Climate Change Flashcards
What are the characteristics of greenhouse and icehouse conditions?
Greenhouse
-High co2 levels in the atmosphere
-Temperature rise
-Transgressive eustatic sea level rise
-Thermal expansion
-Melting of ice, stored in oceans as water
-Submergent landforms
Icehouse
-Low co2
-Temperature fall
-Regressive eustatic change
-Thermal contraction
-Water stored as ice
-Emergent landforms
What are the 5 periods of differing climates?
- Mid-cretaceous - 100ma, greenhouse conditions
- Oligocene - 35ma, coolhouse, glaciation of Antarctica
- Quaternary - 2.6ma (Ice age) fluctuated temperatures
- Holocene - 11700 - Now, little ice age
- Anthropocene - Now, Period where man is influencing climate
What were the characteristics of the mid-cretaceous period?
Avg temperatures - 6-8 degrees more than today
-Co2 levels 5x higher than today
-No polar ice caps (continental drift) which affected currents in the ocean
What were the characteristics of the Oligocene period?
-Rapid transition from greenhouse to icehouse conditions
-Co2 levels dropped from 500ppm to 110 ppm
What caused the glaciation of Antarctica?
-Tectonic processes lead to Antarctica moving towards the south pole.
-The Antarctica circumpolar current isolated Antarctica from warmer currents so didn’t melt
-South Sandwich Islands. Submerged volcanos that distribute deep water currents isolating Antarctica from warmer currents.
What was the main feature of the Quaternary period?
The cyclic changes of climate. Long periods of cold, glacial periods lasting 100,000 years. And shorter periods of warmer interglacial periods
-1/3 of continental land mass was covered by snow/ice
-During the last glacial maximum 18,000 years ago, NW Europe was < 0 degrees
What were the characteristics of the Holocene?
-Steady warming, but periods of cooling
-Co2 levels were in dynamic equilibrium fluctuating around 280ppm.
-1-2 degrees higher than today, sea levels increased by 100m
-Major decline in ice cover
-Little ice age
What are the main characteristics of the anthropocene?
-The last 200 years since industrialisation
-Co2 levels no longer in dynamic equilibrium
-Human activity rather than natural causes
-C02 levels risen from 280ppm to 420ppm
Explain the natural greenhouse effect?
-Input of short wave solar radiation
-30% is reflected back into space (albedo effect)
-Remaining 70% is absorbed by the atmosphere, land and oceans, and re-emitted as longwave terrestrial radiation.
-Some of this terrestrial radiation leaves the atmosphere but most of it is absorbed by GHG
What is the global energy budget?
is the balance between incoming solar radiation and outgoing terrestrial radiation. It is the ditributor of this balance that causes climate change. 1/3 is reflected by clouds
1/5 is absorbed by water
2/3 is lost to space
Rest is absorbed by GHG
What are natural forcing’s and what are the two external forcing’s and the 4 internal forcing’s?
Forcing’s that affect the Earths energy budget induce climate change. They can be internal or external
External - Sunspots, Milankovitch cycles (orbital forcing’s)
Internal- Volcanic eruptions, continental drift, ocean circulation, greenhouse gases
Explain how eccentricity can alter the climate
-Shape of the Earths orbit, changes from circular to elliptical every 100,000 years
-Circular - Earths distance to the sun is the same all year, so equal solar input
-Elliptical - Not the same distance from the sun, so there are points of close and far - Different temperatures depending on how close or far away
Perihelion - Close
Aphelion - Away
Explain how obliquity and how it can alter the climate
-The Earth rotates on its axis between 22 degrees and 24.5 degrees. The tilt is what causes seasons and how long / intense they are on a 41,000 year cycle
-When the tilt is 22 degrees, seasonal temperatures are reduced. Summers are cooler and winters are warmer
-When the tilt is less than 22 degrees, winters are colder, summers are warmer.
is what causes interglacial periods.
Explain precession and how it can alter the climate
The Earth wobbles on its axis, in cycles of 26,000 years
-As it wobbles, the Earths axis position changes, which determines how much solar energy each hemisphere receives, and is reponsible for the timings of the seasons
-Long term
Explain how sunspots alter the climate.
-Sun Spots, solar flares and hot gassy ejections occur on the sun. These reach Earth and can change the climate
-Follow an 11 year cycle
-In the little ice age, there was little sun spot activity, which cooled the Earth
How does volcanic activity alter climate?
Volcanic eruptions trigger short term climate change (Months - Years)
-Mount Pinatubo erupted and released an ash cloud, with 20 million tonnes of SO2
-This increases the albedo effect and cools the Earth’s climate
How can plate tectonics and continental drift alter the climate?
Sea floor spreading, slab bull, ridge push, convection currents move plates from land maass
This caused more landmass in the Northern Hemisphere
How can plate tectonics and continental drift alter the climate?
Sea floor spreading, slab bull, ridge push, convection currents move plates from land maass
This caused more landmass in the Northern Hemisphere
How can plate tectonics and continental drift alter the climate?
Sea floor spreading, slab bull, ridge push, convection currents move plates from land maass
This caused more landmass in the Northern Hemisphere
How can plate tectonics and continental drift alter the climate?
Sea floor spreading, slab bull, ridge push, convection currents move plates from land mass
This caused more landmass in the Northern Hemisphere so will therefore absorb more solar radiation, and melt land ice faster, decreasing the albedo effect
Also caused Antarctica to move towards the South pole, which cooled it.
How does ocean circulation effects the Earths climate?
-Before 5ma ago, ocean currents were weak due to NA and SA not being connected so warm water could not reach the poles
-5ma, NA joined with SA which made currents stronger so they could reach the North Pole.
How do natural greenhouse gases change the climate of the Earth
Natural GHG causes icehouse and greenhouse conditions. We know this because of direct correlation between CO2 levels and temperature. They are added by decomposition and respiration. They are removed from dissolving with water vapour and photosynthesis.
What are the 6 methods used to construct past climates?
- Historical data
- Dendrochronology
- Ice cores
- Sea floor sediments
- Lake sediments - Varves
- Lake sediments - Pollen
How can historical data provide evidence for past climate change?
-Daniel Gabriel Fahrenheit developed the first thermometer 300 years ago. Climate records have been found dating back 140 years ago. Books from 1000 years ago also are used but is qualitative data and may be inaccurate due to less reliable measurement tools. It doesn’t date far back either.