A: Climate Change Flashcards
What is climate change
Any significant change in the earths climate over a long period
What’s the quaternary period
The most recent geological time period spanning from about 2.6 million years ago to the present day
In the period before the Quaternary, the earths climate was warmer and quite stable.
Then things changed a lot
During the Quaternary global temperature has shifted between
Coldplate your periods that last for around 100,000 years and Walma into glaze your periods that last for around 10,000 years
The last glacial Period ended around
15,000 years ago since then the climate has been warming
Global warming is the term used to describe
The sharp rise in global temperatures over the last century. It’s a type of climate change
Quaternary period
Millions of years ago
How can scientists work out how the climate has changed over time
Ice and sediment cores
Pollen analysis
Tree rings
Temperature records
What is ice and sediment cores
Ice sheets are made up of layers of ice - One layer is formed each year
Scientist drill into ice sheets to get long cores of ice
By analysing the gasses trapped in the layers of ice, they can tell what the temperature was each year
One icicle from Antarctica shows the temperature changes over the 400,000 past years
The remains of organisms found in calls taken from ocean sediments can also be analysed. This can extend the temperature record back at least 5 million years
Describe how tree rings work
As the tree grows it forms the new ring each year
The tree rings are thicker and warm and wet conditions
Scientist take calls and count the rings to find the age of a tree the thickness of each ring shows what the climate was like
Three rings are a reliable source of evidence of climate change for the past 10,000 years
Describe pollen analysis
Pollen from plants gets preserved in sediment, e.g. at the bottom of Lakes or in peat bogs
Scientists can identify and date the preserved pollen to show which species were living at that time
Scientist know the conditions that plants are living now so preserved pollen from similar plants shows that climate conditions were similar
How do you temperature records work
Since the 1850s global temperatures have been measured accurately using thermometers. This gives a reliable but short-term record of temperature change
Historical records (eg harvest dates, newspaper weather reports) can extend the record of climate change a bit further back
What are natural factors that cause climate change
Orbital changes
Volcanic activity
Solar output
What is orbital changes
The way the Earth moves around the Sun changes for example the path of the Earths orbit around the Sun changes from an almost perfect circle to on the lips and back again about every 96,000 years
These changes affect the amount of solar radiation (how much energy) the Earth receives. If the Earth receives more energy, it gets warmer
Orbital changes may have caused the glacial and interglacial cycles of the quaternary period
What is volcanic activity
Major volcanic eruptions eject large quantities of material into the atmosphere
Some of these particles reflect the suns rays back out to space so the surface cools
Okay nose also release CO2 (greenhouse gas) but not enough to cause warming
Volcanic activity may cause short-term changes in climate E.G.the cooling that followed in the eruption of Mount Pinatubo in 1991
What is solar output
The suns output of energy isn’t constant – it changes in short cycles for about 11 years, and possibly also on longer cycles of several hundred years
Period one so the output is reduced may cause as climate to become cooler in some areas
Most scientists think that changes in solar output don’t have a major affect on global climate change
What is the greenhouse effect
Where greenhouse gases such as carbon dioxide and methane absorber outgoing heat So less is lost to space it’s essential for keeping the planet warm
Humans also are responsible for the cause of climate change through
Increasing the concentration of greenhouse gases
How are humans increasing the concentration of greenhouse gases
Burning fossil fuels
Farming
Cement production
Deforestation