Earth and Space Science Flashcards
Biosphere
The zone that encompasses all living organisms on the planet.
Atmosphere
The layers of gas that surround the planet.
Lithosphere
The upper layer of the mantle and the crust and includes all geological features on the surface of the planet.
Hydrosphere
Includes all forms of water present on the planet in solid, liquid or gaseous states.
Carbon Cycle
The carbon cycle is the process by which carbon moves through Earth’s four spheres—atmosphere, biosphere, hydrosphere, and lithosphere. It’s a continuous loop that includes absorption by plants through photosynthesis, release by organisms through respiration, decomposition, fossilisation, and combustion. This cycle maintains the balance of carbon on Earth to support life and regulate the climate.
Photosynthesis, respiration, decomposition, fossilization, combustion, carbon sinks/resevoirs.
Natural Greenhouse Effect
Natural process that maintains the temperature of the Earth.
Process:
1. Solar Radiation: The Sun emits solar radiation, which reaches Earth’s atmosphere.
2. Absorption: Earth’s surface absorbs about 70% of this solar energy, warming up.
3. Infrared Radiation: The warmed Earth re-emits energy as infrared radiation (heat).
4. Greenhouse Gases: Gases like CO₂, CH₄, H₂O, and N₂O in the atmosphere trap some of this infrared radiation.
5. Re-radiation: The trapped heat is re-radiated back towards Earth’s surface, keeping it warm.
Importance:
~ Maintains Average Temperature: Without this effect, Earth’s average temperature would be around -18°C (0°F), instead of the current 15°C (59°F).
~ Supports Life: Regulates a stable climate and supports the water cycle, making Earth habitable.
Major greenhouse gases (GHG): CO2, H2O, methane, nitrous oxides
Carbon Resevoirs/Sinks
A feature of the environment that absorbs and/or stores carbon therefore keeping it out of the stmosphere. Examples: limestone, forests, oceans, and fossil fuels.
Climate Cycles
Glacial periods (ice ages):
Are periods of time where global temperatures drop significantly enough so that large glaciers appear across approximately 30% of the Earth’s surface. These periods are significant increases in land ice as well as sea ice. Within the last half a million years, glacial periods have been estimated to last around 70-90,000 years.
Inter-glacial periods:
Are periods of time where global temperatures increase where glaciers retreat and melt into the oceans causing sea level rises across the Earth. These periods are estimated to last around 10,000 years only. The current inter-glacial period (called the Holocene) is estimated to have lasted closer to 11,000 years and this may be attributed to human influences on climate change. Some scientists believe the Holocene may last as long as 150,000 years.
Thermohaline Circulation for Deep Currents:
~ Ocean current system is driven by temperature and salinity differences, crucial for distributing heat and nutrients and regulating Earth’s climate.
~ Thermo = temperature-related
~ Haline = salinity and density related
~ Thermohaline = mixing of current controlled by temperature and density
~ As water sinks, some water needs to rise to replace it.
~ Sinking water is cold and dense, rising water is warm and less dense
~ As the water rises, it brings nutrients from the ocean floor
~ As water sinks, dissolved oxygen heads to the sea floor.
Deep Currents
~ As fresh water freezes, ice forms from freshwater
~ Salt is left behind in this cold water, increasing density of the sea water
~ This liquid water sinks to the sea floor
As it sinks, it takes the place of slightly warmer water and this water moves slighly. (a few cms a year)
Surface Currents
~ Driven by trade winds and the Coriols Effect
~ Surface waters push underlying layers of water in the same direction
~ As the water moves it begins to rotate in Ocean basins
~ These rotations are called ‘gyres’
~ Gyres spin clockwise in the Northern hemisphere and counter-clockwise in the Southern hemisphere
~ Surface currents are responsible for taking heat from equatorial regions to polar regions
Enhanced Greenhouse Effect
~ Human influences have led to an increase of greenhouse gas concentrations in the atmosphere
~ This enhanced effect essantially traps more of the solar radiation within the atmosphere while letting out less
~ This increases global temperature around the globe, impacting weather systems
~ The most recognised human influence is the burning of fossil fuels that release carbon back into the atmosphere
Anthropogenic Gases (Enhanced Greenhouse Effect)
Anthropogenic: Originating in human activities.
~ The word ‘anthropogenic’ refers to gases that are released into the atmosphere by human interactions
~ This increase of these anthropogenic gases is how the greenhouse effect has been enhanced by humans
~ Humans undertake a number of different activities that release these gases
Coal (Enhanced Greenhouse Effect)
~ Coal is a natural mineral that is formed uner the surface of the Earth from ancient vegetation and is a long complex hydrocarbon
~ Humans extract this coal and use it to power energy grid across the Earth via burning
~ The aount of energy (and carbon) that humans release from coal is determined by the type of coal that has been extracted from underground
~ The four types of coal from lowest energy and least carbon content to highest are: Peat, Lignite, Bituminous and finally Anthracite
~ Humans use Bituminous coal to power most of our coal-fired power stations
~ The medium-grade coal has the second-highest level of coal and when burned, relseases carbon dioxide
~ In many countries there is a shit away from coal as a power source due to the large volume of carbon prouced per volume
Crude Oil (Enhanced Greenhouse Effect)
~ Crude oil, much like coal is made of carbon from ancient fossilised organisms such as animals and algae
~ It also ahs a long hydrocarbon structure but smaller and less complex than that of coal
~ This structure has more hydrogen-carbon bonds and less carbon-carbon bonds meaning per unit of volume it releases less atmospheric carbon
~ Humans refine and combust oil for a number of industrial and commercial processes which releases the carbon stored inside it
~ Oil is extracted from resevoirs on land or under the surface of oceans and is then refined into a range of petroleum products such including diesel, lubricating oils, and petrochemical feedstocks for making urbbers and plastics
~ Each of these products, when destroyed or combusted, release carbon back into the atmosphere