time
- relatively rapid warming of the atmosphere
What are some characteristics of the climate of the past 70 million years (3)?
- warmer
- tropical environments extended further
- cooling trend 50 million years ago
What is significant about the climate of the past five million years (3)?
- oversaw the evolution of modern humans
- rise of agriculture and civilizations
- included an ice age
What is significant about the climate of the past 20,000 years?
there have been more sources of data to analyze climate
What is dendrochronology (4)?
- each ring represents a year of growth
- the thicker the ring, the wetter the conditions
- the thinner the ring, the dryer the conditions
- scars form forest fires
What are the mechanisms of natural climate change (4)?
- solar variability
- Earth’s orbital cycles
- continental position and topography
- atmospheric gases and aerosols
How does solar variablity affect climate change (4)?
- variations in amount of energy coming into Earth’s system
- solar output has increased by 1/3
- changes in the sun’s magnetic field
- susnpot activity
How does Earth’s orbital cycles affect climate change (5)?
- distance between Earth and sun varies
- elliptical orbit around sun varies
- shape of ellipse varies
- Earth’s orientation towards sun
- axial tilt varies
How does continental position and topograpy affect climate change (4)?
- composition of continents impacts atmospheric and oceanic circulation
- example: formation of Himalyan Mountains affects jet stream and rain shadow
- example: formation of Panamanian Bridge prevents ocean flow
- position and structure impacts Earth’s albedo
How do atmospheric gases and aerosols affect climate change (3)?
- more carbon dioxide = warmer
- less carbon dioxide = cooler
- aerosols cause cooler conditions
What is feedback (3)?
- feedback: systems produce outputs that influence their own operations
- positive feedback: feedback amplifies system changes; destabilizes system
- negative feedback: a reduction in system changes; stabilizes system
What are some examples of feedback that impact climate (2)?
- ice-albedo feedback
- water vapor feedback
What is the carbon budget?
the exchange of carbon between sources and sinks in all of Earth’s spheres
What is the Carbon Cycle (3)?
- some processes remove carbon from the atmosphere (photosynthesis)
- some add carbon to the atmosphere (respiration and decomposition)
- must remain balanced
What are some human impacts on the Carbon Cycle (2)?
- clearing forests: decreases carbon sinks
- industrial revolution: burning of fossil fuels
What is the Keeling Curve?
- shows increase of carbon dioxide since 1955
- fluctuation caused by seasonality and photosynthesis
How do oceans affect the carbon cycle (5)?
- absorption of carbon by ocean results in smaller than expected amount of CO2 in atmosphere
- absorption causes formation of carbonic acid in ocean
- ocean acidity negatively impacts marine life
- the world’s oceans have absorbed about 50% of atmospheric carbon
- as the ocean’s temperature increases, its ability to dissolve carbon decreases
How do plants affect the carbon cycle?
- plants grow at a quicker rate and store more carbon
- but as temperature increases, photosynthesis decreases
What serves as evidence for present climate change (5)?
- sources of climate data
- rising temperatures
- melting ice
- rising sea levels
- increased atmospheric water vapor
What are some sources of climate data (4)?
- weather data
- satellites
- weather balloons, ships, buoys, etc.
- aircrafts
How do rising temperatures explain climate change (2)?
- warmest time in last 120,000 years
- increse in 20th century temperature happened faster than any other increase in the last 1,000 years
How does melting ice explain climate change (3)?
- melting sea ice does not increase sea level, but exposes lower albedo ocean water, resulting in increasing temperatures
- glacial ice is decreasing in Antarctice and Greenland
- permafrost has been thawing