Temperature

Climate proxies (indicators) are preserved physical characteristics of the past that stand in for direct meteorological measurements and enable scientists to reconstruct the climatic conditions. They provide the only means for scientists to determine climatic patterns before record-keeping began (around 1880) (Wikipedia). The most common climate proxies are gas bubbles, pollens, dinocysts, isotopes, the quantities of which tell us something about past climate conditions. Proxies are found in lake sediment, marine sediment, peat bogs, ice, speleothems, tree rings and coral skeleton rings. Coring is often used to extract the proxies.

Let’s look at the temperature variations of surface ice in Greenland (deduced from ice cores) which is assimilated with temperatures in the European area and possibly in the whole Mediterranean area, and let’s compare it with the initiation of the major civilisations.

Civilisation changes and Climate changes
based on Greenland reconstructed paleotemperatures from six ice cores,
Vinther (2009).

The so-called Holocene Climatic Optimum (7000-4000 BC) is clearly visible with a thermal maximum around 6000 BC. It can be noted that the drop of temperature between this maximum and the 20th c. temperature is around 3°C. The temperature variations between warm and cold peaks are in the order of 1°C, except for the 8200 BP event where it is around 2°C. A quick look at the intervals between the warm peaks shows that they are fairly equidistant with an average of ca. 400 years. This is perhaps showing some astronomical influence?[5]

The main Holocene warm and cold periods are listed very schematically as follows[2]:

  • Around 6200 BC: cold peak: 8200 BP Cold Period
  • Around 6000 BC: warm peak (Holocene Thermal Maximum)
  • Around 4900 BC: warm peak
  • Around 4500 BC: warm peak
  • Around 3800 BC: warm peak
  • Around 3300 BC: warm peak (Initiation of Harappa-Indus Valley civilisation)
  • Around 3000 BC: warm peak (Initiation of Egyptian and Sumerian civilisations)
  • Around 2900 BC: cold peak (Piora Cold Period)
  • Around 2300 BC: cold peak
  • Around 2200 BC: warm peak with severe drought (Initiation of Minoan civilisation, start of First Intermediate Period in Egypt)
  • Around 1900 BC: cold peak (Early Neoglacial Anomaly, ENA) (migration of the Harappa-Indus Valley civilisation)
  • Around 1800 BC: warm peak (start of Second Intermediate Period in Egypt)
  • Around 1600 BC: warm peak (initiation of Mycenaean and Hittite civilisations, and of New Kingdom in Egypt)
  • Around 1200 BC: warm peak (Sea Peoples raiding the eastern Med, end of Bronze Age)[3]
  • Around 1000 BC: warm peak (start of Third Intermediate Period in Egypt)
  • Around 700 BC: Iron Age Cold Period
  • Around 500 BC: warm peak (initiation of Greek civilisation during a period of rising temperatures starting in 700 BC)
  • Around 200 BC: cold peak
  • Around 0 AD: Roman Warm Period (initiation of Roman civilisation during a period of rising temperatures starting in 200 BC)
  • 100-200 AD: cold period: decline of Roman Empire
  • Around 400 AD: warm peak: Byzantine civilisation
  • 400-900 AD: Late Antique Little Ice Age or Late Neoglacial Anomaly (LNA) (Migration Period, Arab Conquest, European Dark Age)
  • 900 -1350 AD: Medieval Warm Period (initiation of European Renaissance)
  • 1350-1850 AD: Little Ice Age.

Eventhough such a comparison between temperatures and the initiation of civilisations leaves some room for wishful thinking, it is quite striking that the initiation of civilisations[4] occurred around the warm peaks. It might perhaps be suggested that civilisations were initiated during periods with rising temperature and collapsed with prolonged droughts of several decades combined with falling temperatures. This would make sense from a farming point of view.
But again, the climate is not the only factor involved: to explain the end of the Bronze Age, Cline (2014) adds earthquakes/volcanic activity, droughts/famines, internal mismanagement/rebellion/civil war, outside migrants/pandemics/invaders with new technologies, disruption of international trade with domino-effect on inter-dependent states. All of these factors may have co-operated in some way to generate the ‘Perfect Storm’ that put an end to the Bronze Age and to the Roman Empire …


References

[1] VINTHER, B., et al., 2009, “Holocene thinning of the Greenland ice sheet”, Nature, volume 461, (p 385-388). See: https://www.carbonbrief.org/factcheck-what-greenland-ice-cores-say-about-past-and-present-climate-change. According to Richard B ALLEY (2010), “ice cores are remarkably faithful recorders of past climate”. The temperature reconstruction produced using 18O isotope data from six ice cores is shown in the figure, and spans the period from 9690 BC to 1970 AD. It has a resolution of around 20 years, meaning that each data point represents the average temperature of the surrounding 20 years. So, the end of the record (1970) shows the average temperature between 1960 and 1980. The present author added a 200-year triangular filtering in order to smooth the signal without altering the main peaks.

[2] See also: https://en.wikipedia.org/wiki/Holocene & http://www.dandebat.dk/eng-klima7.htm

[3] CLINE, E., 2014, “1177 BC, The Year Civilisation Collapsed”, Princeton University Press, (264 p).

[4] WIENER, M., 2018, “The Collapse of Civilizations”, Belfer Center Paper, Harvard, (22 p).
GIOSAN, L., 2018, “Neoglacial Climate Anomalies and the Harappan Metamorphosis”, Climate of the Past, https://doi.org/10.5194/cp-2018-37

[5] TURNER, T., et al., 2016, “Solar cycles or random processes? Evaluating solar variability in Holocene climate records”, Scientific Reports, 6, 23961, https://www.nature.com/articles/srep23961 .

Further reading

ALLEY, R., 2010, “Reliability of ice-core science: historical insights”,Journal of Glaciology, Vol. 56, No. 200, (p 1095-1103).

CUFFEY, K., CLOW, G., 1997, “Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition”, Journal of Geophysical Research, Vol. 102, No. C12, (p 26 383-26 396).

KANIEWSKI, D., et al., 2010, “Late second–early first millennium BC abrupt climate changes in coastal Syria and their possible significance for the history of the Eastern Mediterranean”, Quaternary Research, 74, (p 207-215).

KANIEWSKI, D., et al., 2019, “Cold and dry outbreaks in the eastern Mediterranean 3200 years ago”, Geological Society of America, Geology, Volume XX, Number XX, (5 p).

O’BRIEN, S., et al., 1995, “Complexity of Holocene Climate as Reconstructed from a Greenland Ice Core”, Science, New Series, Vol. 270, Issue 5244, (p 1962-1964).

PLUMKETT, G., SWINDLES, G., 2008 “Determining the Sun’s influence on Lateglacial and Holocene climates: a focus on climate response to centennial-scale solar forcing at 2800 cal. BP”, Quaternary Science Reviews, 27, (p 175-184).

SHARIFI, A., et al., 2015, “Abrupt climate variability since the last deglaciation based on a high-resolution, multi-proxy peat record from NW Iran: The hand that rocked the Cradle of Civilization?”, Quaternary Science Reviews, 123, (p 215-230).

VAN GEEL, B., BUURMAN, J., WATERBOLK, H., 1996, “Archaeological and palaeological indications of an abrupt climate change in The Netherlands, and evidence for climatological teleconnections around 2650 BP”, Journal of Quaternary Science Reviews, 11, (p 451-460).

VAN GEEL, B., & ZIEGLER, P., 2013, “IPCC underestimates the sun’s role in Climate Change”, Energy & Environment, Vol. 24, No. 3/4, (p 431-453).