Climate change Flashcards
Global average temperatures have increased by about…
1 degree Celsius (1.8 degrees Fahrenheit) since the late 19th century.
The rate of warming has accelerated in recent decades…
the five warmest years on record all occurring since 2010.
The oceans have absorbed much of this heat…
The top 700 meters (2,300 feet) of ocean warming by about 0.4 degrees Celsius (0.7 degrees Fahrenheit) since 1969.
Arctic sea ice has decreased by…
about 13% per decade since 1979.
Sea levels have risen by…
About 8 inches since 1880.
Palaeoclimatic indicators
Ice cores
Palynology
Fossils
Foraminifera
Paintings / novels
Past weather records
Ice cores; What they do, Pros / Cons.
Snow settles on the surface, oxygen and carbon from the atmosphere within the snow become compressed when a new layer forms, again and again until these layers are preserved in the ice sheet.
O18 and 016 oxygen isotopes can be examined; 018 evaporates from ocean at higher temperatures. Therefore if a core layer has more 018, it indicates a warmer year.
In addition, the amount of co2 present in the ice can indicate how warm the climate was in such period.
Pros:
Can be used to see past temperatures of up to 800,000 years ago in antarctica
Cons:
Can be difficult to distinguish the ice core layers when examining older samples, as the pressure causes regelation in the ice which distorts layers.
Also expensive to do.
May not be indicative of the global climate, and more just the area where they were drilled from.
Micro fossils
By examining micro fossils found in ocean sediment samples, the climate at the time can be deduced through 2 ways:
O16 / O18 oxygen isotope ratio in the fossil
Type / species of fossil, as only certain species can survive in certain temperatures, due to foraminifera being highly sensitive to climatic changes.
Dated using radio carbon dating techniques; Oldest microfossils on Earth around 3.5 billion years old, however, less than 100 million years old to actually work out past temp.
Cons:
Very hard to identify if old due to breaking up over time
Can move location due to currents.
Paintings / books / other media
Paintings / novels can be used to depict what past temperatures were like, such as Charles Dickens a Christmas carol which took place during the victorian era during the little ice age in the uk, which lasted approx from 1300 to 1850. This therefore shows how it can be used to indicate past temps, as there is vivid detail on how the thames used to freeze and people would ice skate / winter markets.
Cons:
Quantitative, can be bias / up to interpretation, not accurate
Palynology
The amount of pollen found in sediment deposits, such as peats and bogs, can indicate past climates;
For example, they can show:
Type of species pollen was from, which indicates temp, as plants can only survive in certain temps
Also show the amount of pollen, as higher amounts of pollen found which are dated to a certain year indicate that it was a warmer year and more plants bloomed.
Cons:
Like micro-fossils, pollen samples can be moved around due to a variety of factors such as landslides, tectonic movement, washed away during rainfall etc. Also not as accurate as other proxies.
Internal forcing mechanisms:
Tectonic plate movement / ocean currents changing
Volcanic eruptions
Greenhouse gases
external forcing mechanisms
Milankovitch cycles
Sunspots
How can tectonic plate movement cause climate change?
Creation on the Panama Isthmus about 3 million years ago had a profound impact on the Earth’s climate. The isthmus blocked the flow of water between the Pacific / Atlantic, forming the gulf stream, which is a warm ocean current that flows from the Gulf of Mexico up the Eastern coast of the US.
Before the isthmus, currents could flow between both oceans via the central american seaway, which cooled the climate. After this was blocked, the gulf stream warmed the earth by approx. 2/3*C
How can volcanic erection cause climate change
The average temperature in the Northern Hemisphere was about 0.2 degrees Celsius cooler than average during the months following the eruption of Eyjafjallajokull.
Due to the increased albedo of the ash clouds.
Eccentricity
Eccentricity: The Earth’s orbit around the Sun is not perfectly circular, but rather it is slightly elliptical. This means that the Earth’s distance from the Sun varies throughout the year. The eccentricity of the Earth’s orbit changes over time, with periods of high eccentricity (when the Earth’s orbit is more elliptical) and periods of low eccentricity (when the Earth’s orbit is more circular). The eccentricity of the Earth’s orbit has a cycle of about 100,000 years.
Obliquity
Obliquity: The Earth’s axis is tilted relative to its orbital plane. This tilt is what causes the seasons. The Earth’s obliquity changes over time, with periods of high obliquity (when the Earth’s axis is more tilted) and periods of low obliquity (when the Earth’s axis is less tilted). The obliquity of the Earth’s axis has a cycle of about 41,000 years.
Precession
Precession: The Earth’s axis precesses, or wobbles, like a spinning top. This precession is caused by the gravitational pull of the Sun and the Moon. The Earth’s precession has a cycle of about 26,000 years.
Sunspots
Sunspots are areas of intense magnetic activity on the surface of the sun. Sunspots release higher amounts of solar radiation.
Cycle lasts around 11 years, with the peak and minimum of this short term cycle not effecting temp. significantly (0.1% of solar radiation variation)
However, over centuries sunspot activity can effect the global temperature to a higher effect; e.g. The maunder minimum which caused colder winters and lower global avg. temps from 1650-1720 due to less sunspot activity according to scientists.