Oge oyi nke Oge Iron

Iron Age Cold Epoch (nkè a na-akpọkwa Iron Age climate pessimum ma ọ bụ Iron Age neoglaciation) bụ ógè ihu igwe oyi na-adịghị ahụkebe na mpaghara North Atlantic, nke sitere na 900 BC ruo ihe dị ka 300 BC, ya na oke oyi karịsịa na 450 BC n'oge mgbasa nke Gris ógè ochie. Oge okpomọkụ nke Rom (250 BC) sochiri ya. Gill Plunkett na Graeme T. Swindles nke Queen's University Belfast jiri ntụ ọkụ na radiocarbon dating mee ihe iji gbochie mmalite nkè Iron Age climate deterioration na Ireland ruo 750 BC.

Okpomọkụ ice nke Greenland na-akọwa na 18O isotope site na 6 ice cores (Vinther, B., et al., 2009)

Ihe

• Gribbin (1978). "Climatic change in historical times", in Gribbin, J.: Climatic change. Cambridge: Cambridge University Press, 68–82. ISBN 0-521-21594-3. 
• Plunkett (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 (1–2): 175–184. DOI:10.1016/j.quascirev.2007.01.015. 
• Swindles (2007). "A delayed climatic response to solar forcing at 2800 cal. BP: multiproxy evidence from three Irish peatlands". The Holocene 17 (2): 177–182. DOI:10.1177/0959683607075830. 
• Van Geel (1998). "Archaeological and palaeoecological indications of an abrupt climate change in The Netherlands, and evidence for climatological teleconnections around 2650 BP". Journal of Quaternary Science 11 (6): 451–460. DOI:<451::AID-JQS275>3.0.CO;2-9 10.1002/(SICI)1099-1417(199611/12)11:6<451::AID-JQS275>3.0.CO;2-9.