Page 75 - The World About Us
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Weather balloon
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          Global temperature data                                  Recently collected data can then be cross-referenced to
                                                                ice core samples for the same year. This improves our
             In recent decades the amount of weather data collected   understanding of the ice found in the layers created prior to
          from around the world has increased drama cally. Data   the development of modern technology.
          from countries such as the UK and USA is incredibly detailed.
          Developing countries may not have such an extensive   Ocean floor sediments
          network of weather sta ons as the UK, but the data collected
          is improving every year. Powerful computers collect and   Scien sts also require a reliable method of interpre ng
          collate all the data from ground sta ons and combine it with   clima c condi ons from periods older than the age of ice. A
                                                                valuable source of climate data is deep ocean sediments. On
          data from satellites, weather balloons and oceanic weather
                                                                the sea bed of the oceans, sediments build up over  me into
          buoys. This data helps create detailed maps of global
          weather and climate.                                  layers. These sediments are made up of the remains of
            Fig.205 Collec ng data with weather balloons, Hawaii.  surface dwelling plankton and other creatures which have
                                                                sunk to the seabed when they died.

                                                                   Chemical analysis of these sediments, such as looking at
                                                                the carbon and oxygen locked up as carbonates in skeletal
                                                                and shell material, can be used to suggest the clima c
                                                                condi ons prevalent when the plankton was alive.
                                                                  Fig.206 Ocean sediments contain climate data.





















                                                                   Have we entered the
                          1. What is an eon? (1)
           2. Which eon are we currently living in? (1)            Anthropocene epoch?
           3. “Mass ex nc ons are a common feature of the
           Phanerozoic.” Discuss this statement. (6)                  In August 2016 a group of scien sts recommended that
           4. What is meant by the term 'Cambrian explosion'? (2)  the world recognise that we are now in a new geological
                                                                   epoch, to be known as the Anthropocene. They dated this
           5. When did oxygen first appear in the Earth’s
                                                                   new epoch to have started on July 16th 1945 (seconds
           atmosphere, and why? (3)
                                                                   before the first ever nuclear bomb test).
           6. How old is the human species, Homo sapiens? (1)
                                                                      They argued that a new dis nct epoch has begun as the
           7. Contrast 'glacial' and 'interglacial' during the     result of the impact of human-induced climate change on
           Quaternary. (3)                                         the geological and biological systems of the planet.
           8. What is meant by the Medieval Warm Period? (2)          At the  me of wri ng, the Interna onal Union of

           9. What, and when, was the Li le Ice Age? (3)           Geological Sciences had yet to make a formal decision on
                                                                   whether we are now living in the Anthropocene and, if so,
           10. Describe the various methods of measuring past      when this new epoch actually started.
           changes in global temperatures. (4)
                                                                      Others are already convinced, ci ng as evidence the
           11. Why might ice cores samples be more accurate than   very high rate of ex nc on for species (between 1,000 and
           cave pain ngs at showing past climate change? (4)       10,000  mes the natural rate) taking place before our eyes.




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                                                             The climate has changed from the start of the Quaternary period.
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