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Paleoclimatology --- Climatic extremes --- Glacial climates --- Climats glaciaires --- Agnotozoic --- Algonkian --- Proterozoic Era --- Climates, Glacial --- Glacials --- Climate extremes --- Extremes, Climatic --- Climatology --- Climatic normals

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Historically, climate fluctuations, such as the Little Ice Age, show that interglacial climate change in not entirely stable, but responds to even subtle changes in radiative forcing. Through research, it has been made clear that even an abrupt change of climate within years is not just a theoretical possibility but has in fact happened in the prehistoric past. It is therefore clear that in principal it could happen again. Human civilization has exploded under the mild and relatively stable climatic conditions that have prevailed over the last 11,000 years. This book focuses on

Paleoclimatology --- Glacial climates --- Climatic changes --- Paléoclimatologie --- Climats glaciaires --- Climat --- Changements --- Paléoclimatologie --- Climatic changes. --- Climatology. --- Climate --- Climate science --- Climate sciences --- Science of climate --- Atmospheric science --- Climates, Quaternary --- Quaternary climates --- Quaternary climatology --- Quaternary paleoclimatology --- Quaternary Period --- Paleoclimatology - Quaternary

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Climates [Glacial ] --- Climats glaciaires --- Eiszeitalter --- Eiszeiten --- Englacement --- Englaciation --- Glaciaire [Période ] --- Glacial climates --- Glacial epoch --- Glaciale perioden --- Glacials --- Glaciation --- Glaciations --- Ice age --- Ijstijd --- Ijstijden --- Ijstijdvakken --- Paleo-ecologie --- Paleoecology --- Paléoécologie --- Période glaciaire --- Périodes glaciaires --- Âge glaciaire --- Époque glaciaire --- Époques glaciaires --- 551.33 --- Climates, Glacial --- Paleoclimatology --- Palaeoecology --- Ecology --- Paleobiology --- Ice Age --- Geology, Stratigraphic --- Glacial geology --- 551.33 Glacial geology