climate change (1A), (2A) Flashcards
what are the 3 ways, that climate change can be assed (timescale wise)
- long term ( or geological) - over hundreds of thousands to millions of years.
- medium- term (historical) - within the last few thousand years
- short-term recent) - within the last few decades
what is the Holocene period
the period, that we would refer to as the current geographical period, which began at the end of the last glacial period (11,700 years ago)
what is the quaternary period?
- the period of time, that spans the last 2.6 million years.
- its main features, are its glacial and interglacial periods.
typically, how often to glaciers form?
every 100,000 years
what is the largest glacial system on the planet
the Artic
why is the Younger Dryas important ?
as it shows the last major abrupt climate change event at the last period of deglaciation.
what are the 5 ways we can construct past climates
- marine sediments
- ice cores
- fossils
- dendrochronology
- lake sediments (pollen and beetles)
describe how marine sediment is used, to construct past climates
- fossils of tiny sea creatures, are found on the sea floor,
- they can find the chemical compound in the shell of the fossil to estimate past temperatures.
describe how ice cores are used, to construct past climates
- contain tiny air bubbles, that are records of different oxygen isotopes (O16 or O18).
- the size of each piece of ice can tell scientist the length of each period
- clear ice equals a period of warming
- opaque ice equals a period of cooling
describe how fossils are used, to construct past climates
- plants and animals are adapted to different climates, so scientist can look at the adaptions of animals to predict past climates
describe how dendrochronology is used to construct past climates
- scientists, can determine the climate based on the cambium tissue (in a tree)
- the larger the rings the greater the growth (greater growth suggest warmer climate)
describe how lake sediments (pollen and beetles are used, to construct past climates)
- scientist, can find remans of beetles and pollen that was produced millions of years ago.
- they can compare the pollen and peoples to know species and see how the climates compared, to get a rough idea of what the past climate may have been like.
what is eccentricity (orbit)
- the more elliptical the earth, the colder the climate.
- the greater the ellipse of the earth, the longer time that the earth spends away from the sun, thus explaining why there is a cooler climate.
what is obliquity (tilt)
- the smaller the tilt, the less seasonal variation/colder climate.
- tilt varies between 22 degrees and 24.5 degrees, the closer to 22 degrees the cooler the climate.
what is precession (wobble)
- affects the point, in the year that the earth is closest to the sun.
- when the earth is further away during the northern hemisphere summer, the climate gets cooler.
what is plate tectonics (the effect it has on climate change) an example of?
a positive feedback loop
what is the albedo effect
The definition of the albedo effect is the ability of a surface to reflect sunlight.
- white surfaces reflect light (e.g. ice)
- dark surfaces absorb light (e.g. oceans)
what is the natural greenhouse effect
The natural greenhouse effect is how the atmosphere works to absorb and reflect radiation to keep the Earth warm. The sun emits short wave radiation towards the Earth. The Earth’s atmosphere absorbs this heat and then radiates long wave (infrared) radiation away from Earth.
what are the two types of sun spots
- black (lower solar irradiance - smaller solar output)
- white (higher solar irradiance - greater solar output)
what were the immediate and local impacts of the Laki eruption (1783)
- 25% of the Icelandic population died due to either famine or the toxic gases and lava.
- most of the Icelandic population, died due to famine