Sediments deposited in the ocean leave a fantastic archive of past climate, which scientists can retrieve by drilling cores.
Sediments deposited in the ocean leave a fantastic archive of past climate, which scientists can retrieve by drilling cores.

Past changes in climate

Climate changes in the past

Studying past climate is the key to understanding climate changes today and projecting scenarios for climate change in the future.

Future climate changes will be a combination of natural climate variability and human activities (e.g. fossil fuel consumption and land use). To be able to distinguish between climate changes caused by humans and the natural variations in climate, we need to know how climate changed before the Industrial Revolution.

Climate varies at a range of spatial and time scales. As an example, the variability, or fluctuation of temperature at a particular point on the Earth’s surface will be much larger than the global average. This is particularly true for climate fluctuations shorter in duration than 100 years. For example, warmer periods during Medieval Warm Period occurred primarily near the polar regions, while the tropics were not affected.

Archives of past climate changes

Reliable climate data measured by instruments only date back to about 1860 and provide a perspective that is much to brief to be able to draw conclusions on how climate has fluctuated in the past. Researchers in the field of past climate, also called palaeoclimatology, therefore focus research on reconstructing the climate (e.g. temperature/precipitation/ocean currents) with as little margin of uncertainty and as fine a time resolution as possible back in time. Then they try to find the causes of the climate changes they observe. To reconstruct climate, researchers must apply indirect data from a variety of different archives. Among these sources are:

  • Geological data (marine organisms, sediment composition)
  • Land data (sediment from lakes, moraines, calcium deposits in caves)
  • Glaciological data (ice cores and glacial moraines)
  • Biological data (pollen, plant remains, insects, tree rings)
  • Bones and skeleton remains
  • Historical data (recorded information in church annals, letters etc.)
  • Marine fossils in (these include fossils of organisms preserved in sediments on the ocean floor and reflect temperature, nutrient content and salinity in the water at the time these lived.
  • Sediment composition and the size distribution of subsea particles and debris (these give information on the strength of ocean currents, sea ice distribution and drop-stones from drifting icebergs)

Record high CO2 concentration

CO2 concentration Ice core data from Antarctica and Greenland show that the during the past 150 years atmospheric concentrations of CO2 and methane have exceeded the natural variations throughout the past one million years. Since the pre-industrial era, the concentration of CO2 has increased by nearly 40 per cent, and the concentration of methane by 17 per cent. Warming during the second half of the preceding century occurred during a period in which the natural drivers should have resulted in a slight cooling of the Earth, not a warming of the planet. It is likely that the radiative forcing from human activities since the Industrial Revolution and up until today amounts to more than five times the changes caused by irradiance from the sun.

Key examples of past climate changes

  • During the Middle Ages (900–1350 A D), areas of the Northern Hemisphere experienced a warm climate with a mean temperature 1–2 °C higher than the average temperature during the 20THcentury. The warmer climate made it possible for northern settlers to live in Greenland.
  • Trees grew on the Hardanger plateau during the Stone Age 8000–6000 years ago, and at the same time, many of the largest glaciers in Norway had melted away. This was enabled by higher temperatures in the northern areas, which were due to the Earth being closer to the Sun during the summer coupled with the fact that the tilt of the Earth was greater than today’s.
  • During the Last Ice Age, Norway was covered with an ice sheet that was more than 1 km thick.
  • About one-third of the Greenland Ice Sheet melted and sea level was 4–6 m higher about 125,000 years ago. This was a period when the Earth was closer to the Sun during the summer season. As a result, summer temperatures in the northern areas were 3–5 °C warmer than in the 20TH century.
  • Over thousands of years, slight variations in the Earth’s orbit around the Sun cause fluctuation between ice ages and warmer periods. Variations in solar irradiance that accompany such changes have not changed during the past centuries and therefore cannot explain the global warming that has occurred since the 1900s.

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This article is from the free online course:

Causes of Climate Change

University of Bergen